Freer, Jim E. and Aulenbach, Brent T. and Peters, Norman E. (2003) Hydrological dynamics of the Panola Mountain Research Watershed, Georgia, USA. Ground Water. Groundwater, 41 (7). pp. 973-988. ISSN 0017-467XFull text not available from this repository.
Relations between stormflow characteristics and soil-moisture content, water table elevation in wells along several transects perpendicular to the stream, and precipitation were evaluated for the Panola Mountain Research Watershed, Georgia, from water years 1986 through 2001 to refine the conceptualization of streamflow generation, including the relations between ground water dynamics and streamflow. For 759 rainstorms during 16 water years, stormflow water yield correlates best with maximum soil-moisture content and with maximum water table elevation; the relations are linear above thresholds for the entire period and vary by season. For moderate to large rainstorms, relations among wetness parameters and stormflow water yield are better (less scatter) and more consistent when the watershed is seasonally wet than when the watershed is dry. During rainstorms, soil-moisture content (minimum or maximum) is highly correlated among soil depths and with water table elevations. The soil-moisture measurements were made at one site at the base of a hillslope, and the values at any depth are likely to vary spatially and with respect to timing, other landscape positions, and soil types. Stormflow water yield is linearly related to soil-moisture content at the deepest location (70 cm) above 37% volumetric moisture content, which occurs 20% of the time. Maximum water table elevation is linearly related to maximum soil-moisture content above a threshold, and the soil-moisture threshold increases with upslope position; the soil-moisture threshold for flow to occur at a trench hillslope site is 41%, which occurs <0.5% of the time. The general relations among streamflow, soil moisture, and water table response are attributed to variable source areas, particularly the ground water contribution from a riparian zone aquifer ≤5 m thick that expands as the watershed becomes wetter.
|Journal or Publication Title:||Groundwater|
|Additional Information:||NEP is lead USGS scientist for the Panola experiment, but much of the data on which this paper was based was from instrumentation designed and installed by JEF for the hillslope and groundwater monitoring. JEF also made a major contribution to the data analysis and manuscript development. RAE_import_type : Journal article RAE_uoa_type : Earth Systems and Environmental Sciences|
|Subjects:||G Geography. Anthropology. Recreation > GE Environmental Sciences|
|Departments:||Faculty of Arts & Social Sciences > Applied Social Science|
|Deposited On:||08 Apr 2008 16:25|
|Last Modified:||07 Dec 2016 01:16|
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