Assessment of hydrogeochemical characteristics and quality of groundwater resources in relation to risk of gastric cancer: comparative analysis of high- and low-risk areas in Iran

The chemical quality of groundwater supplies in two high-risk area (HRA) and low-risk area (LRA) for gastric cancer in Iran was assessed through hydrogeochemical analysis and water quality indices. For this aim, Piper and Schoeller diagrams and water quality index (WQI) were applied. In addition, ex...

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Veröffentlicht in:Environmental geochemistry and health 2021, Vol.43 (1), p.1-21
Hauptverfasser: Ghaffari, Hamid Reza, Yunesian, Masud, Nabizadeh, Ramin, Nasseri, Simin, Pourfarzi, Farhad, Poustchi, Hossein, Sadjadi, Alireza, Eshraghian, Ahad
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container_title Environmental geochemistry and health
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creator Ghaffari, Hamid Reza
Yunesian, Masud
Nabizadeh, Ramin
Nasseri, Simin
Pourfarzi, Farhad
Poustchi, Hossein
Sadjadi, Alireza
Eshraghian, Ahad
description The chemical quality of groundwater supplies in two high-risk area (HRA) and low-risk area (LRA) for gastric cancer in Iran was assessed through hydrogeochemical analysis and water quality indices. For this aim, Piper and Schoeller diagrams and water quality index (WQI) were applied. In addition, exposure to nitrate via drinking water and its corresponding risk were also assessed using Monte Carlo simulation technique. Data on physicochemical properties of groundwater resources were obtained from Iran Water Resources Management Company. Sampling and analysis of tap water for nitrate concentration were conducted in two cities of Shiraz (as a representative of LRA) and Ardabil (as a representative of HRA). According to Piper diagrams, the dominant hydrogeochemical facies of groundwater supplies in HRA and LRA were Na–HCO 3 (43.75%) and Ca–HCO 3 (41.77%), respectively. The predominant cations in groundwater resources of HRA were found to be Na + (68.06%) and Ca 2+ (31.94%). For LRA, the typical cations were in decreasing trend: Ca 2+ (39.64%) > Mg 2+ (18.35%) > Na + (17.26%). For two areas, HCO 3 − , SO 4 2− and Cl − were, respectively, the most frequent anions. Two-sample Wilcoxon test showed that there were statistically significant difference between two areas in terms of anions and cations concentrations ( p value 
doi_str_mv 10.1007/s10653-020-00562-x
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For this aim, Piper and Schoeller diagrams and water quality index (WQI) were applied. In addition, exposure to nitrate via drinking water and its corresponding risk were also assessed using Monte Carlo simulation technique. Data on physicochemical properties of groundwater resources were obtained from Iran Water Resources Management Company. Sampling and analysis of tap water for nitrate concentration were conducted in two cities of Shiraz (as a representative of LRA) and Ardabil (as a representative of HRA). According to Piper diagrams, the dominant hydrogeochemical facies of groundwater supplies in HRA and LRA were Na–HCO 3 (43.75%) and Ca–HCO 3 (41.77%), respectively. The predominant cations in groundwater resources of HRA were found to be Na + (68.06%) and Ca 2+ (31.94%). For LRA, the typical cations were in decreasing trend: Ca 2+ (39.64%) &gt; Mg 2+ (18.35%) &gt; Na + (17.26%). For two areas, HCO 3 − , SO 4 2− and Cl − were, respectively, the most frequent anions. Two-sample Wilcoxon test showed that there were statistically significant difference between two areas in terms of anions and cations concentrations ( p value &lt; 0.05). The mean of total hardness (Ca 2+  + Mg 2+ ) concentration of water supplies in LRA (528.1 mg/L) was higher than HRA (263.1 mg/L), whereas the mean of Na + concentration was found to be lower in LRA (90.6 mg/L) compared with HRA (108.1 mg/L). The sum of nitrate intake and its risk in LRA was higher than HRA. WQI results showed that drinking water quality in HRA and LRA ranged from excellent to poor and most water resources were of a good quality class. 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For this aim, Piper and Schoeller diagrams and water quality index (WQI) were applied. In addition, exposure to nitrate via drinking water and its corresponding risk were also assessed using Monte Carlo simulation technique. Data on physicochemical properties of groundwater resources were obtained from Iran Water Resources Management Company. Sampling and analysis of tap water for nitrate concentration were conducted in two cities of Shiraz (as a representative of LRA) and Ardabil (as a representative of HRA). According to Piper diagrams, the dominant hydrogeochemical facies of groundwater supplies in HRA and LRA were Na–HCO 3 (43.75%) and Ca–HCO 3 (41.77%), respectively. The predominant cations in groundwater resources of HRA were found to be Na + (68.06%) and Ca 2+ (31.94%). For LRA, the typical cations were in decreasing trend: Ca 2+ (39.64%) &gt; Mg 2+ (18.35%) &gt; Na + (17.26%). For two areas, HCO 3 − , SO 4 2− and Cl − were, respectively, the most frequent anions. Two-sample Wilcoxon test showed that there were statistically significant difference between two areas in terms of anions and cations concentrations ( p value &lt; 0.05). The mean of total hardness (Ca 2+  + Mg 2+ ) concentration of water supplies in LRA (528.1 mg/L) was higher than HRA (263.1 mg/L), whereas the mean of Na + concentration was found to be lower in LRA (90.6 mg/L) compared with HRA (108.1 mg/L). The sum of nitrate intake and its risk in LRA was higher than HRA. WQI results showed that drinking water quality in HRA and LRA ranged from excellent to poor and most water resources were of a good quality class. Further studies are suggested to investigate the role of drinking water in the etiology of gastric cancer in Iran.</description><subject>Aetiology</subject><subject>Anions</subject><subject>Anions - analysis</subject><subject>Calcium</subject><subject>Calcium ions</subject><subject>Cancer</subject><subject>Cations</subject><subject>Cations - analysis</subject><subject>Comparative analysis</subject><subject>Dietary Exposure - analysis</subject><subject>Drinking water</subject><subject>Drinking Water - chemistry</subject><subject>Drinking Water - standards</subject><subject>Earth and Environmental Science</subject><subject>Environment</subject><subject>Environmental Chemistry</subject><subject>Environmental Health</subject><subject>Environmental Monitoring</subject><subject>Etiology</subject><subject>Gastric cancer</subject><subject>Geochemistry</subject><subject>Groundwater</subject><subject>Groundwater - chemistry</subject><subject>Groundwater - standards</subject><subject>Groundwater quality</subject><subject>Humans</subject><subject>Hydrogeochemistry</subject><subject>Iran - epidemiology</subject><subject>Magnesium</subject><subject>Monte Carlo simulation</subject><subject>Nitrates</subject><subject>Nitrates - analysis</subject><subject>Original Paper</subject><subject>Physicochemical processes</subject><subject>Physicochemical properties</subject><subject>Public Health</subject><subject>Risk Assessment</subject><subject>Sodium</subject><subject>Soil Science &amp; 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For this aim, Piper and Schoeller diagrams and water quality index (WQI) were applied. In addition, exposure to nitrate via drinking water and its corresponding risk were also assessed using Monte Carlo simulation technique. Data on physicochemical properties of groundwater resources were obtained from Iran Water Resources Management Company. Sampling and analysis of tap water for nitrate concentration were conducted in two cities of Shiraz (as a representative of LRA) and Ardabil (as a representative of HRA). According to Piper diagrams, the dominant hydrogeochemical facies of groundwater supplies in HRA and LRA were Na–HCO 3 (43.75%) and Ca–HCO 3 (41.77%), respectively. The predominant cations in groundwater resources of HRA were found to be Na + (68.06%) and Ca 2+ (31.94%). For LRA, the typical cations were in decreasing trend: Ca 2+ (39.64%) &gt; Mg 2+ (18.35%) &gt; Na + (17.26%). For two areas, HCO 3 − , SO 4 2− and Cl − were, respectively, the most frequent anions. Two-sample Wilcoxon test showed that there were statistically significant difference between two areas in terms of anions and cations concentrations ( p value &lt; 0.05). The mean of total hardness (Ca 2+  + Mg 2+ ) concentration of water supplies in LRA (528.1 mg/L) was higher than HRA (263.1 mg/L), whereas the mean of Na + concentration was found to be lower in LRA (90.6 mg/L) compared with HRA (108.1 mg/L). The sum of nitrate intake and its risk in LRA was higher than HRA. WQI results showed that drinking water quality in HRA and LRA ranged from excellent to poor and most water resources were of a good quality class. Further studies are suggested to investigate the role of drinking water in the etiology of gastric cancer in Iran.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><pmid>32458268</pmid><doi>10.1007/s10653-020-00562-x</doi><tpages>21</tpages></addata></record>
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subjects Aetiology
Anions
Anions - analysis
Calcium
Calcium ions
Cancer
Cations
Cations - analysis
Comparative analysis
Dietary Exposure - analysis
Drinking water
Drinking Water - chemistry
Drinking Water - standards
Earth and Environmental Science
Environment
Environmental Chemistry
Environmental Health
Environmental Monitoring
Etiology
Gastric cancer
Geochemistry
Groundwater
Groundwater - chemistry
Groundwater - standards
Groundwater quality
Humans
Hydrogeochemistry
Iran - epidemiology
Magnesium
Monte Carlo simulation
Nitrates
Nitrates - analysis
Original Paper
Physicochemical processes
Physicochemical properties
Public Health
Risk Assessment
Sodium
Soil Science & Conservation
Statistical analysis
Statistical methods
Stomach Neoplasms - chemically induced
Stomach Neoplasms - epidemiology
Terrestrial Pollution
Water hardness
Water Pollutants, Chemical - analysis
Water quality
Water resources
Water resources management
Water supply
title Assessment of hydrogeochemical characteristics and quality of groundwater resources in relation to risk of gastric cancer: comparative analysis of high- and low-risk areas in Iran
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