2020
DOI: 10.1007/s12403-020-00348-7
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Hydrogeochemical Characteristics and Health Effects of Iodine in Groundwater in Wei River Basin

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Cited by 16 publications
(6 citation statements)
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“…It is a representative region in the western and northern parts of China. Located in a semi-humid to semi-arid warm temperature climate zone, the basin has a continental monsoon climate [61], and the elevation ranges from 324 m to 3911 m. The downstream region has annual precipitation ranges from 600~800 mm, while the annual precipitation at the upstream region ranges from 350~500 mm. The period from June to October accounts for 65~80% of the total annual precipitation.…”
Section: Research Area and Datamentioning
confidence: 99%
“…It is a representative region in the western and northern parts of China. Located in a semi-humid to semi-arid warm temperature climate zone, the basin has a continental monsoon climate [61], and the elevation ranges from 324 m to 3911 m. The downstream region has annual precipitation ranges from 600~800 mm, while the annual precipitation at the upstream region ranges from 350~500 mm. The period from June to October accounts for 65~80% of the total annual precipitation.…”
Section: Research Area and Datamentioning
confidence: 99%
“…The review paper also reviewed the effective and efficient measures for arsenicosis and fluorosis management including techniques for arsenic and fluoride removal Similar to fluoride, iodine is also an essential element for human health but becomes toxic in high intake dosage. In the research paper, Duan et al (2020), taking the Wei River basin as a case study area, investigated the groundwater iodine level and its spatial distribution, and analyzed the hydrochemical characteristics and factors affecting the iodine concentration in groundwater. They used a parabolic equation to describe the relationship of iodine content in groundwater and iodine-disease prevalence in different subsystems of the basin.…”
Section: Papers In This Special Issuementioning
confidence: 99%
“…The hydrochemical composition of natural groundwater is governed by many factors including recharge water, rock/medium types, and hydrochemical processes along the flow paths (Helena et al, 2000;Venkatramanan et al, 2017). In natural conditions, some substances such as fluoride, arsenic, and iodine may release from the rocks/mediums into groundwater and result in geogenic poor quality groundwater (Liu et al, 2015;Zhang et al, 2018;Zhi et al, 2019;Wang Y. et al, 2020). Natural evaporation maybe significantly strong and lead to the salinity of groundwater, especially in an arid environment .…”
Section: Introductionmentioning
confidence: 99%
“…Ali et al (2019) obtained similar conclusions for the fluoride contaminants in phreatic groundwater, and also pointed out that the arid climatic conditions may potentially aggravate the geogenic fluoride contamination through promoting the evaporation process, etc. Other minor elements such as arsenic, iodine, and heavy metals in phreatic aquifers were also reported as being able to originate from geogenic sources and be regulated by external factors (Taylor, 1996;Arslan et al, 2017;Voutchkova et al, 2017;Zeng et al, 2018;Zhi et al, 2019;Duan et al, 2020). With the rapid development of industry, agriculture, and urbanization, groundwater contamination induced by human activities has become more and more severe in recent decades (Baalousha, 2011;Souid et al, 2017;Houéménou et al, 2020).…”
Section: Introductionmentioning
confidence: 99%