Liquid pressure increases with depth. P = ρgh (density × gravity × depth).
Why do ears pop on planes?
Because atmospheric pressure decreases as altitude increases, creating a pressure difference between the inner ear and outside.
What is standard pressure?
Standard pressure is defined as 1 atm, 101.325 kPa, or 760 mmHg.
Background & Theory
Pressure is defined as normal force distributed over a surface: P = F / A. The force must act perpendicular to the surface, and the area is the contact area over which that force is spread. Because only magnitude matters at a given point, pressure is a scalar quantity even though force is a vector. The SI unit is the pascal (Pa), equal to one newton per square meter, which is a very small unit: a sheet of paper lying flat on a desk exerts roughly 1 Pa, while the atmosphere at sea level exerts 101,325 Pa. This calculator applies the definition directly, dividing the force you enter in newtons by the area you enter in square meters, so it assumes the load is uniformly distributed and acts at right angles to a flat surface.
Two distinctions matter when reading the result. First, absolute versus gauge pressure: a tire gauge reading 220,000 Pa means 220,000 Pa above the surrounding air, so the absolute pressure inside the tire is about 321,325 Pa. Second, static contact pressure versus fluid pressure: in a resting liquid the pressure at depth follows P = rho x g x h and acts equally in every direction, which is why the P = F / A form used here suits solids, punches, presses and contact loads rather than columns of water. The inverse relationship with area explains everyday behaviour, since snowshoes lower pressure by enlarging A while a sharpened blade or a stiletto heel raises it by shrinking A to a few square millimetres.
History
The measurement of pressure began with a puzzle about pumps: Italian well diggers could not lift water more than about ten metres, and no one could say why. In 1643 Evangelista Torricelli, working from Galileo's notes, inverted a sealed tube of mercury into an open dish and found the column settled at roughly 760 millimetres, concluding that the atmosphere itself was pressing down on the dish. Blaise Pascal extended the idea in 1648 by having his brother-in-law carry a Torricellian tube up the Puy de Dome in the Auvergne; the mercury column fell as altitude rose, confirming that air has weight. Pascal went on to state the principle that pressure applied to a confined fluid is transmitted undiminished throughout it, and Otto von Guericke dramatised the same forces in 1654 with the evacuated Magdeburg hemispheres that teams of horses could not pull apart.
Practical instruments followed much later. Eugene Bourdon patented his coiled flattened-tube gauge in 1849, and its descendants still sit on boilers, air compressors and scuba tanks today. Naming caught up last of all: the pascal was formally adopted as the SI unit of pressure by the General Conference on Weights and Measures in 1971. That late arrival is why so much older equipment is still marked in bar, atmospheres, torr, millimetres of mercury or pounds per square inch, and why unit conversion remains an unavoidable part of any pressure calculation.
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