Application of Geo-informatics for Soil Erosion Mapping

Susheel Dangol, Umesh Mandal
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Abstract

Soil erosion is a most severe environmental problem in hilly area. The study is carried out on Upper Bagmati River basin, North of Kathmandu valley having an area of 61 Sq.km. (approx). Universal Soil Loss Equation (USLE) model, with Geographic Information System (GIS) has been used to quantify the soil loss. Erosion modelling requires huge amount of information and data, usually coming from different sources and available in different formats and scales and for management of these data, GIS was used, which helped considerably in organizing the spatial data representing the effects of each factor affecting soil erosion. Five essential parameters of USLE Rainfall erosivity factor (R), Soil erodibility Factor (K), Slope length and steepness (LS) factor, Cropping management factor (C) and Support practice factor (P) have been used to estimate soil loss amount in the study area. All of these layers have been prepared in Arc GIS using various data sources and data preparation methods. DEM was prepared from the contour data with the interval of 20m which was used to generate LS factor. The monthly rainfall data (2010) of 17 rain gauge stations within the catchment area have been used to predict the R factor. K, C and P factors in basin area are adopted from the literature. The spatial distribution map of soil loss of the basin has been generated and classified into six categories depending on the calculated soil erosion amount. The annual predicted soil loss ranges between 0 and 292.878 t/ha/y. Low soil loss (mean 9.7 t/ha/y) have been recorded under forested areas. The high rate (mean 40.4 t/ha/y) of soil erosion was found in the cultivation area.
地理信息学在土壤侵蚀制图中的应用
土壤侵蚀是丘陵地区最严重的环境问题。该研究是在加德满都谷地北部的上巴格马蒂河流域进行的,面积为61平方公里。(大约)。采用通用土壤流失方程(USLE)模型,结合地理信息系统(GIS)对土壤流失进行量化。侵蚀建模需要大量的信息和数据,这些信息和数据通常来自不同的来源,有不同的格式和尺度,为了管理这些数据,使用了地理信息系统,它在组织代表影响土壤侵蚀的每个因素的影响的空间数据方面有很大的帮助。采用USLE 5个基本参数降雨侵蚀力因子(R)、土壤可蚀性因子(K)、坡长陡度因子(LS)、种植管理因子(C)和支护实践因子(P)估算研究区土壤流失量。所有这些层都是在Arc GIS中使用各种数据源和数据准备方法编制的。利用等高线数据,以20m为间隔,编制DEM,生成LS因子。利用流域内17个雨量站2010年的月降雨量数据对R因子进行了预测。盆地区K、C、P因子采用文献。生成了流域土壤流失量空间分布图,并根据计算的土壤流失量将流域土壤流失量划分为6类。年预测土壤流失量在0 ~ 292.878 t/ha/y之间。森林地区的土壤流失量较低(平均9.7吨/公顷/年)。耕地土壤侵蚀率较高,平均为40.4 t/ha/y。
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