Abstract
The agricultural economy of the southern Great Plains relies on practices that incorporate grazed winter wheatand associated summer management practices. Information exists about the impact of these practices on water quality, butdata related to runoff and associated nutrient and sediment movement due to high intensity, late summer storms in the southernGreat Plains are limited. This study examined runoff and runoff water quality from two winter wheat management strategies:winter wheat with summer chemical fallow (WWF) and winter wheat with summer legumes (WWSL) and two grazingtreatments (grazed and ungrazed) from 1998 to 2002. Four pastures were planted in conservation winter wheat and grazedfrom November to May. Summer legumes were direct seeded in two of the pastures in March and grazed mid-July to September.Runoff from plots (1.5 3 m) was quantified with a rainfall simulator, with rainfall intensities representing a late summer,short duration (15 min), high intensity (10 cm/h) summer storm. Runoff samples were analyzed for nitrate-N (NO3-N),bioavailable and water-soluble phosphorus (BAP and WSP, respectively), and sediment yield. Overall, the WWF practice hadgreater runoff, sediment, and nutrient losses than the WWSL strategy. Likewise, grazing produced greater runoff, sediment,and nutrient losses than ungrazed plots. The worst-case scenario was WWF pastures that incorporated winter grazing, with71% of applied rainfall lost as runoff. The greatest losses for sediment (284 kg/ha), NO3-N (124 kg/ha), BAP (380 g/ha), andWSP (38 g/ha) were found with the grazed WWF practice. Understanding the mechanism of interaction between late summerstorms and summer management practices will improve large-scale mitigation strategies to reduce erosion and enhancecapture of water resources.
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