印度乔塔那格浦尔高原东部边缘伊尔加流域的土壤侵蚀评估

Q1 Social Sciences
Ratan Pal, Buddhadev Hembram, Narayan Chandra Jana
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引用次数: 0

摘要

人类为提高生活质量而开展的活动加快了水土流失的自然速度。反过来,这些自然灾害也对人类造成了巨大影响。人类活动,尤其是将植被地转化为农田和建筑区,是造成水土流失的主要因素。本研究调查了位于印度恰尔肯德邦乔塔那格浦尔高原东部边缘的伊尔加流域的水土流失风险,该流域主要为砂质壤土和砂质粘壤土,土壤有机碳(SOC)含量较低。研究采用了修订的通用土壤流失方程(RUSLE)和地理信息系统(GIS)技术来确定土壤侵蚀率。应用 RUSLE 的五个参数(降雨-径流侵蚀率 (R) 因子、土壤可侵蚀性 (K) 因子、坡长和坡度 (LS) 因子、覆盖管理 (C) 因子和支持实践 (P) 因子),可以更准确地呈现伊尔加流域的土壤侵蚀分布特征。结果表明,R因子与降雨量呈正相关,且与降雨量的分布规律相同。研究区域北部的 K 系数值相对较低,而南部则相对较高。LS 系数的平均值为 2.74,由于伊尔加流域地势平坦,LS 系数较低。归一化植被指数(NDVI)与 C 因子之间呈负线性相关,NDVI 低的地方 C 因子值高。P 因子的平均值为 0.210,范围在 0.000 至 1.000 之间。计算所有参数后,我们得出土壤侵蚀率平均值为 1.43 t/(hm2-a),最高可达 32.71 t/(hm2-a)。因此,研究区域面临的水土流失风险较低。然而,为避免未来水土流失对生产和建设活动造成损害,必须采取预防措施。本研究还确定了水土流失率的空间分布,这将有助于决策者实施有针对性的水土流失控制措施。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of soil erosion in the Irga watershed on the eastern edge of the Chota Nagpur Plateau, India

Human activities to improve the quality of life have accelerated the natural rate of soil erosion. In turn, these natural disasters have taken a great impact on humans. Human activities, particularly the conversion of vegetated land into agricultural land and built-up area, stand out as primary contributors to soil erosion. The present study investigated the risk of soil erosion in the Irga watershed located on the eastern fringe of the Chota Nagpur Plateau in Jharkhand, India, which is dominated by sandy loam and sandy clay loam soil with low soil organic carbon (SOC) content. The study used the Revised Universal Soil Loss Equation (RUSLE) and Geographical Information System (GIS) technique to determine the rate of soil erosion. The five parameters (rainfall-runoff erosivity (R) factor, soil erodibility (K) factor, slope length and steepness (LS) factor, cover-management (C) factor, and support practice (P) factor) of the RUSLE were applied to present a more accurate distribution characteristic of soil erosion in the Irga watershed. The result shows that the R factor is positively correlated with rainfall and follows the same distribution pattern as the rainfall. The K factor values in the northern part of the study area are relatively low, while they are relatively high in the southern part. The mean value of the LS factor is 2.74, which is low due to the flat terrain of the Irga watershed. There is a negative linear correlation between Normalized Difference Vegetation Index (NDVI) and the C factor, and the high values of the C factor are observed in places with low NDVI. The mean value of the P factor is 0.210, with a range from 0.000 to 1.000. After calculating all parameters, we obtained the average soil erosion rate of 1.43 t/(hm2•a), with the highest rate reaching as high as 32.71 t/(hm2•a). Therefore, the study area faces a low risk of soil erosion. However, preventative measures are essential to avoid future damage to productive and constructive activities caused by soil erosion. This study also identifies the spatial distribution of soil erosion rate, which will help policy-makers to implement targeted soil erosion control measures.

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来源期刊
Regional Sustainability
Regional Sustainability Social Sciences-Urban Studies
CiteScore
3.70
自引率
0.00%
发文量
20
审稿时长
21 weeks
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