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The higher dust contents of soils on south-facing slopes was associated with formation of argillic horizons, lower saturated hydrologic conductivity and increased water holding capacity.
The results showed a novel mechanism of shallow landslides: a significant vertical change in saturated hydrologic conductivity causes the accumulation of infiltrated water, and subsequently leading to an increase pore pressures and landslides in unsaturated soil layer.
It is also interesting to note that that alluvial plain groundwater has high fluoride levels due to alteration of mud and clay layers in the subsurface lithology which has very low hydrologic conductivity.
Low concentration of F− is observed in northwestern part of the study area as subsurface lithology has very low hydrologic conductivity and the clays present in the highly weathered rock mass might have resulted in the removal of F− by OH molecules through the process of ion exchange (Misra 2005; Singaraja et al. 2012; Manikandan et al. 2012).
A detailed three-dimensional characterization of the hydrologic conductivity heterogeneity of the site was obtained using slug tests.
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We found significant relationships between the hydrologic properties hydraulic conductivity and water yield and peat chemistry as described by 13C NMR and the MMM.
These losses were partially offset by groundwater discharge from the upland aquifer, which demonstrated strong hydrologic connectivity with the fen in spite of most construction materials having lower than targeted saturated hydraulic conductivities.
Springs emerging within massifs of crystalline rocks were monitored for discharge rate (Q), and the Q values combined with geomorphic and hydrographic parameters in a hydrologic model to calculate hydraulic conductivity (K) and effective porosity (ne) of the spring watersheds.
The spill and subsequent dissolution of DNAPLs was simulated in domains having different hydrologic characteristics (variance of the log conductivity field = 0.2, 1 and 3) using the multiphase flow and transport simulator UTCHEM.
We also perform a collection of experiments to analyze the effect of model discretization, hydraulic conductivity heterogeneity, and land cover change on hydrologic model response.
In response, we developed hydrologic and mass budgets for agricultural wetlands using electrical conductivity (EC) as a natural conservative tracer.
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