fluid flow
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principles of physical scienceDissectionā¦the differential equations that describe fluid motion (see fluid mechanics).
Read Moreā¦the differential equations that describe fluid motion (see fluid mechanics).
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principles of physical scienceNonconservative fieldsā¦in the mathematical description of fluid motion, in which the local velocity v(r) of fluid particles constitutes a field to which the notions of divergence and curl are naturally applicable.
Read Moreā¦in the mathematical description of fluid motion, in which the local velocity v(r) of fluid particles constitutes a field to which the notions of divergence and curl are naturally applicable.
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Congo RiverHydrology of the Congo RiverThe Congo has a regular flow, which is fed by rains throughout the year. At Kinshasa the flow has for many years remained between the high level of 2,310,000 cubic feet (65,000 cubic meters) per second, recorded during the flood of 1908, and the low level of 756,000 cubic feetā¦
Read MoreThe Congo has a regular flow, which is fed by rains throughout the year. At Kinshasa the flow has for many years remained between the high level of 2,310,000 cubic feet (65,000 cubic meters) per second, recorded during the flood of 1908, and the low level of 756,000 cubic feetā¦
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glacierFlow of the ice sheetsFlow rates in the interior of an ice sheet are very low, being measured in centimetres or metres per year, because the surface slope is minuscule and the ice is very cold. As the ice moves outward, the rate of flow increases to a fewā¦
Read MoreFlow rates in the interior of an ice sheet are very low, being measured in centimetres or metres per year, because the surface slope is minuscule and the ice is very cold. As the ice moves outward, the rate of flow increases to a fewā¦
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glacierFlow of mountain glaciersThese glaciers generally flow at rates of 0.1 to 2 metres per day, faster at the surface than at depth, faster in midchannel than along the margins, and usually fastest at or just below the equilibrium line. Cold, polar glaciers flow relatively slowly, because the constitutive law ofā¦
Read MoreThese glaciers generally flow at rates of 0.1 to 2 metres per day, faster at the surface than at depth, faster in midchannel than along the margins, and usually fastest at or just below the equilibrium line. Cold, polar glaciers flow relatively slowly, because the constitutive law ofā¦
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