Nickel Speciation and Complexation Kinetics in Freshwater by Ligand Exchange and DPCSV

A technique of ligand exchange with DMG (dimethylglyoxime) and DPCSV was applied to determine Ni speciation in lake, river, and groundwater samples. The working conditions related to ligand-exchange equilibrium were optimized, and the ligand-exchange kinetics were examined. The observed pseudo-first...

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Published inEnvironmental science & technology Vol. 35; no. 3; pp. 539 - 546
Main Authors Xue, Han Bin, Jansen, Stefan, Prasch, Andreas, Sigg, Laura
Format Journal Article
LanguageEnglish
Published Washington, DC American Chemical Society 01.02.2001
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Abstract A technique of ligand exchange with DMG (dimethylglyoxime) and DPCSV was applied to determine Ni speciation in lake, river, and groundwater samples. The working conditions related to ligand-exchange equilibrium were optimized, and the ligand-exchange kinetics were examined. The observed pseudo-first-order rate, k obsd, was about 3 × 10-5 (s-1) for Ni(DMG)2 complex formation with an excess of DMG (μM) over Ni (nM) at pH 7.1−7.7. The second-order exchange kinetic constants, k exch, were between 1.2 × 102 and 5.7 × 103 s-1 M-1 for ligand exchange of NiEDTA with DMG and between 5 × 102 and 7 × 103 s-1 M-1 for exchange of natural ligands with DMG in the freshwater samples under similar conditions. Ni ligand exchange between natural ligands and DMG occurred over days with half-lifes of 5−95 h. Total dissolved Ni concentrations in samples from various freshwater systems in Switzerland ranged from 4 nM in an oligotrophic lake to 30 nM in a small river affected by inputs from sewage effluents and agriculture. Free ionic Ni2+ concentrations were determined in the range of 10-13−10-15 M (pNi =12.2−14.7), indicating that more than 99.9% of dissolved Ni was bound by organic ligands with strong affinity (log K 12.1−14.9) and low concentrations (13−100 nM) at pH 7.2−8.2. Because of slow ligand-exchange kinetics, Ni speciation in natural waters may in many cases not reach equilibrium.
AbstractList A technique of ligand exchange with DMG (dimethylglyoxime) and DPCSV was applied to determine Ni speciation in lake, river, and groundwater samples. The working conditions related to ligand-exchange equilibrium were optimized, and the ligand-exchange kinetics were examined. The observed pseudo-first-order rate, kobsd, was about 3 x 10-5 (s-1) for Ni(DMG)2 complex formation with an excess of DMG (M) over Ni (nM) at pH 7.1-7.7. The second-order exchange kinetic constants, kexch, were between 1.2 x 102 and 5.7 x 103 s-1 M-1 for ligand exchange of NiEDTA with DMG and between 5 x 102 and 7 x 103 s-1 M-1 for exchange of natural ligands with DMG in the freshwater samples under similar conditions. Ni ligand exchange between natural ligands and DMG occurred over days with half-lifes of 5-95 h. Total dissolved Ni concentrations in samples from various freshwater systems in Switzerland ranged from 4 nM in an oligotrophic lake to 30 nM in a small river affected by inputs from sewage effluents and agriculture. Free ionic Ni2 concentrations were determined in the range of 10-13-10-15 M (pNi =12.2-14.7), indicating that more than 99.9␘f dissolved Ni was bound by organic ligands with strong affinity (log K 12.1-14.9) and low concentrations (13-100 nM) at pH 7.2-8.2. Because of slow ligand-exchange kinetics, Ni speciation in natural waters may in many cases not reach equilibrium
A technique of ligand exchange with DMG (dimethylglyoxime) and DPCSV was applied to determine Ni speciation in lake, river, and groundwater samples. The working conditions related to ligand-exchange equilibrium were optimized, and the ligand-exchange kinetics were examined. The observed pseudo-first-order rate, k sub(obsd), was about 3 x 10 super(-5) (s super(-1)) for Ni(DMG) sub(2) complex formation with an excess of DMG ( mu M) over Ni (nM) at pH 7.1-7.7. The second-order exchange kinetic constants, k sub(exch), were between 1.2 x 10 super(2) and 5.7 x 10 super(3) s super(-1) M super(-1) for ligand exchange of NiEDTA with DMG and between 5 x 10 super(2) and 7 x 10 super(3) s super(-1) M super(-1) for exchange of natural ligands with DMG in the freshwater samples under similar conditions. Ni ligand exchange between natural ligands and DMG occurred over days with half-lifes of 5-95 h. Total dissolved Ni concentrations in samples from various freshwater systems in Switzerland ranged from 4 nM in an oligotrophic lake to 30 nM in a small river affected by inputs from sewage effluents and agriculture. Free ionic Ni super(2+) concentrations were determined in the range of 10 super(-13)-10 super(-15) M (pNi =12.2-14.7), indicating that more than 99.9% of dissolved Ni was bound by organic ligands with strong affinity (log K 12.1-14.9) and low concentrations (13-100 nM) at pH 7.2-8.2. Because of slow ligand-exchange kinetics, Ni speciation in natural waters may in many cases not reach equilibrium.
A technique of ligand exchange with DMG (dimethylglyoxime) and DPCSV was applied to determine Ni speciation in lake, river, and groundwater samples. The working conditions related to ligand-exchange equilibrium were optimized, and the ligand-exchange kinetics were examined. The observed pseudo-first-order rate, k obsd, was about 3 × 10-5 (s-1) for Ni(DMG)2 complex formation with an excess of DMG (μM) over Ni (nM) at pH 7.1−7.7. The second-order exchange kinetic constants, k exch, were between 1.2 × 102 and 5.7 × 103 s-1 M-1 for ligand exchange of NiEDTA with DMG and between 5 × 102 and 7 × 103 s-1 M-1 for exchange of natural ligands with DMG in the freshwater samples under similar conditions. Ni ligand exchange between natural ligands and DMG occurred over days with half-lifes of 5−95 h. Total dissolved Ni concentrations in samples from various freshwater systems in Switzerland ranged from 4 nM in an oligotrophic lake to 30 nM in a small river affected by inputs from sewage effluents and agriculture. Free ionic Ni2+ concentrations were determined in the range of 10-13−10-15 M (pNi =12.2−14.7), indicating that more than 99.9% of dissolved Ni was bound by organic ligands with strong affinity (log K 12.1−14.9) and low concentrations (13−100 nM) at pH 7.2−8.2. Because of slow ligand-exchange kinetics, Ni speciation in natural waters may in many cases not reach equilibrium.
A technique of ligand exchange with DMG (dimethylglyoxime) and DPCSV was applied to determine Ni speciation in lake, river, and groundwater samples. The working conditions related to ligand-exchange equilibrium were optimized, and the ligand-exchange kinetics were examined.
A technique of ligand exchange with DMG (dimethylglyoxime) and DPCSV was applied to determine Ni speciation in lake, river, and groundwater samples. The working conditions related to ligand-exchange equilibrium were optimized, and the ligand-exchange kinetics were examined. The observed pseudo-first-order rate, kobsd, was about 3 x 10(-5) (s-1) for Ni(DMG)2 complex formation with an excess of DMG (microM) over Ni (nM) at pH 7.1-7.7. The second-order exchange kinetic constants, kexch, were between 1.2 x 10(2) and 5.7 x 10(3) s-1 M-1 for ligand exchange of NiEDTA with DMG and between 5 x 10(2) and 7 x 10(3) s-1 M-1 for exchange of natural ligands with DMG in the freshwater samples under similar conditions. Ni ligand exchange between natural ligands and DMG occurred over days with half-lifes of 5-95 h. Total dissolved Ni concentrations in samples from various freshwater systems in Switzerland ranged from 4 nM in an oligotrophic lake to 30 nM in a small river affected by inputs from sewage effluents and agriculture. Free ionic Ni2+ concentrations were determined in the range of 10(-13)-10(-15) M (pNi = 12.2-14.7), indicating that more than 99.9% of dissolved Ni was bound by organic ligands with strong affinity (log K 12.1-14.9) and low concentrations (13-100 nM) at pH 7.2-8.2. Because of slow ligand-exchange kinetics, Ni speciation in natural waters may in many cases not reach equilibrium.
Author Jansen, Stefan
Sigg, Laura
Xue, Han Bin
Prasch, Andreas
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Issue 3
Keywords Complexation
Organic matter
Pollutant behavior
Geochemistry
Oxime
Stability constant
Nickel
Water pollution
Experimental study
Chemical reaction kinetics
Speciation
Heavy metal
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Snippet A technique of ligand exchange with DMG (dimethylglyoxime) and DPCSV was applied to determine Ni speciation in lake, river, and groundwater samples. The...
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SubjectTerms Applied sciences
Biological and physicochemical phenomena
Earth sciences
Earth, ocean, space
Engineering and environment geology. Geothermics
Environmental impact
Exact sciences and technology
Kinetics
Laboratorium voor Fysische chemie en Kolloïdkunde
Ligands
Metals
Models, Theoretical
Natural water pollution
Nickel - chemistry
Oximes
Physical Chemistry and Colloid Science
Pollution
Pollution, environment geology
Sewage
Soils
Switzerland
Water Pollutants - analysis
Water pollution
Water treatment and pollution
WIMEK
Title Nickel Speciation and Complexation Kinetics in Freshwater by Ligand Exchange and DPCSV
URI http://dx.doi.org/10.1021/es0014638
https://api.istex.fr/ark:/67375/TPS-8MNG3JRQ-P/fulltext.pdf
https://www.ncbi.nlm.nih.gov/pubmed/11351726
https://www.proquest.com/docview/230145715
https://search.proquest.com/docview/18022478
http://www.narcis.nl/publication/RecordID/oai:library.wur.nl:wurpubs%2F120813
Volume 35
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