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Adeyeye OA, Xiao C, Yawe AS, Zhang Z, Yang W, Nnanwuba UE, Liang X. Temporal groundwater quality, health risks and source point management zonation of multi-aquifers in Jilin Qian'an, Northeastern China. Environ Geochem Health 2023; 45:6069-6094. [PMID: 37246206 DOI: 10.1007/s10653-023-01622-8] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/23/2022] [Accepted: 05/15/2023] [Indexed: 05/30/2023]
Abstract
Jilin Qian'an, located in Northeastern China's Songnen Plain, relies almost exclusively on groundwater for drinking. The quaternary phreatic aquifer (Q3) is distinguished by high geogenic fluoride and arsenic concentrations, which necessitates reliance on quaternary confined (Q1) and neogene confined (N) aquifers (deeper aquifers) as source point management (SPM) alternatives. However, deeper aquifers are contaminated, necessitating temporal monitoring and unique management strategies. Using 165 samples, this study investigated the appropriateness of deeper restricted aquifers as a continuous SPM alternative by assessing the spatiotemporal groundwater quality and human health risk of the multi-aquifers in Jilin Qian'an from the 1980s to the 2010s. In addition, a source point management zonation (SPMZ) was implemented to define the specific intervention necessary in various portions of the study area. Results indicate water quality parameters were within recommended limits for most samples except fluoride, while arsenic was the most significant heavy metal pollutant. Mean groundwater mineralization in all the aquifers increased with time. Deeper aquifers are still a better alternative to the shallow phreatic aquifer as groundwater quality in the study is of the order N > Q1 > Q3 in the respective aquifers. Cancer risk assessment (CR) shows increases from 2001 to the 2010s in all aquifers except in Q3. SPMZ delineated: High As and high F zones; high As and low F zones; high As zones; high F zones; low F zones; and safe zones. Localized intervention based on SPMZ is recommended, along with the use of alternative water sources.
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Affiliation(s)
- Oluwafemi Adewole Adeyeye
- Key Laboratory of Groundwater Resources and Environment, Jilin University,, Ministry of Education, Changchun, 130021, China
- National Local Joint Engineering Laboratory of In-Situ Conversion, Drilling and Exploitation Technology for Oil Shale, Changchun, 130021, China
- College of New Energy and Environment, Jilin University, Changchun, 130021, China
- College of Resources and Environment, Southwest University, Chongqing, 400700, China
- Global Geosolutionz, Typesetters Biz Complex, Department of Geology Building, Ahmadu Bello University, Zaria, 810107, Nigeria
| | - Changlai Xiao
- Key Laboratory of Groundwater Resources and Environment, Jilin University,, Ministry of Education, Changchun, 130021, China
- National Local Joint Engineering Laboratory of In-Situ Conversion, Drilling and Exploitation Technology for Oil Shale, Changchun, 130021, China
- College of New Energy and Environment, Jilin University, Changchun, 130021, China
| | - Achivir Stella Yawe
- Key Laboratory of Groundwater Resources and Environment, Jilin University,, Ministry of Education, Changchun, 130021, China
- National Local Joint Engineering Laboratory of In-Situ Conversion, Drilling and Exploitation Technology for Oil Shale, Changchun, 130021, China
- College of New Energy and Environment, Jilin University, Changchun, 130021, China
- Global Geosolutionz, Typesetters Biz Complex, Department of Geology Building, Ahmadu Bello University, Zaria, 810107, Nigeria
| | - Zhihao Zhang
- Shenyang Academy of Environmental Sciences, Shenyang, 110000, China
| | - Weifei Yang
- Key Laboratory of Groundwater Resources and Environment, Jilin University,, Ministry of Education, Changchun, 130021, China
- National Local Joint Engineering Laboratory of In-Situ Conversion, Drilling and Exploitation Technology for Oil Shale, Changchun, 130021, China
- College of New Energy and Environment, Jilin University, Changchun, 130021, China
| | | | - Xiujuan Liang
- Key Laboratory of Groundwater Resources and Environment, Jilin University,, Ministry of Education, Changchun, 130021, China.
- National Local Joint Engineering Laboratory of In-Situ Conversion, Drilling and Exploitation Technology for Oil Shale, Changchun, 130021, China.
- College of New Energy and Environment, Jilin University, Changchun, 130021, China.
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Adeyeye OA, Xiao C, Zhang Z, Yawe AS, Liang X. Groundwater fluoride chemistry and health risk assessment of multi-aquifers in Jilin Qianan, Northeastern China. Ecotoxicol Environ Saf 2021; 211:111926. [PMID: 33472111 DOI: 10.1016/j.ecoenv.2021.111926] [Citation(s) in RCA: 14] [Impact Index Per Article: 4.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/29/2020] [Revised: 12/23/2020] [Accepted: 01/08/2021] [Indexed: 06/12/2023]
Abstract
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 (Q1), and quaternary phreatic aquifer (Q3) 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 Q1, 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 Q3 (2017) > Q3 (2001) > Q1 > 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 Q1 and Q3 (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 Q3 (2017) > Q3 (2001) > Q1 > 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 Q3 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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Affiliation(s)
- Oluwafemi Adewole Adeyeye
- Key Laboratory of Groundwater Resources and Environment, Jilin University, Ministry of Education, Changchun 130021, China; National Local Joint Engineering Laboratory of In-situ Conversion, Drilling and Exploitation Technology for Oil Shale, Changchun 130021, China; College of New Energy and Environment, Jilin University, Changchun 130021, China; Global Geosolutionz, Typesetters Biz Complex, Department of Geology, Ahmadu Bello University, Zaria 810107, Nigeria
| | - Changlai Xiao
- Key Laboratory of Groundwater Resources and Environment, Jilin University, Ministry of Education, Changchun 130021, China; National Local Joint Engineering Laboratory of In-situ Conversion, Drilling and Exploitation Technology for Oil Shale, Changchun 130021, China; College of New Energy and Environment, Jilin University, Changchun 130021, China.
| | - Zhihao Zhang
- Key Laboratory of Groundwater Resources and Environment, Jilin University, Ministry of Education, Changchun 130021, China; National Local Joint Engineering Laboratory of In-situ Conversion, Drilling and Exploitation Technology for Oil Shale, Changchun 130021, China; College of New Energy and Environment, Jilin University, Changchun 130021, China
| | - Achivir Stella Yawe
- Key Laboratory of Groundwater Resources and Environment, Jilin University, Ministry of Education, Changchun 130021, China; National Local Joint Engineering Laboratory of In-situ Conversion, Drilling and Exploitation Technology for Oil Shale, Changchun 130021, China; College of New Energy and Environment, Jilin University, Changchun 130021, China; Global Geosolutionz, Typesetters Biz Complex, Department of Geology, Ahmadu Bello University, Zaria 810107, Nigeria
| | - Xiujuan Liang
- Key Laboratory of Groundwater Resources and Environment, Jilin University, Ministry of Education, Changchun 130021, China; National Local Joint Engineering Laboratory of In-situ Conversion, Drilling and Exploitation Technology for Oil Shale, Changchun 130021, China; College of New Energy and Environment, Jilin University, Changchun 130021, China.
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