Hyder et al. (KGS Model) Slug Test Solution for Confined and Unconfined Aquifers
Description
A mathematical solution by Hyder et al. (1994) is useful for determining the hydraulic
conductivity of unconfined and confined aquifers. Analysis
involves matching a type curve solution to water-level displacement data collected during
a slug test.
AQTESOLV provides
visual and automatic methods for matching the KGS Slug Test Model to slug 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 KGS Slug Test Model:
aquifer has infinite areal extent
aquifer is homogeneous and of uniform thickness
aquifer potentiometric surface is initially horizontal
test well is fully or partially penetrating
a volume of water, V, is injected or discharged from the well instantaneously
aquifer is confined or unconfined
flow is unsteady
Solution Options
AQTESOLV provides the following options for the KGS Slug
Test Model:
partially penetrating wells
hydraulic conductivity anisotropy
wellbore skin effect
observation wells
Benchmark
Comparison of AQTESOLV
(blue line) and computer program available from KGS (symbols) for a slug
test in a confined aquifer.
References
Hyder, Z, J.J. Butler, Jr., C.D. McElwee and W. Liu, 1994. Slug tests in partially
penetrating wells, Water Resources Research, vol. 30, no. 11, pp. 2945-2957.