dc.contributor.author | McCarter, Colin | |
dc.contributor.author | Rezanezhad, Fereidoun | |
dc.contributor.author | Gharedaghloo, Behrad | |
dc.contributor.author | Price, Jonathan S. | |
dc.contributor.author | Van Cappellen, P. | |
dc.date.accessioned | 2020-01-06 16:55:43 (GMT) | |
dc.date.available | 2020-01-06 16:55:43 (GMT) | |
dc.date.issued | 2019-08 | |
dc.identifier.uri | https://doi.org/10.1016/j.jconhyd.2019.103497 | |
dc.identifier.uri | http://hdl.handle.net/10012/15405 | |
dc.description | The final publication is available at Elsevier via https://doi.org/10.1016/j.jconhyd.2019.103497. © 2019. This manuscript version is made available under the CC-BY-NC-ND 4.0 license
http://creativecommons.org/licenses/by-nc-nd/4.0/ | en |
dc.description.abstract | The dual-porosity structure of peat and the extremely high organic matter content give rise to a complex medium that typically generates prolonged tailing and early 50% concentration breakthrough in the breakthrough curves (BTCs) of chloride (Cl−) and other anions. Untangling whether these observations are due to rate-limited (physical) diffusion into inactive pores, (chemical) adsorption or anion exclusion remains a critical question in peat hydrogeochemistry. This study aimed to elucidate whether Cl− is truly conservative in peat, as usually assumed, and whether the prolonged tailing and early 50% concentration breakthrough of Cl− observed is due to diffusion, adsorption, anion exclusion or a combination of all three. The mobile-immobile (MiM) dual-porosity model was fit to BTCs of Cl− and deuterated water measured on undisturbed cores of the same peat soils, and equilibrium Cl− adsorption batch experiments were conducted. Adsorption of Cl− to undecomposed and decomposed peat samples in batch experiments followed Freundlich isotherms but did not exhibit any trends with the degree of peat decomposition and sorption became negligible below aqueous Cl− concentrations of ~310 mg L−1. The dispersivity determined by fitting the Cl− BTCs whether assuming adsorption or no adsorption were significantly different than determined by the deuterated water (p < .0001). However, no statistical differences in dispersivity (p = .27) or immobile water content (p = .97) was observed between deuterated water and Cl− when accounting for anion exclusion. A higher degree of decomposition significantly increased anion exclusion (p < .0001) but did not influence the diffusion of either tracer into the immobile porosity. Contrary to previous assumptions, Cl− is not truly conservative in peat due to anion exclusion, and adsorption at higher aqueous concentrations, but the overall effect of anion exclusion on transport is likely minimal. | en |
dc.description.sponsorship | The authors acknowledge funding through the Canada Excellence Research Chair (CERC) program to PVC. | en |
dc.language.iso | en | en |
dc.publisher | Elsevier | en |
dc.rights | Attribution-NonCommercial-NoDerivatives 4.0 International | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/4.0/ | * |
dc.subject | conservative tracer | en |
dc.subject | breakthrough curve | en |
dc.subject | equilibrium adsorption | en |
dc.subject | pore structure | en |
dc.subject | solute transport | en |
dc.title | Transport of chloride and deuterated water in peat: The role of anion exclusion, diffusion, and anion adsorption in a dual porosity organic media | en |
dc.type | Article | en |
dcterms.bibliographicCitation | C.P.R. McCarter, F. Rezanezhad, B. Gharedaghloo, et al., Transport of chloride and deuterated water in peat: The role of anion exclusion, diffusion, and anion adsorption in a dual porosity organic media, Journal of Contaminant Hydrology, https://doi.org/10.1016/j.jconhyd.2019.103497 | en |
uws.contributor.affiliation1 | Faculty of Environment | en |
uws.contributor.affiliation1 | Faculty of Science | en |
uws.contributor.affiliation2 | Earth and Environmental Sciences | en |
uws.contributor.affiliation2 | Geography and Environmental Management | en |
uws.contributor.affiliation2 | Water Institute | en |
uws.typeOfResource | Text | en |
uws.peerReviewStatus | Reviewed | en |
uws.scholarLevel | Faculty | en |
uws.scholarLevel | Graduate | en |