Explain a pressure decrease with kinetic, height and loss terms
Bernoulli’s ideal relation is an energy account along a streamline for steady incompressible flow with negligible dissipation. Each term p, ρv²/2 and ρgz has units J/m³, equivalent to Pa. Pressure work can become kinetic or gravitational energy; pressure itself is not a complete energy budget.
Learning outcome: Vary elevation while holding loss fixed, then vary loss at one elevation. Close the four-term power budget and distinguish reversible height or speed changes from the specified irreversible loss.
Starting recap
Declare density, pressure reference, flow regime and admissible force constraints. Convert area and volume units before balancing forces, mass or energy.
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With zero elevation and zero loss, outlet gauge pressure is 28500 Pa. At unchanged flow, adding 2500 Pa loss lowers that pressure by 2500 Pa and converts 5 W of mechanical power.
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Multiplying a pressure drop by volume flow gives:
Experiment
Vary elevation while holding loss fixed, then vary loss at one elevation. Close the four-term power budget and distinguish reversible height or speed changes from the specified irreversible loss.
Distinguish pressure conversion from irreversible flow loss
Worked teaching model · synthetic values · Steady incompressible water, rho=1000, g=10, Q=.002 m³/s; inlet/outlet areas .002/.001 m². Inlet gauge pressure 30000 Pa, atmospheric 100000 Pa. Uniform section speeds, no pump, specified nonnegative mechanical loss. No cavitation or real installation claim.
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Outlet pressure at prescribed loss
Unlike graph quantities rescale independently; read units and values, not screen angles. 1: extended Bernoulli ledger (solid). Joined curves show the supplied model, not additional observations.
Equivalent numerical coordinates for Outlet pressure at prescribed loss
extended Bernoulli ledger
| outlet elevation (m) | outlet gauge pressure (Pa) |
|---|---|
| 0 | 23500 |
| 0.05 | 23000 |
| 0.1 | 22500 |
| 0.15 | 22000 |
| 0.2 | 21500 |
| 0.25 | 21000 |
| 0.3 | 20500 |
| 0.35 | 20000 |
| 0.4 | 19500 |
| 0.45 | 19000 |
| 0.5 | 18500 |
| 0.55 | 18000 |
| 0.6 | 17500 |
| 0.65 | 17000 |
| 0.7 | 16500 |
| 0.75 | 16000 |
| 0.8 | 15500 |
| 0.85 | 15000 |
| 0.9 | 14500 |
| 0.95 | 14000 |
| 1 | 13500 |
| 1.05 | 13000 |
| 1.1 | 12500 |
| 1.15 | 12000 |
| 1.2 | 11500 |
| 1.25 | 11000 |
| 1.3 | 10500 |
| 1.35 | 10000 |
| 1.4 | 9500 |
| 1.45 | 9000 |
| 1.5 | 8500 |
| 1.55 | 8000 |
| 1.6 | 7500 |
| 1.65 | 7000 |
| 1.7 | 6500 |
| 1.75 | 6000 |
| 1.8 | 5500 |
| 1.85 | 5000 |
| 1.9 | 4500 |
| 1.95 | 4000 |
| 2 | 3500 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
| Quantity | Value | Unit |
|---|---|---|
| Inlet mean speed | 1 | m/s |
| Outlet mean speed | 2 | m/s |
| Outlet gauge pressure | 13500 | Pa |
| Outlet absolute pressure | 113500 | Pa |
| Mechanical loss power | 10 | W |
| Elevation energy flux increase | 20 | W |
| Kinetic energy flux increase | 3 | W |
| Pressure-work flux decrease | 33 | W |
A pressure-work decrease supplies kinetic and height increases plus the prescribed loss.
p1+rho v1²/2+rho g z1=p2+rho v2²/2+rho g z2+loss. Every term is energy per volume, with Pa units; multiply by Q for power. A negative gauge pressure can still have positive absolute pressure. The specified loss is not predicted from an ideal Bernoulli equation, and pressure alone does not certify a real flow regime.
Predict before inspecting the values. Save contrasting records with assumptions and one alternative explanation. This virtual display does not certify practical measurement technique.
A pressure-work decrease supplies kinetic and height increases plus the prescribed loss.
p1+rho v1²/2+rho g z1=p2+rho v2²/2+rho g z2+loss. Every term is energy per volume, with Pa units; multiply by Q for power. A negative gauge pressure can still have positive absolute pressure. The specified loss is not predicted from an ideal Bernoulli equation, and pressure alone does not certify a real flow regime.
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Why can one not explain every low pressure merely by saying the fluid moves faster?
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