Calculator · Fluid Mechanics

Manometer Calculator

A manometer reading is a walk: start at a known pressure, then move through each fluid in turn, adding ρgΔh whenever you go down and subtracting it whenever you go up. Build the path your instrument actually follows, in order, from the first tap to the second.

Starting pressure

Gauge pressure is measured relative to the ambient pressure, so 0 kPa means ambient. It may legitimately be negative. No atmospheric pressure is added anywhere in this calculation.

Path steps, in order

Step 1

Step 2

Results

Pressure difference along the path

-123.034 kPa

End pressure -123.034 kPa gauge, from a start of 0 Pa.

Pressure after each step of the manometer path
StepFluid ρMoveΔp = ±ρgΔhPressure after step
11000 kg/m³down 1 m9.80665 kPa9.80665 kPa
213546 kg/m³up 1 m-132.841 kPa-123.034 kPa

Assumptions

  • · Each column is a static fluid of constant density.
  • · Every pressure in the walk shares the reference kind of the starting pressure.

Path schematic

Schematic of the path only — the order and direction of the moves, not a scale drawing of a specific manometer. Every pressure is in the table above.schematic path — not a scale drawing of a specific manometer12p₁p₂

Schematic of the path only — the order and direction of the moves, not a scale drawing of a specific manometer. Every pressure is in the table above.

Explore in the Lab

Open this path in the Hydrostatics Lab

The same ordered path, next to the pressure field it belongs to.

Technical reference

p_end = p_start + Σ ±ρᵢ g Δhᵢ

going down: Δp = +ρ g Δh

going up: Δp = −ρ g Δh

p_start
known pressure at the first tap[Pa]
ρᵢ
density of the fluid in step i[kg/m³]
Δhᵢ
vertical distance travelled in step i[m]
p_end
pressure at the far end of the path[Pa]

Only the vertical distance matters. A horizontal run inside one fluid changes nothing, which is why the path is entered as vertical moves rather than as tube lengths.

The step order is the order you physically travel. Reversing the path reverses the sign of the total.

Each step carries the density of the fluid actually in that leg. A mercury leg in a water system is a separate step with the mercury density.

The result is stated in whatever reference the starting pressure was: a walk changes pressure, never the reference it is measured against.

This is a general pressure walk, not a model of one particular instrument. A U-tube, an inclined tube and a differential manometer are all just different sequences of these steps.

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