Physics 14.1-14.4 - Particle model and density

Physics 14.1-14.4 - Particle model and density

A particle model can explain why solids keep their shape, liquids flow and gases spread out, even though the particles themselves are too small to see. Density then gives a precise way to compare how much mass is packed into a volume. In this lesson, you will use both ideas and learn the core practical for measuring the densities of a solid and a liquid.

The kinetic particle model

Matter can be represented using a kinetic particle model. "Kinetic" refers to movement: the model describes both the arrangement of particles and how they move. A particle may represent an atom or a molecule, depending on the substance.

The circles in a particle diagram are not photographs and are not drawn to scale. They are a model that helps us reason about matter. The gaps are spaces between particles; they are not filled with air unless the substance itself is a mixture containing air.

StateParticle arrangementParticle movementWhat the model explains
SolidVery close together, usually in an ordered arrangementVibrate about fixed positionsA solid keeps a fixed shape and volume
LiquidClose together in an irregular arrangementMove around and past one anotherA liquid flows, takes the shape of its container and keeps a fixed volume
GasFar apart in a random arrangementMove rapidly in random directionsA gas spreads out to fill its container and can be compressed

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Diagram

The particles in a solid are not motionless. They vibrate while remaining centred on fixed positions. In a liquid, particles remain close but can change neighbours. In a gas, particles are separated by much larger gaps and move freely through the available space.

This lesson's particle model, density equation and core practical are common to both Foundation and Higher tier.

Density as mass per unit volume

Two objects can have the same size but different masses. Density compares them fairly by asking how much mass there is in each unit of volume.

Density

Density is the mass per unit volume of a substance.

The symbol for density is the Greek letter ρ\rho (rho). Mass is mm and volume is VV.

Density

density=massvolume\text{density}=\frac{\text{mass}}{\text{volume}} ρ=mV\rho = \frac{m}{V}

In SI units, mass is in kilograms (kg), volume is in cubic metres (m3\mathrm{m^3}), and density is in kilograms per cubic metre (kg m−3\mathrm{kg\,m^{-3}}).

In a laboratory, mass is often measured in grams and volume in cubic centimetres, so density may be calculated in g cm−3\mathrm{g\,cm^{-3}}. Keep one consistent unit set throughout a calculation:

  • kg with m3\mathrm{m^3} gives kg m−3\mathrm{kg\,m^{-3}};
  • g with cm3\mathrm{cm^3} gives g cm−3\mathrm{g\,cm^{-3}};
  • 1 g cm−3=1000 kg m−31\,\mathrm{g\,cm^{-3}}=1000\,\mathrm{kg\,m^{-3}}.

For volume conversion, cube the length conversion: 1 cm=10−2 m1\,\mathrm{cm}=10^{-2}\,\mathrm{m}, so 1 cm3=10−6 m31\,\mathrm{cm^3}=10^{-6}\,\mathrm{m^3}. Hence 1 g cm−3=10−3/10−6=103 kg m−31\,\mathrm{g\,cm^{-3}}=10^{-3}/10^{-6}=10^3\,\mathrm{kg\,m^{-3}}. Dividing a cubic-centimetre value by 100 alone is not a volume conversion.

You may need either rearranged form:

m=ρVandV=mρm = \rho V \qquad\text{and}\qquad V = \frac{m}{\rho}

Worked example: calculating density

A block has a mass of 0.540 kg0.540\,\mathrm{kg} and a volume of 2.00×10−4 m32.00 \times 10^{-4}\,\mathrm{m^3}. Calculate its density.

Solution

  1. The values already use kg and m3\mathrm{m^3}, so no conversion is needed.
  2. Select the equation: ρ=m/V\rho = m/V.
  3. Substitute: ρ=0.540/(2.00×10−4)\rho = 0.540/(2.00 \times 10^{-4}).
  4. Calculate: ρ=2700 kg m−3=2.70×103 kg m−3\rho = 2700\,\mathrm{kg\,m^{-3}} = 2.70 \times 10^3\,\mathrm{kg\,m^{-3}}.

The answer has three significant figures, matching the data. A value of a few thousand kg m−3\mathrm{kg\,m^{-3}} is physically plausible for a dense solid.

Worked example: rearranging to find volume

A metal sample has mass 96.0 g96.0\,\mathrm{g} and density 8.00 g cm−38.00\,\mathrm{g\,cm^{-3}}. Find its volume.

Solution

V=mρ=96.0 g8.00 g cm−3=12.0 cm3V = \frac{m}{\rho} = \frac{96.0\,\mathrm{g}}{8.00\,\mathrm{g\,cm^{-3}}} = 12.0\,\mathrm{cm^3}

The units are consistent, and multiplying the answer back by the density gives 12.0×8.00=96.0 g12.0 \times 8.00 = 96.0\,\mathrm{g}, so the rearrangement passes a sense-check.

Core practical: density of a solid

The purpose is to determine the density of an irregular, non-porous solid. Its mass is measured directly. Its volume is found from the volume of water it displaces.

Apparatus: a balance, measuring cylinder, water, thin thread and a dry irregular solid that does not dissolve in or absorb water.

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Diagram

Method

  1. Place the dry solid on a zeroed balance and record its mass mm in g.
  2. Part-fill a measuring cylinder with enough water to cover the solid. At eye level, read the bottom of the water's meniscus and record the initial volume V1V_1 in cm3\mathrm{cm^3}.
  3. Lower the solid gently into the water using thin thread. Make sure it is fully submerged, with no trapped air bubbles and no water spilled.
  4. Read the new volume V2V_2 at eye level using the same part of the meniscus.
  5. Calculate the solid's volume: V=V2−V1V = V_2 - V_1.
  6. Calculate its density: ρ=m/V\rho = m/V.
  7. Return the water to a suitable starting level and repeat the displacement measurement at least three times. Investigate unexpected readings, repeat them where possible, and calculate a mean from valid results. Do not discard a value just because it disagrees with your prediction.

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