Variation in saturated hydraulic conductivity at the outcrop scale, the Whanganui Basin, New Zealand.
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DOI: 10.1111/gwat.12948
Abstract: Groundwater flow and contaminant transport are strongly influenced by hydrogeological spatial variation. Understanding the textural heterogeneity of aquifer and aquitard units is critical for predicting preferential flow pathways, but is often hindered by sparse hydrogeological… read more here.
Keywords: hydraulic conductivity; variation; whanganui basin; saturated hydraulic ... See more keywords