Shallow groundwater systems are important as a source of water, for
sustenance of stream baseflow, and for wetland and riparian
ecosystems. They are also central to waterlogging, and dryland and
irrigation salinity problems. Response time to hydrologic change
and pollutant loadings is fast among shallow aquifiers, and it is
important that hydrogeologists and natural resource managers
understand the unsaturated zone processes which links human
activity at the soil surface and the underlying groundwater, and
vice versa. This volume of papers explores practical aspects of
soil and surface water interactions with groundwater, including
modelling of flow and contaminant transport in the unsaturated and
saturated zones.
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