A Study Case on Estimation of Soil Loss and Sediment Yield in Curtin University, Malaysia

Hui Yee Ngieng, L. K. Yong, Striprabu Strimari
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引用次数: 2

Abstract

Because of human activities, soil erosion has been one of the most concerning issues in Malaysia in the past decades. This study aimed to estimate the amount of soil loss and sediment yield at Curtin University, Malaysia by using the Revised Universal Soil Loss Equation (RUSLE) and the Modified Universal Soil Loss Equation (MUSLE), respectively. The parameters of RUSLE include rainfall erosivity factor (R), soil erodibility factor (K), slope length factor (L), slope steepness factor (S), cover-management factor (C) and support practice factor (P). The rainfall data (10 years) from the Sarawak Meteorological Department was used to determine the R-factor. The K-factor was determined by sieve analysis, hydrometer analysis, the Standard Proctor Test (SPT), and organic content testing. The L-and S-factors were performed by measuring on site and using Google Earth. The C-and P-factors were based on the ground surface cover condition (bare soil in this study). In the MUSLE, the runoff factor comprises V and Qp, while the other parameters are the same as in the RUSLE. The runoff depth, V, is equivalent to the rainfall intensity. Rainfall intensities were recorded by using a rain gauge. The highest rainfall intensity was used for runoff depth. The Rational method has been utilized to calculate Qp. The amount of soil loss estimated was 119.97 tons/ha/year and the sediment yield amount estimated was 0.76 ton/storm event in Curtin University, Malaysia.
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马来西亚科廷大学水土流失及产沙估算研究案例
在过去的几十年里,由于人类活动,土壤侵蚀一直是马来西亚最受关注的问题之一。本研究旨在利用修正通用土壤流失方程(RUSLE)和修正通用土壤流失方程(MUSLE)分别估算马来西亚科汀大学的土壤流失量和产沙量。RUSLE的参数包括降雨侵蚀力因子(R)、土壤可蚀性因子(K)、坡长因子(L)、坡度因子(S)、覆盖管理因子(C)和支持实践因子(P), R因子采用砂拉越气象局10年降水数据确定。k因子采用筛分分析法、比重计分析法、标准普氏试验(SPT)和有机含量测定。l因子和s因子采用谷歌Earth进行现场测量。c和p因子基于地表覆盖条件(本研究为裸土)。在MUSLE中,径流因子包括V和Qp,其他参数与RUSLE相同。径流深度V相当于降雨强度。降雨强度由雨量计记录。径流深度采用最高降雨强度。采用Rational方法计算Qp。马来西亚科廷大学估算的土壤流失量为119.97吨/公顷/年,产沙量为0.76吨/次风暴。
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