3.2.4 - Density, pressure and upthrust

3.2.4 - Density, pressure and upthrust

Density tells you how much mass is packed into a volume. Pressure tells you how a force is spread over an area. In fluids, these ideas combine: pressure increases with depth, and the pressure difference around an object produces upthrust. By the end of this lesson, you should be able to use the equations accurately and explain floating, sinking and apparent weight using Archimedes' principle.

Density

Density is a property of a material or object that compares its mass with the volume it occupies. A small object can have a large mass if its material is dense; a large object can have a small mass if it contains a lot of empty space.

The density and pressure relationships in this lesson are supplied in the OCR data booklet, but you still need to choose the correct equation, use consistent SI units, and explain the physical meaning of the symbols.

Density

Density is mass per unit volume.

Density

ρ=mV\rho=\frac{m}{V}

Here, ρ\rho is density in kgm−3\mathrm{kg} \mathrm{m}^{-3}, mm is mass in kg\mathrm{kg}, and VV is volume in m3\mathrm{m}^{3}. The same equation can be rearranged to m=ρVm = \rho V or V=m/ρV = m/\rho.

The SI unit kgm−3\mathrm{kg} \mathrm{m}^{-3} matters. Many density values are first measured using grams and cubic centimetres, especially in school laboratory work, but OCR calculation answers normally need SI units unless the question states otherwise.

Useful conversions:

  • 1 g=1×10−3 kg1\,\mathrm{g} = 1 \times 10^{-3}\,\mathrm{kg}
  • 1 cm3=1×10−6 m31\,\mathrm{cm}^{3} = 1 \times 10^{-6}\,\mathrm{m}^{3}
  • 1 g cm−3=1000 kg m−31\,\mathrm{g}\,\mathrm{cm}^{-3} = 1000\,\mathrm{kg}\,\mathrm{m}^{-3}

Worked example: finding density from mass and volume

A metal cube has mass 0.432 kg0.432\,\mathrm{kg} and volume 54.0 cm354.0\,\mathrm{cm}^{3}. Calculate its density in kgm−3\mathrm{kg} \mathrm{m}^{-3}.

First convert the volume:

54.0 cm3=54.0×10−6 m3=5.40×10−5 m354.0\,\mathrm{cm}^{3} = 54.0 \times 10^{-6}\,\mathrm{m}^{3} = 5.40 \times 10^{-5}\,\mathrm{m}^{3}

Now use the density equation:

ρ=mV=0.4325.40×10−5=8.00×103 kg m−3\rho=\frac{m}{V}=\frac{0.432}{5.40\times10^{-5}}=8.00\times10^3\ \text{kg m}^{-3}

The density is 8.00×103 kg m−38.00 \times 10^{3}\,\mathrm{kg}\,\mathrm{m}^{-3}.

In practical work, the method depends on the shape.

  • For a regular solid, measure dimensions with a ruler, vernier caliper or micrometer, calculate volume from geometry, and measure mass with a balance.
  • For an irregular solid that does not dissolve or absorb liquid, measure mass with a balance and find volume from the rise in water level in a measuring cylinder, or from displaced water.
  • For a liquid, measure mass of a known volume. Use the mass of the empty container and the mass of container plus liquid, then subtract.

Common uncertainty points are meniscus reading, parallax, zero error in measuring instruments, trapped air bubbles around an object, and judging the volume of an irregular object from a scale with limited resolution.

Pressure

Pressure is not just another word for force. It tells you how concentrated a normal force is over a surface area. A force spread over a large area gives a smaller pressure than the same force acting over a small area.

Pressure

Pressure is normal force per unit area.

Pressure

p=FAp=\frac{F}{A}

Here, pp is pressure in pascals, Pa\mathrm{Pa}, FF is the force normal to the surface in newtons, N\mathrm{N}, and AA is the area in square metres, m2\mathrm{m}^{2}. One pascal is one newton per square metre:

1 Pa=1 N m−21\ \text{Pa}=1\ \text{N m}^{-2}

The force must be perpendicular to the area. If a book rests flat on a table, it exerts a normal contact force on the table. This equals its weight when the book is in vertical equilibrium; the weight itself acts on the book. If a gas pushes on the wall of a container, the pressure force on each small part of the wall is normal to that wall.

Worked example: pressure on a floor

A box has weight 240 N240\,\mathrm{N}. It rests on a rectangular base of area 0.080 m20.080\,\mathrm{m}^{2}. Calculate the pressure on the floor.

p=FA=2400.080=3000 Pap=\frac{F}{A}=\frac{240}{0.080}=3000\ \text{Pa}

The pressure is 3.0×103 Pa3.0 \times 10^{3}\,\mathrm{Pa}.

Now imagine the same box placed on a smaller face with area 0.020 m20.020\,\mathrm{m}^{2}.

p=2400.020=12000 Pap=\frac{240}{0.020}=12000\ \text{Pa}

The weight has not changed, but the pressure has increased because the area is smaller.

This same idea applies to solids, liquids and gases, but the mechanism differs. A solid may press because of its weight or an applied force. A fluid exerts pressure because its particles transfer force to surfaces, and in a gravitational field the weight of fluid above a point affects the pressure at that depth.

Pressure In A Fluid

In a fluid at rest, pressure increases with depth. The deeper point has more fluid above it, so the weight of that fluid column is larger. This is why a diver feels increasing pressure under water and why a dam must be stronger near the bottom than near the top.

The pressure due to a column of fluid is:

Pressure Due To A Fluid Column

p=hρgp=h\rho g

Here, pp is the pressure due to the fluid in Pa\mathrm{Pa}, hh is the vertical depth below the fluid surface in m\mathrm{m}, ρ\rho is the fluid density in kgm−3\mathrm{kg} \mathrm{m}^{-3}, and gg is gravitational field strength in Nkg−1\mathrm{N} \mathrm{kg}^{-1} or ms−2\mathrm{m} \mathrm{s}^{-2}.

[DIAGRAM: asset_name: 3.2.4 - Density, pressure and upthrust - diagram 1; asset_slug: 3_02_4_density_pressure_and_upthrust__diagram_01; recommended_method: drawn_physics; caption: The weight of a fluid column produces a pressure difference with depth.; description: A fluid column of depth h and area A is used to derive pressure difference from its weight.]
The weight of a fluid column produces a pressure difference with depth.

You can derive the equation from p=F/Ap = F/A.

For a fluid column of height hh and cross-sectional area AA:

V=AhV=Ah

The mass of fluid in the column is:

m=ρV=ρAhm=\rho V=\rho Ah

Its weight is:

W=mg=ρAhgW=mg=\rho Ahg

The pressure on the base of the column is force divided by area:

p=FA=ρAhgA=hρgp=\frac{F}{A}=\frac{\rho Ahg}{A}=h\rho g

The area cancels. That cancellation is important: in a static fluid, the pressure at a depth depends on hh, ρ\rho and gg, not on the shape or total width of the container. Two points at the same depth in the same static fluid have the same pressure due to the fluid, even if one side of the container is wide and the other is narrow.

Boundary note: p=hρgp = h \rho g gives the pressure due to the fluid column. If a question asks for total pressure in an open liquid, atmospheric pressure at the surface would also be included. In this lesson, unless a question explicitly says total or absolute pressure, treat p=hρgp = h \rho g as the pressure due to the fluid.

Worked example: pressure and force under water

A small horizontal hatch on a tank is 1.80 m1.80\,\mathrm{m} below the water surface. The density of water is 1000 kg m−31000\,\mathrm{kg}\,\mathrm{m}^{-3}. Take g=9.81 N kg−1g = 9.81\,\mathrm{N}\,\mathrm{kg}^{-1}.

Pressure due to the water:

p=hρg=1.80×1000×9.81=1.77×104 Pap=h\rho g=1.80\times1000\times9.81=1.77\times10^4\ \text{Pa}

If the hatch has area 0.0250 m20.0250\,\mathrm{m}^{2}, the force due to this pressure is:

F=pA=(1.80×1000×9.81)×0.0250=441 NF=pA=(1.80\times1000\times9.81)\times0.0250=441\ \text{N}

The pressure is set by depth, density and gg; the force also depends on the area being pushed.

Upthrust And Archimedes' Principle

An object in a fluid experiences pressure on all its surfaces. The pressure is greater lower down, so the upward pressure force on the bottom of the object is larger than the downward pressure force on the top. The horizontal pressure forces on opposite sides cancel for a fully surrounded object in a static fluid. The resultant fluid force is upward: this is upthrust.

Upthrust

Upthrust is the resultant upward force exerted by a fluid on an object in the fluid.

[DIAGRAM: asset_name: 3.2.4 - Density, pressure and upthrust - diagram 2; asset_slug: 3_02_4_density_pressure_and_upthrust__diagram_02; recommended_method: drawn_physics; caption: Greater pressure below an immersed body produces upthrust.; description: Pressure is greater at the bottom of an immersed body than at the top, producing upthrust; horizontal pressure forces cancel.]
Greater pressure below an immersed body produces upthrust.

Archimedes' principle gives the size of the upthrust without needing to add up all the pressure forces on every surface.

Archimedes' Principle

Archimedes' principle states that the upthrust on an object immersed in a fluid is equal to the weight of the fluid displaced by the object.

This means:

U=weight of displaced fluidU=\text{weight of displaced fluid}

If the displaced fluid has density ρf\rho_{f} and the displaced volume is VdV_{d}, then:

U=ρfVdgU=\rho_f V_d g

This expression is not a new law separate from Archimedes' principle; it is just "weight of displaced fluid" written using m=ρVm = \rho V and W=mgW = mg.

Two details decide many answers.

  1. Use the density of the fluid that has been displaced, not the density of the object.
  2. Use the displaced volume. If the object is fully submerged, this is the whole object volume. If it is floating partly above the surface, this is only the submerged volume.

Worked example: upthrust on a fully submerged object

A solid object of volume 3.40×10−4 m33.40 \times 10^{-4}\,\mathrm{m}^{3} is fully submerged in water of density 1000 kg m−31000\,\mathrm{kg}\,\mathrm{m}^{-3}. Calculate the upthrust.

The displaced volume is the full object volume:

Vd=3.40×10−4 m3V_{d} = 3.40 \times 10^{-4}\,\mathrm{m}^{3}

Using Archimedes' principle:

U=ρfVdg=1000×(3.40×10−4)×9.81=3.34 NU=\rho_f V_d g=1000\times(3.40\times10^{-4})\times9.81=3.34\ \text{N}

The upthrust is 3.34 N3.34\,\mathrm{N} upward.

When released from rest with no other significant forces, an object whose weight exceeds this upthrust initially accelerates downward. If upthrust exceeds weight it initially accelerates upward. Drag then develops as it moves; a rising object can settle floating partly submerged.

For a submerged cuboid of horizontal cross-section AA, the top and bottom depths are h1h_1 and h2h_2. Subtract the downward top pressure force from the upward bottom pressure force:

U=(p2−p1)A=ρfg(h2−h1)A=ρfgVd.U=(p_2-p_1)A=\rho_f g(h_2-h_1)A=\rho_f gV_d.

Any common surface pressure cancels. This derives Archimedes' result directly for the cuboid; the general principle applies to other shapes too.

Floating, Sinking And Practical Evidence

Floating and sinking are force-equilibrium questions. For an object in a fluid, the main vertical forces are usually weight downward and upthrust upward. If the object is stationary or floating at rest, the resultant force is zero.

For a floating object:

U=WU=W

So:

weight of displaced fluid=weight of object\text{weight of displaced fluid}=\text{weight of object}

This does not mean the object has displaced its whole volume. A floating object displaces just enough fluid for the upthrust to equal its weight.

For a fully submerged object released from rest, with no other significant forces initially:

  • if W>UW > U, the resultant force is downward and the object sinks;
  • if U>WU > W, the resultant force is upward and the object rises;
  • if U=WU = W, the object is in vertical equilibrium.

Average density is a useful way to predict floating. If an object's average density is less than the density of the surrounding fluid, it can float. A steel ship floats because its overall volume includes air; its average density is much lower than solid steel. A helium balloon rises in air because the gasbag and helium together have lower average density than the displaced air, provided the upthrust exceeds the total weight.

Worked example: floating fraction

A wooden block has density 640 kg m−3640\,\mathrm{kg}\,\mathrm{m}^{-3} and floats in water of density 1000 kg m−31000\,\mathrm{kg}\,\mathrm{m}^{-3}. Find the fraction of the block's volume below the water surface.

Let the block's total volume be VV and the submerged volume be VsV_{s}.

The block's weight is:

W=ρblockVgW=\rho_\text{block}Vg

The upthrust is the weight of displaced water:

U=ρwaterVsgU=\rho_\text{water}V_sg

For floating equilibrium, U=WU = W:

ρwaterVsg=ρblockVg\rho_\text{water}V_sg=\rho_\text{block}Vg

Cancel gg and rearrange:

VsV=ρblockρwater=6401000=0.640\frac{V_s}{V}=\frac{\rho_\text{block}}{\rho_\text{water}}=\frac{640}{1000}=0.640

So 64.0%64.0\% of the block's volume is submerged.

A practical way to test Archimedes' principle is to measure the apparent weight of an object in air and then when it is fully submerged.

  1. Measure the object's weight in air with a newton meter.
  2. Lower it fully into water without touching the bottom or sides of the container.
  3. Record the smaller apparent weight.
  4. The reduction in the newton-meter reading is the upthrust. The gravitational weight itself has not changed: the meter measures the supporting tension, and T+U=WT+U=W.
  5. Compare this with the weight of water displaced, found from the displaced water volume and ρVg\rho V g.

Good practical answers mention controlling trapped air bubbles, keeping the object fully submerged when required, reading the newton meter at eye level, avoiding contact with the container, repeating readings, and using a measuring cylinder or displacement can with suitable resolution.

Takeaway

For upthrust questions, write the physical link: upthrust equals the weight of displaced fluid. Then decide whether the object is in equilibrium, rising, sinking or only partly submerged.