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Determine in brief about the soil texture
The texture is generally determined by the relative proportions of sand, silt and clay. If various size fractions of the particles could be isolated and their relative proportion determined the soil texture can be defined. Following methods are generally used for the purpose of determining the relative proportion of the particles in a soil sample.
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If the Quabbin Reservoir Watershed is 100 km2, the average precipitation in New England is 130 cm/year, and the volume of the reservoir is 1.5 x 1012 liters, what is the residence
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