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首页> 外文期刊>Geocarto international >Soil erosion prediction based on land cover dynamics at the Semenyih watershed in Malaysia using LTM and USLE models
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Soil erosion prediction based on land cover dynamics at the Semenyih watershed in Malaysia using LTM and USLE models

机译:利用LTM和USLE模型,基于Malaysia的Semenyih流域土地覆盖动力学的土壤侵蚀预测

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摘要

This study attempts to identify and forecast future land cover (LC) by using the Land Transformation Model (LTM), which considers pixel changes in the past and makes predictions using influential spatial features. LTM applies the Artificial Neural Networks algorithm) in conducting the analysis. In line with these objectives, two satellite images (Spot 5 acquired in 2004 and 2010) were classified using the Maximum Likelihood method for the change detection analysis. Consequently, LC maps from 2004 to 2010 with six classes (forest, agriculture, oil palm cultivations, open area, urban, and water bodies) were generated from the test area. A prediction was made on the actual soil erosion and the soil erosion rate using the Universal Soil Loss Equation (USLE) combined with remote sensing and GIS in the Semenyih watershed for 2004 and 2010 and projected to 2016. Actual and potential soil erosion maps from 2004 to 2010 and projected to 2016 were eventually generated. The results of the LC change detections indicated that three major changes were predicted from 2004 to 2016 (a period of 12years): (1) forest cover and open area significantly decreased at rates of almost 30 and 8km(2), respectively; (2) cultivated land and oil palm have shown an increment in sizes at rates of 25.02 and 5.77km(2), respectively; and, (3) settlement and Urbanization has intensified also by almost 5km(2). Soil erosion risk analysis results also showed that the Semenyih basin exhibited an average annual soil erosion between 143.35 ton ha(-1)year(-1) in 2004 and 151 in 2010, followed by the expected 162.24tonha(-1)year(-1). These results indicated that Semenyih is prone to water erosion by 2016. The wide range of erosion classes were estimated at a very low level (0-1t/ha/year) and mainly located on steep lands and forest areas. This study has shown that using both LTM and USLE in combination with remote sensing and GIS is a suitable method for forecasting LC and accurately measuring the amount of soil losses in the future.
机译:本研究试图通过使用土地转换模型(LTM)来识别和预测未来的陆地覆盖(LC),该模型(LTM)考虑了过去的像素变化并使用有影响力的空间特征进行预测。 LTM应用人工神经网络算法进行分析。符合这些目标,使用最大似然方法进行两个卫星图像(2004年和2010年收购的位置5),用于改变检测分析的最大似然方法。因此,从2004年到2010年的LC地图与六级(森林,农业,油棕种植,开放区域,城市,城市和水体)从测试区产生。对2004年和2010年Semenyih流域的遥感和GIS结合遥感和GIS的实际土壤侵蚀和土壤侵蚀速率对2004年和2010年的实际土壤腐蚀和土壤侵蚀率进行了预测,并预计到2016年。2004年的实际和潜在土壤侵蚀地图到2010年并预计最终会产生2016年。 LC变更检测的结果表明,从2004年到2016年预测了三项重大变化(12年的时间):(1)森林覆盖和开放面积分别在近30%和8公里(2)的率下显着降低; (2)耕地和油棕,分别为25.02和5.77km(2)的尺寸增加了尺寸; (3)结算和城市化也加剧了近5公里(2)。土壤侵蚀风险分析结果还表明,7004年和2010年,2004年和2010年的143.35吨哈(-1)年(-1)年平均土壤侵蚀(-1),其次是预期的162.2444(-1)年( - 1)。这些结果表明,到2016年,Semenyih容易发生水侵蚀。估计广泛的侵蚀课程在极低的水平(0-1t / ha /年),主要位于陡峭的土地和森林地区。本研究表明,使用LTM和USLE结合遥感和GIS是一种适用于预测LC的合适方法,并准确地测量未来的土壤损失量。

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