Copper binding by dissolved organic matter: I. Suwannee River fulvic acid equilibria
A cupric ion-selective electrode measured free Cu in solutions of Suwannee River fulvic acid (FA) in a series of 30 titrations carried out both at variable and at constant (5.14, 7.00, 8.44) pH. Total Cu varied 0.1–100 μM, dissolved organic carbon (DOC) 1–10 mg C/l, Ca and Mg 0–10 mM, and ionic stre...
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Veröffentlicht in: | Geochim. Cosmochim. Acta; (United States) 1988, Vol.52 (1), p.185-193 |
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creator | Cabaniss, S.E. Shuman, M.S. |
description | A cupric ion-selective electrode measured free Cu in solutions of Suwannee River fulvic acid (FA) in a series of 30 titrations carried out both at variable and at constant (5.14, 7.00, 8.44) pH. Total Cu varied 0.1–100 μM, dissolved organic carbon (DOC) 1–10 mg C/l, Ca and Mg 0–10 mM, and ionic strength 0.005–0.1. Copper complexation by FA is first order in DOC for 1–10 mg C/liter, and variable-order in pH. Increasing Ca
++ or Mg
++ from 0 to 10 mM slightly increases Cu
++ activity, while increasing ionic strength from 0.005 to 0.1 significantly increases Cu
++ activity. An empirical
N-
site
model was calibrated using a pooled set of six titrations with varying pH and DOC. Five binding components of varying proton dependence predict Cu binding by FA over a range of pH, DOC and total Cu in two verification tests of the model parameters. Parameters in this and other models tested are only empirical constructs. |
doi_str_mv | 10.1016/0016-7037(88)90066-X |
format | Article |
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++ or Mg
++ from 0 to 10 mM slightly increases Cu
++ activity, while increasing ionic strength from 0.005 to 0.1 significantly increases Cu
++ activity. An empirical
N-
site
model was calibrated using a pooled set of six titrations with varying pH and DOC. Five binding components of varying proton dependence predict Cu binding by FA over a range of pH, DOC and total Cu in two verification tests of the model parameters. Parameters in this and other models tested are only empirical constructs.</description><identifier>ISSN: 0016-7037</identifier><identifier>EISSN: 1872-9533</identifier><identifier>DOI: 10.1016/0016-7037(88)90066-X</identifier><language>eng</language><publisher>United States: Elsevier Ltd</publisher><subject>580400 - Geochemistry- (-1989) ; CALCIUM IONS ; CARBON IONS ; CHARGED PARTICLES ; CHEMICAL ANALYSIS ; CHEMICAL COMPOSITION ; CHEMICAL REACTIONS ; CHEMISTRY ; COPPER IONS ; EQUILIBRIUM ; FULVIC ACIDS ; GEOCHEMISTRY ; GEOSCIENCES ; IONS ; MAGNESIUM IONS ; MATHEMATICAL MODELS ; MOLECULAR MODELS ; ORGANIC ACIDS ; ORGANIC COMPOUNDS ; PH VALUE ; RIVERS ; STOICHIOMETRY ; STREAMS ; SURFACE WATERS ; WATER CHEMISTRY</subject><ispartof>Geochim. Cosmochim. Acta; (United States), 1988, Vol.52 (1), p.185-193</ispartof><rights>1988</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a300t-bc0f26ddaff2f5f6d74344bf6e2d8230019a9c6089bbf21facd61fa30cc6a94f3</citedby><cites>FETCH-LOGICAL-a300t-bc0f26ddaff2f5f6d74344bf6e2d8230019a9c6089bbf21facd61fa30cc6a94f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/0016-7037(88)90066-X$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,885,3548,4021,27921,27922,27923,45993</link.rule.ids><backlink>$$Uhttps://www.osti.gov/biblio/7222736$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Cabaniss, S.E.</creatorcontrib><creatorcontrib>Shuman, M.S.</creatorcontrib><creatorcontrib>Univ. of North Carolina, Chapel Hill (USA)</creatorcontrib><title>Copper binding by dissolved organic matter: I. Suwannee River fulvic acid equilibria</title><title>Geochim. Cosmochim. Acta; (United States)</title><description>A cupric ion-selective electrode measured free Cu in solutions of Suwannee River fulvic acid (FA) in a series of 30 titrations carried out both at variable and at constant (5.14, 7.00, 8.44) pH. Total Cu varied 0.1–100 μM, dissolved organic carbon (DOC) 1–10 mg C/l, Ca and Mg 0–10 mM, and ionic strength 0.005–0.1. Copper complexation by FA is first order in DOC for 1–10 mg C/liter, and variable-order in pH. Increasing Ca
++ or Mg
++ from 0 to 10 mM slightly increases Cu
++ activity, while increasing ionic strength from 0.005 to 0.1 significantly increases Cu
++ activity. An empirical
N-
site
model was calibrated using a pooled set of six titrations with varying pH and DOC. Five binding components of varying proton dependence predict Cu binding by FA over a range of pH, DOC and total Cu in two verification tests of the model parameters. Parameters in this and other models tested are only empirical constructs.</description><subject>580400 - Geochemistry- (-1989)</subject><subject>CALCIUM IONS</subject><subject>CARBON IONS</subject><subject>CHARGED PARTICLES</subject><subject>CHEMICAL ANALYSIS</subject><subject>CHEMICAL COMPOSITION</subject><subject>CHEMICAL REACTIONS</subject><subject>CHEMISTRY</subject><subject>COPPER IONS</subject><subject>EQUILIBRIUM</subject><subject>FULVIC ACIDS</subject><subject>GEOCHEMISTRY</subject><subject>GEOSCIENCES</subject><subject>IONS</subject><subject>MAGNESIUM IONS</subject><subject>MATHEMATICAL MODELS</subject><subject>MOLECULAR MODELS</subject><subject>ORGANIC ACIDS</subject><subject>ORGANIC COMPOUNDS</subject><subject>PH VALUE</subject><subject>RIVERS</subject><subject>STOICHIOMETRY</subject><subject>STREAMS</subject><subject>SURFACE WATERS</subject><subject>WATER CHEMISTRY</subject><issn>0016-7037</issn><issn>1872-9533</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1988</creationdate><recordtype>article</recordtype><recordid>eNp9kEtLxDAUhYMoOI7-AxfBheiimkcnaV0IMvgCQfAB7kKa3Gik04xJO-K_N3XEpZtzN985nHsQ2qfkhBIqTkmWQhIuj6rquCZEiOJlA01oJVlRzzjfRJM_ZBvtpPROCJGzGZmgp3lYLiHixnfWd6-4-cLWpxTaFVgc4qvuvMEL3fcQz_DtCX4cPnXXAeAHv8o2N7SrDGjjLYaPwbe-iV7voi2n2wR7v3eKnq8un-Y3xd399e384q7QnJC-aAxxTFirnWNu5oSVJS_LxglgtmIZobWujSBV3TSOUaeNFVk5MUbounR8ig7WuSH1XiXjezBvJuR-pleSMSa5yNDhGlrG8DFA6tXCJwNtqzsIQ1KUy0pKyjNYrkETQ0oRnFpGv9DxS1Gixp3VOKIaR1RVpX52Vi_Zdr62Qf505SGORaAzYH0ce9jg_w_4BldJhR8</recordid><startdate>1988</startdate><enddate>1988</enddate><creator>Cabaniss, S.E.</creator><creator>Shuman, M.S.</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>OTOTI</scope></search><sort><creationdate>1988</creationdate><title>Copper binding by dissolved organic matter: I. Suwannee River fulvic acid equilibria</title><author>Cabaniss, S.E. ; Shuman, M.S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a300t-bc0f26ddaff2f5f6d74344bf6e2d8230019a9c6089bbf21facd61fa30cc6a94f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1988</creationdate><topic>580400 - Geochemistry- (-1989)</topic><topic>CALCIUM IONS</topic><topic>CARBON IONS</topic><topic>CHARGED PARTICLES</topic><topic>CHEMICAL ANALYSIS</topic><topic>CHEMICAL COMPOSITION</topic><topic>CHEMICAL REACTIONS</topic><topic>CHEMISTRY</topic><topic>COPPER IONS</topic><topic>EQUILIBRIUM</topic><topic>FULVIC ACIDS</topic><topic>GEOCHEMISTRY</topic><topic>GEOSCIENCES</topic><topic>IONS</topic><topic>MAGNESIUM IONS</topic><topic>MATHEMATICAL MODELS</topic><topic>MOLECULAR MODELS</topic><topic>ORGANIC ACIDS</topic><topic>ORGANIC COMPOUNDS</topic><topic>PH VALUE</topic><topic>RIVERS</topic><topic>STOICHIOMETRY</topic><topic>STREAMS</topic><topic>SURFACE WATERS</topic><topic>WATER CHEMISTRY</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Cabaniss, S.E.</creatorcontrib><creatorcontrib>Shuman, M.S.</creatorcontrib><creatorcontrib>Univ. of North Carolina, Chapel Hill (USA)</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>OSTI.GOV</collection><jtitle>Geochim. Cosmochim. Acta; (United States)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Cabaniss, S.E.</au><au>Shuman, M.S.</au><aucorp>Univ. of North Carolina, Chapel Hill (USA)</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Copper binding by dissolved organic matter: I. Suwannee River fulvic acid equilibria</atitle><jtitle>Geochim. Cosmochim. Acta; (United States)</jtitle><date>1988</date><risdate>1988</risdate><volume>52</volume><issue>1</issue><spage>185</spage><epage>193</epage><pages>185-193</pages><issn>0016-7037</issn><eissn>1872-9533</eissn><abstract>A cupric ion-selective electrode measured free Cu in solutions of Suwannee River fulvic acid (FA) in a series of 30 titrations carried out both at variable and at constant (5.14, 7.00, 8.44) pH. Total Cu varied 0.1–100 μM, dissolved organic carbon (DOC) 1–10 mg C/l, Ca and Mg 0–10 mM, and ionic strength 0.005–0.1. Copper complexation by FA is first order in DOC for 1–10 mg C/liter, and variable-order in pH. Increasing Ca
++ or Mg
++ from 0 to 10 mM slightly increases Cu
++ activity, while increasing ionic strength from 0.005 to 0.1 significantly increases Cu
++ activity. An empirical
N-
site
model was calibrated using a pooled set of six titrations with varying pH and DOC. Five binding components of varying proton dependence predict Cu binding by FA over a range of pH, DOC and total Cu in two verification tests of the model parameters. Parameters in this and other models tested are only empirical constructs.</abstract><cop>United States</cop><pub>Elsevier Ltd</pub><doi>10.1016/0016-7037(88)90066-X</doi><tpages>9</tpages></addata></record> |
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source | ScienceDirect Journals (5 years ago - present) |
subjects | 580400 - Geochemistry- (-1989) CALCIUM IONS CARBON IONS CHARGED PARTICLES CHEMICAL ANALYSIS CHEMICAL COMPOSITION CHEMICAL REACTIONS CHEMISTRY COPPER IONS EQUILIBRIUM FULVIC ACIDS GEOCHEMISTRY GEOSCIENCES IONS MAGNESIUM IONS MATHEMATICAL MODELS MOLECULAR MODELS ORGANIC ACIDS ORGANIC COMPOUNDS PH VALUE RIVERS STOICHIOMETRY STREAMS SURFACE WATERS WATER CHEMISTRY |
title | Copper binding by dissolved organic matter: I. Suwannee River fulvic acid equilibria |
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