Geoinformatic approach to potential soil erosion risk assessment in Tulasi watershed

Q4 Engineering
V. S. Pawar-Patil, P. T. Patil, V. A. Chougule, S. Panhalkar, B. Nikam
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引用次数: 0

Abstract

The disintegration of soil grains caused by raindrops initiates the erosion process and is the primary source of erosion on small and steep slopes. Soil loss occurs all across the world, but poor countries are more vulnerable to it due to failure to replenish lost soil and minerals. Asian countries have been highlighted as one of the locations on the globe where soil erosion has proven to be a difficult challenge in terms of development and land resource conservation. Because India is the world's second most populous country and agriculture is the backbone of the Indian economy, sustainable land management approaches are urgently needed to protect production potential and provide an adequate supply of healthy food for millions. The Tulasi watershed in Maharashtra, India, is distinguished by heavy rain during the monsoon season, undulating and rocky topography and bare hilltops, all of which increase runoff capacity and make top soil more prone to detachment and loosening. In light of this, the current study employs geo-information technologies and the RUSLE model to derive erosion factors such as rainfall erosivity, soil erodibility, slope length and steepness, land cover and management and to estimate the amount and spatial distribution of soil loss in the study area.
土拉西流域潜在土壤侵蚀风险评估的地理信息学方法
雨滴引起的土壤颗粒崩解启动了侵蚀过程,是小陡坡侵蚀的主要来源。土壤流失在世界各地都有发生,但由于无法补充流失的土壤和矿物质,贫穷国家更容易受到土壤流失的影响。亚洲国家被强调为全球土壤侵蚀在发展和土地资源保护方面是一项艰巨挑战的地区之一。由于印度是世界第二人口大国,农业是印度经济的支柱,因此迫切需要可持续的土地管理方法来保护生产潜力,并为数百万人提供充足的健康食品供应。印度马哈拉施特拉邦的图拉西流域以季风季节的大雨、起伏的岩石地形和裸露的山顶而闻名,所有这些都增加了径流能力,使表层土壤更容易脱落和松动。有鉴于此,本研究利用地理信息技术和RUSLE模型推导了降雨侵蚀力、土壤可蚀性、边坡长度和坡度、土地覆盖和管理等侵蚀因子,并估计了研究区的土壤流失量和空间分布。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Disaster Advances
Disaster Advances 地学-地球科学综合
CiteScore
0.70
自引率
0.00%
发文量
57
审稿时长
3.5 months
期刊介绍: Information not localized
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