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A two-well method of determining the hydraulic conductivity of discretelayers in layered saturated soils in the field

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Anisotropy and depth‐related heterogeneity of hydraulic conductivity in a bog peat. I: laboratory measurements
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Hydrological Processes. 2003 17(1). p.89
Contribution of climatic and anthropogenic effects to the hydric deficit of peatlands
Auterives Chrystelle, Aquilina Luc, Bour Olivier, Davranche Mélanie, Paquereau Valérie
Hydrological Processes. 2011 25(18). p.2890

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