Erosivity density as an indicator of soil erosion risk in South Asia

IF 5.7 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Catena Pub Date : 2025-04-01 Epub Date: 2025-02-11 DOI:10.1016/j.catena.2025.108766
Ishita Afreen Ahmed , Manabendra Saharia , Sumedha Chakma
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Abstract

Soil erosion presents substantial environmental issues, affecting agriculture, water quality, and biodiversity, with approximately 24 billion tonnes of productive soil lost annually worldwide. This is especially critical for South Asia, which is a hotspot for soil loss and has an economy dependent on agricultural productivity. Rainfall is a primary agent of erosion, and erosivity density (ED), which is the rainfall erosivity per unit of precipitation, is a measure of the interaction between the kinetic energy of rainfall and the soil surface. But a large-scale assessment of erosivity density currently doesn’t exist for South Asia. Using precipitation data from 1980 to 2018 and analytical techniques such as Mann-Kendall trend analysis and wavelet transform analysis, this study detects significant trends in erosivity density, highlighting regions most susceptible to soil erosion. Rainfall erosivity (R-factor) was calculated using high-resolution precipitation data (I60) and kinetic energy equations. Prominent areas with high erosivity density were detected in the Western Ghats and Northeastern Himalayas. Additionally, high ED values were observed in northeastern India, certain areas of Pakistan, and central and southern India. An increasing trend in ED was detected in the Indo-Gangetic plain, suggesting increased erosion risk. In contrast, declining patterns in certain regions of Pakistan and northern India indicated a decrease in rainfall intensity or frequency, potential impacting water availability. The wavelet transform analysis showed significant biennial and decadal patterns in ED, indicating climatic influences in South Asia. Biennial cycles showed variations in power levels, ranging from 0.75 to 1.05 in certain years, highlighting significant fluctuations in erosivity density intensity that result in substantial changes in soil erosion risk, demanding robust and adaptive conservation strategies. The study highlights the necessity for region-specific soil conservation techniques to mitigate erosion risks, providing a foundation for effective soil conservation and land management strategies in South Asia.
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侵蚀力密度作为南亚土壤侵蚀风险的指标
土壤侵蚀带来了严重的环境问题,影响农业、水质和生物多样性,全世界每年损失约240亿吨生产性土壤。这对南亚尤其重要,因为南亚是土壤流失的热点地区,经济依赖于农业生产力。降雨是土壤侵蚀的主要动因,而侵蚀力密度(ED),即每单位降水的降雨侵蚀力,是衡量降雨动能与土壤表面相互作用的指标。但目前南亚还没有大规模的侵蚀密度评估。利用1980 - 2018年的降水数据,结合Mann-Kendall趋势分析和小波变换分析等分析技术,本研究发现了侵蚀力密度的显著趋势,突出了最易受土壤侵蚀的区域。利用高分辨率降水数据(I60)和动能方程计算降雨侵蚀力(r因子)。在西高止山脉和喜马拉雅山脉东北部发现了高侵蚀密度的突出地区。此外,在印度东北部、巴基斯坦的某些地区以及印度中部和南部观察到高ED值。印度恒河平原ED呈上升趋势,表明侵蚀风险增加。相比之下,巴基斯坦和印度北部某些地区的下降模式表明降雨强度或频率下降,这可能影响到水的供应。小波变换分析显示南亚地区ED具有显著的两年和年代际变化特征,表明气候对南亚地区的影响。两年周期显示出功率水平的变化,在某些年份从0.75到1.05不等,突出表明侵蚀力密度强度的显著波动,导致土壤侵蚀风险发生重大变化,需要强有力的适应性保护战略。该研究强调了区域土壤保持技术减轻侵蚀风险的必要性,为南亚有效的土壤保持和土地管理战略提供了基础。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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