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Hydraulic gradient

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Hydraulic gradient

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It is ratio of height to length ie., h/L.

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FS= critical hydraulic gradient/exist hydraulic gradient

icr=(saturated unit wt - water unit wt)/water unit wt

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Saturated hydraulic conductivity is a quantitative measure of a saturated soil's ability to transmit water when subjected to a hydraulic gradient. It can be thought of as the ease with which pores of a saturated soil permit water movement.

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  1. hydraulic energy
  2. solar energy
  3. wind energy
  4. biomass energy
  5. geothermal energy
  6. ocean thermal gradient energy
  7. tide energy
  8. ....
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