Experimental determination of barium isotope fractionation during diffusion and adsorption processes at low temperatures

van Zuilen, Kirsten; Müller, Thomas; Nägler, Thomas; Dietzel, Martin; Küsters, Tim (2016). Experimental determination of barium isotope fractionation during diffusion and adsorption processes at low temperatures. Geochimica et cosmochimica acta, 186, pp. 226-241. Elsevier Science 10.1016/j.gca.2016.04.049

[img] Text
1-s2.0-S0016703716302186-main.pdf - Published Version
Restricted to registered users only
Available under License Publisher holds Copyright.

Download (939kB)

Variations in barium (Ba) stable isotope abundances measured in low and high temperature environments have recently received increasing attention. The actual processes controlling Ba isotope fractionation, however, remain mostly elusive. In this study, we present the first experimental approach to quantify the contribution of diffusion and adsorption on mass- dependent Ba isotope fractionation during transport of aqueous Ba2+ ions through a porous medium. Experiments have been carried out in which a BaCl2 solution of known isotopic composition diffused through u-shaped glass tubes filled with silica hydrogel at 10 C and 25 C for up to 201 days. The diffused Ba was highly fractionated by up to -2.15‰ in d137/134Ba, despite the low relative difference in atomic mass. The time-dependent isotope fractionation can be successfully reproduced by a diffusive transport model accounting for mass-dependent differences in the effective diffusivities of the Ba isotope species (D137Ba/D134Ba = (m134/m137)^b). Values of b extracted from the transport model were in the range of 0.010–0.011. Independently conducted batch experiments revealed that adsorption of Ba onto the surface of silica hydrogel favoured the heavier Ba isotopes (a = 1.00015 ± 0.00008). The contribution of adsorption on the overall isotope fractionation in the diffusion experiments, however, was found to be small. Our results contribute to the understanding of Ba isotope fractionation pro- cesses, which is crucial for interpreting natural isotope variations and the assessment of Ba isotope ratios as geochemical proxies.

Item Type:

Journal Article (Original Article)

Division/Institute:

08 Faculty of Science > Institute of Geological Sciences
08 Faculty of Science > Institute of Geological Sciences > Isotope Geology

UniBE Contributor:

van Zuilen, Kirsten, Nägler, Frank Thomas

Subjects:

500 Science > 550 Earth sciences & geology

ISSN:

0016-7037

Publisher:

Elsevier Science

Funders:

[4] Swiss National Science Foundation

Language:

English

Submitter:

Frank Thomas Nägler

Date Deposited:

21 Jun 2016 09:36

Last Modified:

02 Mar 2023 23:27

Publisher DOI:

10.1016/j.gca.2016.04.049

BORIS DOI:

10.7892/boris.82747

URI:

https://boris.unibe.ch/id/eprint/82747

Actions (login required)

Edit item Edit item
Provide Feedback