Controlling factors and health risks of groundwater chemistry in a typical alpine watershed based on machine learning methods

Huigui Shen; Wenbo Rao; Hongbing Tan; Hongye Guo; Wanquan Ta; Xiying Zhang

doi:10.1016/j.scitotenv.2022.158737

Controlling factors and health risks of groundwater chemistry in a typical alpine watershed based on machine learning methods

Sci Total Environ. 2023 Jan 1:854:158737. doi: 10.1016/j.scitotenv.2022.158737. Epub 2022 Sep 13.

Authors

Huigui Shen¹, Wenbo Rao², Hongbing Tan¹, Hongye Guo³, Wanquan Ta⁴, Xiying Zhang⁵

Affiliations

¹ School of Earth Sciences and Engineering, Hohai University, Nanjing 210098, China.
² School of Earth Sciences and Engineering, Hohai University, Nanjing 210098, China. Electronic address: raowenbo@163.com.
³ Qinghai Hydrogeology and Engineering Geology and Environgeology Survey Institute, Xining 810008, China.
⁴ Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou 730000, China.
⁵ Qinghai Institute of Salt Lakes, CAS, Xining 810008, China.

PMID: 36108860
DOI: 10.1016/j.scitotenv.2022.158737

Abstract

Groundwater is a key water resource in alpine watersheds, but its quality is deteriorating due to human activities. The Golmud River watershed is a representative alpine watershed in Northwest China, and it was chosen to explore groundwater chemistry, associated controlling factors, source contributions, and potential health risks. The analysis includes the use of a self-organizing map (SOM), positive matrix factorization (PMF), ionic ratios, and a Monte Carlo simulation. The content of total dissolved solids in phreatic water was higher in the dry season and increased from the mountainous zone to the fine-soil plain-overflowing zone. Additionally, the water type varied from HCO₃^- to Cl^- types whereas confined groundwater was chemically stable and of a HCO₃^- type. The SOM results showed a visual correlation between the ions in groundwater. The combination of SOM, PMF, and ionic ratios identified water-rock action as a dominant factor of groundwater chemistry. It was also found that Clusters I and III were mainly influenced by silicate weathering (a total contribution of 38.4 %), whereas evaporation was dominant in Cluster VI (a contribution of 32.5 %). Anthropogenic pollution was mainly associated with clusters V and IV and was related to industrial and agricultural activities during the snowmelt and wet seasons, and fluorine deposition formed by residential coal heating during the dry season (contributions of 1.4 % and 23.8 % in Clusters V and IV, respectively). The sudden increases in B³⁺ and Li⁺ in Cluster II were due to inputs from small tributaries (a contribution of 3.9 %). The probabilistic health risk assessment showed that fluoride posed a greater non-carcinogenic risk to human health than Sr²⁺, B³⁺, and NO₃^-, and its potential threat to children was more significant during the dry season than in other seasons. It is necessary for local governments to establish urgent fluoride emission control policies within the Golmud River watershed.

Keywords: Anthropogenic effects; Golmud River watershed; Groundwater chemistry; Health risk evaluation; Rock weathering; Self-organizing map.