The shaded area's hydraulic conductivity differs from the unshaded area. Calculate hydraulic conductivity of the shaded area and the specific discharge through the aquifer.

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 shaded area's hydraulic conductivity differs from the unshaded area. Calculate hydraulic conductivity of the shaded area and the specific discharge through the aquifer.
Constant head 100 ft
Scale: 1 inch = 50 feet
Note: Steady State
104.
108
112
116
20
124.
132
136-
140
144.
Constant head 150ft
1) The shaded area hydraulic conductivity differs from the unshaded area. Calculate hydraulic
conductivity of the shaded area and the specific discharge through the aquifer.
'hydraulic conductivity of the unshaded region = 3 x 10^-3
Transcribed Image Text:Constant head 100 ft Scale: 1 inch = 50 feet Note: Steady State 104. 108 112 116 20 124. 132 136- 140 144. Constant head 150ft 1) The shaded area hydraulic conductivity differs from the unshaded area. Calculate hydraulic conductivity of the shaded area and the specific discharge through the aquifer. 'hydraulic conductivity of the unshaded region = 3 x 10^-3
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