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Research paper thumbnail of Field evaluation of methods for determining hydraulic conductivity from grain size data

Determination of hydraulic conductivity (K) and its variation in space is often a major objective... more Determination of hydraulic conductivity (K) and its variation in space is often a major objective of hydrogeological site investigations. However, measurement of K at a high spatial resolution in sedimentary aquifers is a challenge. There are a number of field methods that can be used to determine K, although they differ greatly in terms of their spatial resolution.

Research paper thumbnail of Field evaluation of methods for determining hydraulic conductivity from grain size data

Determination of hydraulic conductivity (K) and its variation in space is often a major objective... more Determination of hydraulic conductivity (K) and its variation in space is often a major objective of hydrogeological site investigations. However, measurement of K at a high spatial resolution in sedimentary aquifers is a challenge. There are a number of field methods that can be used to determine K, although they differ greatly in terms of their spatial resolution.

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