Groundwater quality and its implications for domestic and agricultural water supplies in a semi-arid river basin of Niger
In the River Goulbi Maradi Basin (RGMB), groundwater is a vital source of drinking water and plays a central role in the region’s socio-economic development. The quality and suitability of groundwater for irrigation and drinking-water remain inadequately understood. We examine hydrochemical analyses...
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| Veröffentlicht in: | Environmental earth sciences 2023-07, Vol.82 (13), p.329-329, Article 329 |
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| creator | Issoufou Ousmane, Boukari Nazoumou, Yahaya Favreau, Guillaume Abdou Babaye, Maman Sani Abdou Mahaman, Rabilou Boucher, Marie Sorensen, James P. R. MacDonald, Alan M. Taylor, Richard Graham |
| description | In the River Goulbi Maradi Basin (RGMB), groundwater is a vital source of drinking water and plays a central role in the region’s socio-economic development. The quality and suitability of groundwater for irrigation and drinking-water remain inadequately understood. We examine hydrochemical analyses of 35 groundwater samples from the shallow alluvial (17) and underlying Continental Hamadien (CH) sandstone (18) aquifers and evaluate these against standard measures of their suitability for drinking water (World Health Organization (WHO) guideline values) and irrigation (i.e., sodium adsorption ratio, sodium percentage, and the residual sodium carbonate). Hydrochemical facies are principally of Na–HCO
3
and Na–Cl types. Bivariate plots combined with saturation indices and electrical conductivity monitoring suggest that the main hydrogeochemical processes influencing groundwater quality are cation exchange in the CH aquifer and solute leaching from soils during focused recharge in the alluvial aquifer. 76% (13/17) of groundwater samples from the alluvial aquifer were suitable for irrigation compared to 38% (6/16) of the samples from the CH. The identification of high fluoride concentrations exceeding the WHO drinking-water guideline value (> 1.5 mg/L) in 33% (6/18) of samples from the CH aquifer and 18% (3/17) in the alluvial aquifer, and their respective attribution to the release of fluoride of geogenic origin through cation exchange and local use of fluorapatite fertilisers, provide valuable insight into efforts to address the on-going challenge of fluorosis in the Maradi region of Niger and more widely across African drylands. The health consequences of the widespread observation of Mn in concentrations exceeding the new WHO guideline value (0.08 mg/L) in the alluvial aquifer (6/9 samples), often alongside elevated Fe concentrations, are unclear. |
| doi_str_mv | 10.1007/s12665-023-11016-9 |
| format | Article |
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3
and Na–Cl types. Bivariate plots combined with saturation indices and electrical conductivity monitoring suggest that the main hydrogeochemical processes influencing groundwater quality are cation exchange in the CH aquifer and solute leaching from soils during focused recharge in the alluvial aquifer. 76% (13/17) of groundwater samples from the alluvial aquifer were suitable for irrigation compared to 38% (6/16) of the samples from the CH. The identification of high fluoride concentrations exceeding the WHO drinking-water guideline value (> 1.5 mg/L) in 33% (6/18) of samples from the CH aquifer and 18% (3/17) in the alluvial aquifer, and their respective attribution to the release of fluoride of geogenic origin through cation exchange and local use of fluorapatite fertilisers, provide valuable insight into efforts to address the on-going challenge of fluorosis in the Maradi region of Niger and more widely across African drylands. 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Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a326t-fbe39721d379603bbad27d5a596dfd618372bc429695a2b9f6ec273c0cd046883</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12665-023-11016-9$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12665-023-11016-9$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Issoufou Ousmane, Boukari</creatorcontrib><creatorcontrib>Nazoumou, Yahaya</creatorcontrib><creatorcontrib>Favreau, Guillaume</creatorcontrib><creatorcontrib>Abdou Babaye, Maman Sani</creatorcontrib><creatorcontrib>Abdou Mahaman, Rabilou</creatorcontrib><creatorcontrib>Boucher, Marie</creatorcontrib><creatorcontrib>Sorensen, James P. R.</creatorcontrib><creatorcontrib>MacDonald, Alan M.</creatorcontrib><creatorcontrib>Taylor, Richard Graham</creatorcontrib><title>Groundwater quality and its implications for domestic and agricultural water supplies in a semi-arid river basin of Niger</title><title>Environmental earth sciences</title><addtitle>Environ Earth Sci</addtitle><description>In the River Goulbi Maradi Basin (RGMB), groundwater is a vital source of drinking water and plays a central role in the region’s socio-economic development. The quality and suitability of groundwater for irrigation and drinking-water remain inadequately understood. We examine hydrochemical analyses of 35 groundwater samples from the shallow alluvial (17) and underlying Continental Hamadien (CH) sandstone (18) aquifers and evaluate these against standard measures of their suitability for drinking water (World Health Organization (WHO) guideline values) and irrigation (i.e., sodium adsorption ratio, sodium percentage, and the residual sodium carbonate). Hydrochemical facies are principally of Na–HCO
3
and Na–Cl types. Bivariate plots combined with saturation indices and electrical conductivity monitoring suggest that the main hydrogeochemical processes influencing groundwater quality are cation exchange in the CH aquifer and solute leaching from soils during focused recharge in the alluvial aquifer. 76% (13/17) of groundwater samples from the alluvial aquifer were suitable for irrigation compared to 38% (6/16) of the samples from the CH. The identification of high fluoride concentrations exceeding the WHO drinking-water guideline value (> 1.5 mg/L) in 33% (6/18) of samples from the CH aquifer and 18% (3/17) in the alluvial aquifer, and their respective attribution to the release of fluoride of geogenic origin through cation exchange and local use of fluorapatite fertilisers, provide valuable insight into efforts to address the on-going challenge of fluorosis in the Maradi region of Niger and more widely across African drylands. The health consequences of the widespread observation of Mn in concentrations exceeding the new WHO guideline value (0.08 mg/L) in the alluvial aquifer (6/9 samples), often alongside elevated Fe concentrations, are unclear.</description><subject>alluvial aquifer</subject><subject>Alluvial aquifers</subject><subject>apatite</subject><subject>Aquifers</subject><subject>Arid lands</subject><subject>Arid zones</subject><subject>basins</subject><subject>Biogeosciences</subject><subject>Bivariate analysis</subject><subject>Carbonates</subject><subject>Cation exchange</subject><subject>Cation exchanging</subject><subject>Cations</subject><subject>Drinking water</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Economic development</subject><subject>Electrical conductivity</subject><subject>Electrical resistivity</subject><subject>Environmental Science and Engineering</subject><subject>Fluorapatite</subject><subject>Fluorides</subject><subject>Fluorosis</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Groundwater</subject><subject>Groundwater irrigation</subject><subject>Groundwater quality</subject><subject>guidelines</subject><subject>Hydrochemicals</subject><subject>Hydrogeochemistry</subject><subject>Hydrology/Water Resources</subject><subject>Irrigation</subject><subject>Irrigation water</subject><subject>Leaching</subject><subject>Manganese</subject><subject>Niger</subject><subject>Original Article</subject><subject>River basins</subject><subject>Rivers</subject><subject>Sandstone</subject><subject>Saturation</subject><subject>Saturation index</subject><subject>Sedimentary facies</subject><subject>Sedimentary rocks</subject><subject>Socioeconomic aspects</subject><subject>socioeconomic development</subject><subject>Sodium</subject><subject>sodium adsorption ratio</subject><subject>Sodium carbonate</subject><subject>Solutes</subject><subject>Terrestrial Pollution</subject><subject>Water analysis</subject><subject>Water quality</subject><subject>Water sampling</subject><subject>Water supply</subject><subject>watersheds</subject><subject>World Health Organization</subject><issn>1866-6280</issn><issn>1866-6299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kU9LwzAYh4MoOOa-gKeAFy_V_GnfNkcZOoWhFz2HNElHRttsSavs2xtXUfBgLgnJ8_x4ww-hS0puKCHlbaQMoMgI4xmlhEImTtCMVgAZMCFOf84VOUeLGLckLU65IDBDh1XwY28-1GAD3o-qdcMBq95gN0Tsul3rtBqc7yNufMDGdzYOTh8JtQlOj-0wBtXiKSCOu2TYZPZY4Wg7l6ngDA7uPb3WKqZ73-Bnt7HhAp01qo128b3P0dvD_evyMVu_rJ6Wd-tMcQZD1tSWi5JRw0sBhNe1Mqw0hSoEmMYArXjJap0zAaJQrBYNWM1Krok2JIeq4nN0PeXugt-PaXzZuaht26re-jFKTgtOBRc5JPTqD7r1Y-jTdJJVDISAqsgTxSZKBx9jsI3cBdepcJCUyK9C5FSITIXIYyFSJIlPUkxwn77_G_2P9QkVbo7e</recordid><startdate>20230701</startdate><enddate>20230701</enddate><creator>Issoufou Ousmane, Boukari</creator><creator>Nazoumou, Yahaya</creator><creator>Favreau, Guillaume</creator><creator>Abdou Babaye, Maman Sani</creator><creator>Abdou Mahaman, Rabilou</creator><creator>Boucher, Marie</creator><creator>Sorensen, James P. 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R.</au><au>MacDonald, Alan M.</au><au>Taylor, Richard Graham</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Groundwater quality and its implications for domestic and agricultural water supplies in a semi-arid river basin of Niger</atitle><jtitle>Environmental earth sciences</jtitle><stitle>Environ Earth Sci</stitle><date>2023-07-01</date><risdate>2023</risdate><volume>82</volume><issue>13</issue><spage>329</spage><epage>329</epage><pages>329-329</pages><artnum>329</artnum><issn>1866-6280</issn><eissn>1866-6299</eissn><abstract>In the River Goulbi Maradi Basin (RGMB), groundwater is a vital source of drinking water and plays a central role in the region’s socio-economic development. The quality and suitability of groundwater for irrigation and drinking-water remain inadequately understood. We examine hydrochemical analyses of 35 groundwater samples from the shallow alluvial (17) and underlying Continental Hamadien (CH) sandstone (18) aquifers and evaluate these against standard measures of their suitability for drinking water (World Health Organization (WHO) guideline values) and irrigation (i.e., sodium adsorption ratio, sodium percentage, and the residual sodium carbonate). Hydrochemical facies are principally of Na–HCO
3
and Na–Cl types. Bivariate plots combined with saturation indices and electrical conductivity monitoring suggest that the main hydrogeochemical processes influencing groundwater quality are cation exchange in the CH aquifer and solute leaching from soils during focused recharge in the alluvial aquifer. 76% (13/17) of groundwater samples from the alluvial aquifer were suitable for irrigation compared to 38% (6/16) of the samples from the CH. The identification of high fluoride concentrations exceeding the WHO drinking-water guideline value (> 1.5 mg/L) in 33% (6/18) of samples from the CH aquifer and 18% (3/17) in the alluvial aquifer, and their respective attribution to the release of fluoride of geogenic origin through cation exchange and local use of fluorapatite fertilisers, provide valuable insight into efforts to address the on-going challenge of fluorosis in the Maradi region of Niger and more widely across African drylands. The health consequences of the widespread observation of Mn in concentrations exceeding the new WHO guideline value (0.08 mg/L) in the alluvial aquifer (6/9 samples), often alongside elevated Fe concentrations, are unclear.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s12665-023-11016-9</doi><tpages>1</tpages></addata></record> |
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| subjects | alluvial aquifer Alluvial aquifers apatite Aquifers Arid lands Arid zones basins Biogeosciences Bivariate analysis Carbonates Cation exchange Cation exchanging Cations Drinking water Earth and Environmental Science Earth Sciences Economic development Electrical conductivity Electrical resistivity Environmental Science and Engineering Fluorapatite Fluorides Fluorosis Geochemistry Geology Groundwater Groundwater irrigation Groundwater quality guidelines Hydrochemicals Hydrogeochemistry Hydrology/Water Resources Irrigation Irrigation water Leaching Manganese Niger Original Article River basins Rivers Sandstone Saturation Saturation index Sedimentary facies Sedimentary rocks Socioeconomic aspects socioeconomic development Sodium sodium adsorption ratio Sodium carbonate Solutes Terrestrial Pollution Water analysis Water quality Water sampling Water supply watersheds World Health Organization |
| title | Groundwater quality and its implications for domestic and agricultural water supplies in a semi-arid river basin of Niger |
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