The infinite dilution diffusion coefficient for A1(OH)4- at 25°C

James E. Mackin; Robert C. Aller

doi:10.1016/0016-7037(83)90162-X

The infinite dilution diffusion coefficient for A1(OH)₄^- at 25°C

James E. Mackin
, Robert C. Aller

Office of the Dean SOMAS

The University of Chicago

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14 Scopus citations

Abstract

The infinite dilution diffusion coefficient for Al(OH)₄^- necessary to calculate fluxes of dissolved Al between sediments and overlying waters, was determined at 25°C. Measurements were made using the diaphragm-cell method by diffusing Al(OH)₄^- spiked KBr solutions against KCL over a range of ionic strengths. The mean of 9 separate measurements gives 1.04 ± .02 × 10^-5cm²/s as the infinite dilution diffusion coefficient for Al(OH)₄^- at 25°C.

Original language	English
Pages (from-to)	959-961
Number of pages	3
Journal	Geochimica et Cosmochimica Acta
Volume	47
Issue number	5
DOIs	https://doi.org/10.1016/0016-7037(83)90162-X
State	Published - May 1983

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title = "The infinite dilution diffusion coefficient for A1(OH)4- at 25°C",

abstract = "The infinite dilution diffusion coefficient for Al(OH)4- necessary to calculate fluxes of dissolved Al between sediments and overlying waters, was determined at 25°C. Measurements were made using the diaphragm-cell method by diffusing Al(OH)4- spiked KBr solutions against KCL over a range of ionic strengths. The mean of 9 separate measurements gives 1.04 ± .02 × 10-5cm2/s as the infinite dilution diffusion coefficient for Al(OH)4- at 25°C.",

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AU - Aller, Robert C.

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N2 - The infinite dilution diffusion coefficient for Al(OH)4- necessary to calculate fluxes of dissolved Al between sediments and overlying waters, was determined at 25°C. Measurements were made using the diaphragm-cell method by diffusing Al(OH)4- spiked KBr solutions against KCL over a range of ionic strengths. The mean of 9 separate measurements gives 1.04 ± .02 × 10-5cm2/s as the infinite dilution diffusion coefficient for Al(OH)4- at 25°C.

AB - The infinite dilution diffusion coefficient for Al(OH)4- necessary to calculate fluxes of dissolved Al between sediments and overlying waters, was determined at 25°C. Measurements were made using the diaphragm-cell method by diffusing Al(OH)4- spiked KBr solutions against KCL over a range of ionic strengths. The mean of 9 separate measurements gives 1.04 ± .02 × 10-5cm2/s as the infinite dilution diffusion coefficient for Al(OH)4- at 25°C.

UR - https://www.scopus.com/pages/publications/0021083916

U2 - 10.1016/0016-7037(83)90162-X

DO - 10.1016/0016-7037(83)90162-X

M3 - Article

AN - SCOPUS:0021083916

SN - 0016-7037

VL - 47

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JO - Geochimica et Cosmochimica Acta

JF - Geochimica et Cosmochimica Acta

IS - 5

ER -

The infinite dilution diffusion coefficient for A1(OH)₄^- at 25°C

Abstract

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