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Stream functions in three-dimensional groundwater flow

, : Stream functions in three-dimensional groundwater flow. Water Resources Research 29(9): 3125-3133

In this paper, two partial differential equations of stream functions chi and lambda in three-dimensional groundwater flow are developed. It is assumed that the curl of pseudopotential gradient ( Delta x Delta beta ) is equal to zero. Pseudopotential gradient is the hydraulic gradient in the direction of flow. The equations of chi and lambda are expressed in terms of pseudopotential conductivity. Pseudopotential conductivity is the hydraulic conductivity in the direction of flow.


DOI: 10.1029/93wr01199

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