Determining effective diffusion coefficients of chlorohydrocarbons in natural clays: Unique results from highly resolved controlled release field experiments.

1D and 3D modelling Chlorinated solvents Controlled release field experiments Effective diffusion coefficients High resolution sampling Low permeability clay-rich sediments

Journal

Journal of contaminant hydrology
ISSN: 1873-6009
Titre abrégé: J Contam Hydrol
Pays: Netherlands
ID NLM: 8805644

Informations de publication

Date de publication:
10 2022
Historique:
received: 22 06 2022
revised: 15 08 2022
accepted: 06 09 2022
pubmed: 18 9 2022
medline: 5 10 2022
entrez: 17 9 2022
Statut: ppublish

Résumé

This study aims to precisely determine the effective diffusion coefficients of chlorohydrocarbons in low permeable units under in-situ field conditions. To this end, two controlled release field experiments using TCE and PCE as dense non-aqueous phase liquids (DNAPLs) were conducted in two natural clayey deposits. Several months to years after the controlled DNAPL release, highly resolved concentration profiles were determined for the chlorohydrocarbons that had diffused into the clayey deposits. Effective diffusion coefficients for TCE and PCE were then determined by calibrating a 3D numerical and 1D analytical model, respectively, to the measured high-resolution concentration profiles. The simulations revealed that the effective diffusion coefficients vary by as much as a factor of four within the same low permeability unit being consistent with observed small-scale heterogeneities. The determined chlorohydrocarbon effective diffusion coefficients were further used to determine the equivalent thickness of DNAPL that would completely dissolve in an idealized, parallel-plate fracture by diffusion transport into clayey deposits for the time periods of the controlled release field experiments. The equivalent TCE and PCE DNAPL film thicknesses ranged between 36 and 581 μm, respectively, comparable and exceeding fracture apertures measured in naturally fractured clay rich deposits. Hence, films of DNAPL initially contained within fractures in clay-rich deposits can completely dissolve away within a few months to a few years due to diffusion. This stored contaminant mass poses a risk to adjacent aquifers if it is re-released due to diffusion out of the matrix after source depletion or remediation.

Identifiants

pubmed: 36115173
pii: S0169-7722(22)00123-1
doi: 10.1016/j.jconhyd.2022.104075
pii:
doi:

Substances chimiques

Delayed-Action Preparations 0
Hydrocarbons, Chlorinated 0
Water Pollutants, Chemical 0
Trichloroethylene 290YE8AR51
Clay T1FAD4SS2M

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

104075

Informations de copyright

Copyright © 2022 The Authors. Published by Elsevier B.V. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of Competing Interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

Beth L Parker (BL)

Morwick G360 Groundwater Research Institute, College of Engineering and Physical Sciences, University of Guelph, 50 Stone Road East, Guelph, Ontario N1G 2W1, Canada.

John A Cherry (JA)

Morwick G360 Groundwater Research Institute, College of Engineering and Physical Sciences, University of Guelph, 50 Stone Road East, Guelph, Ontario N1G 2W1, Canada.

Philipp Wanner (P)

Department of Earth Sciences, University of Gothenburg, Guldhedsgatan 5A, 413 20 Gothenburg, Sweden. Electronic address: philipp.wanner@gu.se.

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Classifications MeSH