141. For a clay slope of height of 10 m, the stability number is 0.05,7 = 2.0 t/m3, C = 2.5 t/m2, the critical height of the slope of the soil, is
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142. The compression resulting from a long term static load and consequent escape of pore water, is known as
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143. Compression of soil occurs rapidly if voids are filled ?with
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144. The compressibility of clays, is caused due to :
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145. The pressure that builds up in pore water due to load increment on the soil, is termed
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146. The reduction in volume of soil due to squeezing out of water from the voids, is termed
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147. A clay subjected to pressure in excess to its present over-burden, is said to be
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