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Soil erodibility and surface runoff potentiality for water pollution management of Melaka Tengah watersheds in Malaysia

机译:马来西亚马六甲登加流域水污染管理的土壤易蚀性和地表径流潜力

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摘要

The relationships among surface runoff, precipitation and soil erodibility are significant in addressing environmental pollution as like water pollution and in predicting the benefits of Melaka Tengah watershed management practices. Land use pattern, soil series and slope percentage are also major factors to develop these relationships. Rainfall data (2009 to 2012) were collected from six rainfall station and analyzed for variations in precipitation at monthly and daily scale for calculating the surface runoff of these watersheds. Soil texture and structure, organic matter percentage, and hydraulic conductivity were analyzed for the particular soil series in this study area. Soil Conservation Services (SCS) and Weighted Curve Number (CNw) methods were introduced to calculate the surface runoff on daily basis. Henceforth, monthly surface runoff was calculated by summing the daily runoff and surface runoff map was produced by ArcGIS tools. Thenceforth, Tew equation was introduced to identify the soil erodibility of watershed soils for predicting the soil erosion probability. Results indicated the weighted curve number varies from 82 to 85 and monthly runoff varies from 23% to 30% among the five watersheds. Soil erodibility varies from 0.038 to 0.06 (ton/ha)(ha.hr/MJ.mm). Linau-Telok-Local Alluvium, Malacca-Munchong, Munchong-Malacca-Serdang and Malacca-Munchong-Tavy are the dominant soil series of this region having the average soil erodibility of about 0.042 (ton/ha)(ha.hr/MJ.mm). The main focus of this study is to provide the information of surface runoff potentiality, and soil erodibility for watershed water resources management, water pollution and flood control for watersheds.
机译:地表径流,降水量和土壤易蚀性之间的关系对于解决像水污染这样的环境污染以及预测马六甲腾加流域管理做法的收益具有重要意义。土地利用方式,土壤系列和坡度百分比也是发展这些关系的主要因素。从六个降雨站收集了降雨数据(2009年至2012年),并分析了每月和每天尺度下的降水变化,以计算这些流域的地表径流。分析了该研究区特定土壤系列的土壤质地和结构,有机质百分比和水力传导率。引入了土壤保护服务(SCS)和加权曲线数(CNw)方法来计算每天的地表径流。此后,通过将每日径流量相加来计算每月的地面径流量,然后使用ArcGIS工具生成地面径流量图。此后,引入Tew方程来识别流域土壤的土壤易蚀性,以预测土壤侵蚀的可能性。结果表明,在五个流域中,加权曲线数从82到85不等,月径流量从23%到30%不等。土壤侵蚀性从0.038到0.06(吨/公顷)(ha.hr/MJ.mm)不等。 Linau-Telok-Local冲积层,马六甲-Munchong,Munchong-Malacca-Serdang和马六甲-Munchong-Tavy是该地区的主要土壤系列,平均土壤可蚀性约为0.042(ton / ha)(ha.hr/MJ)。毫米)。本研究的主要重点是为流域水资源管理,流域水污染和防洪提供地表径流潜力和土壤易蚀性信息。

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