The excess water pressure in the ocean at a depth of h = 300 m is 31.5•105 Pa. It is required to determine: the density of sea water at this depth in general terms; density of sea water at this depth in the areas of the North Pole and the equator (gpol = 9.831 kg/m3, geq = 9.781 kg/m3).
Detailed solution. Format jpg
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