Abstract
The Gram-Schmidt orthonormalization procedure is presented as a numerical method easily adaptable to digital computation for the soltuion to steady-state ground-water flow problems. The advantages of this method are: (i) A series solution is attined and (ii) arbitrary shaped aquifers with arbitrary boundary conditions can be handled. The method is illustrated by application to a well flow problem in a confined acquifer
| Original language | English |
|---|---|
| Pages (from-to) | 285-292 |
| Number of pages | 8 |
| Journal | ASCE J Hydraul Div |
| Volume | 99 |
| Issue number | HY2 973) |
| State | Published - 1973 |
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