1994
DOI: 10.3133/wri934020
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Nonlinear-regression flow model of the Gulf Coast aquifer systems in the south-central United States

Abstract: Function, depth (48, 95). Base of Naperian logarithms, 2.71828 (46). Expectation of Y (40). Acceleration due to gravity (18). Pressure head (18). Water table altitude (37) Head triggering value for subsidence (54). Intrinsic permeability tensor (18). Number of observations (40). Number of parameters (46). Number of point observations of head used to formulate pressure head (56). Specific discharge (18). Radius (56). Aquifer layer (61). Time. Number expressing departure from ideal situation (63). Variance (76).… Show more

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