Determining anisotropic transmissivity using a simplified Papadopulos method

Ground Water
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Abstract

The straight-line method presented by Papadopulos requires a minimum of three observation wells for determining the transmissivity tensor of a homogeneous and anisotropic aquifer. A simplification of this method was developed for fractured aquifers where the principal directions of the transmissivity tensor are known prior to implementation, such as when fracture patterns on outcropping portions of the aquifer may be used to infer the principal directions. This new method assumes that observation wells are drilled along the two principal directions from the pumped well, thus reducing the required number of observation wells to two. This method was applied for an aquifer test in the fractured Navajo Sandstone of southwestern Utah and yielded minimum and maximum principal transmissivity values of 70 and 1800 m 2/d, respectively, indicating an anisotropy ratio of ???24 to 1.

Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Determining anisotropic transmissivity using a simplified Papadopulos method
Series title Ground Water
DOI 10.1111/j.1745-6584.2006.00210.x
Volume 44
Issue 5
Year Published 2006
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Ground Water
First page 749
Last page 753
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