Follow the connected liquid
Height increases upward. Extra pressure on the left lowers that surface and raises the right. All heights are converted to metres.
IN04 · Pressure needs a reference
Do two liquid heights tell you an absolute pressure or a pressure difference? The liquid-height difference measures the pressure difference between the two surfaces. An open end supplies atmospheric pressure as the reference; an evacuated end supplies a nearly zero reference. Add the reference pressure to recover the unknown absolute pressure.
Connect the U-tube to air, a trapped gas or an ideal vacuum. Move the pressure dial and ruler datum, check the zero and infer pressure from saved height pairs.
Saved simulated heights
| No. | Left | Right | Zero | Head after zero |
|---|
An equal-pressure check measures the difference of the two reading offsets. The sealed pocket uses its recorded initial volume, initial absolute pressure and temperature. Its current volume follows from the measured head and liquid-volume conservation.
Static, incompressible liquid and ideal gas; both ports share a height. Liquid density and volume use a constant teaching expansion coefficient between ten and thirty-five degrees Celsius. The gas cell is prepared at twenty degrees each time it is connected; zero checking takes place before that connection. The vacuum reference has zero pressure and the model liquid has no vapour pressure. Gas weight, capillarity, tube expansion and dynamic sloshing are omitted. The height uncertainty includes reading scatter, ruler resolution and the saved zero-mean uncertainty; density, reference-pressure and material-model uncertainties remain separate. Tube widths are enlarged; vertical heights retain one scale.
Physics tutorial
BackgroundGas presses on both liquid surfaces. A deeper column supplies more pressure at the bottom, so unequal pushes settle at unequal heights.
Why it mattersA height becomes an absolute pressure only after you identify what pushes on the other side.
Start with the essentials
Height increases upward. Extra pressure on the left lowers that surface and raises the right. All heights are converted to metres.
The gas pocket was closed at a known initial pressure, volume and temperature. Kelvin temperatures and absolute pressures are required.
Both readings share a ruler datum. Equalizing the pressures measures only the difference of the reading offsets.
Typical misconceptionEqual liquid levels mean that neither surface is under pressure.
Better mental modelBoth surfaces can be pressed equally by the atmosphere. Their pressures cancel in the height difference, and the absolute pressure remains.
Drag the gold datum rail, then save another pair.
What to observe: Both raw ruler readings shift together. Their difference and the inferred pressure stay nearly the same, within rounding.Drag the gold hose plug from Air to Gas pocket.
What to observe: The right side compresses a gas pocket. The reference pushes back, so the same source pressure produces a smaller head.Choose A vacuum reference. Then change the liquid to Water-like liquid.
What to observe: The dense-liquid column fits the tube; the water column would need more than ten metres and cannot be saved in this apparatus.Change Differential reading offset, then choose Equalize & check zero and return to Positive gauge pressure.
What to observe: The new calibration changes later measurements. Earlier height pairs keep their original zero check.How physics instruments measure · Reading path
Articles on this path that use this experiment, followed by the other experiments they suggest.