Hman = Hgeo + Δp/(ρ·g) + Hv
Besides the plain height difference, the pump must also overcome any pressure difference between source and destination vessel and all flow losses.
Besides the plain height difference, the pump must also overcome any pressure difference between source and destination vessel and all flow losses.
Select a target and calculate.
Besides the plain height difference, the pump must also overcome any pressure difference between source and destination vessel and all flow losses.
Hgeo=10 m, Δp=0.5 bar, ρ=1,000 kg/m³ and Hv=2 m give Hman=10+5.10+2≈17.10 m.
Steady operation at constant flow rate; Hv must already come from a separate pipeline-loss calculation and is not determined here itself.
This calculator determines the total head a pump must actually deliver between two vessels, complementing the existing NPSH calculation (suction-side cavitation reserve) with the discharge side of the system.
Manometric total head has three components: geodetic lift Hgeo, any pressure difference between the vessels Δp/(ρg), and the sum of all pipeline losses Hv: Hman=Hgeo+Δp/(ρg)+Hv.
Hman = Hgeo + Δp/(ρ·g) + Hv
Hman = Hgeo + Δp/(ρ·g) + Hv| Symbol / input | Meaning |
|---|---|
| Manometric total head Hman | Total head the pump must deliver overall. |
| Geodetic lift Hgeo | Height difference between the liquid level in the source and destination vessel. |
| Pressure difference between vessels Δp | Difference between the pressures acting on the liquid surfaces, e.g. for a pressurised destination vessel. |
| Fluid density ρ | Density of the pumped liquid. |
| Gravitational acceleration g | Local gravitational acceleration, about 9.81 m/s² near sea level. |
| Pipeline loss head Hv | Sum of all friction and minor loss heads in the suction and discharge piping. |
Hgeo is the height difference between liquid levels, Δp the pressure difference between the vessel interiors, ρ fluid density, g gravitational acceleration, and Hv the already-computed sum of pipeline losses.
Take Hgeo from the system drawing, Δp from vessel pressures (0 if both are open), and derive Hv from a separate pipeline-loss calculation (e.g. Darcy-Weisbach).
Hgeo=10 m, Δp=0.5 bar, ρ=1,000 kg/m³ and Hv=2 m give Hman=10+5.10+2≈17.10 m.
The pump must deliver at least Hman at the required flow rate at its best-efficiency point; an undersized pump will not reach the required flow rate.
Hgeo, Hv and Hman are lengths (heads), Δp a pressure, ρ a density, g an acceleration.
Selecting a pump from its performance curve, a basis for determining specific speed, and plausibility-checking existing systems.
Steady operation at constant flow rate; the velocity-head term (vII²−vI²)/(2g) of Dubbel Eq. (6) is dropped because still vessel surfaces are assumed. Hv must already come from a separate calculation. Start-up transients, pressure surges and time-varying vessel levels are excluded.
Common mistake: Do not forget Hv or confuse it with geodetic lift; omitting the loss head underestimates the pump power actually required.
Selecting a pump from its performance curve, a basis for determining specific speed, and plausibility-checking existing systems.
Hgeo is the height difference between liquid levels, Δp the pressure difference between the vessel interiors, ρ fluid density, g gravitational acceleration, and Hv the already-computed sum of pipeline losses.
Steady operation at constant flow rate; the velocity-head term (vII²−vI²)/(2g) of Dubbel Eq. (6) is dropped because still vessel surfaces are assumed. Hv must already come from a separate calculation. Start-up transients, pressure surges and time-varying vessel levels are excluded.