基于地理空间技术的土壤侵蚀估算——尼泊尔廓尔喀Jyadul Khola盆地研究

S. Adhikari, Prabesh Prabesh Shrestha, Motilal Ghimire
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摘要

在评估流域土壤侵蚀的严重程度及其对农业、森林、荒地、水体和建成区的影响时,估算流域土壤侵蚀是必不可少的。Jyadul Khola流域对廓尔喀地区东南侧Budhigandaki河的生态过程影响显著。本文试图在侵蚀严重等级的基础上估算平均侵蚀速率。本研究采用地球资源数据分析系统(ERDAS) Imagine、地理信息系统(GIS)和修正通用水土流失方程(RUSLE)模型处理的“紫苑三号”遥感影像。利用混淆矩阵对土地利用土地覆被分类结果进行验证,计算总体精度为95%,kappa系数为0.94。根据侵蚀严重程度将流域划分为6类。结果表明:92.7%的土地(0 ~ 5 t ha-1年-1)为轻度严重,其次为中度2.39% (10 ~ 20 t ha-1年-1)、中度2.07% (5 ~ 10 t ha-1年-1)、重度2.04% (20 ~ 40 t ha-1年-1)、重度0.67% (40 ~ 80 t ha-1年-1)和重度0.10% (80 ~ 80 t ha-1年-1)。研究区年平均土壤流失量为13526.60 t / a,土壤侵蚀等级为0 ~ 305.34 t / a / a。Kuwapani、Lakuri Bhanjyang、Khadkagaun、Garapani和Kaulebhagar地区最容易受到土壤侵蚀。土壤贫瘠、坡度陡、降雨强度大是造成土壤侵蚀危害的主要因素。这一结果可作为决策者保护高风险地区和规划有效措施以减轻即将发生的灾害的基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil Erosion Estimation Using Geospatial Technology: A Study of Jyadul Khola Basin, Gorkha, Nepal
Estimation of soil erosion from drainage basins is essential while assessing the severity and its impact on agriculture, forests, barren land, waterbodies, and built- up areas. Jyadul Khola basin significantly affects the ecological processes that feed into the Budhigandaki River in the south-eastern side of Gorkha District. This paper has attempted to estimate the mean erosion rate based on the erosion severity classes. Remotely sensed Ziyuan-3 satellite image processed in Earth Resources Data Analysis System (ERDAS) Imagine, Geographical Information System (GIS), and Revised Universal Soil Loss Equation (RUSLE) model were used in this study. The land use land cover (LULC) classification results were validated by using confusion matrix by computing overall accuracy and kappa coefficient which is 95% and 0.94 respectively. The basin had been classified into 6 categories based on erosion severity. The results indicated 92.7% of land (0-5 t ha–1 yr–1) is low severe followed by 2.39% (10-20 t ha–1 yr–1) moderate, 2.07% (5-10 t ha–1 yr–1) high, 2.04% (20-40 t ha–1 yr–1) very high, 0.67% (40-80 t ha–1 yr–1) severe and 0.10% of land (>80 t ha–1 yr–1) which is very severe for soil erosion. The total annual mean soil loss was found to be 13526.60 t yr–1 and soil erosion classes ranges from 0 to 305.34 t ha–1 yr–1 for the entire study area. Kuwapani, Lakuri Bhanjyang, Khadkagaun, Garapani and Kaulebhagar area are the most susceptible to soil erosion. It is observed that barren land, steep slopes, and high intensity of rainfall are major factors for soil erosion hazard. This outcome can serve as a foundation for decision-makers to conserve high risk areas and plan effective measure to lessen impending disasters.
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