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GRADE 8 · THERMAL PHENOMENA

Kinetic particle theory and surface phenomena

The ideas of kinetic particle theory, states of matter, wetting and capillaries.

22 minutes4 theory cards
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Understanding step by step

Dip the edge of a paper towel into water. The wet patch creeps upwards even though gravity pulls the water down. What lifts the water, and why will it eventually stop rising?

No one is lifting the waterabovethe levelpaperWater moves through narrow channels
The edge of a paper towel is dipped into a glass, and the wet boundary rises well above the water level. No one lifts it: the water moves up the paper's narrow channels by itself.

Remember the particles

Remember: a gas is easy to compress, but water is not. Water flows, whereas ice keeps its shape. One model connects these observations: matter consists of particles that move continuously and attract and repel one another. These are the three main ideas of kinetic particle theory. In a liquid, particles are close together but change neighbours. To explain the shape of water, we therefore need both particle motion and particle interactions.

Motion in a liquidInteractionattractionrepulsionParticle sizes are schematic
On the left is a greatly enlarged, schematic piece of liquid: the particles are close together, with velocity arrows pointing in different directions. On the right, the interaction forces on a pair are shown separately: attraction at one separation and repulsion when very close. Velocities and forces are not mixed in the same diagram.

Why is a drop round?

Why is a small, freely falling drop almost spherical? Particles at the surface have different surroundings from those inside. Creating more surface takes energy, so a liquid tends to reduce its surface area while keeping the same volume. A sphere has the smallest area for that volume. This is an effect of surface tension. The model applies when gravity and other external effects distort the drop only slightly: gravity noticeably flattens a large drop resting on a table.

RoundedDeformedsmaller arealarger areaThe same liquid volumeCreating surface takes energy
For a given volume, a sphere has the smallest surface area. The diagram shows a sphere and a stretched drop of equal volume, represented as an ellipsoid of revolution. After being deformed, a free drop tends to become round again. The arrow represents a change of shape, not a force. Gravity is neglected.

A liquid meets a surface

Now place equal drops on clean glass and on wax. Water spreads out more on the glass and beads up on the wax. This spreading is called wetting. Contact changes the interfaces between the liquid, solid and air; the final shape depends on interactions at all these interfaces. So water is not simply a liquid that “wets everything”: the material, cleanliness and condition of the surface matter.

The same water in airclean glasswaxspreads out morewets less well
Water spreads out more on clean glass and forms a rounder drop on wax. Equal volumes of water in air are shown as schematic spherical caps. Wetting depends on the pair of materials and the condition of the surface.

What does the meniscus tell us?

Look closely at water beside the wall of a glass: the surface rises at the edge. This curved surface is called a meniscus. Water wets clean glass, and surface forces hold the curve against gravity. With a non-wetting liquid, the edge dips instead. The meniscus shape therefore gives a clue to whether the level will rise or fall in a narrow tube.

WettingNon-wettingedges riseedges dipThe curved surface is a meniscus
For a liquid that wets the wall, the edges of the surface rise along it, producing a concave meniscus. For a non-wetting liquid, the surface at the wall dips instead.

Why does the water rise?

Place a narrow, clean glass tube in water. Surface forces at its wall have a net upward component that lifts the liquid. As the column grows, however, its mass and weight increase. The rise stops when the weight balances the surface force. The rise or fall of liquid in narrow channels is called capillary action. Equilibrium does not stop the thermal motion of individual particles.

Weight limits the risehEquilibriumupweightwaterOpen at the bottom
The glass tube is open at the bottom. The bracket h runs from the outside water level to the centre of the meniscus. On the right, the force balance for the raised water is shown separately: the net vertical surface force equals the weight. The growing weight limits the rise. The tube is drawn wider for clarity.

Comparing the heights

Why does water rise higher in a narrower tube? Halving the radius halves the length of the boundary at the wall, but reduces the column's cross-sectional area to one quarter. The surface force decreases less than the weight of a column of the original height, so balance is reached higher up. The height h, measured in metres, is the vertical difference between the levels in the tube and the wide container. This comparison requires the same liquid, wetting conditions and temperature.

Change only the widthradius rradius r / 2h₁h₂Same water, glass and temperature
The level in the wide container is the common zero for height. The brackets reach the centre of each concave meniscus. The liquid, glass cleanliness and temperature are the same; the narrower tube gives a greater rise. Tube widths are exaggerated for clarity, and both surfaces have the same wetting behaviour.

Capillaries around us

A paper towel replaces a single tube with many winding, narrow gaps between fibres. If water wets the fibres, it spreads through these channels, including upwards. This explains our first observation and part of the movement of water through porous soil. Capillary action also plays a part in plants, but a single-tube model cannot explain a tall tree: evaporation from the leaves and continuous columns of water are also essential.

PaperSoilbetween fibresbetween grainsTall trees need more than this
In paper and soil, water moves through connected pores. Blue arrows show the directions in which water spreads between fibres and grains; they are not force arrows. The narrow channels are schematic. Capillary action alone cannot explain water rising through tall trees.

Two glass tubes

Two clean glass tubes are dipped into the same water. One has half the radius of the other. In which tube will the water be higher at equilibrium?

Equilibrium levels — ???radius rradius r / 2Same water, clean glass
Two clean glass tubes in the same water have radii r and r/2. This is the experimental setup: the equilibrium levels inside the tubes are still unknown and marked with question marks. The liquid, material, cleanliness and temperature are the same. We need to compare the eventual rise.

Worked example · 1

Both tubes contain the same water and have clean glass walls. We compare only their radii, keeping temperature and wetting conditions unchanged.

One pair: water and glass??radius rradius r / 2Both have the same wetting
We keep both tubes from the original experiment, their radii and their shared container. The same water wets the clean glass walls in both tubes. Wetting is a condition held constant; the equilibrium height remains the result to be compared.

Worked example · 2

In the tube with half the radius, the boundary at the wall is half as long and the column's cross-sectional area is one quarter as large. The surface force is therefore greater relative to the weight of a column of the same height.

The narrow column rises higherradius rradius r / 2Weight limits the rise
The same setup at equilibrium. The second tube has half the radius. For equal heights, the cross-sectional area and weight of the column fall to one quarter, while the boundary length and surface force fall to one half. The narrower column therefore rises higher. The widths are exaggerated for clarity; the menisci and common zero are retained.

Worked example · 3

The water must rise higher in the narrow tube for its weight to balance this force. For ideal narrow, circular capillaries, the height is inversely proportional to the radius.

Check the result

The water rises higher in the narrower tube: its smaller weight per unit height allows a taller column to be supported.

Key idea · 1

Drops and menisci take their shape because particles interact and the liquid tends to reduce its surface energy.

Key idea · 2

Wetting depends on the combination of liquid and surface; contamination can change the result.

Key idea · 3

Water rises in a capillary until surface forces and weight balance. This does not violate conservation of energy.

What comes next

Thermal motion depends on temperature. Next we will distinguish temperature from an object's total internal energy.

Basic Concepts

3 concepts

Capillary action

Liquid rises or falls in a narrow tube because of surface forces and its wetting interaction with the walls.

The narrower a capillary wetted by the liquid, the greater the rise. This effect helps water move through pores in soil and plants.

Wetting and non-wetting

Wetting is the spreading of a liquid over a solid surface; on a non-wetting surface, the liquid forms more pronounced droplets.

The shape of a drop or meniscus depends on interactions at the interfaces between the liquid, solid and surrounding gas, as well as the condition of the surface. Water wets clean glass well and wax less well. Comparing just two attractive forces is not enough for a general explanation.

The main ideas of kinetic particle theory

Substances consist of particles that move continuously and interact through attraction and repulsion.

These three ideas explain diffusion, gas pressure, elasticity and the differences between states of matter.

Physical quantities

1 magnitude

Height of capillary rise

h

The vertical change in liquid level in a narrow tube.

Unit: metre · \mathrm{м}

Related formulas

The same formulas in the reference, with symbols and units.

Problems on this topic

Statements, answer options and the walkthrough.