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新冠疫情封锁期间恒河上游和亚穆纳河河水系的水质评估:河流复苏的印记

Water quality assessment of Upper Ganga and Yamuna river systems during COVID-19 pandemic-induced lockdown: imprints of river rejuvenation.

作者信息

Tiwari Sameer K, Yadav Jairam Singh, Sain Kalachand, Rai Santosh K, Kharya Aditya, Kumar Vinit, Sethy Pratap Chandra

机构信息

Wadia Institute of Himalayan Geology, 33 GMS Road, Dehradun, 248001, Uttarakhand, India.

出版信息

Geochem Trans. 2024 Sep 28;25(1):8. doi: 10.1186/s12932-024-00092-w.

Abstract

Clean river water is an essential and life-sustaining asset for all living organisms. The upper Ganga and Yamuna river system has shown signs of rejuvenation and tremendous improvement in the water quality following the nationwide lockdown due to the coronavirus pandemic. All the industrial and commercial activity was shut down, and there was negligible wastewater discharge from the industries. This article addresses the water quality assessment from the study area, which is based on the original data of physical parameters, major and trace elements, and stable isotopes (hydrogen and oxygen) systematics during the nationwide lockdown. The impact of the lockdown could be seen in terms of an increase in dissolved oxygen (DO). Water samples were collected from the Upper Ganga and Yamuna river basins (Alaknanda, Bhagirathi, and Tons rivers) during an eight-week lockdown in Uttarakhand, India. We discussed the signs of rejuvenation of riverine based on physical parameters, major ions, trace elements, isotopic ratios, and water pollution index (WPI). Results reveal that the water quality of the entire upper basins of the Ganga has significantly improved by 93%, reflecting the signs of self-rejuvenation of the rivers. Multivariate analysis suggests a negative factor loading for an anthropogenic element ( ), implying that they contribute little to the river water during the lockdown. Further, bicarbonate ( ) is a dominant element in both river basins. The geochemical facies are mainly characterized by the ( ) type of water, suggesting that silicate rock weathering dominates with little influence from carbonate weathering in the area. The positive factor loadings of some cations, like , , and reflect their strong association with the source of origin in the lockdown phases. Stable isotopic reveals that the glaciated region contributed the most to the river basin, as evidenced by the low d-excess in riverine water compared to anthropogenic contributions. Rivers can self-rejuvenate if issues of human influence and anthropogenic activities are adequately resolved and underline our responsibility for purifying the ecosystem. We observed that this improvement in the river water quality will take a shorter time, and quality will deteriorate again when commercial and industrial activity resumes.

摘要

清洁的河水是所有生物赖以生存的重要资源。由于新冠疫情全国封锁,恒河上游和亚穆纳河河水系统出现了恢复生机的迹象,水质有了显著改善。所有工商业活动都已停止,工业废水排放微乎其微。本文基于全国封锁期间物理参数、主要和微量元素以及稳定同位素(氢和氧)系统的原始数据,对研究区域的水质进行了评估。封锁的影响体现在溶解氧(DO)增加方面。在印度北阿坎德邦为期八周的封锁期间,从恒河上游和亚穆纳河流域(阿拉克南达河、巴吉拉蒂河和通斯河)采集了水样。我们根据物理参数、主要离子、微量元素、同位素比率和水污染指数(WPI)讨论了河流恢复生机的迹象。结果表明,恒河整个上游流域的水质显著改善了93%,这反映了河流自我恢复的迹象。多变量分析表明,人为元素( )的因子载荷为负,这意味着在封锁期间它们对河水的贡献很小。此外,碳酸氢根( )是两个流域的主要元素。地球化学相主要以( )型水为特征,这表明该地区硅酸盐岩石风化占主导,碳酸盐风化影响较小。一些阳离子,如 、 和 的正因子载荷反映了它们在封锁阶段与水源的强烈关联。稳定同位素显示,冰川地区对流域的贡献最大,这从河流水与人为贡献相比较低的氘过量可以看出。如果人类影响和人为活动问题得到充分解决,河流可以自我恢复生机,这也凸显了我们净化生态系统的责任。我们观察到,河水质量的这种改善所需时间较短,而当商业和工业活动恢复时,水质将再次恶化。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5888/11439316/074bd7b3eaed/12932_2024_92_Fig1_HTML.jpg

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