Soil water studies for California rangelands have focussed on near-surface
hydrologic processes, limiting our understanding of spatial-temporal dynami
cs of the water regime below the root zone. Soil moisture content and poten
tial were monitored for 16 months in 12 locations in an annual grass domina
ted 20 ha catchment. The data collected were analyzed by ANOVA to determine
significant spatial and temporal differences in soil moisture, Further: an
alysis identified variables that influenced the amount of moisture present
at a particular subsurface location. It was determined that there were sign
ificant differences in the amount of soil moisture present along the vertic
al profile of each site and between sites. Soil texture, type of vegetation
cover, and elevation were the significant variables that influenced the so
il moisture status.