Water quality and hydrochemical assessments of thermal springs, Gandaki Province, Nepal

被引:6
|
作者
Chalise, Baburam [1 ]
Paudyal, Prem [2 ]
Kunwar, Buddha Bahadur [3 ]
Bishwakarma, Kiran [4 ]
Thapa, Bina [5 ]
Pant, Ramesh Raj [5 ]
Neupane, Bhanu Bhakta [1 ]
机构
[1] Tribhuvan Univ, Inst Sci & Technol, Cent Dept Chem, Kathmandu 44613, Nepal
[2] Kathmandu Upatyaka Khanepani Ltd, Water Waste Water Qual Assurance Div, Kathmandu 44600, Nepal
[3] Govt Nepal, Dept Food Technol & Qual Control, Elemental Anal Lab, Kathmandu 44600, Nepal
[4] Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China
[5] Tribhuvan Univ, Inst Sci & Technol, Cent Dept Environm Sci, Kathmandu 44613, Nepal
关键词
Hydrogeochemistry; Hot springs; Water quality; Heavy metals; Multivariate analysis; HIMALAYA;
D O I
10.1016/j.heliyon.2023.e17353
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Thermal springs are the sites where the water temperature lies above ambient temperature. They are widely used for power generation, hot water spas, balneotherapy, agriculture, laundering, and aquaculture. In Nepal, many thermal springs are reported but scientific understanding on water quality and hydrogeochemistry of the springs is very limited. In this study, a total of 28 physicochemical parameters were measured in water samples collected from 12 thermal springs from Gandaki Province, Nepal. Correlation matrix and multivariate statistical analysis such as principal component analysis (PCA) and cluster analysis were used to understand the water quality and hydrogeochemistry of the hot water springs. The pH, temperature, electrical conductivity, total dissolved solids, and turbidity in the hot water springs ranged from 7.3 to 8.8, 31.6-64.3 degrees C, 206-16270 & mu;S/cm, 115-6637 mg/L, and 0.21-63.7 NTU; respectively. The dominance order of major anions and cations were: Cl- > HCO3- > SO42- > NO3- > F- and Na+ > Ca2+ > K+ > Mg2+; respectively. Comparison of the water quality parameters with the WHO and National Water Quality Standards suggested that the majority of the parameters were within the safe limit. Out of 9 heavy metals and trace elements analyzed Zn2+, Ni2+, Cr3+, Cd+2, Hg (total), and Pb2+ were found below the safe limit but Fe (total), As (total) and Cu (total) were found higher than the WHO safe limit in total of 3, 5 and 1 sampling sites; respectively. The water quality index (WQI), sodium absorption ratio (SAR), and magnesium hazard (MH) ratio in the hot water springs ranged from 40.9 to 573, 2.2-49.3, 7.1-70.8; respectively. The result of PCA analysis showed that four principal components are required to explain hydrogeochemistry. Cluster analysis suggested that the sampling sites can be grouped into three distinct clusters based on total dissolved solids. Interestingly, the classification of hydrochemical facies using a Piper diagram suggested that 7 out of 12 thermal springs have Na-Cl type water. Finally, a perspective on the suitability of the hot springs for hot water spas and balneotherapy and policy recommendation is provided.
引用
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页数:15
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