Mechanical Properties of Fluids
1. What this chapter covers
A fluid is anything that flows — liquids and gases together. The previous chapter asked how solids resist being deformed. This one asks what happens when a material has no fixed shape to defend.
| Textbook section | Topic |
|---|---|
| 9.1 | Introduction |
| 9.2 | Pressure — Pascal's law, depth, atmospheric and gauge pressure, hydraulic machines |
| 9.3 | Streamline flow and the equation of continuity |
| 9.4 | Bernoulli's principle, Torricelli's law, dynamic lift |
| 9.5 | Viscosity, Stokes' law, terminal velocity |
| 9.6 | Surface tension, surface energy, angle of contact, drops, bubbles, capillary rise |
Not in the 2026-27 chapter
| Topic | Status |
|---|---|
| Archimedes' principle | Zero occurrences in the chapter, and CBSE does not list it here |
| Venturi-meter | Zero occurrences, and not listed — CBSE names only Torricelli's law and dynamic lift as Bernoulli applications |
| Reynolds number | Zero occurrences — but see the warning below |
The Reynolds number one needs care. CBSE's Unit VII entry for this chapter lists critical velocity. The chapter mentions the idea once, calling it critical speed — "beyond a limiting value, called critical speed, this flow loses steadiness and becomes turbulent" — but gives no formula and no Reynolds number, which is what older editions used to define it with.
So you can be asked about critical velocity, and the book will give you the concept without the arithmetic. Worse, Exercise 9.13 asks you to check whether a flow is laminar, which cannot be done without the Reynolds number. Section 8 below supplies it.
2. What makes a fluid different from a solid
The sharpest way to put it is a comparison Exercise 9.3 draws out:
| Solid | Fluid | |
|---|---|---|
| Shearing stress is proportional to | shear strain | rate of shear strain |
| Resists | being deformed | the speed of the deformation |
| Sustains a shear indefinitely? | Yes | No — it just keeps flowing |
Push sideways on a block of rubber and it settles at a new shape and stays there. Push sideways on water and it does not settle anywhere — it keeps moving for as long as you push. That is the whole definition of a fluid, and it is why a fluid has a viscosity rather than a shear modulus.
3. Pressure in a fluid at rest
Pressure is a scalar, and this gets asked directly. Force is a vector and area has an orientation, so the ratio looks as though it should have a direction. But in a fluid at rest the pressure at a point is the same in every direction — turn a tiny test surface any way you like and the force per unit area is unchanged. A quantity with no preferred direction cannot be a vector.
Pascal's law
Blaise Pascal observed that the pressure in a fluid at rest is the same at all points at the same height. Everything in this section follows from it.
How pressure varies with depth
The extra term is just the weight of the fluid column above you, spread over its area.
Two consequences worth carrying:
- Blood pressure is higher at your feet than at your brain, by roughly over the 1.5 m between them.
- Pressure depends on depth, not on the shape of the vessel. A narrow tube and a wide tank filled to the same level have the same pressure at the bottom.
Absolute against gauge pressure
| Term | Meaning |
|---|---|
| Absolute pressure | The total, |
| Gauge pressure | The excess over atmospheric, — what a tyre gauge reads |
Where students go wrong: in Bernoulli's equation it makes no difference which you use, because the constant atmospheric term appears on both sides and cancels. But you must use the same one at every point. Mixing them leaves an uncancelled Pa in the working. Exercise 9.12 is exactly this question.
Why the atmosphere thins so fast
Atmospheric pressure halves in about the first 6 km, even though the atmosphere is over 100 km deep. This is not gravity weakening — over 6 km that change is negligible.
It is because air is compressible while a liquid is not. The lower layers are squeezed by the weight above them, so most of the atmosphere's mass sits close to the ground. Pressure counts the weight above you, not the height above you.
Torricelli's barometer
Evangelista Torricelli (1608-1647) devised the first method of measuring atmospheric pressure. A long tube closed at one end is filled with mercury and inverted into a trough. The space above the column contains only mercury vapour, at negligible pressure, so:
which gives the familiar 0.76 m of mercury.
Why mercury, and not something cheaper? Since , the height needed is inversely proportional to density. Pascal repeated the experiment with wine at 984 kg m⁻³ and needed a column over 10 metres tall — that is Exercise 9.6. The densest convenient liquid gives the shortest, most practical instrument.
4. Pascal's law at work: hydraulic machines
Apply pressure to an enclosed fluid and it is transmitted undiminished to every part of the fluid and to the walls of the container.
Put a small piston of area and a large one of area into the same closed fluid. The pressure is the same at both, so:
Say this precisely, because the exam wants the distinction: the pressure is transmitted unchanged; the force is multiplied, by the ratio of the areas. A hydraulic lift is not a way of getting free energy — the large piston moves through a correspondingly smaller distance.
| Application | How it uses the law |
|---|---|
| Hydraulic lift | A small force on a small piston raises a car on a large one |
| Hydraulic brakes | One pedal force is transmitted equally to all four wheel cylinders, so the braking is even |
5. Streamline flow and continuity
Streamline (steady) flow means the velocity at any fixed point does not change with time. Every particle passing through a given point follows the same path — the streamline.
Turbulent flow is the opposite: irregular, eddying, with the velocity at a point changing constantly. The chapter's example is a fast stream hitting rocks, forming white-water rapids.
Between them lies the critical speed — "beyond a limiting value, called critical speed, this flow loses steadiness and becomes turbulent."
The equation of continuity
This is conservation of mass, nothing more. Whatever volume enters one end per second must leave the other end per second, so a narrower pipe forces a higher speed.
Keep this separate from Bernoulli. Continuity tells you the fluid speeds up at a constriction; Bernoulli then tells you the pressure there drops. Exercise 9.3(d) turns on exactly this division of labour — the speeding-up follows from conservation of mass, not from Bernoulli.
Partly block a tap with your fingers and the water jets out fast for the same reason: you cut , so must rise.
6. Bernoulli's principle
For steady, streamline, non-viscous, incompressible flow:
It is conservation of energy per unit volume — a pressure term, a kinetic term and a potential term.
Those four assumptions are examinable. Exercise 9.11 asks whether Bernoulli applies to a river rapid, and the answer is no: a rapid is turbulent and unsteady, and it dissipates energy as heat and sound, so the total is not conserved along the path.
Torricelli's law — speed of efflux
For a liquid escaping through a small hole a depth below the surface:
That is exactly the speed of a body dropped from height . The liquid behaves as though it had simply fallen that far, which is a memorable way to hold the result.
Dynamic lift
The air moves faster over the curved upper surface of an aerofoil than under it. By Bernoulli, faster means lower pressure, so the higher pressure underneath pushes the wing up.
The spinning ball is the same idea. A spinning cricket ball drags air around with it — on one side that dragged air adds to the airflow and on the other it opposes it. Unequal speeds mean unequal pressures, so there is a sideways force, and the ball swerves off its parabola. This is the Magnus effect.
And blowing over a sheet of paper lifts it for the same reason: fast air above, ordinary still air below, so the pressure underneath wins.
7. Viscosity
Viscosity is internal friction in a fluid — the resistance of one layer sliding over the next. For a fluid,
where is the coefficient of viscosity, measured in Pa s.
Temperature does opposite things to liquids and gases
| Mechanism | Effect of heating | |
|---|---|---|
| Liquids | Intermolecular attraction between layers | Viscosity decreases |
| Gases | Molecules crossing between layers, carrying momentum | Viscosity increases |
This reversal is a favourite one-mark question. Heating a liquid weakens the bonds that resist sliding. Heating a gas makes its molecules dart between layers faster, transferring more momentum, so the resistance goes up.
Poiseuille's equation
For steady laminar flow through a narrow tube:
Look at that fourth power. Halving the radius cuts the flow to one sixteenth. This is why the needle size of a syringe controls the flow rate far more effectively than the doctor's thumb pressure — a point Exercise 9.4(c) makes directly.
8. Stokes' law, terminal velocity, and the missing Reynolds number
Stokes' law
A sphere of radius moving at speed through a fluid of viscosity feels a retarding force:
Terminal velocity
As the sphere accelerates, the drag grows until it balances the weight minus the upthrust. After that the sphere falls at constant speed:
where is the sphere's density and the fluid's.
Read what it depends on: terminal velocity goes as the square of the radius and inversely as the viscosity. Double the radius and the sphere falls four times faster; double the viscosity and it falls half as fast.
The Reynolds number, which the chapter no longer has
This is not in the 2026-27 chapter, but CBSE lists critical velocity and Exercise 9.13 asks you to check that a flow is laminar. Here is what you need:
| Value | Flow |
|---|---|
| Below about 1000 | Laminar |
| Above about 2000 | Turbulent |
It is a pure number with no units — a ratio of inertial to viscous forces.
It also answers Exercise 9.3(e): turbulence begins at a fixed Reynolds number, which depends on the product of speed and size. A wind-tunnel model is smaller than the real aircraft, so it must be tested at a greater speed to reach the same Reynolds number.
9. Surface tension
The molecules at a liquid's surface have neighbours below and beside them but not above, so they are pulled inward. Creating new surface therefore costs energy, and the liquid behaves as though its surface were an elastic skin under tension.
Two equivalent definitions, and both get used:
| As | Definition | Units |
|---|---|---|
| Surface tension | Force per unit length of a line in the surface | N m⁻¹ |
| Surface energy | Energy per unit area of surface | J m⁻² |
They are numerically identical, which is worth checking as a dimensional exercise.
Surface tension does not depend on the area of the surface. Both definitions are per-unit ratios, so making the surface bigger changes nothing. Exercise 9.18 turns entirely on this: three films of different heights and shapes but the same edge length all support the same weight.
And it falls as temperature rises, because faster molecules feel a weaker net inward pull.
Why a free drop is spherical
With no external force, surface tension acts to minimise surface area. For a given volume the sphere has the least possible surface area, so that is what a free drop becomes.
Excess pressure — get the factor right
This is the most error-prone corner of the chapter, because the number of surfaces changes.
| Case | Surfaces | Excess pressure |
|---|---|---|
| Liquid drop (e.g. mercury in air) | 1 | |
| Air bubble inside a liquid | 1 | |
| Soap bubble in air | 2 |
A soap bubble is the only one with two. It is a thin film with air on both sides, so it has an inner and an outer surface. A drop of liquid, or a bubble of air inside a liquid, has a single interface. Exercise 9.20 deliberately puts both cases in one question.
Notice is in the denominator: smaller bubbles have larger excess pressure. Connect a small bubble to a large one and the small one blows into the large one.
10. Angle of contact and capillary rise
Every liquid-solid pair has two competing forces:
- Cohesion — between liquid molecules
- Adhesion — between liquid and solid molecules
Which one wins decides everything.
| Water on glass | Mercury on glass | |
|---|---|---|
| Stronger force | Adhesion | Cohesion |
| Angle of contact | Acute | Obtuse |
| Behaviour | Spreads, wets the glass | Beads up, does not wet |
| In a capillary tube | Rises | Falls |
Detergents work by lowering the angle of contact. Water only penetrates the narrow gaps between fibres if it wets them, and wetting means a small angle of contact — which is what Exercise 9.2(d) is asking.
Capillary rise
The Latin capilla means hair — a hair-thin tube gives a very large rise.
The rise is inversely proportional to the radius, so halving the tube's bore doubles the height the liquid climbs. This is why sap reaches the top of tall trees, and why the hairs of a paintbrush draw together into a fine tip when wet.
If is obtuse, as for mercury, is negative and comes out negative — the liquid is depressed below the outside level rather than raised.
Summary
- A solid resists a shear strain; a fluid resists only the rate of shear strain, which is why fluids flow indefinitely under a steady push.
- Pressure is a scalar: at a point in a fluid at rest it is the same in every direction.
- Pascal's law — pressure in a fluid at rest is the same at all points at the same height.
- ; pressure depends on depth, never on the shape of the vessel.
- Gauge pressure is the excess over atmospheric. Either convention works in Bernoulli, provided it is used at every point.
- The atmosphere halves in 6 km because air is compressible, not because gravity weakens.
- Torricelli's barometer gives ; mercury is used because a lighter liquid needs an impractically tall column.
- In a hydraulic machine the pressure is transmitted undiminished and the force is multiplied by the area ratio.
- Continuity, constant, is conservation of mass — it, not Bernoulli, is what makes fluid speed up at a constriction.
- Bernoulli: constant, valid only for steady, streamline, non-viscous, incompressible flow.
- Torricelli's law: — the same speed as a body dropped through .
- Dynamic lift, the Magnus effect on a spinning ball, and paper rising when you blow over it are all the same Bernoulli argument.
- Heating decreases the viscosity of a liquid but increases that of a gas — different mechanisms entirely.
- Poiseuille's flow rate goes as , which is why needle size beats thumb pressure.
- Stokes' law gives — terminal velocity goes as the square of the radius.
- Reynolds number is absent from the 2026-27 chapter but CBSE lists critical velocity and Exercise 9.13 needs it: , laminar below ~1000.
- Surface tension is force per unit length and equals surface energy per unit area. It is independent of the area and decreases with temperature.
- Excess pressure is for a drop or a submerged air bubble, but for a soap bubble, which has two surfaces.
- Adhesion beating cohesion gives an acute contact angle and wetting; cohesion winning gives an obtuse angle and beading.
- Capillary rise — inversely proportional to the tube radius, and negative for mercury.
- Archimedes' principle and the Venturi-meter are in neither the 2026-27 chapter nor the syllabus for it.
