Abstract
Exact solutions are determined for two cases of two‐dimensional flow in aquifers with clay laminae. Approximate solutions are obtained by the use of the technique presented in part 1 of this paper and are compared with the exact ones. It appears that the agreement is good, provided that the ratio of aquifer length to aquifer thickness is sufficiently large.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 993-1004 |
| Number of pages | 12 |
| Journal | Water Resources Research |
| Volume | 17 |
| Issue number | 4 |
| DOIs | |
| State | Published - Aug 1981 |