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Little River, Georgia
An ARS Benchmark Research Watershed

- Characteristics
The USDA-ARS Southeast Watershed Research Lab has collected hydrologic and climatic data on the 334 km2 Little River Watershed (LRW) (Figure 1) near Tifton, Georgia since 1968. The watershed is typical of the heavily vegetated, slow moving stream systems in the Coastal Plain Region of the U.S. Land use within the watershed is approximately 40% woodland, 36% row crops (primarily peanuts and cotton), 18% pasture, and 4% water. The LRW is located in the Southern Coastal Plain physiographic province in the Tifton Upland subprovince. The watershed is located on sands, silts, and clay underlain by the limestone that form the Floridian aquifers. The major soil series within the watershed are loamy sands with infiltration rates of approximately 5 cm/hr. Upland slopes within the watershed are 2 to 5% while channel slopes are on the order of 0.1 to 0.5%. Precipitation occurs almost exclusively as rainfall, with an annual mean at Tifton, Georgia of 1200 mm. Distribution of rainfall within the year is highly variable, although the fall months are typically dry. Water balance studies on the watershed indicate streamflow is around 30% of annual rainfall, evapotranspiration is 70%, and percolation to deep groundwater is negligible. The streamflow is composed of direct surface runoff (6% of annual rainfall) and return flow from the shallow aquifer (24% of annual rainfall). Deep seepage and recharge to regional groundwater systems is impeded by the Hawthorn geologic material 0 to 6 m below the land surface, promoting lateral movement of excess water from uplands downslope as shallow return flow to surface drainage systems. While sediment and agrochemical losses from upland cultivated fields can be high, filtering within the dense riparian buffers which surround the watershed streams reduces the loading to streams substantially. Based upon GA-EPD monitoring, many streams within the Coastal Plain are impaired by low dissolved oxygen. Preliminary assessments indicate that on the average, a 40% reduction in nitrogen and phosphorous loading must be achieved in the impaired watersheds. Because of their widespread use within the region, pesticides in streamflow are also a concern.
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