Groundwater contamination with arsenic in Sherajdikhan, Bangladesh: geochemical and hydrological implications
An integrated study has been carried out to elucidate the distribution and occurrence of arsenic in selected groundwater samples in the area of Sherajdikhan, Bangladesh. Arsenic and other parameters (T, pH, EC, Na⁺, K⁺, Ca²⁺, Mg²⁺, Cl⁻, NO₃ ⁻, SO₄ ²⁻, HCO₃ ⁻, PO₄ ³⁻, Fe, Mn and DOC) have been measur...
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| Veröffentlicht in: | Environmental earth sciences 2009-07, Vol.58 (1), p.73-84 |
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| creator | Halim, M. A Majumder, R. K Nessa, S. A Oda, K Hiroshiro, Y Saha, B. B Hassain, S. M Latif, Sk. A Islam, M. A Jinno, K |
| description | An integrated study has been carried out to elucidate the distribution and occurrence of arsenic in selected groundwater samples in the area of Sherajdikhan, Bangladesh. Arsenic and other parameters (T, pH, EC, Na⁺, K⁺, Ca²⁺, Mg²⁺, Cl⁻, NO₃ ⁻, SO₄ ²⁻, HCO₃ ⁻, PO₄ ³⁻, Fe, Mn and DOC) have been measured in groundwater samples collected from shallow/deep tube wells at different depths. Hydrogeochemical data suggest that the groundwaters are generally Ca-Mg-HCO₃ and Mg-Ca-HCO₃ types with bicarbonate (HCO₃ ⁻) as the dominant anion, though the other type of water has also been observed. Dissolved arsenic in groundwater ranged from 0.006 to 0.461 mg/l, with 69% groundwater samples exceeded the Bangladesh limit for safe drinking water (0.05 mg/l). Correlation and principal component analysis have been performed to find out possible relationships among the examined parameters in groundwater. Low concentrations of NO₃ ⁻ and SO₄ ²⁻, and high concentrations of DOC, HCO₃ ⁻ and PO₄ ³⁻ indicate the reducing condition of subsurface aquifer where sediments are deposited with abundant organic matter. Distinct relationship of As with Fe and Mn, and strong correlation with DOC suggests that the biodegradation of organic matter along with reductive dissolution of Fe-Mn oxyhydroxides has being considered the dominant process to release As in the aquifers studied herein. |
| doi_str_mv | 10.1007/s00254-008-1493-8 |
| format | Article |
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A ; Majumder, R. K ; Nessa, S. A ; Oda, K ; Hiroshiro, Y ; Saha, B. B ; Hassain, S. M ; Latif, Sk. A ; Islam, M. A ; Jinno, K</creator><creatorcontrib>Halim, M. A ; Majumder, R. K ; Nessa, S. A ; Oda, K ; Hiroshiro, Y ; Saha, B. B ; Hassain, S. M ; Latif, Sk. A ; Islam, M. A ; Jinno, K</creatorcontrib><description>An integrated study has been carried out to elucidate the distribution and occurrence of arsenic in selected groundwater samples in the area of Sherajdikhan, Bangladesh. Arsenic and other parameters (T, pH, EC, Na⁺, K⁺, Ca²⁺, Mg²⁺, Cl⁻, NO₃ ⁻, SO₄ ²⁻, HCO₃ ⁻, PO₄ ³⁻, Fe, Mn and DOC) have been measured in groundwater samples collected from shallow/deep tube wells at different depths. Hydrogeochemical data suggest that the groundwaters are generally Ca-Mg-HCO₃ and Mg-Ca-HCO₃ types with bicarbonate (HCO₃ ⁻) as the dominant anion, though the other type of water has also been observed. Dissolved arsenic in groundwater ranged from 0.006 to 0.461 mg/l, with 69% groundwater samples exceeded the Bangladesh limit for safe drinking water (0.05 mg/l). Correlation and principal component analysis have been performed to find out possible relationships among the examined parameters in groundwater. Low concentrations of NO₃ ⁻ and SO₄ ²⁻, and high concentrations of DOC, HCO₃ ⁻ and PO₄ ³⁻ indicate the reducing condition of subsurface aquifer where sediments are deposited with abundant organic matter. Distinct relationship of As with Fe and Mn, and strong correlation with DOC suggests that the biodegradation of organic matter along with reductive dissolution of Fe-Mn oxyhydroxides has being considered the dominant process to release As in the aquifers studied herein.</description><identifier>ISSN: 0943-0105</identifier><identifier>ISSN: 1866-6280</identifier><identifier>EISSN: 1432-0495</identifier><identifier>EISSN: 1866-6299</identifier><identifier>DOI: 10.1007/s00254-008-1493-8</identifier><language>eng</language><publisher>Berlin/Heidelberg: Berlin/Heidelberg : Springer-Verlag</publisher><subject>Aquifers ; Arsenic ; Arsenic content ; Biodegradation ; Drinking water ; Earth and Environmental Science ; Earth Sciences ; Earth, ocean, space ; Engineering and environment geology. Geothermics ; Environmental geology ; Exact sciences and technology ; Geochemistry ; Geology ; Groundwater pollution ; Hydrogeology ; Hydrologic analysis ; Hydrology. 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Arsenic and other parameters (T, pH, EC, Na⁺, K⁺, Ca²⁺, Mg²⁺, Cl⁻, NO₃ ⁻, SO₄ ²⁻, HCO₃ ⁻, PO₄ ³⁻, Fe, Mn and DOC) have been measured in groundwater samples collected from shallow/deep tube wells at different depths. Hydrogeochemical data suggest that the groundwaters are generally Ca-Mg-HCO₃ and Mg-Ca-HCO₃ types with bicarbonate (HCO₃ ⁻) as the dominant anion, though the other type of water has also been observed. Dissolved arsenic in groundwater ranged from 0.006 to 0.461 mg/l, with 69% groundwater samples exceeded the Bangladesh limit for safe drinking water (0.05 mg/l). Correlation and principal component analysis have been performed to find out possible relationships among the examined parameters in groundwater. Low concentrations of NO₃ ⁻ and SO₄ ²⁻, and high concentrations of DOC, HCO₃ ⁻ and PO₄ ³⁻ indicate the reducing condition of subsurface aquifer where sediments are deposited with abundant organic matter. Distinct relationship of As with Fe and Mn, and strong correlation with DOC suggests that the biodegradation of organic matter along with reductive dissolution of Fe-Mn oxyhydroxides has being considered the dominant process to release As in the aquifers studied herein.</description><subject>Aquifers</subject><subject>Arsenic</subject><subject>Arsenic content</subject><subject>Biodegradation</subject><subject>Drinking water</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Environmental geology</subject><subject>Exact sciences and technology</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Groundwater pollution</subject><subject>Hydrogeology</subject><subject>Hydrologic analysis</subject><subject>Hydrology. 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A</au><au>Majumder, R. K</au><au>Nessa, S. A</au><au>Oda, K</au><au>Hiroshiro, Y</au><au>Saha, B. B</au><au>Hassain, S. M</au><au>Latif, Sk. A</au><au>Islam, M. A</au><au>Jinno, K</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Groundwater contamination with arsenic in Sherajdikhan, Bangladesh: geochemical and hydrological implications</atitle><jtitle>Environmental earth sciences</jtitle><stitle>Environ Geol</stitle><date>2009-07-01</date><risdate>2009</risdate><volume>58</volume><issue>1</issue><spage>73</spage><epage>84</epage><pages>73-84</pages><issn>0943-0105</issn><issn>1866-6280</issn><eissn>1432-0495</eissn><eissn>1866-6299</eissn><abstract>An integrated study has been carried out to elucidate the distribution and occurrence of arsenic in selected groundwater samples in the area of Sherajdikhan, Bangladesh. Arsenic and other parameters (T, pH, EC, Na⁺, K⁺, Ca²⁺, Mg²⁺, Cl⁻, NO₃ ⁻, SO₄ ²⁻, HCO₃ ⁻, PO₄ ³⁻, Fe, Mn and DOC) have been measured in groundwater samples collected from shallow/deep tube wells at different depths. Hydrogeochemical data suggest that the groundwaters are generally Ca-Mg-HCO₃ and Mg-Ca-HCO₃ types with bicarbonate (HCO₃ ⁻) as the dominant anion, though the other type of water has also been observed. Dissolved arsenic in groundwater ranged from 0.006 to 0.461 mg/l, with 69% groundwater samples exceeded the Bangladesh limit for safe drinking water (0.05 mg/l). Correlation and principal component analysis have been performed to find out possible relationships among the examined parameters in groundwater. Low concentrations of NO₃ ⁻ and SO₄ ²⁻, and high concentrations of DOC, HCO₃ ⁻ and PO₄ ³⁻ indicate the reducing condition of subsurface aquifer where sediments are deposited with abundant organic matter. Distinct relationship of As with Fe and Mn, and strong correlation with DOC suggests that the biodegradation of organic matter along with reductive dissolution of Fe-Mn oxyhydroxides has being considered the dominant process to release As in the aquifers studied herein.</abstract><cop>Berlin/Heidelberg</cop><pub>Berlin/Heidelberg : Springer-Verlag</pub><doi>10.1007/s00254-008-1493-8</doi><tpages>12</tpages></addata></record> |
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| subjects | Aquifers Arsenic Arsenic content Biodegradation Drinking water Earth and Environmental Science Earth Sciences Earth, ocean, space Engineering and environment geology. Geothermics Environmental geology Exact sciences and technology Geochemistry Geology Groundwater pollution Hydrogeology Hydrologic analysis Hydrology. Hydrogeology Mineralogy Organic matter Original Article Pollution, environment geology Principal components analysis Silicates Water analysis Water geochemistry Water sampling |
| title | Groundwater contamination with arsenic in Sherajdikhan, Bangladesh: geochemical and hydrological implications |
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