尼泊尔拉姆萨尔湿地Koshi Tappu湿地的水化学特征

Shristi Neupane, R. Pant, L. Thapa, D. Shah, Birendra Gautam, Barsha Adhikari, Barsha Khanal, Anueva Acharya, K. Bishwakarma, S. Adhikari
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摘要

尼泊尔拥有大量的淡水水体,从亚热带低地到冰川滋养的高原,水质各不相同。本研究评估了Koshi Tappu湿地水质的空间变化。Koshi Tappu湿地是尼泊尔第一个拉姆萨尔湿地,位于Koshi Tappu野生动物保护区内的Tarai东部地区。选取湿地内21个不同采样点的19个水质参数进行分析。现场分析pH、EC、TDS、浊度、DO等参数,实验室分析HCO3-、Cl-、NH4+、NO3-、SO42- PO43-、K+、TH、Ca2+、Mg2+、CaH、MgH、Na+、Fe3+。采用层次聚类分析(CA)和主成分分析(PCA)等多变量方法,以及piper图和混合图等地球化学指标对水质空间变异进行了评价。结果表明,Ca2+是主要的阳离子,HCO3-是主要的阴离子。基于主成分分析,观察到3个空间聚类的化学成分变化,主成分分析结果突出了采样地点的主要污染源和控制因素,占总方差的84.13%。主成分分析和离子关系分析结果表明,Koshi Tappu湿地的水化学主要受碳酸盐风化过程控制,硅酸盐风化和人为活动的影响较小。
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Hydrochemical characterization of the Ramsar-listed Koshi Tappu Wetland, Nepal
Nepal abounds a vast array of freshwater bodies, from sub-tropical lowlands to glacier-fed highlands with varying water quality. This study evaluated the spatial variations in water quality at the Koshi Tappu Wetland, the first Ramsar site of Nepal, located in the eastern Tarai region within the Koshi Tappu Wildlife Reserve. Nineteen water quality parameters were chosen and analyzed from twenty-one different sampling points within the wetland. Parameters including pH, EC, TDS, turbidity, and DO were analyzed on-site, whereas HCO3-, Cl-, NH4+, NO3-, SO42- PO43-, K+, TH, Ca2+, Mg2+, CaH, MgH, Na+, and Fe3+ were analyzed in the laboratory. Multivariate methods such as hierarchical agglomerative cluster analysis (CA) and principal component analysis (PCA), and geochemical indices such as piper and mixing diagrams were applied to assess the spatial variation in water quality. Findings indicated Ca2+ as the principal cation and HCO3- as the principal anion regulating the hydrochemistry of the wetland. Based on CA, three spatial clusters were observed, which depicted variations in chemical composition with the PCA results highlighting the primary contamination sources and controlling factors of the sampling locations with 84.13% of the total variance. Findings from the PCA and ionic relationship analyses elucidated that the hydrochemistry of the Koshi Tappu wetland is mainly controlled by carbonate weathering processes with a minor contribution of silicate weathering and anthropogenic activities.
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