Dupuit-Forchheimer assumptions are used for analyzing groundwater flow in
(A) confined aquifers
(B) leaky confined aquifers
(C) unconfined aquifers
(D) both confined and unconfined aquifers

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Dupuit-Forchheimer assumptions are used for analyzing groundwater flow in
(A) confined aquifers
(B) leaky confined aquifers
(C) unconfined aquifers
(D) both confined and unconfined aquifers