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Effects of Land Use and Slope Gradient on Soil Erosion in a Red Soil Hilly Watershed of Southern China

机译:南方红壤丘陵小流域土地利用和坡度对土壤侵蚀的影响

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A study was undertaken to develop an appropriate plan of land use under suitable slope gradient to control soil erosion from a red soil hilly watershed of southern China by using the GeoWEPP (Geo-spatial Interface for the Water Erosion Prediction Project) model. The model was calibrated and validated using monitoring data of the outlet from 2010 to 2012, in which the 2010 and 2012 annual total runoff and sediment yield data were used for calibration, and the 2011 monthly runoff and sediment yield data for validation. The performance of the model in validation period were good with a high coefficient of determination values of 0.98 and 0.93 and Nash-Sutcliffe simulations of 0.96 and 0.91 while low root mean square error values of 6.91 mm and 0.35 t respectively for runoff and sediment yield. Subsequently, the model was used to simulate four typical land use (forest, farm, orchard, and fallow land) in the study area to evaluate their impacts on soil erosion production. The results showed that the runoff decreased by 44.7% and 61.1% for forest and orchard land compared to the current land use, as well as the sediment yield decreased by 43.7% and 68.6%. While the runoff and sediment yield increased by 52.2% and 42.6% for farm land, and 48.8% and 29.6% for fallow land. As the same time, soil erosion increased with increasing of the slope gradient of the quadratic regression equation for all land use. The critical slope gradient of 15° for returning the farmland to forest or others is suitable in the red soil region but is not accurate. The result of the study provides good scientific evidence for developing an appropriate plan of land use in the watershed and other similar areas.
机译:进行了一项研究,通过使用GeoWEPP(水蚀预报项目的地理空间界面)模型,在合适的坡度梯度下制定了合适的土地利用计划,以控制中国南方红壤丘陵流域的土壤侵蚀。使用2010年至2012年出口的监测数据对模型进行校准和验证,其中使用2010年和2012年的年度总径流量和泥沙产量数据进行校准,并使用2011年的每月径流量和泥沙产量数据进行验证。该模型在验证期的性能良好,确定系数值分别为0.98和0.93,Nash-Sutcliffe模拟值分别为0.96和0.91,而径流和沉积物产量的均方根误差分别较低,分别为6.91 mm和0.35 t。随后,该模型用于模拟研究区域中的四种典型土地利用(森林,农场,果园和休耕地),以评估其对土壤侵蚀产生的影响。结果表明,林地和果园地的径流与当前土地利用相比分别减少了44.7%和61.1%,沉积物产量减少了43.7%和68.6%。耕地径流和沉积物产量分别增加52.2%和42.6%,休耕地增加48.8%和29.6%。同时,所有土地利用都随着二次回归方程坡度的增加而增加土壤侵蚀。用于退耕还林或其他的临界坡度为15°,适用于红壤地区,但不准确。研究结果为在流域和其他类似地区制定适当的土地利用计划提供了良好的科学依据。

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