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Adsorption of Cs+ and IO3- ions by pseudoboehmite before and after the decomposition of citrate adsorbed on its surface
Citrate is distributed widely in the Earth's surface environments as a biological product released by microbes and plants. Citrate is also often used as a chelating agent for the selective dissolution of iron coatings and free iron oxides in soils. Adsorption experiments of Cs+ and IO3- before...
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Published in: | Clays and clay minerals 2018-08, Vol.66 (4), p.370-378 |
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description | Citrate is distributed widely in the Earth's surface environments as a biological product released by microbes and plants. Citrate is also often used as a chelating agent for the selective dissolution of iron coatings and free iron oxides in soils. Adsorption experiments of Cs+ and IO3- before and after the complexation of citrate with the pseudoboehmite surface were conducted to evaluate the effects of citrate on the adsorption of these ions on the surface of pseudoboehmite. Additional adsorption experiments of Cs+ and IO3- after the decomposition of citrate adsorbed on the pseudoboehmite surface were also performed to confirm the recovery of the original surface properties. Citrate decomposition was carried out by means of 10% H2O2 treatments at 75°C and pH 5, 7, and 9. The results indicated that citrate complexation decreased remarkably the adsorption of both Cs+ and IO- in the pH range 3-10, which was due to a decrease in the number of active charged sites available for adsorption of these ions. Decomposition of citrate adsorbed on the pseudoboehmite surface was found to be complete after three rounds of treatment with 10% H2O2 at 75°C and pH > 7. After the decomposition of citrate adsorbed on the pseudoboehmite surface, the adsorption of both Cs+ and IO3- was restored completely to the initial amounts before citrate complexation, and the inhibition effect of citrate on the adsorption of these ions disappeared under all pH conditions. |
doi_str_mv | 10.1346/CCMN.2018.064105 |
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Citrate is also often used as a chelating agent for the selective dissolution of iron coatings and free iron oxides in soils. Adsorption experiments of Cs+ and IO3- before and after the complexation of citrate with the pseudoboehmite surface were conducted to evaluate the effects of citrate on the adsorption of these ions on the surface of pseudoboehmite. Additional adsorption experiments of Cs+ and IO3- after the decomposition of citrate adsorbed on the pseudoboehmite surface were also performed to confirm the recovery of the original surface properties. Citrate decomposition was carried out by means of 10% H2O2 treatments at 75°C and pH 5, 7, and 9. The results indicated that citrate complexation decreased remarkably the adsorption of both Cs+ and IO- in the pH range 3-10, which was due to a decrease in the number of active charged sites available for adsorption of these ions. Decomposition of citrate adsorbed on the pseudoboehmite surface was found to be complete after three rounds of treatment with 10% H2O2 at 75°C and pH > 7. After the decomposition of citrate adsorbed on the pseudoboehmite surface, the adsorption of both Cs+ and IO3- was restored completely to the initial amounts before citrate complexation, and the inhibition effect of citrate on the adsorption of these ions disappeared under all pH conditions.</description><identifier>ISSN: 0009-8604</identifier><identifier>EISSN: 1552-8367</identifier><identifier>DOI: 10.1346/CCMN.2018.064105</identifier><language>eng</language><publisher>Cham: Clay Minerals Society</publisher><subject>adsorption ; alkali metals ; Biogeosciences ; boehmite ; cesium ; chemical properties ; citrates ; clay mineralogy ; complexing ; Earth and Environmental Science ; Earth Sciences ; experimental studies ; Geochemistry ; iron oxides ; Medicinal Chemistry ; metals ; Mineralogy ; Nanoscale Science and Technology ; oxides ; rock, sediment, soil ; sed rocks, sediments ; Sedimentary petrology ; Soil Science & Conservation</subject><ispartof>Clays and clay minerals, 2018-08, Vol.66 (4), p.370-378</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute. Reference includes data from GeoScienceWorld @Alexandria, VA @USA @United States. Abstract, Copyright, Clay Minerals Society</rights><rights>Clay Minerals Society 2018</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-g163t-21c80b45cf824e2eb7e6dcfb3ad55ad6c3773c40b9bc921a861113cb2ac585d63</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27922,27923</link.rule.ids></links><search><creatorcontrib>Kawano, Motoharu</creatorcontrib><creatorcontrib>Yamada, Eri</creatorcontrib><title>Adsorption of Cs+ and IO3- ions by pseudoboehmite before and after the decomposition of citrate adsorbed on its surface</title><title>Clays and clay minerals</title><addtitle>Clays Clay Miner</addtitle><description>Citrate is distributed widely in the Earth's surface environments as a biological product released by microbes and plants. Citrate is also often used as a chelating agent for the selective dissolution of iron coatings and free iron oxides in soils. Adsorption experiments of Cs+ and IO3- before and after the complexation of citrate with the pseudoboehmite surface were conducted to evaluate the effects of citrate on the adsorption of these ions on the surface of pseudoboehmite. Additional adsorption experiments of Cs+ and IO3- after the decomposition of citrate adsorbed on the pseudoboehmite surface were also performed to confirm the recovery of the original surface properties. Citrate decomposition was carried out by means of 10% H2O2 treatments at 75°C and pH 5, 7, and 9. The results indicated that citrate complexation decreased remarkably the adsorption of both Cs+ and IO- in the pH range 3-10, which was due to a decrease in the number of active charged sites available for adsorption of these ions. Decomposition of citrate adsorbed on the pseudoboehmite surface was found to be complete after three rounds of treatment with 10% H2O2 at 75°C and pH > 7. After the decomposition of citrate adsorbed on the pseudoboehmite surface, the adsorption of both Cs+ and IO3- was restored completely to the initial amounts before citrate complexation, and the inhibition effect of citrate on the adsorption of these ions disappeared under all pH conditions.</description><subject>adsorption</subject><subject>alkali metals</subject><subject>Biogeosciences</subject><subject>boehmite</subject><subject>cesium</subject><subject>chemical properties</subject><subject>citrates</subject><subject>clay mineralogy</subject><subject>complexing</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>experimental studies</subject><subject>Geochemistry</subject><subject>iron oxides</subject><subject>Medicinal Chemistry</subject><subject>metals</subject><subject>Mineralogy</subject><subject>Nanoscale Science and Technology</subject><subject>oxides</subject><subject>rock, sediment, soil</subject><subject>sed rocks, sediments</subject><subject>Sedimentary petrology</subject><subject>Soil Science & Conservation</subject><issn>0009-8604</issn><issn>1552-8367</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid/><recordid>eNpFkEtLw0AUhQdRsFb3LmdfUuedZFmC2kK1G12Hedy0U9pMmEkp_nsTq7i6cDjfufAh9EjJnHKhnqrq7X3OCC3mRAlK5BWaUClZVnCVX6MJIaTMCkXELbpLaU8IU4KzCTovXAqx631ocWhwlWZYtw6vNjzDQ5aw-cJdgpMLJsDu6HvABpoQ4aemmx4i7neAHdhw7ELyf0vW91EPbT3uG3B4iH2fcDrFRlu4RzeNPiR4-L1T9Pny_FEts_XmdVUt1tmWKt5njNqCGCFtUzABDEwOytnGcO2k1E5ZnufcCmJKY0tGdaEopdwapq0spFN8iuhlN3XRt1uI9T6cYju8rCmpR3P1aK4ezdUXcwMzuzBbCMl6aC2cQzy4f3Rol_XgkAnBvwEO_3Gq</recordid><startdate>20180801</startdate><enddate>20180801</enddate><creator>Kawano, Motoharu</creator><creator>Yamada, Eri</creator><general>Clay Minerals Society</general><general>Springer International Publishing</general><scope/></search><sort><creationdate>20180801</creationdate><title>Adsorption of Cs+ and IO3- ions by pseudoboehmite before and after the decomposition of citrate adsorbed on its surface</title><author>Kawano, Motoharu ; Yamada, Eri</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-g163t-21c80b45cf824e2eb7e6dcfb3ad55ad6c3773c40b9bc921a861113cb2ac585d63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>adsorption</topic><topic>alkali metals</topic><topic>Biogeosciences</topic><topic>boehmite</topic><topic>cesium</topic><topic>chemical properties</topic><topic>citrates</topic><topic>clay mineralogy</topic><topic>complexing</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>experimental studies</topic><topic>Geochemistry</topic><topic>iron oxides</topic><topic>Medicinal Chemistry</topic><topic>metals</topic><topic>Mineralogy</topic><topic>Nanoscale Science and Technology</topic><topic>oxides</topic><topic>rock, sediment, soil</topic><topic>sed rocks, sediments</topic><topic>Sedimentary petrology</topic><topic>Soil Science & Conservation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kawano, Motoharu</creatorcontrib><creatorcontrib>Yamada, Eri</creatorcontrib><jtitle>Clays and clay minerals</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kawano, Motoharu</au><au>Yamada, Eri</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Adsorption of Cs+ and IO3- ions by pseudoboehmite before and after the decomposition of citrate adsorbed on its surface</atitle><jtitle>Clays and clay minerals</jtitle><stitle>Clays Clay Miner</stitle><date>2018-08-01</date><risdate>2018</risdate><volume>66</volume><issue>4</issue><spage>370</spage><epage>378</epage><pages>370-378</pages><issn>0009-8604</issn><eissn>1552-8367</eissn><abstract>Citrate is distributed widely in the Earth's surface environments as a biological product released by microbes and plants. Citrate is also often used as a chelating agent for the selective dissolution of iron coatings and free iron oxides in soils. Adsorption experiments of Cs+ and IO3- before and after the complexation of citrate with the pseudoboehmite surface were conducted to evaluate the effects of citrate on the adsorption of these ions on the surface of pseudoboehmite. Additional adsorption experiments of Cs+ and IO3- after the decomposition of citrate adsorbed on the pseudoboehmite surface were also performed to confirm the recovery of the original surface properties. Citrate decomposition was carried out by means of 10% H2O2 treatments at 75°C and pH 5, 7, and 9. The results indicated that citrate complexation decreased remarkably the adsorption of both Cs+ and IO- in the pH range 3-10, which was due to a decrease in the number of active charged sites available for adsorption of these ions. Decomposition of citrate adsorbed on the pseudoboehmite surface was found to be complete after three rounds of treatment with 10% H2O2 at 75°C and pH > 7. After the decomposition of citrate adsorbed on the pseudoboehmite surface, the adsorption of both Cs+ and IO3- was restored completely to the initial amounts before citrate complexation, and the inhibition effect of citrate on the adsorption of these ions disappeared under all pH conditions.</abstract><cop>Cham</cop><pub>Clay Minerals Society</pub><doi>10.1346/CCMN.2018.064105</doi><tpages>9</tpages></addata></record> |
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source | Springer Nature:Jisc Collections:Springer Nature Read and Publish 2023-2025: Springer Reading List |
subjects | adsorption alkali metals Biogeosciences boehmite cesium chemical properties citrates clay mineralogy complexing Earth and Environmental Science Earth Sciences experimental studies Geochemistry iron oxides Medicinal Chemistry metals Mineralogy Nanoscale Science and Technology oxides rock, sediment, soil sed rocks, sediments Sedimentary petrology Soil Science & Conservation |
title | Adsorption of Cs+ and IO3- ions by pseudoboehmite before and after the decomposition of citrate adsorbed on its surface |
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