Point A is 500 m away from river B. Water table at A is 30 m deep to the impervious base and at river B is 25 m deep to
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Point A is 500 m away from river B. Water table at A is 30 m deep to the impervious base and at river B is 25 m deep to
Point A is 500 m away from river B. Water table at A is 30 m deep to the impervious base and at river B is 25 m deep to the impervious base. Hydraulic conductivity is 0.7 m/day. Use Dupuit Approximation to calculate the groundwater flow between A and B (in m</day).
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