Hear about 'swimming' robot gliders in Lunchtime Labs!
Have you ever seen a robot swim? Researchers from UEA’s School of Environmental Sciences use a ‘swimming’ robot called a Seaglider to gather data from the farthest reaches of our seas and oceans – from the polar ice caps to the Bay of Bengal. Learn more in this Lunchtime Lab!
Visit https://norwichsciencefestival.co.uk/whats-on/lunchtime-labs-sea-gliding-science and scroll down to download the activity pack that accompanies this Lunchtime Lab.
Our researchers will be in YouTube chat from 12.15pm to 1.15pm on Saturday 24 October, ready to answer your questions!
(This Lunchtime Lab was recorded across several weeks during summer 2020. The presenters are in the same bubble, and social distancing rules were complied with by the film crew and everyone involved.)
Featuring talks and activities developed and presented by:
Elizabeth Siddle, School of Environmental Sciences, University of East Anglia
Jack Mustafa, School of Environmental Sciences, University of East Anglia
Recommended ages 7+
Runtime: 25 minutes + Q&A
Set up a YouTube account and log in during the event to join the live chat where you can ask questions and share your thoughts!
Part of Norwich Science Festival At Home, brought to you by The Forum, Norwich, with UEA and Norwich Research Park. Norwich Science Festival At Home is a free, online mini programme of events from 24-28 October. The full Festival will return in 2021.
hi everyone I'm Beth and I'm jJack and
in today's lunchtime lab we're going to teach you a bit about oceanography which
is the study of oceans and how they work. In this lunchtime lab we're going to walk you
through a few experiments that we've performed which will help you to understand some
of the things that we as oceanographers have got to understand and think
about when we look at the oceans, and some of them you'll be able
to do along with us at home. At the end we're going to take y
ou down to the
tank room and there'll be some robots there and we can show you how they work and how
we use them to help us study the oceans. In this experiment we're going to
look at something called density. Density is a scientific word which explains
how much material there is in a certain space. To look at this idea I've got a wooden
block and a metal block in front of me. Both of them have a mass of 100 grams and
because they have the same mass that means in my hands they feel pretty
much the same.
However of course the wooden block is a lot bigger than the metal block that is because in
the metal block all of the particles and atoms are packed into a much smaller
space but you could say that there's pretty much the same number of
particles but just in a smaller space. So that means that this metal block
is more dense than the wooden block. Why is density an important thing for us as
oceanographers? Why does it matter? It's because in the water in the oceans the density
of objects
controls where they are, whether or not they're at the top or at the bottom and to explain this
I'm going to put these objects in the water. The metal block sinks to the bottom of the water
very very easily whereas the wooden block sits on top even if I try to push it down that's
because in water if an object is very dense then it will sink down to the bottom. But if
like the wooden block an object is not very dense it will float at the top and in water different
things can mak
e water have different densities so if you get water which is very dense and water
which is not very dense, then the water which is very dense will sit at the bottom and the
water which is less dense will sit at the top. So there are a few things that we have
to think about when we study the ocean, and these are temperature and salinity or
how salty the sea is so we think about these because these have an influence on density.
First off our temperature - if something's really cold it's going
to be more dense and sit
at the bottom then something which is hot and going to be less dense and float at the top. So
if you had cold water it would be underneath hot water whereas if we look at salinity or how
salty or fresh something is so fresh means water that's not got very much salt in it and
salty is water that's got lots of salt in it. So salty water has all the salt particles mixed
in with the water and that makes it more dense so it'll be at the bottom whereas fresh water
will
float at the top because it's less dense. So we have to think about all these
things when we're studying the ocean and what we're going to do now is we're going
to take two very cold ice cubes and we're going to put one in our tank of salty water here and
one in our tank of fresh water and we're going to have a look at what happens and use that
to show you a little bit more about density. So what do you think might
happen before we put them in? I'm back with two ice cubes and we're going
t
o pop these in our tank of salty water and a tank of fresh water to see what happens.
So these ice cubes have been made with purple food dye so that you can see the water
spread out throughout the tanks as they melt. Now ice is less dense than water so when we put
these in the tanks they're going to float on top of the water but the water that melts out of
the ice cubes might do something different. What do you think might
happen when I put these in? Let's find out. So we can see now our ice
cubes are in our
tanks of water and if we look at our fresh tank first our ice cube is starting to melt and
we can see all this purple water that's really cold and fresh from our ice cubes sinking down
to the bottom of our tank and that's because this cold water is more dense than the room
temperature water that's in that tank already. But if we look at our salty tank things look
a little bit different and why might that be? So our ice cube is still melting and giving
out really cold wate
r but this time it seems to be floating at the top and that's all to do
with the salinity of our tank so remember this tank is full of really salty water and what's
happening is we're putting fresh water into that so our fresh water is floating at the top
because it's less dense. So that's the fresh water from our ice cube melting even though it's
cold - it's still floating on top of the tank. Cool so to recap, in this experiment we've been
looking at density and if we remember there are tw
o things that affect the density of water
- that is the temperature and the salinity. We saw that the temperature affected the water
in the fresh water tank because the cold water coming from the ice cube sunk to the bottom.
So we showed that cold water sinks in the salty tank; we showed that salty water sinks because the
salt water in the main tank stayed below the fresh water with no salt that came out of the ice cube.
So if you like this experiment you can try it at home by getting yoursel
f some table salt, a
container, some tap water and some food dye. Now you might need a parent or guardian's help
to do this one and you're going to freeze some ice cubes with some food dye mixed in and
use gloves so you don't stain your fingers, and then mix yourself up a salty tank and a
fresh tank. You can make your salty tank by using 35 grams of table salt in a litre of water. And
take your ice cubes once they're frozen and have a look and see what happens when you put them
in the wate
r - do they sink or do they float? So now we're going to take our tank of
salty water and a tank of fresh water some pencils and some plasticine and we're
going to look a bit more about density and try and teach her about buoyancy. So if we take a pencil and put it in a tank
of fresh water what do you think might happen? So it floats up to the top and this is because
our pencil is less dense than our fresh water, whereas if we take some
plasticine what might happen here? Pop it in the water
it's more dense than
the water so it sinks to the bottom. So now what might happen if we take another
pencil and a blob of plasticine and put the two of them together to make one object. I'm going
to start with just a little bit of plasticine and put it on the end of the pencil... ...like that okay so if I put this now in the tank
of fresh water do we think it will float because the pencil's less dense in the water or sink
because the plaster seems more dense in the water? It floats to the
top and that's because
there's not very much plasticine so the density of the overall object
is less dense than the fresh water. But what happens now if we put even
more plasticine onto the object? Okay, that's quite a lot of plasticine that
we've got on the object now. So what happens if we put this back in the fresh water that
sinks to the bottom which means that now because of the extra plasticine the overall
object is more dense than the fresh water. So earlier we took a pencil and pu
t just
the right amount of plasticine on it so that it'll have the same
density as our fresh water. So what do you think might happen if
we put this in the water? Let's see... So what's happened is our pencil was hovered
in the water just where we put it and that is because it has the same density as the water.
And this is something called neutral buoyancy. So what happens now if we take this
pencil out of the fresh water tank (if I can actually grab it) and put it in the
salt water tank w
hich we know is more dense than the fresh water tank? Will it float sink or be
neutrally buoyant in this tank? Let's take a look. It floats in the salty water tank which means that
this object which is the same density as the fresh water which is why it was neutrally buoyant in
this tank is less dense than the salty water. So earlier we've repaired a
pencil with some plasticine on it just the right amount of plasticine so that
it's neutrally buoyant in our salty tank here. So if we pop this
in the water... again it's going to hover just where we left
it and that is because it has the same density as the salt water.
So what do you think will happen now if we put this pencil and
plasticine back into the fresh water tank? Will it sink float or be neutrally
buoyant? Remembering that the fresh water is less dense than the salty water and
it was neutrally buoyant in the salty water. It sinks to the bottom which again is what we
expected because the fresh water it's easier for thing
s to sink in it because it's less dense.
So this object is more dense than the fresh water. So just to recap we've shown
you that our salty water is more dense than our fresh water and what
neutral buoyancy is, which is where the our pencil and our plasticine had the
same density as the water it was in. So you can try this experiment at
home if you get a clear mixing bowl. You measure out 35 grams of salt and put it
in a litre of water, mix it all together. Find yourself a pencil into plast
icine or if
you don't have any some blue tack will work too, and see if you can make your pencil float sink and
be neutrally buoyant in your bowl of salty water. In this experiment we're going to
be salt tasting which is something that you guys at home can join in with us for.
In front of me I've got four different containers full of different amounts of table salt and soon
I'm going to add some water into all of them and stir them up so that they all look the same.
A fun fact that you might
not know is that different seas and oceans around the world are not
all exactly as salty as each other some of them are more salty and some of them are more fresh.
The table on screen now is showing how to make these four different solutions at home with
your own table salt, water and containers. I'm going to add water to these four
containers and once I've done that I'm going to bring Beth here and she's going
to try and taste the four different samples and see if she can work out which on
e represents
which sea in which ocean from around the world. Welcome Beth in front of us we've
got four different containers full of solutions of salty water and all
of them have different amounts of salt in. They represent different seas and oceans from
around the world. The seas and oceans that they represent are melted Antarctic sea ice, the Baltic
sea, the Mediterranean sea and the Dead sea, but they're not necessarily in that order.
So your job is to try and take a small taste from eac
h of them and work out by
how salty they are which one's which. If you're doing this experiment with us at
home please be careful when you're tasting the different solutions of water because
the salty ones will taste rather nasty and it might make you a little bit ill so please
only taste a little bit and don't swallow any! So can you talk us through which ones you would
expect to be the most and the least salty and why? Okay so I think the and melted sea ice from
Antarctica is going to be
the least salty and that's because sea ice doesn't really
have much salt in it from where the water in the sea is frozen to make the ice.
And then I think the one from the Dead sea is probably going to be the most salty
and that's because the Jordan river flows into the Dead sea but there's no
rivers that float out of the Dead sea. So the water evaporates that's in the Dead sea
and goes up into the air and that leaves all the salt behind and makes it really really salty.
And then the Medite
rranean and the Baltic I'm not sure which way around they're going to
be so I'll have to taste them and find out. That's interesting thank you, I'll let
you taste them now and you can see. Okay I'll switch something
How did that one taste? It's a little bit salty but not too bad. Okay. Oh that one tastes a bit more salty number three. That one tastes almost like regular
tap water. That tastes quite fresh. Interesting, okay. Number four. Oh that's very salty.
Oh interesting. So I think number
four is going to be the Dead
sea because that's the saltiest by quite far. I think number three is going to be the
sea ice because that's the freshest. And then Mediterranean and Baltic. I
think the saltier one which was number two is going to be the Mediterranean which
makes number one the Baltic. Was that right? Well done! That was four out of four.
That was a very good effort indeed. So perhaps we should give a quick explanation
of why the Mediterranean is more salty than the Baltic, bec
ause they're pretty close. But there's
a little bit of a difference - there's a little bit more rain over the Baltic sea which means and
of course rain is fresh water. So if you get rain over a sea it makes it less salty which is why
the Baltic is more fresh than the Mediterranean. Wonderful you did a very good job there!
So we hope you were able to work these out alongside us at home but if not just
to recap number one is the Baltic sea, number two is the Mediterranean sea,
number three is
a melted Antarctic sea ice, and number four is the Dead sea.
Thanks for joining in! So next we're going to show you a
little bit more about density and we're going to teach you about pressure.
Now pressure is the force acting in an area so if I take my fingers and push against the
bottle here you've got the force of me pressing on the bottle and the area that's happening
is where my fingers are touching the bottle. And what we're going to do is we're going
to use this idea of pressure I'm g
oing to show you how it works by using these little
divers that we have in our bottles here. So in water you can't really squash water
very far because all of the bits that make up the water, the molecules and the atoms
are already really tightly packed together, whereas in air which is a gas all of the molecules
and atoms that make it up are spread out all over the place and they're all whizzing around
really quickly and so we can squash them all together and make it a lot smaller.
Cool. S
o as Beth says if you put pressure on the outside of the bottle then that pressure
increases the pressure inside the bottle as well. So what happens if I start to squeeze the bottle
I'm increasing the pressure on the outside and that pressure means that everything
on the inside is trying to get smaller, but as Beth said you can't really make water
smaller. However you can make air smaller and these little divers on the inside of the
bottle, there's air inside them so when we squeeze the bot
tle the air inside the diver will
start to compress inwards and as it does that the little hole in the back of the diver will
start to suck the water from the bottle into it to fill the gap where the air is getting smaller.
And what that means is that as the water is going into the diver the diver is going to get denser
because there's more material inside it and as it gets denser that means that if I squeeze
it hard enough it will get denser than the water in the bottle, which means that it
sinks.
And now if I start to release my pressure so if I start to lighten my fingers then the air inside
the diver will start to expand outwards again and that means that it's become less
dense in the surrounding water once again. For our final segment we're here in the
tank room at the University of East Anglia and we're going to look at one of the robots
that we use to learn about the oceans, which is here in the tank next to us.
We're also going to look at this glider here which is clear
which means that
we can look closely at the inside of it to see how what's happening on the inside of this
one, which is exactly the same as the inside of that one, affects the way that it moves.
So if we think back to our pencil buoyancy experiment that we did earlier we managed to make
our pencil and our plasticine together neutrally buoyant so it's sat in the middle of our tank.
That's exactly what we've done with our sea glider here ready to do our experiments so
how does this glider mo
ve you might wonder it doesn't have an engine on the inside of it
like a car or like a ship and that's because we want gliders like this to be able to stay
in the oceans for lots of months at a time and engines have to be re-fueled quite frequently.
So instead we've got to be very clever about the ways that we make it move and we're
going to show you now how we do that. We're going to start by showing you how we get
our sea glider to go down through the water. Once the sea glider is in the
ocean we want it to sink down so we can study what's happening deep
down all the way to a thousand meters. I you think back to our bottle diver experiment
from earlier we made the diver sink by filling the diver with water as the air bubble
was squashed when we squeezed our bottle. What we do with our sea glider is very similar
in the back of the sea glider we have a bladder which is a bit like a balloon containing oil.
When we put the sea glider in the water this section of the sea glider f
ills
up with the water from around it. If we suck some of the oil out of the
bladder and further into the sea glider then more water goes into this back section
to fill the space where our bladder was. This makes the glider more
dense overall so it sinks. That's great. S now we know how to get the
glider to sink deep into the ocean below the surfac,e but right now it's only going
straight downwards so is there any way we can get the sea glider to travel forward through
the ocean too, so t
hat it can explore more of it? Yes there is. We have to make the glider
point its nose a little bit downwards and then the way the ocean water pushes
on the sea glider wings as it's sinking will push it forwards as well as going downwards. To make the nose of the glider point
downwards we have to move things around inside the sea glider so that the
front becomes more heavy than the back. So we use the glider battery this big thing in
the middle which has a metal weight attached to it as wel
l to make it even heavier and we move
that forward towards the nose of the glider. Let's see what happens when we send
this command to the sea glider. So we can see that the nose of the sea
glider has just tilted down as the battery has gone forward towards the nose.
If you're wondering why the sea glider isn't traveling forwards now
that we've got it tilted forwards it's because it's got to be sinking at the
same time as having its nose pointing forwards. Now we've seen how the glider
can
get down deep into the ocean, but we need it to get back to the surface.
Think back to our bottle diver experiment again the diver floated back up when
we stopped squeezing the bottle and let the extra water back out
of the diver as the air expanded. Again we do something very
similar with our sea glider. If we make the bladder fill up with oil from
further inside the sea glider, this makes the bladder take up more space which forces some of
that water out in the back section making the se
a glider less dense, and help it float back to
the surface, through the surrounding sea water. So now we have a glider that can move up down
and forwards but what happens if the sea glider isn't going in the direction we want it to go?
What happens if we want to turn it? Can we do that? We can - again we use the battery from
before and instead of moving it forwards and backwards we twist it and that means that we're
changing the bit the side of the glider which is heavier the heavier side of
the glider will then
sink downwards and it'll cause the glider to roll. So let's see what happens
when we rotate the battery and help the sea glider keep moving
forwards as well as upwards when it's rising and not just straight upwards, we can do the
opposite of what we did earlier and tilt the nose upwards instead of downwards, so the glider will
be rising and be tilted upwards at the same time. We can see what happens when we send this command
to the sea glider. To do this we have to mo
ve the battery further away from the nose.
We've shown that our glider can move up down and forward through the water
and can also change direction by rolling. So now we have a robot that can explore
anywhere down to a thousand meters in the ocean but what do we scientists do with it?
So we put sensors on our sea gliders to measure lots of different things in the ocean.
This glider in the tank has sensors in three different places which help us
measure temperature, salinity, pressure, amount
of light in the water
and amount of chlorophyll in the water. We can add other sensors to our sea
gliders to measure even more things like the amount of oxygen in the water or
even listens to sounds that are in the water. When we launch our gliders into the ocean
we use measurements like these to learn more about what happens in the ocean itself.
The glider group has previously studied areas of the ocean where the oxygen levels are
becoming so low that animals can't survive. In other areas
we've managed to use sea
gliders to go out and listen to whales. So when our gliders are out in the ocean,
we can't plug a cable in like we did in the tank to give commands.
So what do we do instead? We have to use satellites to talk to our sea
gliders and tell them where to go, so then the sea guider does lots and lots of calculations
whilst it's under the water to change its pitch its roll and its density, just like we saw in
the tank so it can try and reach its target. The sea glider can
stay in the water for months
at a time before we go and pick it up with a ship. So now you know lots about sea gliders
and how we study the ocean with them. That's it from Beth and I on
this lunchtime lab on sea glider. We hope that you've enjoyed watching
these experiments and learning about the robots that we use to study the
ocean if you've got any questions, pop them in the comments down below and if you'd
like to learn more about the missions that we do with our sea gliders go to the
UEA glider website
with a link down below. Thanks for watching.
Comments
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In response to Evie's question in the live chat: Great question Evie! Lots of people are involved in the building and designing of the sea gliders. We buy the Seagliders already made then do lots of tests at the university. We don't know exactly how long they take to make, but we would guess several months!
See what UEA's Seagliders are up to on their website: http://ueaglider.uea.ac.uk