8.4 Fluids and Conservation Laws
- Syllabus
- 2024
- Topic
- 8.4
- Level
- —
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.