SECOND-ORDER THEORY OF FLOW IN 3-DIMENSIONAL DEFORMING MEDIA

[41] Theis C., 1938, ECON GEOL, V33, P889, DOI DOI 10.2113/GSECONGEO.33.8.889

[42] The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using ground water storage [J]. TRANSACTIONS-AMERICAN GEOPHYSICAL UNION, 1935, 16 : 519 - 524

[43] Verruijt A., 1969, FLOW POROUS MEDIA, P331

[44] FIELD AND LABORATORY DETERMINATION OF HYDRAULIC DIFFUSIVITY OF A CONFINING BED [J]. WATER RESOURCES RESEARCH, 1970, 6 (01) : 194 - &

[41] Theis C., 1938, ECON GEOL, V33, P889, DOI DOI 10.2113/GSECONGEO.33.8.889

[42] The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using ground water storage [J]. TRANSACTIONS-AMERICAN GEOPHYSICAL UNION, 1935, 16 : 519 - 524

[43] Verruijt A., 1969, FLOW POROUS MEDIA, P331

[44] FIELD AND LABORATORY DETERMINATION OF HYDRAULIC DIFFUSIVITY OF A CONFINING BED [J]. WATER RESOURCES RESEARCH, 1970, 6 (01) : 194 - &