Abstract
A confined isotropic aquifer comprises two or more horizontally adjacent zones with different hydraulic properties. The aquifer is of constant thickness. The pumping and observation wells are fully penetrating.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Bochever FM, Lapshin NN, Oradovskaya AE (1979) Design calculations for wellhead protection areas. Nedra, Moscow (In Russian)
Fenske PR (1984) Unsteady drawdown in the presence of a linear discontinuity. In: Rosenshein JS, Bennett GD (eds) Groundwater hydraulics. Water Resources Monograph Series 9. American Geophysical Union, Washington, pp 125–145
Maksimov VA (1962) On unsteady-state flow of elastic fluid to a well in heterogeneous media. J Appl Mech Tech Phys 3:109–112 (In Russian)
Pykhachov GB, Isayev RG (1973) Groundwater hydraulics. Nedra, Moscow (In Russian)
Shchelkachev VN, Lapuk BB (1949) Groundwater hydraulics. Gostoptehizdat, Moscow (In Russian)
Yeh HD, Yang SY, Peng HY (2003) A new closed-form solution for a radial two-layer drawdown equation for groundwater under constant-flux pumping in a finite-radius well. Adv Water Resour 26(7):747–757
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
Copyright information
© 2017 Springer International Publishing Switzerland
About this chapter
Cite this chapter
Sindalovskiy, L.N. (2017). Horizontally Heterogeneous Aquifers. In: Aquifer Test Solutions. Springer, Cham. https://doi.org/10.1007/978-3-319-43409-4_4
Download citation
DOI: https://doi.org/10.1007/978-3-319-43409-4_4
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-319-43408-7
Online ISBN: 978-3-319-43409-4
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)