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United States Department of Agriculture

Agricultural Research Service

Research Project: SALINITY AND TRACE ELEMENTS ASSOCIATED WITH WATER REUSE IN IRRIGATED SYSTEMS: PROCESSES, SAMPLING PROTOCOLS, AND SITE-SPECIFIC MANAGEMENT Title: Bromide Adsorption by Reference Minerals and Soils

Authors
item GOLDBERG, SABINE
item Kabengi, Nadine -

Submitted to: Vadose Zone Journal
Publication Type: Peer Reviewed Journal
Publication Acceptance Date: May 19, 2010
Publication Date: August 3, 2010
Repository URL: http://www.ars.usda.gov/SP2UserFiles/Place/53102000/pdf_pubs/P2330.pdf
Citation: Goldberg, S.R., Kabengi, N.J. 2010. Bromide Adsorption by Reference Minerals and Soils. Vadose Zone Journal. 9:780-786.

Interpretive Summary: Bromide has been used as a tracer, a substance that can be followed through the course of hydrogeologic processes. Bromide has been considered to be conservative. That is, it does not undergo chemical reactions but moves with the applied water. Our study evaluated the adsorption behavior of bromide on reference minerals and soils. We found that bromide undergoes adsorption at low solution pH and is therefore not likely to act conservatively. Our results are important to scientists designing transport studies because they indicate that careful evaluation of the pH regime of the study site is necessary before choosing bromide as the appropriate tracer.

Technical Abstract: Bromide, Br-, adsorption behavior was investigated on amorphous Al and Fe oxide, montmorillonite, kaolinite, and temperate and tropical soils. Bromide adsorption decreased with increasing solution pH with minimal adsorption occurring above pH 7. Bromide adsorption was higher for amorphous oxides than for clay minerals. Shifts in point of zero charge were observed on amorphous Al and Fe oxide following Br- adsorption suggesting an inner-sphere adsorption mechanism for Br- on these surfaces. Two chemical surface complexation models, the constant capacitance model and the triple layer model, were able to describe Br- adsorption as a function of solution pH on all materials. For the oxides and clay minerals and most of the soils the fit of the constant capacitance model, containing an inner-sphere adsorption mechanism was improved over that of the triple layer model, containing an outer-sphere adsorption mechanism, as measured by the overall variance, VY. Our results indicate that Br- would, most likely, not act as a conservative tracer at soil solution pH values below 7. Therefore, we suggest that researchers carefully evaluate the pH regime of their study site before assuming that Br- can be applied as a conservative tracer for transport experiments.

Last Modified: 9/10/2014
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