高海拔湖泊的水化学和灌溉质量:尼泊尔喜马拉雅山脉拉马鲁山湖群案例研究

Q3 Environmental Science Limnological Review Pub Date : 2024-01-08 DOI:10.3390/limnolrev24010003
B. Thapa, L. Khanal, R. Pant, C. R. Bhatta, Prekshya Subedi, L. Upadhyaya, Chandra Bahadur Sunar, Janaki Poudel, Naresh Pandey, Pensri Kyes, Ankit Kumar Singh, K. Bishwakarma, R. Kyes
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引用次数: 0

摘要

尼泊尔苏都帕斯金省的拉马鲁山湖群(RLC)是一个喜马拉雅山湖群,具有重要的生态、经济、宗教和美学意义。本研究旨在全面描述拉罗山湖区水体的水化学特性,并评估其是否适合灌溉。研究人员从该建筑群的七个不同湖泊中共采集了 38 份水样。然后对理化参数和主要离子进行了分析。区域灌溉中心的水样呈碱性,根据总硬度,水样从软到中等硬度不等。主要离子包括以下几种:Ca2+ > Na+ > Mg2+ > K+ > Fe3+ > NH4+ 和 HCO3- > Cl- > SO42- > NO3- > PO43-。碱土金属(Ca2+ 和 Mg2+)主导碱金属(Na+ 和 K+),弱酸(HCO3-)主导强酸(Cl- 和 SO42-)。湖水的主要水化学类型为 Ca-HCO3 型,表明其岩性为碳酸钙型。碳酸盐岩风化是影响湖水水化学的最主要过程。(Ca2++ Mg2+)/Tz+比率较高,(Na+ + K+)/Tz+比率较低,这表明碳酸盐风化产生的 Ca2+ 和 Mg2+ 占主导地位,而硅酸盐风化的影响很小。不同的灌溉指数显示了 RLC 水的灌溉适宜性。这项研究得出的见解对于保护水质和促进可持续发展至关重要。这项研究还为包括研究人员和政策制定者在内的一系列利益相关者提供了至关重要的基础数据,为推进喜马拉雅淡水湖的水资源管理战略和促进生态系统保护做出了重要贡献,尤其是在面对全球气候变化带来的重大挑战时。
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Hydrochemistry and Irrigation Quality of High-Altitude Lakes: A Case Study of the Ramaroshan Lake Complex, Nepal Himalayas
The Ramaroshan Lake Complex (RLC) in Sudurpaschim Province, Nepal, is a Himalayan lake cluster that holds significant ecological, economic, religious, and esthetic importance. This study aimed to provide a comprehensive characterization of the hydrochemical properties of water within the RLC and assess its suitability for irrigation purposes. A total of 38 water samples were collected from seven different lakes of the complex. The physicochemical parameters and major ions were then analyzed. The water samples from the RLC were alkaline, and based on total hardness, they ranged from soft to moderately hard categories. The presence of major ions included the following: Ca2+ > Na+ > Mg2+ > K+ > Fe3+ > NH4+ and HCO3− > Cl− > SO42− > NO3− > PO43−. The alkaline earth metals (Ca2+ and Mg2+) dominated the alkali metals (Na+ and K+) and weak acids (HCO3−) dominated the strong acids (Cl− and SO42−). The dominant hydrochemical facies of the lake water was a Ca-HCO3 type indicating a calcium carbonate type of lithology. Carbonate rock weathering was the most dominant process in influencing the hydrochemistry of the water. A high ratio of (Ca2++ Mg2+)/Tz+ and a lower ratio of (Na+ + K+)/Tz+ revealed the dominance of Ca2+ and Mg2+ resulting from carbonate weathering, with little contribution from silicate weathering. Different irrigation indices revealed the suitability of the RLC water for irrigation. The insights derived from this study are pivotal in safeguarding water quality and bolstering sustainability efforts. The study also furnishes foundational data crucial to an array of stakeholders including researchers and policymakers and significantly contributes to advancing water management strategies and fostering ecosystem conservation in the Himalayan freshwater lakes, particularly in the face of the overarching challenge posed by global climate change.
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来源期刊
Limnological Review
Limnological Review Environmental Science-Ecology
CiteScore
1.60
自引率
0.00%
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0
审稿时长
16 weeks
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