Jacob-LohmanSolution for Constant-Head Tests in
Confined Aquifers
Description
A mathematical solution by Jacob and Lohman (1952) is useful for determining the hydraulic
properties (transmissivity and storativity) of confined aquifer. Analysis
involves matching the Jacob-Lohman solution to discharge data collected during a
constant-head test. AQTESOLV includes
type curve and
straight-line versions of the Jacob-Lohman solution.
AQTESOLV provides visual and automatic methods for
matching the Jacob-Lohman solution to constant-head test data. This easy-to-use and intuitive software
promotes rapid and accurate determination of aquifer properties.
Assumptions
The following assumptions apply to the use of the Jacob-Lohman solution:
aquifer has infinite areal extent
aquifer is homogeneous, isotropic and of uniform thickness
potentiometric surface is initially horizontal
aquifer is confined
flow is unsteady
wells are fully penetrating
water is released instantaneously from storage with decline of hydraulic head
Solution Options
AQTESOLV provides the following options for the
Jacob-Lohman solution:
recovery
Benchmark
Comparison of AQTESOLV
(blue line) and published data (symbols).
References
Jacob, C.E. and S.W. Lohman, 1952. Nonsteady flow to a well of constant
drawdown in an extensive aquifer, Trans. Am. Geophys. Union, vol. 33, pp.
559-569.