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The results indicate that steady declines in the water table, which are commonly attributed to groundwater evapotranspiration, occurred at both sites during the growing season.
In the Kabul Basin of Afghanistan, water-table declines have been attributed to groundwater withdrawals with inadequate recharge, and rises to recharge following a drought period (Mack et al. 2010b, 2013).
Base flow is the component of the streamflow that can be attributed to groundwater discharge into streams.
Mean baseflow per hydrologic region was greatest in the North Coast, North Lahontan, Sacramento, San Joaquin, South Lahontan and Tulare Lake hydrologic regions where >50% of the total streamflow is attributed to groundwater.
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This implies that a small aquifer dispersivity may be attributed to preferential groundwater flowpaths.
This can be attributed to the groundwater movement from higher slope in the upstream to the downstream in the lower part of coastal area.
Water level responses that occur within hours of the larger precipitation events are attributed to focused groundwater recharge in near field braided stream channels.
The source of high salt accumulation in the upper soil layers in the aforementioned blocks could therefore not be attributed to the groundwater intrusion in the root-zone depth.
At the western end of the transect on the banks of the Old Brahmaputra River (B1), an offset of the depth profile of As towards lower concentrations could also be attributed to lower groundwater ages compared to B2 on the basis of major cation concentrations.
The heterogeneous subsidence observed in the study area (as shown in Fig. 3) is attributed to the various groundwater pumping intensities in different regions.
Actual evapotranspiration greater than precipitation at the plantations was attributed to uptake of groundwater by the root system in parts of the catchments.
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