A spreadsheet method of estimating best-fit hydraulic gradients using head data from multiple wells.
Hydraulic gradients from planar water tables, or piezometric surfaces, and horizontal flow regimes can be quickly and conveniently calculated from data sets involving numerous wells. The matrix-solving functions of a modem spreadsheet program (Excel) were used to determine the equation of a water-table plane, Ax + By + Cz - D = 0, and the equation coefficients were then used to determine the magnitude of the hydraulic gradient, according to gradient = square root of A2 + B2/C2, and its direction, according to alpha = arctan B/A, where alpha is the angle measured from the x-axis. A pre-prepared Excel file constructed to handle data from up to 20 wells at once is available for free downloading at www.geo.ku.edu/hydro/KUHydro.html.
Devlin
J F
JF
Geology Department, University of Kansas, 1475 Jayhawk Blvd., Lawrence, KS 66045, USA. jfdevlin@ku.edu
D005544:Forecasting; D008962:Models, Theoretical; D012987:Soil; D014872:Water Movements
D012987:Soil