The figure above (not to scale) shows a water-saturated 2 m (=a in figure)-deep clay layer within a sandy formation; the saturated clay layer carries 2 m (=b in figure) of unconfined groundwater on top. Below the clay layer is an unsaturated zone which exerts suction: the pF is 1 (= p in figure). The vertical hydraulic conductivity of the clay layer equals 0.001 m per day. Determine the vertical volume flux density in the water-saturated clay layer in mm per day. Give your answer to 1 decimal place.

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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The figure above (not to scale) shows a water-saturated 2 m (=a in figure)-deep clay layer within a sandy formation; the saturated clay layer carries 2 m (=b in figure) of unconfined groundwater on top. Below the clay layer is an unsaturated zone which exerts suction: the pF is 1 (= p in figure). The vertical hydraulic conductivity of the clay layer equals 0.001 m per day. Determine the vertical volume flux density in the water-saturated clay layer in mm per day. Give your answer to 1 decimal place.
Sand
clay
sand
[[b]m
alm
pF= [p]
Transcribed Image Text:Sand clay sand [[b]m alm pF= [p]
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