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Estimation of the Rate of Soil Erosion in the Tasik Chini Catchment, Malaysia using the RUSLE Model Integrated with the GIS

机译:利用RUSLE模型和GIS估算马来西亚Tasik Chini集水区的土壤侵蚀速率

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摘要

The Tasik Chini Catchment, located at the southeast region of Pahang, Malaysia is experiencing soil erosion problems which are of environmental concern. So a study was conducted that involved the integration of the Revised Universal Soil Loss Equation (RUSLE) with the Geographic Information System (GIS) to estimate potential soil loss and identify erosion risk areas. Values for the model on rainfall erosivity (R), topographic factors (LS), land cover (C) and management factors (P) were calculated from rainfall data, together with the use of topographic and land use maps. Soil was analyzed for obtaining the soil erodibility factor (K). Physical properties such as particle size distribution, texture, hydraulic conductivity and organic matter content (OM) were analyzed to support the erosion rate analysis. The mean soil erodibility factors varied from 0.03 to 0.30 Mg h MJ-1 mm-1. From a total of eleven soil series studied, soil erosion results showed that the five soil series with low rate of soil loss were: Tebok, Lating, Bungor, Kekura and Gong Chenak. Two soil series with moderate soil loss were Serdang and Prang. Two soil series with moderately high rate of soil loss were Kuala Brang and Rasau. The Malacca soil series had high erosion rate. The worst-case scenario was the Kedah soil series. The soil erosion potential zones were classified into five classes namely very low, low, moderately high, high and very high soil loss. The results indicated that 71.54% of the study area lay within the very low erosion risk class, 2.94% in the low erosion risk class, 3.38% in the moderately high erosion risk class, 1.45% in the high erosion risk class and 13.25% in the very high erosion risk class. This high erosion rate is expected to generate high sediment yield influx into the water bodies of Tasik Chini making the lake shallower and perhaps even non existent in the near future if precautionary measures are not taken.
机译:位于马来西亚彭亨州东南部的Tasik Chini集水区正在遭受土壤侵蚀问题,这是环境问题。因此,进行了一项研究,将修订的通用土壤流失方程(RUSLE)与地理信息系统(GIS)集成在一起,以估算潜在的土壤流失并确定侵蚀风险区域。通过降雨数据以及地形图和土地利用图的使用来计算该模型的降雨侵蚀力(R),地形因子(LS),土地覆盖率(C)和管理因子(P)的值。分析土壤以获得土壤易蚀性因子(K)。分析了诸如粒度分布,织构,水力传导率和有机质含量(OM)的物理特性,以支持侵蚀速率分析。平均土壤侵蚀因子从0.03到0.30 Mg·h MJ-1 mm-1。从总共研究的11个土壤系列中,土壤侵蚀结果表明,土壤流失率较低的5个土壤系列分别是:Tebok,Lating,Bungor,Kekura和Gong Chenak。土壤流失中等的两个土壤系列是Serdang和Prang。两个土壤流失率较高的土壤系列是瓜拉布朗(Kuala Brang)和拉绍(Rasau)。马六甲的土壤系列具有较高的侵蚀率。最坏的情况是吉打州土壤系列。水土流失潜在区分为非常低,低,中等高,高和非常高的土壤流失五类。结果表明,研究区域的71.54%位于极低侵蚀风险类别中,低侵蚀风险类别为2.94%,中度高侵蚀风险类别为3.38%,高侵蚀风险类别为1.45%,高侵蚀风险类别为13.25%侵蚀风险很高的类别。如果不采取预防措施,预计这种高侵蚀速率将使大量沉积物大量涌入Tasik Chini的水体,使湖泊更浅,甚至在不久的将来甚至不存在。

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