Pressure and Upthrust
Press the flat pad of your thumb hard against the point of a drawing pin. Now press the pin the
other way round, with the sharp point against your thumb, using exactly the same push.
The first way barely marks you; the second way hurts at once and could pierce the skin. Same
force, same thumb, wildly different result — so what changed?
What changed is the area the force was squashed into. The blunt head spreads
your push across a wide patch of skin; the needle-sharp point crams the identical push into a
speck of an area. That "how concentrated is the force" idea is called pressure,
and it decides whether a knife slices, whether snowshoes stop you sinking, and — once we get to
fluids — whether a boat floats.
The pressure formula
Pressure measures how much force
is pushing on each little bit of area. To turn that into a number we simply divide the force by
the area it is spread over:
p = \dfrac{F}{A}
Here F is the force in newtons (N) and
A is the area it presses on in square metres
(\text{m}^2). Because it is newtons divided by square metres, pressure
is measured in pascals: one pascal is one newton spread over one square metre.
1\ \text{Pa} = 1\ \text{N/m}^2.
The formula tells you the whole story in one glance. For a fixed force, shrinking the
area makes the pressure shoot up (a sharp point), while spreading the force over a big area makes
the pressure tiny (lying flat on ice instead of standing on it).
The pressure exerted by a force is the force acting per unit area:
- p = \dfrac{F}{A}
- Rearranged for the force: F = p\,A.
- Rearranged for the area: A = \dfrac{F}{p}.
Pressure is measured in pascals (\text{Pa} = \text{N/m}^2).
The same force gives a bigger pressure on a smaller area.
Worked example 1 — finding the pressure
A brick lies on a table. It presses down with a force (its weight) of
18\ \text{N}, and the face resting on the table has an area of
0.03\ \text{m}^2. What pressure does it put on the table?
Step 1 — write the formula.
p = \dfrac{F}{A}
Step 2 — put the numbers in.
p = \dfrac{18\ \text{N}}{0.03\ \text{m}^2} = 600\ \text{Pa}.
Step 3 — check it makes sense. Stand the very same brick up on its small end
(say 0.01\ \text{m}^2) and the same
18\ \text{N} now gives
18/0.01 = 1800\ \text{Pa} — three times the pressure, from the very
same brick, just because the area is three times smaller.
Worked example 2 — finding the force, then the area
Finding a force. A hydraulic press applies a pressure of
200\,000\ \text{Pa} onto a metal plate of area
0.05\ \text{m}^2. What force does it deliver? Here we know
p and A and want
F, so use F = p\,A:
F = p\,A = 200{,}000\ \tfrac{\text{N}}{\text{m}^2} \times 0.05\ \text{m}^2 = 10{,}000\ \text{N}.
Finding an area. A person of weight 600\ \text{N}
wants to keep the pressure on soft snow down to just 3000\ \text{Pa}
so they do not sink in. What total area of snowshoe do they need? Now rearrange to
A = F/p:
A = \dfrac{F}{p} = \dfrac{600\ \text{N}}{3000\ \text{Pa}} = 0.2\ \text{m}^2.
That is why snowshoes are so wide: to reach the large area that keeps the pressure low. Their
own bare feet, at maybe 0.04\ \text{m}^2, would give
600/0.04 = 15{,}000\ \text{Pa} — five times more — and down they'd
plunge.
Sharp means small area means high pressure
Once you have p = F/A in your head, a whole shelf of everyday things
suddenly makes sense — and they split neatly into two camps.
-
Make a small area on purpose → high pressure. A knife is sharpened to a
razor-thin edge so a gentle push becomes a huge pressure that slices through. A drawing pin,
a nail, a needle, an ice skate's blade and an animal's fang all work the same way: tiny area,
enormous pressure.
-
Make a big area on purpose → low pressure. Snowshoes, skis, a camel's broad
feet, a tractor's fat tyres and the wide caterpillar tracks of a tank all spread the weight
out so the pressure on soft ground stays low enough not to sink in.
Fluids push too: upthrust
Pressure isn't only about solids pressing on solids. A fluid — a liquid or a
gas — presses on everything touching it, and here is the key fact: the deeper you go,
the greater the pressure, because there is more fluid stacked up above weighing down.
Dive to the bottom of a swimming pool and you can feel the extra pressure squeezing your ears.
Now think about an object sitting in water. The water pushes on it from every side. But the
pressure on the bottom face is bigger than the pressure on the top face, simply
because the bottom is deeper. A bigger push up on the bottom than down on the top leaves a
leftover upward force. That net upward push from the fluid is
upthrust (grown-ups also call it buoyancy). It is the reason things
feel lighter in water, and the reason anything floats at all.
This builds directly on
floating and sinking:
there we said "the water pushes up"; now we know why — deeper water pushes harder, so a
submerged object always gets a net shove upwards.
How big is the upthrust? Archimedes' principle
You might expect the up-push to be some complicated thing. It is astonishingly simple. When an
object is put into a fluid it shoves some fluid out of the way — it displaces
it. Archimedes discovered that:
- The upthrust on an object equals the weight of the fluid it
pushes out of the way (the fluid it displaces).
- So the more fluid an object displaces, the harder the fluid pushes back up.
- An object floats when it can displace its own weight of fluid —
then the upthrust exactly balances its weight.
Picture lowering a block slowly into water. As it sinks in, it pushes more and more water aside,
so the upthrust grows. One of two things then happens:
-
If the block can push aside its own weight of water before it is fully under, it
stops sinking and floats, sitting with just enough of itself submerged to
balance its weight.
-
If even the fully-submerged block displaces less than its own weight of water, the
upthrust can never catch up with the weight, so the block keeps going and sinks
to the bottom.
Why a steel ship floats but a steel bolt sinks
This is exactly the same puzzle you met with density. A small steel bolt
dropped in the sea sinks instantly. Yet a colossal steel ship, thousands of
times heavier, floats. Archimedes explains it perfectly.
The bolt is a tiny solid lump. Even fully underwater it shoves aside only a bolt-sized splash of
water — far, far less than its own weight — so the upthrust is feeble and the weight wins. The
ship is spread out wide and hollow, with a vast belly of air. It only has to
sink in a little before it has displaced an enormous amount of water — enough to weigh
as much as the whole ship — and at that point the upthrust balances the weight and it floats.
Same steel; utterly different displaced volume.
For a plain solid lump this is the same as the
density rule: an object floats if it is
less dense than the fluid and sinks if it is denser. A hollow
boat wins because trapping air inside makes the whole boat-plus-air roomier — and so less dense
on average — than the water around it.
See the tug-of-war
Below is a block in a tank of liquid. The down arrow is its
weight; the up arrow is the upthrust from the
liquid. Slide Block density below 1 (lighter than water) and
the block bobs up and floats — it sinks in only far enough to displace its own weight, so the two
arrows match. Push the density above 1 (denser than water) and even
the fully-submerged block can't displace enough: the weight arrow beats the upthrust and it drops
to the floor. The Block size slider grows both the block and, while it floats, the
upthrust with it — a floating block always settles so upthrust equals weight.
-
Pressure is not the same as force. A ballerina on tiptoe and an elephant can
push down with very different forces, yet the ballerina can make the higher pressure,
because her tiny toe-area concentrates her weight. Always ask "over what area?" — a small area
means a big pressure.
-
Upthrust acts on sinking objects too. A stone doesn't sink because it "gets no
upthrust" — it does get some. It sinks because its weight is bigger than the biggest
upthrust it can gather. That is exactly why a rock feels lighter (but not weightless) while it
is under water.
-
Floating isn't about being "light". A giant tree trunk is hugely heavy and
floats; a tiny screw is light and sinks. What matters is density (for a solid lump)
or the weight of fluid displaced — never the weight on its own.
A camel is a heavy animal, yet it strides across soft desert sand where a horse's narrow hooves
would sink. The trick is pure p = F/A: a camel has broad, splayed feet
that spread out further with every step, giving a large area A. The
same weight F divided over that bigger area gives a much smaller
pressure on the sand — low enough that the sand holds firm. It's the desert version of a snowshoe.
Ships have a clever pressure-and-floating trick of their own: the Plimsoll line,
a mark painted on a ship's hull. Load cargo on and the ship sits lower, displacing more water for
more upthrust — but if it sinks past the Plimsoll line it is dangerously overloaded and could go
under. The line is a legal limit, born from Archimedes' principle, that has saved countless
sailors' lives.