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Relating soil solution Zn concentration to DGT measurements in contaminated soils.

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Relating soil solution Zn concentration to DGT measurements in contaminated soils. / Degryse, Fien; Smolders, Erik; Oliver, Ian et al.
In: Environmental Science and Technology, Vol. 37, No. 17, 01.09.2003, p. 3958-3965.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Degryse, F, Smolders, E, Oliver, I & Zhang, H 2003, 'Relating soil solution Zn concentration to DGT measurements in contaminated soils.', Environmental Science and Technology, vol. 37, no. 17, pp. 3958-3965. https://doi.org/10.1021/es034075p

APA

Degryse, F., Smolders, E., Oliver, I., & Zhang, H. (2003). Relating soil solution Zn concentration to DGT measurements in contaminated soils. Environmental Science and Technology, 37(17), 3958-3965. https://doi.org/10.1021/es034075p

Vancouver

Degryse F, Smolders E, Oliver I, Zhang H. Relating soil solution Zn concentration to DGT measurements in contaminated soils. Environmental Science and Technology. 2003 Sept 1;37(17):3958-3965. doi: 10.1021/es034075p

Author

Degryse, Fien ; Smolders, Erik ; Oliver, Ian et al. / Relating soil solution Zn concentration to DGT measurements in contaminated soils. In: Environmental Science and Technology. 2003 ; Vol. 37, No. 17. pp. 3958-3965.

Bibtex

@article{3a889e7bf96a4df5840265ef467ddd37,
title = "Relating soil solution Zn concentration to DGT measurements in contaminated soils.",
abstract = "The technique of diffusive gradients in thin films (DGT) has been suggested to sample an available fraction of metals in soil. The objectives of this study were to compare DGT measurements with commonly measured fractions of Zn in soil, viz, the soil solution concentration and the total Zn concentration. The DGT technique was used to measure fluxes and interfacial concentrations of Zn in three series of field-contaminated soils collected in transects toward galvanized electricity pylons and in 15 soils amended with ZnCl2 at six rates. The ratio of DGT-measured concentration to pore water concentration of Zn, R, varied between 0.02 and 1.52 (mean 0.29). This ratio decreased with decreasing distribution coefficient, Kd, of Zn in the soil, which is in agreement with the predictions of the DGT-induced fluxes in soils (DIFS) model. The R values predicted with the DIFS model were generally larger than the observed values in the ZnCl2-amended soils at the higher Zn rates. A modification of the DIFS model indicated that saturation of the resin gel was approached in these soils, despite the short deployment times used (2 h). The saturation of the resin with Zn did not occur in the control soils (no Zn salt added) or the field-contaminated soils. Pore water concentration of Zn in these soils was predicted from the DGT-measured concentration and the total Zn content. Predicted values and observations were generally in good agreement. The pore water concentration was more than 5 times underpredicted for the most acid soil (pH = 3) and for six other soils, for which the underprediction was attributed to the presence of colloidal Zn in the soil solution.",
author = "Fien Degryse and Erik Smolders and Ian Oliver and Hao Zhang",
year = "2003",
month = sep,
day = "1",
doi = "10.1021/es034075p",
language = "English",
volume = "37",
pages = "3958--3965",
journal = "Environmental Science and Technology",
issn = "0013-936X",
publisher = "American Chemical Society",
number = "17",

}

RIS

TY - JOUR

T1 - Relating soil solution Zn concentration to DGT measurements in contaminated soils.

AU - Degryse, Fien

AU - Smolders, Erik

AU - Oliver, Ian

AU - Zhang, Hao

PY - 2003/9/1

Y1 - 2003/9/1

N2 - The technique of diffusive gradients in thin films (DGT) has been suggested to sample an available fraction of metals in soil. The objectives of this study were to compare DGT measurements with commonly measured fractions of Zn in soil, viz, the soil solution concentration and the total Zn concentration. The DGT technique was used to measure fluxes and interfacial concentrations of Zn in three series of field-contaminated soils collected in transects toward galvanized electricity pylons and in 15 soils amended with ZnCl2 at six rates. The ratio of DGT-measured concentration to pore water concentration of Zn, R, varied between 0.02 and 1.52 (mean 0.29). This ratio decreased with decreasing distribution coefficient, Kd, of Zn in the soil, which is in agreement with the predictions of the DGT-induced fluxes in soils (DIFS) model. The R values predicted with the DIFS model were generally larger than the observed values in the ZnCl2-amended soils at the higher Zn rates. A modification of the DIFS model indicated that saturation of the resin gel was approached in these soils, despite the short deployment times used (2 h). The saturation of the resin with Zn did not occur in the control soils (no Zn salt added) or the field-contaminated soils. Pore water concentration of Zn in these soils was predicted from the DGT-measured concentration and the total Zn content. Predicted values and observations were generally in good agreement. The pore water concentration was more than 5 times underpredicted for the most acid soil (pH = 3) and for six other soils, for which the underprediction was attributed to the presence of colloidal Zn in the soil solution.

AB - The technique of diffusive gradients in thin films (DGT) has been suggested to sample an available fraction of metals in soil. The objectives of this study were to compare DGT measurements with commonly measured fractions of Zn in soil, viz, the soil solution concentration and the total Zn concentration. The DGT technique was used to measure fluxes and interfacial concentrations of Zn in three series of field-contaminated soils collected in transects toward galvanized electricity pylons and in 15 soils amended with ZnCl2 at six rates. The ratio of DGT-measured concentration to pore water concentration of Zn, R, varied between 0.02 and 1.52 (mean 0.29). This ratio decreased with decreasing distribution coefficient, Kd, of Zn in the soil, which is in agreement with the predictions of the DGT-induced fluxes in soils (DIFS) model. The R values predicted with the DIFS model were generally larger than the observed values in the ZnCl2-amended soils at the higher Zn rates. A modification of the DIFS model indicated that saturation of the resin gel was approached in these soils, despite the short deployment times used (2 h). The saturation of the resin with Zn did not occur in the control soils (no Zn salt added) or the field-contaminated soils. Pore water concentration of Zn in these soils was predicted from the DGT-measured concentration and the total Zn content. Predicted values and observations were generally in good agreement. The pore water concentration was more than 5 times underpredicted for the most acid soil (pH = 3) and for six other soils, for which the underprediction was attributed to the presence of colloidal Zn in the soil solution.

U2 - 10.1021/es034075p

DO - 10.1021/es034075p

M3 - Journal article

VL - 37

SP - 3958

EP - 3965

JO - Environmental Science and Technology

JF - Environmental Science and Technology

SN - 0013-936X

IS - 17

ER -