A confined aquifer (permeable soil) is shown. This aquifer has a source of recharge located as shown. The hydraulic conductivity of the aquifer is 40 m/day with a porosity of 25%. The piezometric...


A confined aquifer (permeable soil) is shown. This aquifer has a source of recharge<br>located as shown. The hydraulic conductivity of the aquifer is 40 m/day with a porosity<br>of 25%. The piezometric (head) surface in the two observation wells 1200 m apart are at<br>elevations 65 m and 60 m, respectively from the common datum. The aquifer has an<br>average thickness of 25 m and an average width of 4 km.<br>Determine the value to the seepage velocity in m/day.<br>

Extracted text: A confined aquifer (permeable soil) is shown. This aquifer has a source of recharge located as shown. The hydraulic conductivity of the aquifer is 40 m/day with a porosity of 25%. The piezometric (head) surface in the two observation wells 1200 m apart are at elevations 65 m and 60 m, respectively from the common datum. The aquifer has an average thickness of 25 m and an average width of 4 km. Determine the value to the seepage velocity in m/day.
Recharge<br>El. 65 m<br>El. 60 m<br>Aquifer<br>25 m<br>1200 m<br>

Extracted text: Recharge El. 65 m El. 60 m Aquifer 25 m 1200 m

Jun 10, 2022
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