Water in the vadose zone has a pressure head less than atmospheric pressure, and is retained by a combination of adhesion ("funiculary groundwater"), and capillary action ("capillary groundwater"). If the vadose zone envelops soil, the water contained therein is termed soil moisture. In fine grained soils, capillary action can cause the pores of the soil to be fully saturated above the water table at a pressure less than atmospheric. The vadose zone does not include the area that is still saturated above the water table, often referred to as the capillary fringe.