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It operates on the principle of unequal water pressures.
That gives the team a chance to record sliding speeds, friction, viscosity under various water pressures, porosity of the sediments and such.
Casual divers typically go down no farther than about 100 feet, limiting the water pressures and lung contractions that they experience.
The fastest glaciers (other than those in the act of surging) are thick, temperate glaciers in which high subglacial water pressures produce high rates of sliding.
Normal temperate glaciers ending on land generally have subglacial water pressures in the range of 50 to 80 percent of the ice pressure, but glaciers that end in the sea may have subglacial water pressures almost equal to the ice pressure that is, they almost float.
Geogrid layers could decrease the development of excess pore water pressures and accelerate the dissipation of excess pore water pressures.
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The differences of pore-water pressures among each monitoring points decrease with the duration of rainfall.
The pore-water pressures changes at point T2 and T5 are the most remarkable.
Pore-water pressures increased with the increase in the rainfall duration.
The water table rose, and thus, the pore-water pressures distribution changed with time.
Vibrating wire (VW) piezometers are designed to measure fluid or pore-water pressures in a variety of geotechnical applications.
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