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Pressure increases by about one atmosphere (approximately 14.7 pounds per square inch at sea level) with each 10-metre increment in depth; thus, abyssal pressures range between 200 and 600 atmospheres.
Pressures range from about 30 pounds per square inch (200 kilopascals) for large, soft tires to approximately 100 pounds per square inch (700 kilopascals) for high-pressure, high-load applications.
The cooling of the Eurasian landmass in winter leads to the development of an intense high-pressure cell over the country's interior; mean January pressures range above 1,040 millibars along the southern boundary of Siberia, from which a ridge of high pressure runs westward along Russia's borders with Kazakhstan and Ukraine.
CH4 partial pressures range from 1.1 to 14.6 atm, and n-C4H10 partial pressures range from 0.02 to 1.8 atm.
The applied pressure in the feed channel reportedly reduces the osmotic backwash driving force even where feed pressures range from 5 to 10 bar.
Supply pressures range from 0.06 to 90 MPa, discharge diameters from 4 × 10−4 to 1.32 m, and flame heights from 0.08 to 110 m.
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Inflation pressures ranged from 6 to 15 atm [7].
High-temperature PEM fuel cells may safely operate at pressures ranging from 1.0 to 5.0 atm.
The obvious hysteresis loop can be observed at relative pressures ranging from 0.42 to 1.0.
Deformation experiments were carried out at room temperature at confining pressures (σ3) ranging between 25 and 65 MPa and pore pressures ranging between 25%and90%0% of σ3.
The corresponding measured static pressures ranged from 2 to 2550 Pa m−1.
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