4.7 Article

Groundwater fluoride chemistry and health risk assessment of multi-aquifers in Jilin Qianan, Northeastern China

期刊

出版社

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.ecoenv.2021.111926

关键词

Fluoride; Health risk assessment; Multi-aquifers; Jilin Qianan

资金

  1. National Natural Science Foundation of China [41572216]
  2. China Geological Survey Shenyang Center Hydrogeological Survey of Songnen Plain project [DD20190340-W09]
  3. Geological Survey Foundation of Jilin Province [2018-13]
  4. Petroleum Technology Development Fund (PTDF) Nigeria [PTDF/ED/PHD/OPA/61/18]

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In the multi-aquifer system in Jilin Qianan, fluoride concentrations exceeding recommended guidelines were found in all aquifers except N. The highest health risk from using the water was associated with Q(3) in 2017, with children and infants being the main population at risk of fluoride exposure.
Groundwater from deep confined aquifers is often recommended for use because of it's low fluoride health risk. Thus, this study appraised groundwater fluoride hydrochemistry in a multi-aquifer system in Jilin Qianan to determine the non-carcinogenic health risk liable from exploiting the respective aquifers. 124 samples collected from the tertiary confined aquifer (N), quaternary confined aquifer (Q(1)), and quaternary phreatic aquifer (Q(3)) during surveys in 2001 and 2017 was analyzed using hydrochemical, statistical, spatial, and health risk assessment methods. Results show that the dominant water facies in the respective aquifer layers was Na+K-HCO3+CO3 except in Q(1), where Ca+Mg - HCO3 + CO3 was marginally dominant. Fluoride concentrations outside the recommended guideline occurred in all the aquifers except N, where concentrations were optimum. The mean fluoride concentration of groundwater in the aquifers was of the order Q(3) (2017) > Q(3) (2001) > Q(1) > N ( mean 2.09, 2.03, 1.41 and 0.75 mg/L with 51.85%, 57.44%, 36.36% and 0% occurring beyond recommended guideline values respectively). Silicate weathering, cation exchange, and fluorite dissolution in an alkaline environment were the significant fluoride contributing processes. Evaporation and MgF+ complex additionally influenced Q(1) and Q(3) (2017). The total hazard quotient (THQ) from oral and dermal pathways shows fluoride health risks in the order: infant > children > adult. The associated risks likely from using water in the respective aquifer layers is of the order Q(3) (2017) > Q(3) (2001) > Q(1) > N. The mean groundwater fluoride in 2017 was marginally higher than that of 2001 ( 2.09>2.03 mg/L respectively) although the percentage of age group members disposed to fluoride risk from using water from Q(3) decreased from 2001 to 2017. Knowledge of local hydrogeology in exploiting deep groundwater free of fluoride pollution and on-site defluoridation treatment of groundwater was recommended in the study area and other areas with similar characteristics.

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