The theory of ground-water motion

[11] Lindquist E., 1933, 1 C GRANDS BARR, V5, P81

[12] Muskat M., 1937, FLOW HOMOGENEOUS FLU

[13] Nutting PG, 1930, AAPG B, V14, P1337

[14] PAIGE S, 1936, ECON GEOL, V31, P537

[15] PAIGE S, 1938, ECON GEOL, V33, P647

[16] SLICHTER CS, 1897, 19 US GEOL SURV 2, P295

[17] STEARNS ND, 1928, US GEOL SURV WATER F, V596, P121

[18] STRINGFIELD VT, 1935, T AM GEOPH UNION, P524

[19] Swinnerton A. C., 1932, GEOLOGICAL SOC AM B, V43, P663

[20] 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

[11] Lindquist E., 1933, 1 C GRANDS BARR, V5, P81

[12] Muskat M., 1937, FLOW HOMOGENEOUS FLU

[13] Nutting PG, 1930, AAPG B, V14, P1337

[14] PAIGE S, 1936, ECON GEOL, V31, P537

[15] PAIGE S, 1938, ECON GEOL, V33, P647

[16] SLICHTER CS, 1897, 19 US GEOL SURV 2, P295

[17] STEARNS ND, 1928, US GEOL SURV WATER F, V596, P121

[18] STRINGFIELD VT, 1935, T AM GEOPH UNION, P524

[19] Swinnerton A. C., 1932, GEOLOGICAL SOC AM B, V43, P663

[20] 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