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    水土保持措施因子优化及其对RUSLE模拟精度的影响

    • 摘要: 为优化RUSLE模型的水土保持措施因子(P)取值,提高模型的模拟精度。根据P的定义,基于湖北省不同水土保持措施径流小区监测数据获取一系列P值,逐层融合DEM、土壤类型、土地利用、植被覆盖和梯田数据集,将上述获取的P值匹配到对应的栅格单元,进而优化P因子的取值。并利用径流小区和小流域实测土壤流失量评价优化了P值的RUSLE模型模拟精度。结果显示:(1)高P值即P≥0.600分布于湖北省的西部、东北部和东南部,较低P值即P<0.300分布于中部平原地带。(2)优化前后湖北省土壤侵蚀的时空分布格局与土壤侵蚀发生的重点区域基本一致。(3)基于径流小区观测数据的精度评价: R2为0.816,RMSE为214.6,相对误差为11.22%,优化后的RUSLE预测结果中98%的数据点均位于95%预测带内。(4)基于小流域监测数据的精度评价:优化后的模拟精度达到86.630%,较优化前提高9.798%。(5)优化前强烈侵蚀、极强烈侵蚀、剧烈侵蚀的占比均大于优化后的占比,原因是优化前P因子取值偏高。研究结果表明优化后的P因子取值有效,模型的模拟精度有所提高。

       

      Abstract: The modified general soil loss equation (RUSLE) is widely used in estimating regional soil erosion, but the soil and water conservation measure factor (P), as the most difficult factor to determine, is mainly assigned by literature results, land use type and slope, and there is still room for improvement in accuracy. In order to optimize the value of soil and water conservation measures factor (P) of RUSLE model and improve the simulation accuracy of the model. According to the definition of P, a series of P values were obtained from soil erosion monitoring data of runoff plots and control plots with different soil and water conservation measures at 8 monitoring stations in Huanggang, Wuhan, Shiyan and Xianning in Hubei Province, and DEM, soil type, land use, vegetation cover and terrace data sets were fused layer by layer to match the above obtained P values to the corresponding grid cells, and then optimize the value of P factors to obtain the spatial distribution map of P factors in Hubei Province. Then, based on the P value before optimization and the P value after optimization, the RUSLE model was used to calculate the soil loss in Hubei Province, and the soil erosion modulus before and after optimization was obtained. Finally, the P value was optimized based on the measured soil loss evalua-tion in runoff plots and small watersheds. RUSLE model simulation accuracy. It is feasible to use the measured data of runoff plot combined with multi-source data to optimize the value of P factor of RUSLE model. The proportions of high P values (≥ 0. 600) were 6.540% (0.6), 0.533% (0.7), 0.083% (0.8), and 0.002% (1), respectively, distributed in the west, northeast and southeast of Hubei Province, with lower P values. The areas are located in the central plain.; Before and after optimization, the temporal and spatial distribution pattern of soil erosion in Hubei Province is basically consistent with the key areas where soil erosion occurs. The accuracy evaluation based on the observation data of runoff plots shows that R2 is 0.816, RMSE is 214.6, and the relative error is 11.22%. 98% of the data points in the optimized RUSLE prediction results are located in the 95% prediction band; The accu-racy evaluation based on small watershed observation data shows that the optimized simulation accu-racy reaches 86.630%, which is 9.798% higher than that before optimization; The proportion of strong erosion, extremely strong erosion and severe erosion before optimization is greater than that after op-timization, because the P factor before optimization is higher than that after optimization. The results show that the optimized P-factor value method is effective, and the simulation accuracy of RUSLE model is improved.

       

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