Browse content similar to Gravity and Me: The Force That Shapes Our Lives. Check below for episodes and series from the same categories and more!
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Would you like to lose some weight without doing any exercise | 0:00:02 | 0:00:04 | |
or dieting? | 0:00:04 | 0:00:05 | |
Would you like to age just a bit more slowly than your friends? | 0:00:05 | 0:00:09 | |
Well, you might be surprised to hear, | 0:00:09 | 0:00:11 | |
the laws of physics can help. | 0:00:11 | 0:00:12 | |
The key to unlocking these everyday questions is gravity. | 0:00:15 | 0:00:19 | |
It sculpts the universe. | 0:00:21 | 0:00:23 | |
It warps space and time. | 0:00:24 | 0:00:26 | |
It's a fundamental force of nature. | 0:00:27 | 0:00:29 | |
But gravity's strange powers, discovered by Albert Einstein, | 0:00:32 | 0:00:36 | |
also affect our daily lives in the most unexpected ways. | 0:00:36 | 0:00:41 | |
In this film, we'll be using cutting edge scientific techniques | 0:00:44 | 0:00:48 | |
to investigate how gravity changes your weight... | 0:00:48 | 0:00:52 | |
It's gone up. | 0:00:52 | 0:00:54 | |
..your height... | 0:00:54 | 0:00:55 | |
I really have shrunk. | 0:00:55 | 0:00:57 | |
..and even your posture. | 0:00:57 | 0:00:58 | |
And, with the help of thousands of volunteers, | 0:01:00 | 0:01:02 | |
I'll show you how gravity makes us all age at different rates. | 0:01:02 | 0:01:07 | |
Throughout the day I've just been logging on the phone, | 0:01:09 | 0:01:11 | |
logging on to the app. | 0:01:11 | 0:01:13 | |
As a physicist, gravity is central to my work. | 0:01:13 | 0:01:16 | |
Oh, wow! | 0:01:16 | 0:01:18 | |
And, in exploring it, | 0:01:18 | 0:01:19 | |
I'll be challenged on how I understand this mysterious force. | 0:01:19 | 0:01:23 | |
Wow, OK. I need to go and write this one down. | 0:01:23 | 0:01:26 | |
And I'll have to tackle the very nature of reality itself. | 0:01:28 | 0:01:31 | |
Gravity. | 0:01:40 | 0:01:41 | |
It binds together all the matter in the universe | 0:01:44 | 0:01:48 | |
and it makes our existence here possible. | 0:01:48 | 0:01:51 | |
But in the end, it all boils down to one simple question. | 0:01:54 | 0:01:58 | |
What happens if I drop an object? | 0:02:00 | 0:02:02 | |
Gravity's many mysteries are all contained in this single action. | 0:02:06 | 0:02:11 | |
How an object falls. | 0:02:11 | 0:02:13 | |
Here's the first puzzle. | 0:02:15 | 0:02:16 | |
Why does a hammer fall faster than a feather? | 0:02:16 | 0:02:20 | |
You might think it's because the hammer is heavier. | 0:02:20 | 0:02:23 | |
But that's not the real reason. | 0:02:23 | 0:02:26 | |
The answer is air resistance. | 0:02:27 | 0:02:29 | |
It's not the weight of the objects that matters, it's their shape. | 0:02:30 | 0:02:33 | |
And I can demonstrate this very easily with these two umbrellas. | 0:02:33 | 0:02:37 | |
They both have exactly the same weight, but if I open one of them, | 0:02:37 | 0:02:42 | |
you can be pretty sure it will drop more slowly than the other one. | 0:02:42 | 0:02:46 | |
In fact, all objects would fall at the same rate | 0:02:49 | 0:02:52 | |
if you could only remove the air. | 0:02:52 | 0:02:55 | |
The first person to realise this was the 16th century mathematician, | 0:02:57 | 0:03:01 | |
Galileo Galilei. | 0:03:01 | 0:03:03 | |
Famously, it's said he worked it out | 0:03:04 | 0:03:06 | |
by dropping objects off the Leaning Tower of Pisa. | 0:03:06 | 0:03:09 | |
And he was spectacularly proven right | 0:03:13 | 0:03:16 | |
in an experiment carried out on the moon in 1971. | 0:03:16 | 0:03:21 | |
In my left hand I have a feather. | 0:03:21 | 0:03:24 | |
In my right hand, a hammer. | 0:03:24 | 0:03:27 | |
I'll drop the two of them here, | 0:03:27 | 0:03:28 | |
and hopefully they'll hit the ground at the same time. | 0:03:28 | 0:03:31 | |
It worked perfectly. | 0:03:31 | 0:03:33 | |
How about that? | 0:03:33 | 0:03:35 | |
It proves that Mr Galilei was correct in his findings. | 0:03:35 | 0:03:39 | |
Now, Galileo was obsessed with a second question, too. | 0:03:43 | 0:03:47 | |
When you drop an object, | 0:03:47 | 0:03:49 | |
it's actually quite hard to tell if it falls at a constant speed, | 0:03:49 | 0:03:53 | |
or picks up speed as it drops. | 0:03:53 | 0:03:55 | |
Even in slow motion, it's pretty hard to tell. | 0:03:58 | 0:04:01 | |
But Galileo realised this. | 0:04:06 | 0:04:09 | |
First, drop an object a very short distance. | 0:04:09 | 0:04:12 | |
It lands with very little impact. | 0:04:14 | 0:04:16 | |
But, of course, drop it from higher up... | 0:04:17 | 0:04:20 | |
..this time, the ball easily breaks the tile, | 0:04:24 | 0:04:27 | |
which means it must have accelerated, | 0:04:27 | 0:04:30 | |
gaining in speed and momentum as it dropped. | 0:04:30 | 0:04:34 | |
Galileo had identified something fundamental to all falling objects - | 0:04:36 | 0:04:41 | |
they accelerate. | 0:04:41 | 0:04:42 | |
He realised there might be a way to measure | 0:04:45 | 0:04:48 | |
how much falling objects gain in speed. | 0:04:48 | 0:04:51 | |
What he devised was the first-ever attempt to measure gravity itself. | 0:04:51 | 0:04:57 | |
He built a long wooden ramp, rather like this, | 0:04:57 | 0:05:00 | |
that he had sloping at a shallow angle. | 0:05:00 | 0:05:04 | |
The idea was to roll balls down the ramp and measure their acceleration. | 0:05:04 | 0:05:09 | |
The crucial thing is that the ramp had to be at this shallow angle | 0:05:09 | 0:05:12 | |
to reduce the effects of wind resistance. | 0:05:12 | 0:05:15 | |
It also meant the balls would roll down slowly enough to give him time | 0:05:15 | 0:05:19 | |
to measure their speed. | 0:05:19 | 0:05:21 | |
But the big problem was this - how do you measure time accurately | 0:05:21 | 0:05:25 | |
in an age when there were no accurate timepieces, | 0:05:25 | 0:05:28 | |
let alone stopwatches? | 0:05:28 | 0:05:30 | |
Well, Galileo came up with an ingenious idea | 0:05:30 | 0:05:33 | |
involving the flow of water - | 0:05:33 | 0:05:34 | |
essentially, measuring time from the amount of water collected in a cup. | 0:05:34 | 0:05:39 | |
So, we're going to try and repeat Galileo's experiment. | 0:05:39 | 0:05:42 | |
I say we, because I have a couple of willing volunteers, | 0:05:42 | 0:05:45 | |
Gavin and Johanna. | 0:05:45 | 0:05:47 | |
Three, two, one, go. | 0:05:47 | 0:05:50 | |
And, stop. | 0:05:56 | 0:05:57 | |
OK, there's one. | 0:05:57 | 0:05:59 | |
Now, if you come down a quarter of the way down the ramp. | 0:05:59 | 0:06:03 | |
Go. | 0:06:03 | 0:06:04 | |
Stop. OK. | 0:06:08 | 0:06:09 | |
So, now half of the way down. | 0:06:09 | 0:06:11 | |
Go. | 0:06:11 | 0:06:12 | |
Stop. | 0:06:15 | 0:06:16 | |
Just in time. | 0:06:16 | 0:06:17 | |
OK, and then three-quarters of the way down. | 0:06:20 | 0:06:23 | |
Go. | 0:06:23 | 0:06:24 | |
And, stop. | 0:06:25 | 0:06:27 | |
Right, turn the tap off. | 0:06:27 | 0:06:29 | |
OK, so we have our four measurements. | 0:06:29 | 0:06:32 | |
And I can see a progression from fuller to emptier, | 0:06:32 | 0:06:35 | |
but what we need to do now is find the mathematical pattern | 0:06:35 | 0:06:38 | |
by weighing carefully the water in each glass. | 0:06:38 | 0:06:42 | |
Weighing the water should give us an idea of how long each roll took. | 0:06:43 | 0:06:47 | |
And in our experiment, these were the results. | 0:06:47 | 0:06:51 | |
Now, there's one immediate thing you can tell. | 0:06:52 | 0:06:54 | |
The ball really sped up the longer it rolled. | 0:06:55 | 0:06:59 | |
In fact, our results seem to show | 0:07:01 | 0:07:03 | |
that the time it took to cover the first quarter of the ramp | 0:07:03 | 0:07:07 | |
was about the same time it took to cover the next three-quarters. | 0:07:07 | 0:07:11 | |
So, we have a strong hint of a mathematical pattern. | 0:07:13 | 0:07:17 | |
Now, we'll see if we're right, by placing bells along the ramp, | 0:07:18 | 0:07:22 | |
at intervals which are based on the results. | 0:07:22 | 0:07:26 | |
This arrangement looks a bit strange | 0:07:27 | 0:07:29 | |
because the gap between the first two bells is much shorter | 0:07:29 | 0:07:33 | |
than the gap between the third and fourth bells. | 0:07:33 | 0:07:36 | |
But that's OK, because if we've got our calculations right, | 0:07:36 | 0:07:39 | |
the ball starts off slowly, so it covers a shorter distance, | 0:07:39 | 0:07:43 | |
and as it picks up pace, it'll cover longer and longer distances. | 0:07:43 | 0:07:47 | |
So, we should hear the bells ringing at equal intervals in time. | 0:07:47 | 0:07:52 | |
Go. | 0:07:52 | 0:07:53 | |
BELLS RING | 0:07:53 | 0:07:59 | |
Beautiful. | 0:07:59 | 0:08:01 | |
So, what does this all mean, what's the mathematical formula? | 0:08:03 | 0:08:07 | |
Well, this is something that Galileo worked out. | 0:08:07 | 0:08:10 | |
Let's say, from the start, the ball covers a distance of one metre | 0:08:10 | 0:08:13 | |
in the first second. | 0:08:13 | 0:08:15 | |
After two seconds, it will have covered four metres. | 0:08:15 | 0:08:18 | |
After three seconds, nine metres. | 0:08:18 | 0:08:20 | |
After 4 seconds, 16 metres, and so on. | 0:08:20 | 0:08:25 | |
If you recognise this progression, | 0:08:25 | 0:08:27 | |
you'll see that distance goes like the square of time. | 0:08:27 | 0:08:31 | |
Galileo had found the rates at which gravity speeds up objects. | 0:08:32 | 0:08:37 | |
And he'd found another fundamental principle - | 0:08:38 | 0:08:41 | |
you can measure the strength of gravity | 0:08:41 | 0:08:44 | |
by how much it causes falling objects to accelerate. | 0:08:44 | 0:08:47 | |
Detecting gravity has become exceptionally sophisticated | 0:08:50 | 0:08:54 | |
these days, but still uses exactly the same principle. | 0:08:54 | 0:08:58 | |
This is Herstmonceux Castle in Sussex, | 0:09:00 | 0:09:03 | |
and in its grounds lies the Space Geodesy Facility. | 0:09:03 | 0:09:07 | |
Here, Vicky uses an astonishingly sensitive instrument | 0:09:09 | 0:09:13 | |
to detect the exact strength of gravity on this one spot. | 0:09:13 | 0:09:18 | |
Vicky, tell me about this incredible gravity meter that you work with. | 0:09:18 | 0:09:22 | |
OK, so this is the dropping chamber in a stripped down version. | 0:09:22 | 0:09:26 | |
Essentially what happens | 0:09:26 | 0:09:27 | |
is you've got a cart that gets raised to the top, | 0:09:27 | 0:09:30 | |
and then the cart accelerates away from a mass in the middle, | 0:09:30 | 0:09:33 | |
and so this section lifts off and as it drops, it drops under freefall. | 0:09:33 | 0:09:37 | |
So, this component in the middle as it drops | 0:09:37 | 0:09:40 | |
is basically just Newton's apple falling to the ground? | 0:09:40 | 0:09:43 | |
-Yes. -So this is a stripped down version, but that's the real thing? | 0:09:43 | 0:09:46 | |
-This is the real thing. -How does that actually work? | 0:09:46 | 0:09:49 | |
-In here, it's a vacuum. -So there's no wind resistance as it falls. | 0:09:49 | 0:09:52 | |
There's no wind resistance. | 0:09:52 | 0:09:54 | |
Inside, a laser is used | 0:09:54 | 0:09:56 | |
to measure exactly how fast the mass is accelerating. | 0:09:56 | 0:10:00 | |
This is the 21st-century version of Galileo's ramp | 0:10:00 | 0:10:04 | |
and the balls rolling down. So, can we get it going? | 0:10:04 | 0:10:07 | |
Of course, if you'd just like to press the button on the laptop. | 0:10:07 | 0:10:09 | |
-This one? -Yep. | 0:10:09 | 0:10:11 | |
-OK. -So it's now communicating with it. | 0:10:12 | 0:10:15 | |
-Oh, here we go. -Here we go. | 0:10:15 | 0:10:16 | |
It waits five seconds and then takes the measurement of gravity. | 0:10:16 | 0:10:19 | |
-And again. -Repeats. | 0:10:19 | 0:10:21 | |
And you can see the results appearing now. | 0:10:21 | 0:10:26 | |
Yup, each of those green dots is a measurement of gravity | 0:10:26 | 0:10:29 | |
with the actual number that it's getting for each one. | 0:10:29 | 0:10:32 | |
The unit Vicky uses has a familiar ring. | 0:10:32 | 0:10:35 | |
I see that the number up at the top here, | 0:10:35 | 0:10:38 | |
you've got this unit, micro Gal? | 0:10:38 | 0:10:42 | |
Yes, a Gal is essentially one centimetre per second squared. | 0:10:42 | 0:10:46 | |
The Gal was named after Galileo. | 0:10:46 | 0:10:48 | |
So, we've just taken the measurement of gravity here today | 0:10:48 | 0:10:51 | |
and it's this highly accurate number, | 0:10:51 | 0:10:55 | |
981124007 | 0:10:55 | 0:11:00 | |
micro Gals. | 0:11:00 | 0:11:02 | |
The reading means that the Earth's gravity speeds up a falling object | 0:11:02 | 0:11:06 | |
by around 9.81 metres per second for every second it drops. | 0:11:06 | 0:11:12 | |
Vicky tells me something intriguing. | 0:11:15 | 0:11:17 | |
She takes a reading here every week and she's found that | 0:11:17 | 0:11:21 | |
the strength of gravity changes by tiny amounts over time. | 0:11:21 | 0:11:25 | |
Heavy rainfall, for example, can cause gravity to increase slightly. | 0:11:26 | 0:11:30 | |
Presumably, if gravity is changing here in one spot, | 0:11:32 | 0:11:36 | |
it'll have different values all around the world | 0:11:36 | 0:11:40 | |
and so you can have a gravity map of the entire planet? | 0:11:40 | 0:11:42 | |
That's right, yes. | 0:11:42 | 0:11:44 | |
So what's the reason for these strange fluctuations? | 0:11:45 | 0:11:48 | |
That's what I want to investigate next. | 0:11:48 | 0:11:52 | |
So, gravity changes as we move across the surface of the Earth. | 0:11:53 | 0:11:57 | |
This is at the heart of a challenge that I've set two young volunteers. | 0:11:57 | 0:12:03 | |
I've given them a task to try and find the place in Britain | 0:12:03 | 0:12:07 | |
where gravity is at its weakest. | 0:12:07 | 0:12:10 | |
So, where objects would weigh the least. | 0:12:10 | 0:12:13 | |
I've given them just three days to try and find it. | 0:12:13 | 0:12:16 | |
The volunteers are Astraya, a PhD student. | 0:12:17 | 0:12:22 | |
I've been living in London for five or six years, | 0:12:22 | 0:12:24 | |
and I'm originally from Seville in Spain. | 0:12:24 | 0:12:27 | |
I'm very interested in taking part in this project | 0:12:27 | 0:12:30 | |
because I would really like to know more about how this world works. | 0:12:30 | 0:12:34 | |
And Poppy, a journalist who lives in London. | 0:12:34 | 0:12:38 | |
I did my degree in biomedical science. | 0:12:38 | 0:12:41 | |
And I did biology and chemistry for my A-levels, | 0:12:41 | 0:12:45 | |
but I haven't done any physics since I left school. | 0:12:45 | 0:12:48 | |
I'm fascinated to find out more about gravity | 0:12:48 | 0:12:50 | |
and I actually enjoy a puzzle, I like a challenge. | 0:12:50 | 0:12:54 | |
The team just can't weigh themselves to see changes in gravity. | 0:12:54 | 0:12:57 | |
Body weight fluctuates by a couple of kilos over the course of a day. | 0:12:57 | 0:13:02 | |
Whereas, changes due to gravity as they travel around the country | 0:13:02 | 0:13:07 | |
are going to be tiny in comparison, the matter of a few grams. | 0:13:07 | 0:13:10 | |
So, they're going to have to use sophisticated scientific methods | 0:13:10 | 0:13:14 | |
if they want to measure gravity accurately. | 0:13:14 | 0:13:16 | |
And that's why the volunteers will be joined by three specialists | 0:13:16 | 0:13:20 | |
in gravity science. | 0:13:20 | 0:13:22 | |
PhD student Sonak. | 0:13:23 | 0:13:27 | |
He'll be in charge of some very sensitive measuring apparatus | 0:13:27 | 0:13:30 | |
from the National Physical Laboratory. | 0:13:30 | 0:13:33 | |
Sean, a geologist, who will be using a portable gravity meter. | 0:13:33 | 0:13:40 | |
And Andrew, a cosmologist at University College London, | 0:13:40 | 0:13:44 | |
who will help interpret the results. | 0:13:44 | 0:13:46 | |
We've taken a collective weight for the team before they set off. | 0:13:47 | 0:13:51 | |
It's 380 kilograms. | 0:13:51 | 0:13:54 | |
So, can they find the place in Britain where that will decrease? | 0:13:54 | 0:13:59 | |
They're setting out in Snowdonia National Park in North Wales. | 0:14:00 | 0:14:04 | |
The railway climbs from here to the 1,000 metre summit of Snowdon. | 0:14:06 | 0:14:10 | |
Sean takes his first gravity reading. | 0:14:10 | 0:14:13 | |
The inside is a mass on a beam and you turn this counter, | 0:14:13 | 0:14:18 | |
this dial, until you get the beam central. | 0:14:18 | 0:14:23 | |
By counting the number of turns of the dial, | 0:14:23 | 0:14:26 | |
Sean can calculate the downward pull of gravity | 0:14:26 | 0:14:29 | |
acting on the mass inside the machine. | 0:14:29 | 0:14:32 | |
Sonak has a simpler method. | 0:14:32 | 0:14:36 | |
So, inside the box is a two kilogram mass, | 0:14:36 | 0:14:40 | |
and it's supposed to be sort of as perfectly two kilograms | 0:14:40 | 0:14:42 | |
as it's possible to get. | 0:14:42 | 0:14:44 | |
All right. And place it here. | 0:14:46 | 0:14:49 | |
Oh, it's just coming under, isn't it? | 0:14:50 | 0:14:52 | |
1998.2 grams. | 0:14:52 | 0:14:55 | |
It was two kilos in the laboratory, but now here it's a bit less. | 0:14:55 | 0:14:59 | |
It's the first puzzle. | 0:14:59 | 0:15:01 | |
Why does a two kilo mass tip the scales at just under two kilos? | 0:15:01 | 0:15:07 | |
And it's one which gets straight to the heart | 0:15:07 | 0:15:10 | |
of what the challenge is really about. | 0:15:10 | 0:15:13 | |
Mass is often confused with the related quantity, weight. | 0:15:14 | 0:15:19 | |
The mass of these dumbbells is fixed, it doesn't change. | 0:15:19 | 0:15:24 | |
It's a measure of how much stuff they contain. | 0:15:24 | 0:15:27 | |
Weight is different. | 0:15:27 | 0:15:29 | |
It's a measure of the effects of gravity on these dumbbells. | 0:15:29 | 0:15:33 | |
The downward force pulling them to the ground | 0:15:33 | 0:15:36 | |
in the same way that it's keeping my feet firmly stuck to the ground. | 0:15:36 | 0:15:40 | |
The crucial difference is this, | 0:15:40 | 0:15:42 | |
if I was holding these dumbbells on the moon, | 0:15:42 | 0:15:44 | |
they'd still have exactly the same mass, | 0:15:44 | 0:15:47 | |
but they'd weigh six times less | 0:15:47 | 0:15:50 | |
because the moon's gravity is so much weaker than the Earth's. | 0:15:50 | 0:15:54 | |
So that's why Sonak is bringing along the two kilo mass. | 0:15:56 | 0:16:00 | |
If it changes weight then this should mean | 0:16:00 | 0:16:03 | |
that gravity itself has changed. | 0:16:03 | 0:16:05 | |
Ahead of them is the summit of the highest mountain | 0:16:07 | 0:16:11 | |
in England and Wales, famed for its stunning scenery. | 0:16:11 | 0:16:14 | |
Or it would be stunning if you could see it. | 0:16:16 | 0:16:19 | |
And this is what we came all the way up here for, | 0:16:20 | 0:16:24 | |
this amazing view at the top of Snowdon. | 0:16:24 | 0:16:27 | |
You wouldn't know it, but honestly, we are here. | 0:16:27 | 0:16:30 | |
We're now near the summit of Snowdon and I've set up the gravimeter, | 0:16:32 | 0:16:36 | |
and we're going to see what the difference in the reading is. | 0:16:36 | 0:16:39 | |
He has to turn the dial again and again to try and get a reading. | 0:16:42 | 0:16:46 | |
It's clear gravity has changed, but which way? | 0:16:46 | 0:16:50 | |
Has it got stronger, or weaker? | 0:16:50 | 0:16:53 | |
The team leave Sean to work out his results, | 0:16:53 | 0:16:56 | |
and tries to position the scales as close as possible to the summit. | 0:16:56 | 0:17:00 | |
But the reading is all over the place. | 0:17:01 | 0:17:03 | |
-Oh! -It's gone up. | 0:17:03 | 0:17:07 | |
It's fluctuating quite a lot due to the wind. | 0:17:07 | 0:17:09 | |
I have to say, this is what science is always like, isn't it? | 0:17:09 | 0:17:12 | |
It's never quite what you want it to be. | 0:17:12 | 0:17:14 | |
So, they head inside to the cafe next to the summit. | 0:17:14 | 0:17:18 | |
The wind was being a bit naughty, but hopefully... | 0:17:20 | 0:17:23 | |
Now it's in 00, so it should be all right. | 0:17:23 | 0:17:25 | |
1998.2 down there, | 0:17:25 | 0:17:28 | |
1997.8! | 0:17:28 | 0:17:31 | |
-There you go. -We've got it! That's 0.4 of a gram off. | 0:17:31 | 0:17:35 | |
The mass weighs a tiny bit less. | 0:17:36 | 0:17:39 | |
It's lost about one 5000th of its weight. | 0:17:39 | 0:17:44 | |
And Sean has found that gravity itself has reduced. | 0:17:44 | 0:17:48 | |
At the top of the mountain we took the measurement | 0:17:48 | 0:17:51 | |
and we discovered that the pull of gravity had gone down. | 0:17:51 | 0:17:56 | |
It had gone down the equivalent of 206 turns of the dial. | 0:17:56 | 0:17:59 | |
And we worked out that that's equivalent to 219 milligals. | 0:17:59 | 0:18:04 | |
So it's clear from the team's measurements, | 0:18:06 | 0:18:09 | |
gravity weakens as you go higher, and you get a bit lighter. | 0:18:09 | 0:18:14 | |
It's just an excuse to say where are we, like, the lightest. | 0:18:16 | 0:18:19 | |
-Who cares? -Yes, who does care? | 0:18:19 | 0:18:21 | |
It's actually really interestingly, it's like an illustrative example | 0:18:21 | 0:18:25 | |
of seeing how this is actually fluctuating, | 0:18:25 | 0:18:28 | |
-depending on different factors. -Yeah, absolutely. | 0:18:28 | 0:18:31 | |
And that we could measure it and see it with our own eyes, | 0:18:31 | 0:18:34 | |
it actually makes you think about gravity in a very active way. | 0:18:34 | 0:18:37 | |
It's such a fundamental force phenomenon in nature, | 0:18:37 | 0:18:40 | |
but we don't know much about it. | 0:18:40 | 0:18:42 | |
But why does gravity change with altitude? | 0:18:44 | 0:18:47 | |
To understand that question, | 0:18:48 | 0:18:50 | |
you've to get to grips with the extraordinary discoveries | 0:18:50 | 0:18:53 | |
of the next scientific giant in our story - | 0:18:53 | 0:18:56 | |
Isaac Newton. | 0:18:56 | 0:18:59 | |
Born in England in the middle of the 17th century, | 0:18:59 | 0:19:02 | |
he spent his life wrestling with so many apparently separate questions, | 0:19:02 | 0:19:06 | |
from why things fall to the ground, to why planets orbit the sun. | 0:19:06 | 0:19:11 | |
It took the genius of Newton to realise | 0:19:14 | 0:19:17 | |
there was one single equation that could answer all these questions. | 0:19:17 | 0:19:21 | |
And here it is, his famous law of gravity. | 0:19:23 | 0:19:27 | |
It might look complicated, | 0:19:27 | 0:19:28 | |
but this is one of the most important equations | 0:19:28 | 0:19:31 | |
in the whole of science. | 0:19:31 | 0:19:33 | |
F here is the force. | 0:19:33 | 0:19:34 | |
Newton said there's an attractive force between any two objects | 0:19:34 | 0:19:38 | |
in the universe. | 0:19:38 | 0:19:40 | |
On this side of the equation, G, we call the gravitational constant. | 0:19:40 | 0:19:44 | |
Newton knew it had to be there, but he didn't know what its value was. | 0:19:44 | 0:19:48 | |
M1 and M2 represent the two objects, and R is the distance between them. | 0:19:48 | 0:19:55 | |
Now, the equation tells us that the more massive the objects are, | 0:19:55 | 0:19:59 | |
the bigger M1 and M2, the greater the attractive force. | 0:19:59 | 0:20:04 | |
But the further apart they are, the bigger the value of R here, | 0:20:04 | 0:20:08 | |
the weaker the gravitational force. | 0:20:08 | 0:20:10 | |
With Newton, what was once mysterious now became clear. | 0:20:11 | 0:20:15 | |
Newton's equation describes why an object falls to the ground, | 0:20:16 | 0:20:21 | |
including his famous apple. | 0:20:21 | 0:20:23 | |
But its true genius is that it applies to any object, | 0:20:23 | 0:20:26 | |
anywhere in the universe. | 0:20:26 | 0:20:28 | |
So, it's a very simple and elegant way of describing | 0:20:28 | 0:20:32 | |
some of the seemingly most complicated phenomena in the cosmos. | 0:20:32 | 0:20:37 | |
His law of gravitation can still be used today - | 0:20:41 | 0:20:45 | |
to explain how orbits work, | 0:20:45 | 0:20:48 | |
to predict when a comet will return, | 0:20:48 | 0:20:52 | |
to describe why galaxies spin. | 0:20:52 | 0:20:55 | |
Or to slingshot spacecraft around planets. | 0:20:57 | 0:21:00 | |
Newton tells us to look for the underlying simplicity | 0:21:02 | 0:21:05 | |
in natural phenomena. For instance, how the moon orbits the Earth. | 0:21:05 | 0:21:09 | |
If I let go of this apple, | 0:21:11 | 0:21:13 | |
it'll fall straight down because of the pull of Earth's gravity. | 0:21:13 | 0:21:16 | |
But if I throw it, to begin with, | 0:21:17 | 0:21:19 | |
it travels in a horizontal direction, | 0:21:19 | 0:21:21 | |
that's the direction of travel, | 0:21:21 | 0:21:23 | |
but Earth's gravity is still pulling it downwards, | 0:21:23 | 0:21:25 | |
so it ends up following a curved path. | 0:21:25 | 0:21:28 | |
Now, if I throw it harder, | 0:21:35 | 0:21:36 | |
it'll travel further before it hits the ground and, in principle, | 0:21:36 | 0:21:40 | |
if I could throw it hard enough, I could put it into orbit. | 0:21:40 | 0:21:43 | |
That's exactly what's happening with the moon in orbit around the Earth. | 0:21:43 | 0:21:47 | |
It's a combination of wanting to travel in a straight line, | 0:21:47 | 0:21:51 | |
but also being pulled down by the Earth's gravity. | 0:21:51 | 0:21:53 | |
So, it ends up constantly falling | 0:21:53 | 0:21:56 | |
around the Earth and constantly missing. | 0:21:56 | 0:21:58 | |
Newton's famous equation | 0:22:01 | 0:22:02 | |
also explains the strange effects | 0:22:02 | 0:22:04 | |
which the road-trip team has discovered. | 0:22:04 | 0:22:07 | |
That objects get lighter as you gain in altitude. | 0:22:07 | 0:22:10 | |
When I weigh myself, I'm represented by the first mass, M1. | 0:22:12 | 0:22:16 | |
The second mass, M2, is the Earth itself. | 0:22:16 | 0:22:19 | |
And the force pulling me down, my weight, | 0:22:19 | 0:22:23 | |
depends on the distance between me and the centre of the Earth. | 0:22:23 | 0:22:27 | |
And that's the secret of the road trip. | 0:22:27 | 0:22:29 | |
If you want to find the place where you weigh the least, | 0:22:29 | 0:22:32 | |
then you have to get as far away as you can from the Earth's core. | 0:22:32 | 0:22:36 | |
So, it's the afternoon of day one, | 0:22:44 | 0:22:47 | |
and the road-trip team have to work out where to go next. | 0:22:47 | 0:22:51 | |
Poppy and Astraya have a good idea, | 0:22:51 | 0:22:54 | |
find somewhere higher than Mount Snowdon. | 0:22:54 | 0:22:57 | |
From the measurements that you guys did at Mount Snowdon, | 0:22:57 | 0:23:01 | |
altitude clearly plays an important part in gravity. | 0:23:01 | 0:23:04 | |
So, with that in mind, we've got to go to the highest point in the UK, | 0:23:04 | 0:23:07 | |
which is Ben Nevis. | 0:23:07 | 0:23:08 | |
OK, BUT there's just one thing that we haven't shown you so far. | 0:23:08 | 0:23:13 | |
We actually brought along an extra experiment, | 0:23:13 | 0:23:16 | |
so can we please show you this first before you make the final decision? | 0:23:16 | 0:23:19 | |
-Yes. -Sonak actually has the other part of this experiment. | 0:23:19 | 0:23:23 | |
We always carry around... | 0:23:23 | 0:23:25 | |
Some power tools, as physicists always do. | 0:23:25 | 0:23:27 | |
Let's start it off nice and gentle. | 0:23:27 | 0:23:29 | |
OK. | 0:23:31 | 0:23:32 | |
And then, try and pick up some pace. | 0:23:32 | 0:23:34 | |
Pizza. | 0:23:36 | 0:23:37 | |
-You've got some pizza there. -OK. Point proven. | 0:23:39 | 0:23:42 | |
The point is that when something is spinning, | 0:23:42 | 0:23:44 | |
it kind of gets flung outwards and you can actually use that | 0:23:44 | 0:23:48 | |
to make a nice, flat piece of pizza, but this also applies to the Earth. | 0:23:48 | 0:23:52 | |
The Earth isn't perfectly round. | 0:23:52 | 0:23:55 | |
It's what's known as an "oblate spheroid". | 0:23:55 | 0:23:58 | |
It bulges at the equator | 0:23:58 | 0:24:00 | |
where the spin is greatest. | 0:24:00 | 0:24:03 | |
We've kind of got two competing effects now. | 0:24:03 | 0:24:05 | |
We're trying to get away from the centre, | 0:24:05 | 0:24:08 | |
the actual core of the Earth, | 0:24:08 | 0:24:09 | |
the point at the very centre of this ball. | 0:24:09 | 0:24:12 | |
But now, we can do it in two ways. | 0:24:12 | 0:24:14 | |
We can either go up something tall, | 0:24:14 | 0:24:16 | |
or we can just go down towards the equator. | 0:24:16 | 0:24:20 | |
This is what we find when we're doing gravity surveys, | 0:24:20 | 0:24:23 | |
as you move south, there tends to be an effect from latitude | 0:24:23 | 0:24:27 | |
which is often usually larger than the effect from altitude. | 0:24:27 | 0:24:32 | |
So, the closer to the equator you go, | 0:24:32 | 0:24:36 | |
the further you get from the Earth's core and the lighter you get. | 0:24:36 | 0:24:41 | |
So, guys, the sun's setting just behind me here. This is north. | 0:24:41 | 0:24:46 | |
From the conversations we've just had, | 0:24:46 | 0:24:48 | |
it sounds like we've got to go that way, | 0:24:48 | 0:24:51 | |
down south, is that right? | 0:24:51 | 0:24:52 | |
-Yes, OK. -Let's go. | 0:24:52 | 0:24:54 | |
THEY LAUGH | 0:24:54 | 0:24:56 | |
The team is starting to uncover the reasons why gravity changes | 0:24:56 | 0:25:00 | |
as you cross the surface of the Earth. | 0:25:00 | 0:25:02 | |
Our planet is defined and shaped | 0:25:05 | 0:25:07 | |
by the complicated forces which act upon it. | 0:25:07 | 0:25:11 | |
And detecting tiny fluctuations in its gravity field | 0:25:11 | 0:25:14 | |
can give us important clues. | 0:25:14 | 0:25:18 | |
It can help us understand how our world is changing. | 0:25:18 | 0:25:21 | |
The Space Geodesy Facility at Herstmonceux is one small part | 0:25:23 | 0:25:27 | |
of an enormous global network | 0:25:27 | 0:25:29 | |
which uses satellites to detect the tiniest of changes | 0:25:29 | 0:25:33 | |
in the Earth's gravity field. | 0:25:33 | 0:25:36 | |
Tell me what exactly your job is here? | 0:25:36 | 0:25:38 | |
What we're doing with this telescope | 0:25:38 | 0:25:40 | |
is measuring very accurately | 0:25:40 | 0:25:42 | |
the distances of satellites from here, | 0:25:42 | 0:25:45 | |
so we're using very short laser pulses | 0:25:45 | 0:25:47 | |
which we direct towards the satellite. | 0:25:47 | 0:25:49 | |
On the satellite, there are reflecting cubes, | 0:25:49 | 0:25:52 | |
which return some of that light to us. | 0:25:52 | 0:25:54 | |
We measure how long it takes the light | 0:25:54 | 0:25:56 | |
to go to the satellite and back. | 0:25:56 | 0:25:57 | |
And how far away is the satellite typically? | 0:25:57 | 0:25:59 | |
The one we're tracking now is one of the Galileo satellites, | 0:25:59 | 0:26:02 | |
which is about 20,000 kilometres. | 0:26:02 | 0:26:04 | |
-20,000 kilometres away? -Yes. | 0:26:04 | 0:26:07 | |
OK, so, we've got it aimed at the Galileo satellite | 0:26:07 | 0:26:09 | |
-and you're going to turn the laser on now? -Yes. | 0:26:09 | 0:26:12 | |
Oh, wow! | 0:26:14 | 0:26:16 | |
And that laser beam that's being fired up towards the satellite, | 0:26:16 | 0:26:21 | |
the time it'll take to get there and come back again, | 0:26:21 | 0:26:23 | |
-it's a fraction of a second, isn't it? -It is. | 0:26:23 | 0:26:26 | |
It's about 150 thousandths of a second, 150 milliseconds. | 0:26:26 | 0:26:29 | |
And we're sending about 1,000 of those per second. | 0:26:29 | 0:26:32 | |
This strange-looking object is based on satellite readings. | 0:26:36 | 0:26:40 | |
It's a highly exaggerated representation | 0:26:40 | 0:26:42 | |
of how Earth's gravity field varies over time. | 0:26:42 | 0:26:46 | |
Fluctuations like these can give us important insights | 0:26:48 | 0:26:52 | |
into climate change, | 0:26:52 | 0:26:53 | |
icecaps melting, | 0:26:53 | 0:26:55 | |
sea levels rising, | 0:26:55 | 0:26:58 | |
changes in ground water. | 0:26:58 | 0:27:01 | |
All of these have an effect | 0:27:01 | 0:27:03 | |
on the local strength of gravity. | 0:27:03 | 0:27:05 | |
So, something as important as climate change, | 0:27:05 | 0:27:09 | |
in order to understand it and do something about it, | 0:27:09 | 0:27:11 | |
we need to know the distribution | 0:27:11 | 0:27:13 | |
of the gravitational field of the Earth very accurately? | 0:27:13 | 0:27:16 | |
Absolutely, yes. And it's a global measure that we need. | 0:27:16 | 0:27:20 | |
For the road trippers, it's the start of day two... | 0:27:25 | 0:27:28 | |
..and they're heading for the south coast. | 0:27:30 | 0:27:32 | |
They're stopping off in Herefordshire, | 0:27:34 | 0:27:36 | |
it's a good location as it's the same altitude | 0:27:36 | 0:27:39 | |
as the base of Snowdon, | 0:27:39 | 0:27:41 | |
but they've moved about 80 miles further south. | 0:27:41 | 0:27:44 | |
So, if they find gravity changes here, it must be due to latitude. | 0:27:44 | 0:27:49 | |
It's not a huge difference, but it's noticeable. | 0:27:49 | 0:27:51 | |
Our counter reading at the bottom of the mountain was 4,840. | 0:27:51 | 0:27:55 | |
-Yes. -Our counter reading here's 4,717. | 0:27:55 | 0:27:59 | |
Oh, right, so, we do get to see a difference. | 0:27:59 | 0:28:02 | |
So, we're at the same altitude as the base of Mount Snowdon, | 0:28:02 | 0:28:05 | |
but because we've travelled further down south overnight, | 0:28:05 | 0:28:08 | |
-gravity's less here? -Yes. | 0:28:08 | 0:28:10 | |
They push on. | 0:28:13 | 0:28:14 | |
And by sunset they reach Sidmouth on the south coast. | 0:28:20 | 0:28:24 | |
Sean takes the second gravity reading of the day | 0:28:26 | 0:28:30 | |
and Poppy improvises a map. | 0:28:30 | 0:28:33 | |
Well, sort of a map. | 0:28:33 | 0:28:35 | |
Can we write "not to scale" at the top there. | 0:28:35 | 0:28:38 | |
SHE MOUTHS, ALL LAUGH | 0:28:38 | 0:28:41 | |
So, I drew this map. | 0:28:41 | 0:28:44 | |
Scotland's a bit squashed. | 0:28:44 | 0:28:45 | |
Wales is quite high up and Cornwall is there, but you get the idea. | 0:28:45 | 0:28:51 | |
Sean, we've been travelling with you, | 0:28:51 | 0:28:54 | |
you've done quite a few gravity meter readings, | 0:28:54 | 0:28:57 | |
can you plot them on this not-to-scale, | 0:28:57 | 0:28:59 | |
-badly-drawn map, please? -Sure. | 0:28:59 | 0:29:01 | |
So, if you remember we started off in Mount Snowdon, here, | 0:29:01 | 0:29:06 | |
and that was the zero measurement for our survey. | 0:29:06 | 0:29:09 | |
Then we've come all the way down here to the south coast. | 0:29:09 | 0:29:12 | |
-The difference from the base of Snowdon is -212 milligals. -Wow. | 0:29:14 | 0:29:22 | |
So, the difference between going and measuring gravity | 0:29:22 | 0:29:25 | |
at the base of the mountain and the top of the mountain | 0:29:25 | 0:29:29 | |
is about the same as here at this latitude | 0:29:29 | 0:29:31 | |
and down here at this latitude. | 0:29:31 | 0:29:35 | |
They're quite clearly at sea level, | 0:29:35 | 0:29:37 | |
yet gravity here is roughly the same as it is at the top of Snowdon. | 0:29:37 | 0:29:42 | |
But where next? | 0:29:42 | 0:29:44 | |
We are here. | 0:29:44 | 0:29:46 | |
If we want to find out where we are the lightest, | 0:29:46 | 0:29:50 | |
why don't we travel all the way to the most southerly point in the UK, | 0:29:50 | 0:29:55 | |
-which is here? -But altitude can also help us, | 0:29:55 | 0:29:59 | |
so why not find a place in the country | 0:29:59 | 0:30:02 | |
that is both low in latitude but also as high in altitude | 0:30:02 | 0:30:07 | |
in terms of height above sea level, because that will get us somewhere | 0:30:07 | 0:30:11 | |
that is really far away from the core of the Earth, | 0:30:11 | 0:30:14 | |
whilst staying within the country? | 0:30:14 | 0:30:17 | |
So, the answer to the puzzle lies in a combination of two factors. | 0:30:23 | 0:30:28 | |
How much further south should they go and how much higher? | 0:30:28 | 0:30:32 | |
At the end of day two, Sean's results show that the team | 0:30:34 | 0:30:38 | |
weighs about 80 grams lighter in total | 0:30:38 | 0:30:40 | |
than back at the base of Snowdon. | 0:30:40 | 0:30:42 | |
The way that weight changes is just one example | 0:30:54 | 0:30:57 | |
of Newton's famous equation in action. | 0:30:57 | 0:31:00 | |
But Newton had left his masterpiece incomplete. | 0:31:02 | 0:31:05 | |
He didn't know the value of G, | 0:31:05 | 0:31:07 | |
the gravitational constant, | 0:31:07 | 0:31:10 | |
which sets the size of the force. | 0:31:10 | 0:31:14 | |
To harness the full power of the equation, you need to know G. | 0:31:14 | 0:31:18 | |
And the vital clue came within an incredible experiment | 0:31:18 | 0:31:22 | |
conducted in London at the end of the 18th century. | 0:31:22 | 0:31:25 | |
It was an attempt to work out the mass of the Earth itself. | 0:31:29 | 0:31:33 | |
And it was carried out by an eccentric, | 0:31:33 | 0:31:36 | |
extravagantly rich aristocrat, | 0:31:36 | 0:31:39 | |
Henry Cavendish. | 0:31:39 | 0:31:41 | |
Cavendish was a chronically shy, | 0:31:41 | 0:31:45 | |
deeply solitary man living in total isolation in his house in Clapham. | 0:31:45 | 0:31:49 | |
The story goes that, one day, | 0:31:49 | 0:31:51 | |
he accidentally bumped into a female servant on his staircase. | 0:31:51 | 0:31:55 | |
He was so traumatised by this event | 0:31:55 | 0:31:57 | |
that he had a new staircase built just for him | 0:31:57 | 0:32:00 | |
so that this horrible incident could never happen again. | 0:32:00 | 0:32:03 | |
Cavendish had inherited vast fortunes | 0:32:05 | 0:32:07 | |
and was able to dedicate his life | 0:32:07 | 0:32:09 | |
to devising pioneering experiments - | 0:32:09 | 0:32:13 | |
including one particularly extraordinary piece of equipment. | 0:32:13 | 0:32:16 | |
He set up something a bit like this. | 0:32:21 | 0:32:23 | |
It's called a "torsion balance". | 0:32:23 | 0:32:25 | |
It involves four lead spheres, | 0:32:25 | 0:32:28 | |
two large heavy ones which are held fixed in place, | 0:32:28 | 0:32:31 | |
and suspended by a very thin wire is a wooden rod, | 0:32:31 | 0:32:36 | |
six-feet-long, with two smaller balls on either end. | 0:32:36 | 0:32:40 | |
Now, the crux of the experiment | 0:32:40 | 0:32:42 | |
is the relationship between the large ball and the small ball. | 0:32:42 | 0:32:46 | |
Now, of course, there's a gravitational pull downwards | 0:32:46 | 0:32:49 | |
on both of the balls due to the Earth's gravity. | 0:32:49 | 0:32:52 | |
But Newton also tells us | 0:32:52 | 0:32:53 | |
that there should be a very weak gravitational pull between the balls | 0:32:53 | 0:32:58 | |
and this is effectively what Cavendish was trying to measure. | 0:32:58 | 0:33:01 | |
Any slight movement of the small ball towards the large one | 0:33:01 | 0:33:05 | |
should cause a twist in the torsion wire | 0:33:05 | 0:33:08 | |
and that's what Cavendish was trying to detect. | 0:33:08 | 0:33:11 | |
Of course, this is all much easier said than done. | 0:33:11 | 0:33:14 | |
The experiment was incredibly sensitive. | 0:33:14 | 0:33:16 | |
The tiniest of vibrations, | 0:33:16 | 0:33:18 | |
the slightest breeze, changes in temperature | 0:33:18 | 0:33:21 | |
could all influence the measurements. | 0:33:21 | 0:33:23 | |
So, Cavendish had to isolate the apparatus inside a box | 0:33:23 | 0:33:27 | |
and the box within a shed. | 0:33:27 | 0:33:30 | |
He even realised that his mere presence next to the apparatus | 0:33:30 | 0:33:34 | |
could influence things, so he had to remove himself outside the shed. | 0:33:34 | 0:33:38 | |
What he then did was sit outside the shed, | 0:33:39 | 0:33:41 | |
and through a small hole in the shed wall, | 0:33:41 | 0:33:44 | |
look through a telescope to detect the tiniest of twists in the wire. | 0:33:44 | 0:33:49 | |
It was an incredibly difficult process, but after many months, | 0:33:49 | 0:33:52 | |
he finally felt confident enough that he had a reliable result. | 0:33:52 | 0:33:56 | |
Cavendish found that the small balls did move... | 0:34:03 | 0:34:06 | |
..a tiny four millimetres. | 0:34:08 | 0:34:10 | |
He calculated his results | 0:34:13 | 0:34:14 | |
by comparing the density of the balls | 0:34:14 | 0:34:16 | |
with the density of water. | 0:34:16 | 0:34:18 | |
In the end, the result of Cavendish's experiment | 0:34:20 | 0:34:23 | |
and subsequent calculations | 0:34:23 | 0:34:24 | |
was that the density of the Earth | 0:34:24 | 0:34:27 | |
was about five and a half times that of water. | 0:34:27 | 0:34:30 | |
Or, put another way, | 0:34:30 | 0:34:32 | |
the mass of the Earth was 5.9 trillion trillion kilograms. | 0:34:32 | 0:34:38 | |
What's most remarkable is that Cavendish got this number right | 0:34:38 | 0:34:42 | |
to within an accuracy of 1%. | 0:34:42 | 0:34:45 | |
With Cavendish's astonishing result, | 0:34:45 | 0:34:49 | |
scientists were able to work out G. | 0:34:49 | 0:34:51 | |
Then the equation could be used | 0:34:53 | 0:34:55 | |
to determine the mass of any celestial body | 0:34:55 | 0:34:57 | |
in orbit around another. | 0:34:57 | 0:34:59 | |
So, astronomers were able to calculate the mass of the sun | 0:35:01 | 0:35:05 | |
and the planets, and the moon, | 0:35:05 | 0:35:08 | |
and, eventually, even distant galaxies. | 0:35:08 | 0:35:12 | |
At the end of day two, the team were in Sidmouth on the south coast, | 0:35:17 | 0:35:21 | |
looking for the place in Britain where they'll weigh the least. | 0:35:21 | 0:35:25 | |
They've worked out the answer lies in a combination of two factors - | 0:35:25 | 0:35:30 | |
the right mix of going south and being higher up. | 0:35:30 | 0:35:34 | |
For the final leg of the journey, I'm going to meet up with them. | 0:35:36 | 0:35:39 | |
I asked them to drive a short distance west | 0:35:41 | 0:35:44 | |
to one of the most remote areas in mainland Britain. | 0:35:44 | 0:35:48 | |
Dartmoor National Park. | 0:35:48 | 0:35:50 | |
'It's only 40 miles from the southernmost tip of Britain.' | 0:35:52 | 0:35:55 | |
Hello. Hi, Andrew. | 0:35:55 | 0:35:56 | |
-Good to see you. -Nice to see you. | 0:35:56 | 0:35:58 | |
'And it's very high, very hilly territory.' | 0:35:58 | 0:36:02 | |
Jim, the team got to the south coast yesterday... | 0:36:02 | 0:36:04 | |
-Yes. -..to find gravity at its weakest. | 0:36:04 | 0:36:08 | |
But we haven't quite figured out whether it's altitude or latitude. | 0:36:08 | 0:36:12 | |
Do we go further south or do we go higher up? | 0:36:12 | 0:36:14 | |
You're right to ask, "Do we go as far south as possible | 0:36:14 | 0:36:18 | |
"or as high as possible?" | 0:36:18 | 0:36:20 | |
That's why I've brought you here to Dartmoor. | 0:36:20 | 0:36:23 | |
We've charted the most important points on this map here. | 0:36:23 | 0:36:27 | |
-Right. -Let's have a look. | 0:36:27 | 0:36:29 | |
So, we are here, Two Bridges. | 0:36:29 | 0:36:32 | |
-Yes. -These four dots represent these hills up there behind us, | 0:36:32 | 0:36:37 | |
which are at about 500 metres above sea level. | 0:36:37 | 0:36:40 | |
That's what we want to check out. | 0:36:40 | 0:36:42 | |
'These hills are close to the south coast | 0:36:42 | 0:36:44 | |
'and they're also the highest in the whole of the south of England. | 0:36:44 | 0:36:48 | |
'So, logic suggests they must be the right combination | 0:36:50 | 0:36:53 | |
'of latitude and altitude.' | 0:36:53 | 0:36:55 | |
Well, there's another reason why this makes perfect sense, | 0:36:55 | 0:36:58 | |
one which we haven't looked at yet, | 0:36:58 | 0:37:00 | |
and that's the effect of the underlying rocks on gravity. | 0:37:00 | 0:37:03 | |
And I've got a map here that shows... | 0:37:03 | 0:37:05 | |
-You're going to trump my map with yours, aren't you? -I am! | 0:37:05 | 0:37:08 | |
Here we are, down here, now these blue areas are the lowest areas | 0:37:08 | 0:37:13 | |
according to the density of the rocks underneath. | 0:37:13 | 0:37:17 | |
'The rocks around here are made of granite, | 0:37:17 | 0:37:20 | |
'which will make gravity weaker still.' | 0:37:20 | 0:37:22 | |
So, that's helping - as well as the altitude | 0:37:24 | 0:37:26 | |
and the fact that we're further south. | 0:37:26 | 0:37:28 | |
Yes, it's also playing a part. | 0:37:28 | 0:37:31 | |
'Well, we have a plausible theory. | 0:37:33 | 0:37:35 | |
'But now we need to test it.' | 0:37:35 | 0:37:37 | |
'If I'm right, then, at the top, our gravity reading | 0:37:39 | 0:37:42 | |
'should be by far the lowest reading of the trip.' | 0:37:42 | 0:37:45 | |
'Of course, there's another effect of gravity to deal with now - | 0:37:48 | 0:37:51 | |
'it's knackering when you head uphill.' | 0:37:51 | 0:37:54 | |
OK, I think this is pretty much the start of the hills | 0:37:55 | 0:37:58 | |
we've located on the map. So, let's see if this is the lightest place. | 0:37:58 | 0:38:02 | |
Sean, if you want to get the gravity meter out, | 0:38:02 | 0:38:05 | |
-and we'll take another reading here. -Yep. -OK. | 0:38:05 | 0:38:08 | |
'Sean sets up his equipment one more time.' | 0:38:11 | 0:38:14 | |
What's the news? | 0:38:14 | 0:38:16 | |
Well, the bottom of Mount Snowdon was our zero for this test. | 0:38:16 | 0:38:21 | |
We found we lost a certain amount | 0:38:21 | 0:38:23 | |
by going up to the top of Mount Snowdon. | 0:38:23 | 0:38:25 | |
We found we lost a certain amount coming south to the south coast. | 0:38:25 | 0:38:29 | |
Not only have we beaten that, we've smashed it. | 0:38:29 | 0:38:32 | |
-Brilliant. -We were -219 milligals | 0:38:32 | 0:38:36 | |
lower at the top of Mount Snowdon. | 0:38:36 | 0:38:39 | |
Here on Dartmoor, | 0:38:39 | 0:38:40 | |
-we're -347 milligals lower. -Wow! -Brilliant! | 0:38:40 | 0:38:44 | |
So, it is a combination of three things. | 0:38:44 | 0:38:46 | |
We're far south, so it's the latitude, we're at altitude, | 0:38:46 | 0:38:49 | |
we're quite high up, and we're surrounded by all this granite rock, | 0:38:49 | 0:38:52 | |
which is low-density anyway. | 0:38:52 | 0:38:54 | |
I hope you all think it was worth the climb up here anyway? | 0:38:54 | 0:38:57 | |
-Yes, absolutely. -There you go. Boom, science! | 0:38:57 | 0:39:00 | |
ALL LAUGH | 0:39:00 | 0:39:04 | |
Now, we already know that the altitude of these hills | 0:39:04 | 0:39:07 | |
takes us much further from the Earth's core | 0:39:07 | 0:39:10 | |
than anywhere else further south in Britain, | 0:39:10 | 0:39:12 | |
so gravity must be weakest here. | 0:39:12 | 0:39:16 | |
There's extra evidence, too. | 0:39:16 | 0:39:18 | |
The British Geological Survey | 0:39:18 | 0:39:20 | |
has compiled tens of thousands of gravity readings made in the UK | 0:39:20 | 0:39:24 | |
and the lowest readings ever recorded were all taken around here | 0:39:24 | 0:39:29 | |
on the high hills of Dartmoor. | 0:39:29 | 0:39:31 | |
What do we do to celebrate? | 0:39:32 | 0:39:34 | |
We weigh ourselves, of course. | 0:39:34 | 0:39:36 | |
I bet you don't weigh that much. | 0:39:36 | 0:39:38 | |
Whoa! | 0:39:38 | 0:39:40 | |
It's all them Nutella pancakes for breakfast! | 0:39:40 | 0:39:43 | |
-74, 75. -I need to lose weight! | 0:39:43 | 0:39:46 | |
LAUGHTER | 0:39:46 | 0:39:47 | |
I can tell you that you should weigh something like 20 grams less | 0:39:47 | 0:39:52 | |
than you did at the base of Mount Snowdon. | 0:39:52 | 0:39:55 | |
Guys, I'm guessing something like 25 to 30 grams less. | 0:39:55 | 0:39:59 | |
So, if you want to weigh as little as possible, | 0:39:59 | 0:40:02 | |
this is the place in Britain to come. | 0:40:02 | 0:40:04 | |
But in any case, it's such a tiny amount | 0:40:04 | 0:40:06 | |
that it's going to be wiped out entirely | 0:40:06 | 0:40:08 | |
by whatever it was you had for breakfast this morning. | 0:40:08 | 0:40:11 | |
LAUGHTER | 0:40:11 | 0:40:12 | |
Gravity. What goes up must come down. | 0:40:18 | 0:40:22 | |
All of our lives, we abide by its rules. | 0:40:24 | 0:40:27 | |
It dominates our every action. | 0:40:28 | 0:40:30 | |
But there's one select group of humans | 0:40:31 | 0:40:33 | |
who know what it's like to live free of gravity. | 0:40:33 | 0:40:37 | |
'Two, one... | 0:40:37 | 0:40:39 | |
'zero. | 0:40:39 | 0:40:40 | |
'Lift-off!' | 0:40:40 | 0:40:42 | |
Everybody's used to gravity. | 0:40:46 | 0:40:48 | |
We're used to the oppression of it. | 0:40:48 | 0:40:50 | |
Gravity is the ultimate oppressor. | 0:40:50 | 0:40:52 | |
It grinds us under its heel 24/7 with no release, | 0:40:52 | 0:40:58 | |
until you're in space and then, suddenly, you're free from gravity. | 0:40:58 | 0:41:03 | |
You're weightless in orbit. | 0:41:03 | 0:41:05 | |
Canadian astronaut Chris Hadfield | 0:41:07 | 0:41:09 | |
spent five months on board the International Space Station. | 0:41:09 | 0:41:14 | |
You can pull your knees up to your chest and just tumble. | 0:41:14 | 0:41:17 | |
Or, if you take a wet cloth, | 0:41:17 | 0:41:19 | |
and you get it dripping wet, | 0:41:19 | 0:41:22 | |
and everybody on Earth knows what'll happen when you wring it out. | 0:41:22 | 0:41:25 | |
All the water will fall, inevitably. | 0:41:25 | 0:41:27 | |
If you do that in weightlessness, | 0:41:27 | 0:41:29 | |
the water stays there and it, actually, | 0:41:29 | 0:41:31 | |
because of the surface tension, starts crawling up your arms. | 0:41:31 | 0:41:35 | |
It's a little bit mesmerising and hypnotic to be in weightlessness. | 0:41:40 | 0:41:44 | |
If you're weightless, you don't need a bed, | 0:41:45 | 0:41:48 | |
you don't need a mattress, | 0:41:48 | 0:41:49 | |
you don't need a pillow. | 0:41:49 | 0:41:51 | |
Your body is floating completely suspended, like magic. | 0:41:51 | 0:41:55 | |
Movement becomes effortless. | 0:41:59 | 0:42:00 | |
You can push off with one finger and fly, and it's humble. | 0:42:00 | 0:42:05 | |
You don't need to hold yourself where you are with muscle. | 0:42:05 | 0:42:08 | |
You can just... With a delicate fingertip pressure, | 0:42:08 | 0:42:12 | |
you can stay where you are. | 0:42:12 | 0:42:14 | |
But there is a price to pay. | 0:42:14 | 0:42:17 | |
Astronauts' bones atrophy and their muscles wither away. | 0:42:17 | 0:42:21 | |
One of the things we do on board a space station is exercise, | 0:42:24 | 0:42:28 | |
purely to simulate gravity. | 0:42:28 | 0:42:30 | |
If we don't do something, then our heart will shrink, | 0:42:30 | 0:42:34 | |
our ability to pump blood to our head will diminish, | 0:42:34 | 0:42:37 | |
our bones will start to dissolve and our muscles will waste away. | 0:42:37 | 0:42:40 | |
'OK. Separation confirmed. Timer's on.' | 0:42:44 | 0:42:46 | |
'Backing away at a rate | 0:42:46 | 0:42:48 | |
'of just a little over one tenth of a metre per second.' | 0:42:48 | 0:42:52 | |
Re-entering gravity is a punishing experience. | 0:42:52 | 0:42:56 | |
To come back to Earth is violent. | 0:42:56 | 0:42:58 | |
It can be five times the force of gravity | 0:43:00 | 0:43:03 | |
or eight times the force of gravity, | 0:43:03 | 0:43:05 | |
crushing you down into the floor of the ship for quite a long time. | 0:43:05 | 0:43:10 | |
Then, of course, you hit the ground and tumble | 0:43:10 | 0:43:13 | |
and roll to a stop and now you are the victim of your past. | 0:43:13 | 0:43:18 | |
You're the victim of your decision-making, lying there, | 0:43:18 | 0:43:22 | |
trying to shake your head and get used to being in gravity again. | 0:43:22 | 0:43:26 | |
I remarked, at the time, that I had forgotten that my lips have weight | 0:43:26 | 0:43:31 | |
and my tongue has weight. | 0:43:31 | 0:43:32 | |
You don't think about it. But if you try and talk articulately, | 0:43:32 | 0:43:36 | |
standing on your head, you'll notice that you have to sort of control | 0:43:36 | 0:43:39 | |
your lips and your tongue a little differently, | 0:43:39 | 0:43:41 | |
just because gravity's pushing them the other way. | 0:43:41 | 0:43:43 | |
And it's the same sort of thing, | 0:43:43 | 0:43:45 | |
raising your arm, holding your head up, | 0:43:45 | 0:43:47 | |
turning your head when everything wants to tumble, | 0:43:47 | 0:43:50 | |
just keeping your balance, all of those things. | 0:43:50 | 0:43:54 | |
It's a little bit like relearning to walk again like an infant. | 0:43:54 | 0:43:59 | |
REPORTERS CLAMOUR | 0:43:59 | 0:44:01 | |
'Gravity on Earth grinds us all down. | 0:44:03 | 0:44:06 | |
'Over the course of the day, it actually squeezes your spine, | 0:44:08 | 0:44:12 | |
'an effect you can see for yourself if you use a measuring rod.' | 0:44:12 | 0:44:16 | |
OK, so it's 7:30 in the morning. | 0:44:16 | 0:44:18 | |
I've just got up and I'm going to see how tall I am | 0:44:18 | 0:44:21 | |
before gravity drags me down. | 0:44:21 | 0:44:24 | |
That's 178 centimetres | 0:44:32 | 0:44:34 | |
or just over 5'10. | 0:44:34 | 0:44:37 | |
Over the course of the day, gravity compresses the fluids in your spine. | 0:44:41 | 0:44:45 | |
Right, it is just past 11pm. | 0:44:48 | 0:44:51 | |
I've been standing up for most of the day | 0:44:51 | 0:44:53 | |
so let's see if gravity has had an effect on my height. | 0:44:53 | 0:44:57 | |
That's 176 centimetres, | 0:45:03 | 0:45:07 | |
so I really have shrunk by just over half an inch | 0:45:07 | 0:45:10 | |
over the course of today. | 0:45:10 | 0:45:13 | |
In the longer term, gravity can affect your posture permanently, | 0:45:17 | 0:45:21 | |
but there are exercises you can do to counteract this effect. | 0:45:21 | 0:45:26 | |
Part of my research has been looking at the effects of gravity | 0:45:26 | 0:45:29 | |
on the human body. So people might not be aware | 0:45:29 | 0:45:32 | |
or they might not always think about the effect of gravity | 0:45:32 | 0:45:35 | |
on our physical state, | 0:45:35 | 0:45:36 | |
on our health and, particularly, on our posture. | 0:45:36 | 0:45:39 | |
However, because it's such a constant force, | 0:45:39 | 0:45:42 | |
gravity has a massive impact over the course of our lifetime. | 0:45:42 | 0:45:45 | |
As you get older, you can develop a stoop, | 0:45:45 | 0:45:49 | |
which is damaging to your mobility. | 0:45:49 | 0:45:52 | |
Gokun here has actually got very good posture | 0:45:52 | 0:45:54 | |
but I'd like you to just show not so good posture. | 0:45:54 | 0:45:57 | |
So when... | 0:45:57 | 0:45:59 | |
Poor posture is really rounded shoulders | 0:45:59 | 0:46:02 | |
and then loss of the curve in the back, as well. | 0:46:02 | 0:46:05 | |
Can I just ask you to raise up your arms | 0:46:05 | 0:46:07 | |
-when you're in that posture? -I can't go any higher. | 0:46:07 | 0:46:10 | |
No, and then, just come back down, shoulders back, | 0:46:10 | 0:46:12 | |
and then raise your arms. | 0:46:12 | 0:46:15 | |
You can see the effect of posture on function. | 0:46:15 | 0:46:18 | |
Ironically, the exercises which many gym-goers do | 0:46:19 | 0:46:22 | |
actually make your posture worse. | 0:46:22 | 0:46:24 | |
That's if you only exercise the frontal muscles, | 0:46:24 | 0:46:28 | |
like the chest and abdominals. | 0:46:28 | 0:46:31 | |
So, it's recommended you exercise the back muscles just as much, | 0:46:31 | 0:46:35 | |
to straighten you out and counteract the effects of gravity. | 0:46:35 | 0:46:39 | |
Gravity shapes our bodies and moulds our planet. | 0:46:50 | 0:46:54 | |
Nothing happens on Earth without its power and influence. | 0:46:54 | 0:46:57 | |
Sir Isaac Newton explained so many of its effects | 0:46:59 | 0:47:03 | |
using one simple equation. | 0:47:03 | 0:47:05 | |
And, in the centuries that followed, | 0:47:06 | 0:47:08 | |
his laws of physics led to breakthrough after breakthrough, | 0:47:08 | 0:47:11 | |
spurring on the Industrial Revolution. | 0:47:11 | 0:47:14 | |
But in the first decade of the 20th century, | 0:47:15 | 0:47:18 | |
the next genius in our story | 0:47:18 | 0:47:20 | |
challenged the very foundations of our understanding of gravity. | 0:47:20 | 0:47:24 | |
A young German scientist called Albert Einstein | 0:47:25 | 0:47:28 | |
was churning something over in his mind. | 0:47:28 | 0:47:31 | |
He thought that something in Newton's laws didn't quite add up. | 0:47:33 | 0:47:37 | |
Imagine I'm the sun | 0:47:47 | 0:47:49 | |
and this tennis ball is the Earth in orbit around me. | 0:47:49 | 0:47:52 | |
Newton's laws can describe, very precisely, | 0:47:52 | 0:47:55 | |
the path the Earth takes around the sun | 0:47:55 | 0:47:57 | |
in terms of the mutual gravitational attraction between the two bodies. | 0:47:57 | 0:48:03 | |
But what Newton can't explain is what connects them. | 0:48:03 | 0:48:07 | |
In reality, of course, | 0:48:07 | 0:48:08 | |
there is no invisible string between the Earth and the sun, | 0:48:08 | 0:48:11 | |
holding the two together. | 0:48:11 | 0:48:13 | |
There's just empty space, a complete void. | 0:48:13 | 0:48:16 | |
And yet, according to Newton, | 0:48:16 | 0:48:18 | |
the Earth and sun pull on each other instantaneously | 0:48:18 | 0:48:21 | |
across a vast distance. | 0:48:21 | 0:48:23 | |
How can gravity act in this way | 0:48:23 | 0:48:25 | |
when there's nothing to connect it or transmit it? | 0:48:25 | 0:48:28 | |
After years puzzling over this, | 0:48:32 | 0:48:34 | |
Einstein had a blinding flash of inspiration. | 0:48:34 | 0:48:38 | |
Just like Galileo and his ramp... | 0:48:39 | 0:48:41 | |
..or Newton with his apple, | 0:48:42 | 0:48:44 | |
Einstein's breakthrough came | 0:48:44 | 0:48:46 | |
because he was thinking about one simple action... | 0:48:46 | 0:48:49 | |
..what happens when something falls. | 0:48:53 | 0:48:55 | |
To explain, I'm visiting | 0:49:00 | 0:49:02 | |
this 400-foot-high tower in Northampton... | 0:49:02 | 0:49:06 | |
built to safety-test lifts. | 0:49:06 | 0:49:08 | |
One day in 1907, | 0:49:13 | 0:49:15 | |
Einstein had what he called the "happiest thought of his life". | 0:49:15 | 0:49:18 | |
What if I were standing in a stationary lift, | 0:49:23 | 0:49:26 | |
completely isolated from the outside world, | 0:49:26 | 0:49:28 | |
not feeling anything apart from the pull of gravity on my feet? | 0:49:28 | 0:49:33 | |
What if, then, the lift cable breaks | 0:49:33 | 0:49:36 | |
and I start falling? | 0:49:36 | 0:49:38 | |
What are the forces that I will feel as I'm plummeting to the ground? | 0:49:38 | 0:49:42 | |
CRASHING | 0:49:48 | 0:49:50 | |
Well, I'm not going to try that. | 0:49:50 | 0:49:52 | |
Fortunately, there's another way to test this | 0:49:55 | 0:49:57 | |
without me having to plunge down a lift shaft. | 0:49:57 | 0:50:00 | |
Sorry to disappoint you! | 0:50:00 | 0:50:02 | |
This little device here that I have strapped to this plastic toy | 0:50:04 | 0:50:08 | |
is an industrial accelerometer. | 0:50:08 | 0:50:10 | |
So, it measures acceleration. | 0:50:10 | 0:50:12 | |
Now, I've got it connected to my laptop | 0:50:12 | 0:50:13 | |
and it's showing a measurement of 1G. | 0:50:13 | 0:50:16 | |
Now, that's the downward acceleration | 0:50:16 | 0:50:18 | |
due to the pull of Earth's gravity. | 0:50:18 | 0:50:21 | |
So, basically, it works just like a gravity meter. | 0:50:21 | 0:50:24 | |
But what happens if I were to drop it? | 0:50:24 | 0:50:27 | |
Presumably, it'll carry on measuring 1G | 0:50:27 | 0:50:29 | |
because it's falling in Earth's gravity. | 0:50:29 | 0:50:31 | |
OK, well, let's try that and see. | 0:50:31 | 0:50:33 | |
So, you can see here, along this line at the bottom, | 0:50:52 | 0:50:55 | |
that's when I was holding it still | 0:50:55 | 0:50:57 | |
and it's measuring an acceleration of 1G. | 0:50:57 | 0:51:00 | |
These oscillations here is when I stood up | 0:51:00 | 0:51:03 | |
and there's a bit of disturbance, | 0:51:03 | 0:51:05 | |
but this spike along here is the moment I released it. | 0:51:05 | 0:51:09 | |
And this short duration along here is the time it was falling. | 0:51:09 | 0:51:14 | |
And you see, while it was falling, | 0:51:14 | 0:51:16 | |
it was registering an acceleration of zero. | 0:51:16 | 0:51:20 | |
Now, if you think about it, this is really odd. | 0:51:20 | 0:51:23 | |
The accelerometer is accelerating downwards. | 0:51:23 | 0:51:26 | |
It's plummeting in the full grip of Earth's gravity | 0:51:26 | 0:51:29 | |
and yet it's measuring no acceleration at all. | 0:51:29 | 0:51:33 | |
It's as though gravity has completely disappeared. | 0:51:33 | 0:51:37 | |
Einstein's insight was that when something falls, | 0:51:39 | 0:51:43 | |
it no longer feels the pull of gravity. | 0:51:43 | 0:51:45 | |
In fact, falling is like floating in empty space. | 0:51:46 | 0:51:50 | |
This is the essence of Einstein's "happy thought" | 0:51:52 | 0:51:55 | |
and what we now call his "principle of equivalence". | 0:51:55 | 0:51:59 | |
Einstein's point is that, when the man in the lift falls, | 0:52:00 | 0:52:04 | |
he doesn't just feel weightless, he is weightless. | 0:52:04 | 0:52:09 | |
Einstein said the man feels no force pulling on him | 0:52:09 | 0:52:12 | |
because there is no force pulling on him. | 0:52:12 | 0:52:15 | |
Gravity doesn't act on him, | 0:52:15 | 0:52:17 | |
it acts on the space and time around him, | 0:52:17 | 0:52:20 | |
what we now call the "geometry of space-time". | 0:52:20 | 0:52:23 | |
This was a radical redefinition. | 0:52:30 | 0:52:33 | |
Einstein says to forget the idea of gravity as a force, | 0:52:33 | 0:52:37 | |
acting mysteriously between two objects. | 0:52:37 | 0:52:40 | |
Now we have to think of it as the shape of space-time changing. | 0:52:40 | 0:52:46 | |
You see, Newton saw space and time as independent, | 0:52:47 | 0:52:51 | |
fixed and immutable, | 0:52:51 | 0:52:53 | |
that three-dimensional space is the stage in which things happen, | 0:52:53 | 0:52:58 | |
but time is separate, | 0:52:58 | 0:52:59 | |
it ticks by at the same rate | 0:52:59 | 0:53:01 | |
everywhere in the universe. | 0:53:01 | 0:53:03 | |
According to Newton, an object would travel through space | 0:53:03 | 0:53:07 | |
in a straight line unless acted upon by a force like gravity | 0:53:07 | 0:53:10 | |
that would cause it to deviate from that path. | 0:53:10 | 0:53:14 | |
But Einstein said that space and time aren't fixed and immutable, | 0:53:14 | 0:53:18 | |
they're interconnected, meshed together | 0:53:18 | 0:53:21 | |
in what is known as space-time. | 0:53:21 | 0:53:24 | |
And he said that space-time can be warped - | 0:53:26 | 0:53:29 | |
that matter curves space and time around it. | 0:53:29 | 0:53:33 | |
So, after Einstein, we no longer see gravity | 0:53:39 | 0:53:42 | |
as an invisible string pulling objects together. | 0:53:42 | 0:53:46 | |
Instead, a body like the Earth | 0:53:48 | 0:53:50 | |
warps the structure of space and time around it. | 0:53:50 | 0:53:53 | |
And an object in orbit | 0:53:55 | 0:53:57 | |
follows a path which is as straight as possible | 0:53:57 | 0:54:00 | |
through that space-time. | 0:54:00 | 0:54:03 | |
It's a fundamental part of Einstein's vision of reality. | 0:54:03 | 0:54:08 | |
Space and time can't be disentangled. | 0:54:08 | 0:54:11 | |
You can't talk about space separately from time. | 0:54:11 | 0:54:15 | |
So, matter warps time as well as space. | 0:54:17 | 0:54:21 | |
It's known as "gravitational time dilation", | 0:54:23 | 0:54:27 | |
and it's possibly the strangest of all of Einstein's discoveries. | 0:54:27 | 0:54:31 | |
I've got two identical clocks here. | 0:54:34 | 0:54:36 | |
Now, because the clock lower down | 0:54:36 | 0:54:39 | |
is closer to the centre of the Earth, | 0:54:39 | 0:54:42 | |
it feels ever so slightly a stronger gravitational pull | 0:54:42 | 0:54:46 | |
than the clock higher up. | 0:54:46 | 0:54:47 | |
Einstein's theory says that the lower clock will tick by | 0:54:47 | 0:54:51 | |
at a slightly slower rate than the higher clock. | 0:54:51 | 0:54:55 | |
Basically, gravity slows time down. | 0:54:55 | 0:55:00 | |
It's an extraordinary conception of reality that Einstein describes. | 0:55:01 | 0:55:07 | |
Space is being curved and time is being distorted. | 0:55:08 | 0:55:13 | |
So, why can't we perceive this in our everyday lives? | 0:55:15 | 0:55:20 | |
Einstein had a rather nice way of explaining it. | 0:55:20 | 0:55:22 | |
Most of us have had the experience, as children, | 0:55:25 | 0:55:27 | |
of trying to work out what our parents do for a living. | 0:55:27 | 0:55:30 | |
Well, imagine your father is Albert Einstein. | 0:55:30 | 0:55:33 | |
When he was about 12 years old, | 0:55:33 | 0:55:34 | |
young Eduard Einstein asked his father why he was so famous, | 0:55:34 | 0:55:37 | |
what he'd discovered. Well, this put Einstein Sr on the spot, | 0:55:37 | 0:55:41 | |
but he came up with a beautifully simple analogy. | 0:55:41 | 0:55:44 | |
Einstein told his son, | 0:55:48 | 0:55:50 | |
"When a blind beetle crawls over the surface of a curved branch, | 0:55:50 | 0:55:54 | |
"it doesn't notice that the track it has covered is curved. | 0:55:54 | 0:55:58 | |
"I was lucky enough to notice what the beetle didn't notice." | 0:55:58 | 0:56:02 | |
This is what Einstein meant. | 0:56:04 | 0:56:06 | |
The beetle is free to move in any direction on the branch. | 0:56:06 | 0:56:09 | |
It can move forwards, backwards, left and right, | 0:56:09 | 0:56:12 | |
but it has no concept of a direction up off the branch. | 0:56:12 | 0:56:15 | |
It's as though, for the beetle, | 0:56:15 | 0:56:17 | |
the universe is missing the third dimension. | 0:56:17 | 0:56:20 | |
The beetle may think it's moving in a straight line along the branch, | 0:56:20 | 0:56:24 | |
but we can see that the surface it's walking on | 0:56:24 | 0:56:27 | |
is itself curving and twisted. | 0:56:27 | 0:56:29 | |
Einstein's point was that what we see as the twists and curves | 0:56:33 | 0:56:37 | |
of the branch feel, to the beetle, like forces pushing and pulling it. | 0:56:37 | 0:56:42 | |
OK, so, consider this rather strange example. | 0:56:45 | 0:56:47 | |
Imagine we have two beetles perched on this pumpkin and, | 0:56:47 | 0:56:51 | |
for whatever reason, they want to walk up towards the top. | 0:56:51 | 0:56:55 | |
Now, if they start at the equator, pointing due north, | 0:56:55 | 0:57:00 | |
as they walk, they will begin by moving parallel to each other. | 0:57:00 | 0:57:05 | |
That means their paths should never meet. | 0:57:05 | 0:57:08 | |
But, as they get closer to the top, their paths get closer together. | 0:57:08 | 0:57:13 | |
Now, if they're clever beetles, | 0:57:13 | 0:57:14 | |
they might try and figure out what's going on, | 0:57:14 | 0:57:17 | |
and they could imagine that there's some mysterious force | 0:57:17 | 0:57:19 | |
that's pulling them closer together. | 0:57:19 | 0:57:22 | |
But, for us, from our perspective, | 0:57:22 | 0:57:24 | |
we can see there is no such force. | 0:57:24 | 0:57:26 | |
All they're doing | 0:57:26 | 0:57:27 | |
is following straight paths over a curved surface. | 0:57:27 | 0:57:31 | |
Just as the beetles have no sense | 0:57:34 | 0:57:36 | |
that the surface of the branch is curved, | 0:57:36 | 0:57:39 | |
we completely fail to perceive | 0:57:39 | 0:57:42 | |
the bizarre ways that gravity | 0:57:42 | 0:57:45 | |
shapes the reality we live in. | 0:57:45 | 0:57:47 | |
Einstein's problem was proving that he was right. | 0:57:50 | 0:57:53 | |
After years more thought, he realised that there WAS a way... | 0:57:55 | 0:58:00 | |
by looking far out into the solar system. | 0:58:00 | 0:58:03 | |
Incredibly, here in the grounds of Herstmonceux Castle | 0:58:04 | 0:58:07 | |
is housed one of the original telescopes | 0:58:07 | 0:58:10 | |
that were used to prove Einstein was correct. | 0:58:10 | 0:58:14 | |
In 1915, when Einstein developed his general theory of relativity, | 0:58:17 | 0:58:21 | |
it was just that - it was a theory, it had no proof. | 0:58:21 | 0:58:24 | |
In fact, many people found it completely outlandish. | 0:58:24 | 0:58:27 | |
But then, just four years later, | 0:58:27 | 0:58:30 | |
in 1919, this telescope, and allow me to geek out a bit here | 0:58:30 | 0:58:33 | |
and I'll give it its correct name, | 0:58:33 | 0:58:35 | |
this is the 13-inch astrographic refractor, | 0:58:35 | 0:58:39 | |
this telescope proved that Einstein was, in fact, right. | 0:58:39 | 0:58:43 | |
That gravity does curve space itself. | 0:58:43 | 0:58:47 | |
Marek Kukula is the public astronomer | 0:58:53 | 0:58:56 | |
at the Royal Observatory in London, | 0:58:56 | 0:58:58 | |
and he's recently rediscovered | 0:58:58 | 0:59:00 | |
a neglected treasure in their archives. | 0:59:00 | 0:59:04 | |
This is, perhaps, one of the most important | 0:59:04 | 0:59:06 | |
scientific artefacts we have in the collection here in Greenwich | 0:59:06 | 0:59:10 | |
and, for an astrophysicist like me, | 0:59:10 | 0:59:12 | |
it's almost a holy relic. | 0:59:12 | 0:59:14 | |
It's a glass plate photo of a solar eclipse taken in 1919 | 0:59:15 | 0:59:20 | |
as part of a famous scientific expedition. | 0:59:20 | 0:59:23 | |
British astronomers had travelled all the way to Brazil | 0:59:26 | 0:59:28 | |
and the West Coast of Africa | 0:59:28 | 0:59:30 | |
to take photographs which they hoped would prove Einstein right. | 0:59:30 | 0:59:34 | |
What we're seeing here is the eclipse of 1919. | 0:59:35 | 0:59:38 | |
You can see the black disc of the moon silhouetted against the sun, | 0:59:38 | 0:59:42 | |
blocking its light. Around it is the solar corona, | 0:59:42 | 0:59:45 | |
the sun's outer atmosphere, | 0:59:45 | 0:59:47 | |
and this spectacular prominence of gas leaping off the surface. | 0:59:47 | 0:59:51 | |
But it's not the sun that we're really interested in. | 0:59:51 | 0:59:54 | |
The fundamental point that this photo | 0:59:54 | 0:59:56 | |
and others from the expedition show | 0:59:56 | 0:59:58 | |
is that the positions, the apparent positions, | 0:59:58 | 1:00:01 | |
of the stars in the sky are altered and shifted | 1:00:01 | 1:00:04 | |
from where we would expect them normally to be, | 1:00:04 | 1:00:07 | |
and that proves this very strange thing | 1:00:07 | 1:00:10 | |
that general relativity predicts - | 1:00:10 | 1:00:12 | |
that the mass of the sun | 1:00:12 | 1:00:14 | |
bends the space and time around it, | 1:00:14 | 1:00:16 | |
and that distortion is gravity. | 1:00:16 | 1:00:19 | |
This is a negative of one of the photos. | 1:00:22 | 1:00:25 | |
It has markings showing where the stars' positions | 1:00:25 | 1:00:28 | |
seem to have shifted. | 1:00:28 | 1:00:29 | |
Since then, observation after observation | 1:00:31 | 1:00:34 | |
have confirmed that matter curves space | 1:00:34 | 1:00:37 | |
and slows down time. | 1:00:37 | 1:00:39 | |
So, the simple question of why things fall the way they do | 1:00:42 | 1:00:46 | |
has led us deeper and deeper | 1:00:46 | 1:00:47 | |
into the very nature of space and time itself. | 1:00:47 | 1:00:50 | |
Gravitational science shows us how galaxies, stars and planets form. | 1:00:52 | 1:00:58 | |
By measuring gravity, we've discovered the existence | 1:00:58 | 1:01:01 | |
of dark matter, that 80% of the mass of our universe is invisible | 1:01:01 | 1:01:06 | |
and we don't know what it's made of. | 1:01:06 | 1:01:10 | |
And we've detected exotic objects with extreme gravity... | 1:01:10 | 1:01:14 | |
..like neutron stars, | 1:01:15 | 1:01:17 | |
which have more mass than our sun | 1:01:17 | 1:01:19 | |
yet are only 20 kilometres across. | 1:01:19 | 1:01:22 | |
But it's another mysterious aspect of Einstein's universe | 1:01:25 | 1:01:28 | |
that I want to explore in my next gravity project. | 1:01:28 | 1:01:31 | |
Here at the University of Surrey, | 1:01:34 | 1:01:36 | |
some colleagues and I have been working on it for months. | 1:01:36 | 1:01:39 | |
What we're doing is devising a nationwide citizen science project. | 1:01:40 | 1:01:45 | |
We're developing a smartphone app | 1:01:45 | 1:01:47 | |
that uses the GPS contained on your phone | 1:01:47 | 1:01:50 | |
to explore one of the strangest properties of gravity - | 1:01:50 | 1:01:53 | |
how it affects the rate at which we age. | 1:01:53 | 1:01:56 | |
'I formulated the equations myself... | 1:01:58 | 1:02:01 | |
'..and a small team of computer scientists and software developers | 1:02:02 | 1:02:06 | |
'is using them to devise the app.' | 1:02:06 | 1:02:08 | |
Einstein discovered that, as gravity changes, | 1:02:12 | 1:02:15 | |
so does the rate that time ticks. | 1:02:15 | 1:02:18 | |
This means the strength of gravity you feel | 1:02:20 | 1:02:23 | |
affects how quickly or slowly you age. | 1:02:23 | 1:02:26 | |
The aim of my app is to demonstrate this effect. | 1:02:29 | 1:02:32 | |
It works by using a phone's GPS data | 1:02:32 | 1:02:35 | |
to estimate your local gravity. | 1:02:35 | 1:02:38 | |
And it also calculates the average speed at which you move | 1:02:40 | 1:02:44 | |
because this, too, affects the rate at which you age. | 1:02:44 | 1:02:47 | |
It then uses the equations I've written, | 1:02:50 | 1:02:52 | |
which are based on Einstein's theory of relativity, | 1:02:52 | 1:02:55 | |
to calculate, overall, how fast or slowly you're ageing. | 1:02:55 | 1:03:00 | |
Once the app is ready, I tweet about it. | 1:03:03 | 1:03:05 | |
Thousands of people download it | 1:03:08 | 1:03:10 | |
and we start to gather results from across the country. | 1:03:10 | 1:03:13 | |
Some people send me videos, giving me their results, | 1:03:15 | 1:03:19 | |
how fast they are ageing | 1:03:19 | 1:03:21 | |
compared with how time ticks out in space in zero gravity. | 1:03:21 | 1:03:26 | |
Over the past day, I have aged less by about 172 microseconds. | 1:03:26 | 1:03:31 | |
I have aged less by 10.02 milliseconds. | 1:03:31 | 1:03:37 | |
So, since downloading the app, I have aged less by 1.14 milliseconds. | 1:03:37 | 1:03:43 | |
Since opening Time Warper, | 1:03:43 | 1:03:46 | |
I have aged less by 2.6 milliseconds. | 1:03:46 | 1:03:50 | |
Our aim is to use their results | 1:03:51 | 1:03:53 | |
to build up a map of how time flows | 1:03:53 | 1:03:56 | |
because of gravity. | 1:03:56 | 1:03:57 | |
My smartphone project provides just one insight into the space and time | 1:03:59 | 1:04:04 | |
which Einstein's theories describe. | 1:04:04 | 1:04:07 | |
Gravity and its strange ways | 1:04:22 | 1:04:24 | |
have given us astonishing insights | 1:04:24 | 1:04:26 | |
into the dark secrets of our universe. | 1:04:26 | 1:04:28 | |
Perhaps the weirdest objects in the universe are black holes, | 1:04:30 | 1:04:34 | |
collapsed stars whose gravity is so strong | 1:04:34 | 1:04:37 | |
that not even light can escape their grip. | 1:04:37 | 1:04:40 | |
Now, for the first time ever, their effects have been felt on Earth | 1:04:42 | 1:04:45 | |
and they've been detected through the medium of gravity itself. | 1:04:45 | 1:04:50 | |
It's a story that has revolutionised the study of modern cosmology. | 1:04:52 | 1:04:56 | |
1.3 billion years ago, | 1:05:00 | 1:05:02 | |
in a galaxy far, far away, | 1:05:02 | 1:05:04 | |
two black holes swirled around each other, | 1:05:04 | 1:05:08 | |
drew closer and closer together, | 1:05:08 | 1:05:10 | |
until they finally collided with incredible violence. | 1:05:10 | 1:05:14 | |
In that final fraction of a second, | 1:05:14 | 1:05:16 | |
at the precise moment that they merged, | 1:05:16 | 1:05:19 | |
a disturbance was created | 1:05:19 | 1:05:20 | |
that sent ripples out through the universe. | 1:05:20 | 1:05:23 | |
Gravitational waves are a key prediction of Einstein's theory. | 1:05:26 | 1:05:30 | |
Matter doesn't just curve space time, it can cause waves, | 1:05:32 | 1:05:37 | |
ripples which expand outwards, | 1:05:37 | 1:05:39 | |
exactly like a stone dropped in water. | 1:05:39 | 1:05:41 | |
This particular wave was unimaginably large. | 1:05:44 | 1:05:47 | |
The energy released was greater than all the light being given out | 1:05:48 | 1:05:53 | |
by all the stars in the universe. | 1:05:53 | 1:05:55 | |
The wave rippled through space at the speed of light. | 1:05:57 | 1:06:00 | |
In 1.3 billion years, | 1:06:00 | 1:06:03 | |
it covered a distance of over 10 billion trillion kilometres. | 1:06:03 | 1:06:07 | |
Until, on the morning of the 14th of September, 2015, | 1:06:17 | 1:06:22 | |
it arrived here. | 1:06:22 | 1:06:23 | |
The streets and cafes of New Orleans. | 1:06:25 | 1:06:28 | |
In fact, everything in America - and on Earth - | 1:06:28 | 1:06:33 | |
expanded and contracted very, very slightly | 1:06:33 | 1:06:36 | |
as the wave passed through. | 1:06:36 | 1:06:38 | |
No-one noticed as, by the time it arrived here, | 1:06:40 | 1:06:43 | |
the distortion was phenomenally tiny. | 1:06:43 | 1:06:45 | |
Except that one science laboratory did notice... | 1:06:50 | 1:06:53 | |
..and I'm going to see it. | 1:06:55 | 1:06:57 | |
1,000 scientists across the world are collaborating on it. | 1:07:01 | 1:07:05 | |
It's the culmination of over 50 years of effort | 1:07:08 | 1:07:11 | |
and is one of the most sophisticated experiments | 1:07:11 | 1:07:15 | |
ever devised by humanity. | 1:07:15 | 1:07:17 | |
So, I'm pretty excited to see it. | 1:07:19 | 1:07:21 | |
It's a rather unusual setting. | 1:07:23 | 1:07:25 | |
Here I am, in the middle of rural Louisiana, | 1:07:25 | 1:07:27 | |
about an hour's drive outside New Orleans. | 1:07:27 | 1:07:30 | |
I don't expect to find such a multi-million dollar, | 1:07:30 | 1:07:33 | |
cutting-edge research facility as this, | 1:07:33 | 1:07:36 | |
and yet, this is the place where, recently, | 1:07:36 | 1:07:39 | |
one of the most important scientific discoveries | 1:07:39 | 1:07:41 | |
in human history was made. This is LIGO. | 1:07:41 | 1:07:44 | |
The Laser Interferometer Gravitational Wave Observatory | 1:07:48 | 1:07:52 | |
is an enormous construction shaped like an L... | 1:07:52 | 1:07:56 | |
..with a sophisticated laser system | 1:07:57 | 1:07:59 | |
bouncing up and down the two arms. | 1:07:59 | 1:08:01 | |
So, we're standing on top of one of LIGO's two arms. | 1:08:03 | 1:08:06 | |
This is the first LIGO arm. | 1:08:06 | 1:08:08 | |
And in that tube, there's a laser beam that we bounce back and forth | 1:08:08 | 1:08:12 | |
between a mirror and the end station and a mirror in this building. | 1:08:12 | 1:08:15 | |
And the other bit goes that way four kilometres, | 1:08:15 | 1:08:17 | |
perpendicular to the arm we first saw. | 1:08:17 | 1:08:19 | |
-So, this is the L shape? -It's a big L on the ground. | 1:08:19 | 1:08:21 | |
So, the light bounces back and forth | 1:08:21 | 1:08:23 | |
in that arm and bounces back and forth in this arm, | 1:08:23 | 1:08:26 | |
and what we actually measure with LIGO is the length of this arm | 1:08:26 | 1:08:29 | |
as measured by the light between the two mirrors, | 1:08:29 | 1:08:32 | |
and the length of that arm as measured by the light | 1:08:32 | 1:08:35 | |
between two mirrors. And then the laser interferometer | 1:08:35 | 1:08:37 | |
measures the difference between those two arm lengths. | 1:08:37 | 1:08:40 | |
So, as the gravitational wave passed through, the lasers picked it up. | 1:08:42 | 1:08:47 | |
They detected that LIGO's two arms changed in length | 1:08:47 | 1:08:51 | |
to a very, very tiny degree. | 1:08:51 | 1:08:53 | |
The signal that we saw | 1:08:56 | 1:08:58 | |
was just a few thousandth of the size of the atomic nucleus. | 1:08:58 | 1:09:02 | |
It's the biggest the signal ever got. | 1:09:02 | 1:09:04 | |
So far, far smaller than the size of a single atom? | 1:09:04 | 1:09:08 | |
Oh, much, much smaller, yeah. | 1:09:08 | 1:09:10 | |
And you need something this huge to pick that up? | 1:09:10 | 1:09:13 | |
That's right. This is one of the biggest sources of energy | 1:09:13 | 1:09:17 | |
in the universe, one of the biggest events you'd ever measure, | 1:09:17 | 1:09:20 | |
and we just barely saw it. | 1:09:20 | 1:09:22 | |
The LIGO scientists turned the gravitational waves | 1:09:26 | 1:09:30 | |
into sound waves, | 1:09:30 | 1:09:31 | |
so what you're about to hear is, in a very real sense, | 1:09:31 | 1:09:36 | |
the sound of two black holes colliding. | 1:09:36 | 1:09:39 | |
RHYTHMIC PULSES | 1:09:39 | 1:09:42 | |
It was the first observation of any kind | 1:09:46 | 1:09:49 | |
of pairs of stellar mass black holes. | 1:09:49 | 1:09:51 | |
"Stellar mass" means, you know, | 1:09:51 | 1:09:53 | |
several or a bunch of suns in weight. | 1:09:53 | 1:09:57 | |
And so we learned that they exist, | 1:09:57 | 1:09:59 | |
we learned that there are enough of them that, occasionally, | 1:09:59 | 1:10:02 | |
they run into each other and coalesce. | 1:10:02 | 1:10:04 | |
And... | 1:10:04 | 1:10:06 | |
we also learned, by comparing the waveform we observed | 1:10:06 | 1:10:09 | |
with the general relativity calculations, | 1:10:09 | 1:10:12 | |
that general relativity is, as far as we know, dead-on right. | 1:10:12 | 1:10:16 | |
The long concrete bunker to my left houses the beam line, | 1:10:26 | 1:10:30 | |
one of the LIGO's laser arms. | 1:10:30 | 1:10:33 | |
The detail and the effort that's gone into isolating the beam | 1:10:34 | 1:10:39 | |
from the outside environment | 1:10:39 | 1:10:40 | |
reminds me very much of Cavendish's famous experiment. | 1:10:40 | 1:10:44 | |
He, too, had to worry about isolating his experiment | 1:10:44 | 1:10:47 | |
from external disturbances. | 1:10:47 | 1:10:49 | |
Only, of course, LIGO takes things to a far, far greater degree. | 1:10:49 | 1:10:53 | |
Inside the arm is one of the largest and purest vacuums in the world. | 1:10:54 | 1:10:59 | |
Atmospheric pressure in there | 1:11:00 | 1:11:02 | |
has been reduced to one trillionth of the pressure outside. | 1:11:02 | 1:11:06 | |
The mirrors inside are so reflective | 1:11:06 | 1:11:09 | |
that they only absorb one in three million photons. | 1:11:09 | 1:11:14 | |
And at the end of my little trip, lies a British success story. | 1:11:14 | 1:11:19 | |
Well, I made it all the way to the end of one of the LIGO arms. | 1:11:25 | 1:11:29 | |
To be honest, it took me a bit longer than I thought, | 1:11:29 | 1:11:31 | |
especially in that thing, | 1:11:31 | 1:11:33 | |
but housed inside this building is one of the reflecting mirrors | 1:11:33 | 1:11:37 | |
that bounces the laser beam | 1:11:37 | 1:11:38 | |
all the way back down the four kilometre arm | 1:11:38 | 1:11:41 | |
to the main control centre. | 1:11:41 | 1:11:43 | |
And the technology that went into developing these mirrors | 1:11:43 | 1:11:46 | |
is quite remarkable. | 1:11:46 | 1:11:47 | |
It was developed in the UK at the University of Glasgow. | 1:11:47 | 1:11:51 | |
This is what the mirror looks like. | 1:11:58 | 1:12:00 | |
Its surface is extraordinarily smooth, | 1:12:01 | 1:12:04 | |
no bump bigger than a few billionths of a metre high. | 1:12:04 | 1:12:08 | |
Equally amazing are these... | 1:12:10 | 1:12:12 | |
..fused silica fibres, a few times the thickness of a human hair... | 1:12:13 | 1:12:18 | |
..designed by the University of Glasgow | 1:12:20 | 1:12:22 | |
in conjunction with scientists from other British universities. | 1:12:22 | 1:12:26 | |
They isolate the mirror completely | 1:12:27 | 1:12:30 | |
so it hangs perfectly still. | 1:12:30 | 1:12:33 | |
You could say that in there | 1:12:33 | 1:12:35 | |
is the quietest place on Earth. | 1:12:35 | 1:12:38 | |
Despite this, outside events do sometimes interfere | 1:12:39 | 1:12:42 | |
with the work here, as I witnessed for myself. | 1:12:42 | 1:12:45 | |
I've wandered into the control room here at LIGO because I'm told | 1:12:46 | 1:12:50 | |
something kicked off a few hours ago and they're all very busy. | 1:12:50 | 1:12:54 | |
The image that's flickering up there | 1:12:54 | 1:12:57 | |
is not meant to be like that. | 1:12:57 | 1:12:59 | |
Essentially, what they picked up | 1:12:59 | 1:13:01 | |
is a seismic disturbance, an earthquake. | 1:13:01 | 1:13:03 | |
Now, that's not an earthquake down the road. | 1:13:03 | 1:13:06 | |
It started on the other side of the planet, in Japan. | 1:13:06 | 1:13:10 | |
So, it just gives us a sense | 1:13:10 | 1:13:12 | |
of the tremendous challenges faced by LIGO | 1:13:12 | 1:13:14 | |
and the team here and the level of sensitivity needed | 1:13:14 | 1:13:18 | |
that an earthquake on the other side of the Earth | 1:13:18 | 1:13:21 | |
can disrupt their measurements and they have | 1:13:21 | 1:13:24 | |
to reset everything all over again. | 1:13:24 | 1:13:26 | |
One of the scientists involved in developing this extraordinary place | 1:13:29 | 1:13:33 | |
put it quite succinctly. | 1:13:33 | 1:13:35 | |
"Once we were blind, but now we can see." | 1:13:35 | 1:13:39 | |
Throughout the entire history of astronomy, | 1:13:41 | 1:13:43 | |
we've studied gravity and how it affects matter in the universe | 1:13:43 | 1:13:47 | |
and how it warps space-time, | 1:13:47 | 1:13:50 | |
but only by looking at the light that enters our telescopes, | 1:13:50 | 1:13:54 | |
now, for the first time, | 1:13:54 | 1:13:56 | |
we can study the universe in a different way. | 1:13:56 | 1:13:59 | |
The discovery of gravitational waves means we can see objects | 1:13:59 | 1:14:02 | |
that cause extreme warping of space-time | 1:14:02 | 1:14:05 | |
and its effect on gravity directly. | 1:14:05 | 1:14:08 | |
This essentially opens up a new era in astronomy, | 1:14:08 | 1:14:12 | |
it gives us a new way of looking out at the universe. | 1:14:12 | 1:14:15 | |
Professor Sheila Rowan was one of the scientists | 1:14:18 | 1:14:21 | |
who spearheaded the British effort for LIGO. | 1:14:21 | 1:14:24 | |
For her and her colleagues, | 1:14:24 | 1:14:27 | |
gravitational wave detection is just in its infancy. | 1:14:27 | 1:14:30 | |
New instruments - even more sensitive than LIGO - | 1:14:32 | 1:14:34 | |
are now being developed. | 1:14:34 | 1:14:36 | |
There's so much that we don't understand | 1:14:38 | 1:14:40 | |
about the universe that we live in, | 1:14:40 | 1:14:42 | |
and this has suddenly given us a new tool, a new way, | 1:14:42 | 1:14:46 | |
to probe the dark processes in the universe, | 1:14:46 | 1:14:49 | |
because every time we make the observatories more sensitive, | 1:14:49 | 1:14:54 | |
we can sense gravitational wave signals from further away, | 1:14:54 | 1:14:59 | |
from further out in the universe, from further back in cosmic history. | 1:14:59 | 1:15:03 | |
Things like supermassive black holes spiralling in to collide, | 1:15:03 | 1:15:07 | |
small black holes orbiting round supermassive black holes, | 1:15:07 | 1:15:11 | |
tracing out the dents in space-time of those supermassive objects. | 1:15:11 | 1:15:16 | |
A long-term goal is to probe back further | 1:15:16 | 1:15:20 | |
towards what we think of as the Big Bang, | 1:15:20 | 1:15:22 | |
the earliest moments that we understand | 1:15:22 | 1:15:25 | |
of the universe as we know it. | 1:15:25 | 1:15:28 | |
If you think about it, time and time again in the history of science, | 1:15:41 | 1:15:45 | |
unlocking the mysteries of gravity | 1:15:45 | 1:15:47 | |
have led to a deeper understanding of the universe. | 1:15:47 | 1:15:51 | |
Galileo and his ramp, Newton and his apple, | 1:15:51 | 1:15:54 | |
Einstein and the falling man in the lift. | 1:15:54 | 1:15:56 | |
Each of these characters challenged the scientific consensus of the day. | 1:15:56 | 1:16:02 | |
And even today, understanding the true nature of gravity | 1:16:02 | 1:16:06 | |
remains one of the biggest challenges in science. | 1:16:06 | 1:16:09 | |
Which brings me back to the smartphone app. | 1:16:12 | 1:16:15 | |
And it's at this point that our story, for me, at least, | 1:16:15 | 1:16:19 | |
takes a completely unexpected turn. | 1:16:19 | 1:16:21 | |
Unfortunately, it's all gone a bit pear-shaped. | 1:16:23 | 1:16:27 | |
OK, so, here's what's happened. A couple of months ago, | 1:16:27 | 1:16:31 | |
we launched the app and it was all going really well. | 1:16:31 | 1:16:34 | |
Thousands of people downloaded it | 1:16:34 | 1:16:35 | |
and have been sending us their results. | 1:16:35 | 1:16:38 | |
We've been collecting the data to create this nationwide map | 1:16:38 | 1:16:43 | |
to show how time flows at different rates for different people | 1:16:43 | 1:16:46 | |
around the country. | 1:16:46 | 1:16:48 | |
Unfortunately, I've just realised there's a big problem. | 1:16:48 | 1:16:52 | |
You see, I was going over the scientific literature | 1:16:57 | 1:16:59 | |
and I came across this subtle point about relativity | 1:16:59 | 1:17:03 | |
which basically made me sit bolt upright. | 1:17:03 | 1:17:06 | |
There was this horrible dawning realisation | 1:17:06 | 1:17:09 | |
that I'd made a mistake in the equations that get fed into the app. | 1:17:09 | 1:17:13 | |
What this means is all the results we've been gathering are wrong. | 1:17:15 | 1:17:20 | |
The issue lies in the strange and subtle effects | 1:17:24 | 1:17:27 | |
of Einstein's theories of relativity, | 1:17:27 | 1:17:30 | |
and it's fundamental to the way time flows | 1:17:30 | 1:17:33 | |
across the surface of the globe. | 1:17:33 | 1:17:37 | |
Now, what if I use my smartphone app where I live here, | 1:17:37 | 1:17:40 | |
on the south coast of England | 1:17:40 | 1:17:42 | |
and then go and spend a few days down near the equator? | 1:17:42 | 1:17:45 | |
So, here on the West Coast of Africa. | 1:17:45 | 1:17:48 | |
Now, we know from the road trip that gravity is weaker by the equator. | 1:17:51 | 1:17:55 | |
So, that means time ticks faster there. | 1:17:57 | 1:18:00 | |
But there's another important factor we have to take into account - | 1:18:01 | 1:18:05 | |
movement. | 1:18:05 | 1:18:07 | |
You see, when I'm here, near the equator, | 1:18:07 | 1:18:09 | |
I'm moving more quickly | 1:18:09 | 1:18:11 | |
than I was back in Britain because of the rotation of the Earth. | 1:18:11 | 1:18:15 | |
Einstein says movement slows down time | 1:18:15 | 1:18:18 | |
so clocks will tick slower at the equator. | 1:18:18 | 1:18:21 | |
This is where the error crept in. | 1:18:22 | 1:18:24 | |
You see, I had taken into account these two effects, | 1:18:24 | 1:18:27 | |
but I'd missed a crucial point. | 1:18:27 | 1:18:29 | |
They cancel each other out exactly. | 1:18:29 | 1:18:32 | |
In fact, the Earth bulges out | 1:18:32 | 1:18:34 | |
exactly the right amount for its rotational speed | 1:18:34 | 1:18:39 | |
to make sure they cancel out, | 1:18:39 | 1:18:41 | |
so all clocks on the surface of the Earth, at sea level, tick | 1:18:41 | 1:18:45 | |
at exactly the same rate. | 1:18:45 | 1:18:49 | |
So, now I'm having to go right back to square one | 1:18:49 | 1:18:52 | |
and completely rewrite the equations for the app. | 1:18:52 | 1:18:55 | |
And, to test if it's working, | 1:19:01 | 1:19:03 | |
I'm going to use it over the course of a normal working week. | 1:19:03 | 1:19:06 | |
This is where I live, this is Portsmouth, | 1:19:08 | 1:19:10 | |
which means I'm very close to sea level, | 1:19:10 | 1:19:13 | |
and this is how I start most mornings, | 1:19:13 | 1:19:15 | |
catching the train to work. | 1:19:15 | 1:19:18 | |
The app records my speed as I'm on the train | 1:19:18 | 1:19:23 | |
and calculates how this slows down my personal clock. | 1:19:23 | 1:19:27 | |
I think the train journey | 1:19:27 | 1:19:29 | |
should have slowed my time down by a tiny... | 1:19:29 | 1:19:33 | |
A few trillionths of second. | 1:19:33 | 1:19:35 | |
I'm heading for the BBC's headquarters in Central London, | 1:19:35 | 1:19:39 | |
and gravity should be a bit weaker here. | 1:19:39 | 1:19:42 | |
I'm a few metres above sea level, I guess, here. | 1:19:42 | 1:19:44 | |
And so there will be a speed-up of my time because of altitude. | 1:19:44 | 1:19:48 | |
The app compares the way my time flows | 1:19:48 | 1:19:51 | |
with a stationary clock at sea level. | 1:19:51 | 1:19:54 | |
So, what's my result? | 1:19:54 | 1:19:56 | |
On an average day, my movement makes me age slower by a third | 1:19:56 | 1:20:01 | |
of a nanosecond. That's a third of a billionth of a second. | 1:20:01 | 1:20:06 | |
But the weaker gravity I'm in | 1:20:06 | 1:20:08 | |
means I age faster - overall, | 1:20:08 | 1:20:11 | |
half a nanosecond faster. | 1:20:11 | 1:20:13 | |
I've also given the app to some other volunteers | 1:20:15 | 1:20:18 | |
to compare how they age over an average day. | 1:20:18 | 1:20:20 | |
Nick flies cargo planes. | 1:20:22 | 1:20:25 | |
He flies from Chicago to Germany. | 1:20:25 | 1:20:28 | |
Tomorrow morning, | 1:20:34 | 1:20:36 | |
we have to leave to go first to Milan and then on to Tokyo. | 1:20:36 | 1:20:41 | |
His travel slows down his ageing, | 1:20:41 | 1:20:45 | |
but much weaker gravity at high altitude | 1:20:45 | 1:20:48 | |
speeds his clock up by just a bit more. | 1:20:48 | 1:20:52 | |
Overall, he's ageing five nanoseconds faster | 1:20:52 | 1:20:55 | |
than a stationary clock at sea level. | 1:20:55 | 1:20:58 | |
Vanessa runs a pub in the Yorkshire Dales. | 1:20:58 | 1:21:01 | |
I'm going to take you outside to see the weather conditions here. | 1:21:01 | 1:21:05 | |
So, here we are, outside the Tan Hill Inn. | 1:21:05 | 1:21:07 | |
We live right in the middle of the National Park on the moor. | 1:21:07 | 1:21:10 | |
The Tan Hill Inn is famous as Britain's highest altitude pub | 1:21:10 | 1:21:15 | |
at over 500 metres above sea level. | 1:21:15 | 1:21:18 | |
We don't have any neighbours, we just have sheep. | 1:21:18 | 1:21:21 | |
Her altitude means she ages faster every day | 1:21:21 | 1:21:24 | |
by around four nanoseconds | 1:21:24 | 1:21:27 | |
compared to someone at sea level. | 1:21:27 | 1:21:29 | |
There's Kevin, a mountaineer in the Highlands. | 1:21:30 | 1:21:33 | |
I'm on a mountain in Glencoe called Sgor na h-Ulaidh. | 1:21:33 | 1:21:36 | |
I've been at an altitude generally of between 2,000-3,000 feet | 1:21:36 | 1:21:39 | |
for a lot of the day. Throughout the day, | 1:21:39 | 1:21:41 | |
I've just been logging on to the phone, logging on to the app, | 1:21:41 | 1:21:44 | |
and just checking it out and having a look, | 1:21:44 | 1:21:46 | |
and I've been watching it get bigger | 1:21:46 | 1:21:48 | |
and watching the value get bigger and bigger. | 1:21:48 | 1:21:50 | |
So, it's been quite a lot of fun. | 1:21:50 | 1:21:52 | |
On an average day of climbing, | 1:21:53 | 1:21:55 | |
Kevin's personal clock goes faster by one nanosecond. | 1:21:55 | 1:21:59 | |
Gary works for a Scottish water retailer. | 1:22:02 | 1:22:04 | |
My job takes me all over the UK, | 1:22:05 | 1:22:08 | |
dealing with energy consultants and energy brokers, | 1:22:08 | 1:22:11 | |
as far up north as Inverness, as far down south as London. | 1:22:11 | 1:22:14 | |
I approximately do about 1,000 miles a week, sometimes more, | 1:22:14 | 1:22:17 | |
depending on the number of meetings I have. | 1:22:17 | 1:22:21 | |
Gary's car journeys do slow his time down a bit, | 1:22:21 | 1:22:24 | |
but being above sea level | 1:22:24 | 1:22:26 | |
means he still ages faster by three quarters of a nanosecond. | 1:22:26 | 1:22:30 | |
Our final volunteer is Walter. | 1:22:32 | 1:22:34 | |
He lives close to sea level at the iconic John O'Groats. | 1:22:34 | 1:22:38 | |
I run the tourism business and I started about 50 years ago, | 1:22:39 | 1:22:43 | |
so when people come here, they can actually speak to someone | 1:22:43 | 1:22:47 | |
who's been born in John O'Groats and, if they ask questions, | 1:22:47 | 1:22:50 | |
I can tell them all sorts of useless information | 1:22:50 | 1:22:52 | |
because I'm full of useless information. | 1:22:52 | 1:22:55 | |
So our final results show that, if you want to age more slowly, | 1:22:55 | 1:23:00 | |
try to live near sea level, like Walter. | 1:23:00 | 1:23:03 | |
Or there is another way to do it - | 1:23:05 | 1:23:08 | |
get a job on the International Space Station. | 1:23:08 | 1:23:11 | |
Its 17,000-mile-an-hour orbit will give you a boost. | 1:23:11 | 1:23:16 | |
We did the maths for the astronauts. | 1:23:18 | 1:23:20 | |
Every month, you are about one millisecond younger, | 1:23:20 | 1:23:25 | |
so one thousandth of a second. | 1:23:25 | 1:23:27 | |
So, after six months, | 1:23:27 | 1:23:29 | |
you're that much younger than people on Earth. | 1:23:29 | 1:23:32 | |
So, I'm younger than I should be. | 1:23:32 | 1:23:34 | |
I hope I look it. | 1:23:34 | 1:23:35 | |
Of course, for us on Earth, | 1:23:37 | 1:23:39 | |
time dilation is so utterly minuscule, | 1:23:39 | 1:23:42 | |
a few billionths of a second between us, | 1:23:42 | 1:23:45 | |
you might think it's too frivolous to even bother about. | 1:23:45 | 1:23:48 | |
And yet, in the long and difficult process of designing the app, | 1:23:51 | 1:23:55 | |
I've come to an extraordinary conclusion. | 1:23:55 | 1:23:59 | |
The different ways that time flows | 1:23:59 | 1:24:01 | |
may not be some quirky by-product of gravity. | 1:24:01 | 1:24:06 | |
It may actually BE gravity. | 1:24:06 | 1:24:09 | |
It may be the CAUSE of gravity... | 1:24:09 | 1:24:12 | |
the reason why objects fall. | 1:24:12 | 1:24:14 | |
One of the colleagues I've been consulting is Kip Thorne. | 1:24:17 | 1:24:20 | |
He's one of the world's leading theoretical physicists | 1:24:20 | 1:24:23 | |
and a driving force behind the creation of LIGO. | 1:24:23 | 1:24:26 | |
While I was going back over some of the basic physics behind the app, | 1:24:26 | 1:24:30 | |
I came across an intriguing idea of his. | 1:24:30 | 1:24:33 | |
It's a very interesting and different way | 1:24:33 | 1:24:36 | |
of describing gravity. | 1:24:36 | 1:24:37 | |
This is what Kip says. | 1:24:41 | 1:24:42 | |
"Everything likes to live where it'll age the most slowly, | 1:24:43 | 1:24:48 | |
"and gravity pulls it there." | 1:24:48 | 1:24:50 | |
Kip's based at Caltech in California | 1:24:52 | 1:24:54 | |
and is one of the most respected theoretical physicists in the world. | 1:24:54 | 1:24:59 | |
Firstly, Kip, a serious thank you | 1:24:59 | 1:25:01 | |
for helping out with the debacle over the app! | 1:25:01 | 1:25:05 | |
Well, I sympathise. | 1:25:05 | 1:25:07 | |
I've made so many errors of my own over the years | 1:25:07 | 1:25:10 | |
that I am totally sympathetic. | 1:25:10 | 1:25:13 | |
One of the things that struck me, | 1:25:13 | 1:25:15 | |
thinking about this, is something you wrote, Kip. | 1:25:15 | 1:25:18 | |
You said, "Everything likes to live where it'll age the most slowly, | 1:25:18 | 1:25:23 | |
"and gravity pulls it there." | 1:25:23 | 1:25:26 | |
Was this a way of explaining something | 1:25:26 | 1:25:29 | |
that you felt was a neat explanation | 1:25:29 | 1:25:31 | |
or is there something deeply profound about that? | 1:25:31 | 1:25:34 | |
I think there is something deeply profound, in some sense, | 1:25:34 | 1:25:38 | |
but it's a lovely description | 1:25:38 | 1:25:42 | |
of Einstein's first major insight about gravity. | 1:25:42 | 1:25:48 | |
In 1912, he realised that gravity | 1:25:48 | 1:25:51 | |
that we feel on Earth is due to a slowing of time on Earth. | 1:25:51 | 1:25:55 | |
So, time comes before gravity, in that sense? | 1:25:55 | 1:25:59 | |
On the Earth's surface, time runs more slowly | 1:25:59 | 1:26:01 | |
and that accounts for why gravity wants to keep us there? | 1:26:01 | 1:26:05 | |
Well, I think, in a very deep sense, this is true. | 1:26:05 | 1:26:07 | |
Objects WANT to fall. | 1:26:07 | 1:26:09 | |
The flow of time, or the rate of flow of the time, | 1:26:09 | 1:26:12 | |
is the thing that produces the gravity, | 1:26:12 | 1:26:15 | |
it is the thing that is ultimately responsible for the fall. | 1:26:15 | 1:26:20 | |
So, somehow, it's in the nature of all objects | 1:26:20 | 1:26:23 | |
to move towards a region where time runs slower. | 1:26:23 | 1:26:27 | |
Kip's formulation works anywhere in the universe | 1:26:27 | 1:26:30 | |
where the gravitational field is such as on Earth. | 1:26:30 | 1:26:34 | |
The difference in the rate of flow of time is tiny. | 1:26:35 | 1:26:38 | |
At high altitude and on the surface of the Earth, | 1:26:38 | 1:26:41 | |
the difference in the rate of flow of time is one second in 100 years. | 1:26:41 | 1:26:46 | |
That's not very much! | 1:26:46 | 1:26:48 | |
But that is enough that it's precisely the right amount | 1:26:48 | 1:26:53 | |
to produce the gravitational pull that we feel | 1:26:53 | 1:26:56 | |
and produce the accelerations we're talking about. | 1:26:56 | 1:26:59 | |
Wow, OK. I need to go and write this one down! | 1:26:59 | 1:27:03 | |
THEY LAUGH | 1:27:03 | 1:27:05 | |
So, my investigation deep into the weird ways of gravity | 1:27:07 | 1:27:11 | |
has finally left me face-to-face | 1:27:11 | 1:27:14 | |
with one of the greatest mysteries in all of physics, | 1:27:14 | 1:27:18 | |
the nature of time itself. | 1:27:18 | 1:27:21 | |
It sounds like such a simple question. | 1:27:21 | 1:27:24 | |
Why does the apple fall? | 1:27:24 | 1:27:26 | |
And yet, hundreds of years of scientific enquiry | 1:27:26 | 1:27:29 | |
investigating this single action | 1:27:29 | 1:27:32 | |
have led us to completely redefine | 1:27:32 | 1:27:34 | |
the way we think about the very nature of space and time. | 1:27:34 | 1:27:37 | |
And now I've been presented with this extraordinary proposition, | 1:27:39 | 1:27:42 | |
that somehow, in some profound way, | 1:27:42 | 1:27:46 | |
the apple falls because it's seeking out the place | 1:27:46 | 1:27:49 | |
where time runs the slowest. | 1:27:49 | 1:27:52 | |
So, does gravity dictate the flow of time? | 1:27:52 | 1:27:56 | |
Or does time itself define gravity? | 1:27:56 | 1:28:00 | |
Could this hint to fundamental new laws of physics, | 1:28:00 | 1:28:04 | |
as yet undiscovered? | 1:28:04 | 1:28:05 | |
I think I'm going to have to think about this a bit more. | 1:28:05 | 1:28:08 |