8 Fluids
- Syllabus
- 2024
- Section
- 8
- Level
- —

A fluid is a substance with no fixed shape, so it flows and takes the shape allowed by its container. Both liquids and gases are fluids; a solid retains a fixed shape.
| State | Particle interaction and arrangement | Shape behavior |
|---|---|---|
| Solid | Strong enough to maintain an organized structure | Fixed shape |
| Liquid | Particles remain close but rearrange | No fixed shape; nearly fixed volume |
| Gas | Particles are widely separated and interact weakly except during collisions | No fixed shape; expands to fill available volume |
ρ=Vm
Example: a fluid sample has mass 1.20kg and volume 5.00×10−4m3.
ρ=5.00×10−41.20=2.40×103kgm−3.
Density is mass per unit volume; doubling both mass and volume leaves the density unchanged.
An ideal fluid is modeled as incompressible, so its density does not change, and as having no viscosity, so there is no internal resistance to flow.
Ideal-fluid assumptions simplify later pressure and flow models. They are not claims that every real fluid is perfectly incompressible or frictionless; check whether the model is appropriate for the situation.
Pressure measures how much force acts perpendicular to each unit of surface area. Pressure is a scalar: it has magnitude but no direction.
P=AF⊥
| Quantity | Use in the equation | SI unit |
|---|---|---|
| F⊥ | Component of force perpendicular to the surface | newton (N) |
| A | Area over which that force acts | square metre (m2) |
| P | Perpendicular force per unit area | pascal (Pa=N/m2) |
Example: a perpendicular force of 600N acts over 0.030m2.
P=AF⊥=0.030600=2.0×104Pa.
This value means each square metre would experience 2.0×104N of perpendicular force at the same pressure.
For the same perpendicular force, pressure is inversely proportional to contact area. Halving the area doubles the pressure; doubling the area halves it.
Use only the force component perpendicular to the surface, not the full magnitude of an angled force. In an incompressible-fluid model, changing pressure does not change the fluid's density or volume.
A fluid exerts pressure on a surface through the collective interactions of many fluid particles with that surface. At rest, greater depth means more fluid above the point and therefore greater pressure.
Pgauge=ρgh
P=P0+Pgauge=P0+ρgh
| Location | Gauge pressure | Absolute pressure |
|---|---|---|
| Reference surface, h=0 | 0 | P0 |
| Vertical depth h | ρgh | P0+ρgh |
Here ρ is fluid density, g is gravitational field strength, h is vertical depth below the reference surface, and P0 is the pressure at that surface.
Example: water has ρ=1000kg m−3. At h=2.0m, with g=9.8N kg−1 and surface pressure P0=1.01×105Pa:
Pgauge=(1000)(9.8)(2.0)=1.96×104Pa
P=1.01×105+1.96×104=1.206×105Pa≈1.21×105Pa.
Gauge pressure excludes the reference pressure; absolute pressure includes it. Use vertical depth, not the distance traveled through the fluid. In the same fluid at rest, points at the same depth have the same pressure regardless of container shape.
A fluid system changes its velocity when a net external force changes its momentum. For a constant-mass fluid parcel, a nonzero net force produces acceleration.
∑Fexternal=dtdp=ma
| Interaction | Role for the chosen fluid system |
|---|---|
| Collisions and forces between particles inside the fluid | Internal: transfer momentum between parts of the fluid |
| Gravity, a container wall, a piston, or another object acting on the fluid | External: can change the total momentum of the fluid system |
Microscopic particle interactions transmit forces through the fluid. Together with external forces, these interactions create the macroscopic patterns we observe, such as acceleration or changing flow speed.
Example: model a 2.0kg parcel of fluid as having constant mass. If the net external force is 6.0N to the right,
a=mFnet=2.06.0=3.0m s−2 to the right.
Its velocity therefore changes by 3.0m s−1 each second while that net force acts.
Internal forces do not vanish: they redistribute momentum within the fluid. But for the whole chosen system, internal force pairs cannot by themselves change total momentum; identify the system boundary before deciding which forces are external.
The buoyant force is the net upward force that a fluid exerts on an object. It is the combined result of forces from many fluid particles over the object’s surface.
Fluid pressure is greater on the deeper parts of the object than on the shallower parts. When all the distributed fluid forces are combined, their vertical components produce a net upward force.
FB=ρfluidVdisplacedg
| Quantity | Meaning | SI unit |
|---|---|---|
| ρfluid | Density of the fluid, not the object | kg m−3 |
| Vdisplaced | Volume of fluid displaced by the submerged part | m3 |
| FB | Weight of that displaced fluid | N |
Example: an object displaces 0.020m3 of water with ρ=1000kg m−3. Using g=9.8N kg−1,
FB=(1000)(0.020)(9.8)=196N upward.
This equals the weight of the displaced water.
Buoyant force is upward, but an object does not necessarily accelerate upward. Compare FB with the object’s weight: greater buoyant force gives upward acceleration, equal forces give zero vertical acceleration, and smaller buoyant force gives downward acceleration. Use only the displaced volume—not automatically the object’s full volume.
A pressure difference between two locations can drive fluid flow. In a completely filled tube carrying steady incompressible flow, matter cannot accumulate, so the rate entering equals the rate leaving.
tV=Av
| Quantity | Meaning | SI unit |
|---|---|---|
| V/t | Volume flow rate through a cross section | m3s−1 |
| A | Cross-sectional area perpendicular to the flow | m2 |
| v | Average fluid speed through that cross section | m s−1 |
A1v1=A2v2
For an incompressible fluid, density is constant. Equal mass flow rates therefore mean equal volume flow rates: A1v1=A2v2. A smaller cross-sectional area requires a greater speed to carry the same volume each second.
Example: water moves at 2.0m s−1 through area A1=6.0cm2 and enters a section with A2=3.0cm2.
v2=A2A1v1=3.0(6.0)(2.0)=4.0m s−1.
The area halves, so the speed doubles; the volume flow rate is unchanged.
Continuity does not say pressure stays constant. It conserves mass flow. The simplified form A1v1=A2v2 requires incompressible flow; if density changes, conserve ρAv instead.
In ideal fluid flow, pressure, kinetic, and gravitational energy can change between two locations while their total mechanical energy is conserved.
P1+ρgy1+21ρv12=P2+ρgy2+21ρv22
| Bernoulli term | Energy represented per unit volume |
|---|---|
| P | Pressure energy |
| ρgy | Gravitational potential energy |
| 21ρv2 | Kinetic energy |
Compare the same three terms at locations 1 and 2. At equal height, a larger kinetic term must be balanced by a smaller pressure term. When height changes, keep all three terms.
v=2gΔy
Torricelli example: a small opening is 1.25m below the liquid surface. The surface and opening are both exposed to the same pressure, and the wide surface moves negligibly. Bernoulli’s equation reduces to
ρgΔy=21ρv2, so v=2gΔy.
v=2(9.8)(1.25)=4.95m s−1≈5.0m s−1.
Do not use ‘faster means lower pressure’ without checking height and Bernoulli’s assumptions. Unless stated otherwise here, treat the fluid as ideal and the pipe as completely filled. In Torricelli’s theorem, Δy is the vertical height difference, not the path length.