VZJ
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 21 May 2009
Published in Vadose Zone J 8:404-410 (2009)
DOI: 10.2136/vzj2008.0044
© 2009 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Supplemental Video
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Mumford, K. G.
Right arrow Articles by Dickson, S. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Mumford, K. G.
Right arrow Articles by Dickson, S. E.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Mumford, K. G.
Right arrow Articles by Dickson, S. E.
Related Collections
Right arrow Chlorinated Hydrocarbons
Right arrow Multiphase Fluid Flow
Right arrow Unstable Flow/Fingering

ORIGINAL RESEARCH

New Observations of Gas-Phase Expansion above a Dense Nonaqueous Phase Liquid Pool

Kevin G. Mumforda, James E. Smitha,* and Sarah E. Dicksona

a Dep. of Civil Engineering, McMaster Univ., Hamilton, ON, Canada, L8S 4L7. J. E. Smith, School of Geography and Earth Sciences, McMaster Univ., Hamilton, ON, Canada, L8S 4L7
* Corresponding author (smithja{at}mcmaster.ca).

Received 25 February 2008.

The partitioning of volatile dense nonaqueous phase liquid (DNAPL) compounds to a discontinuous gas phase results in the repeated expansion, fragmentation, and vertical mobilization of gas clusters. This process has the potential to significantly affect the dissolution of DNAPL source zones and the characterization of DNAPL-contaminated sites, but has not been included in common conceptual models. This study presents new observations of discontinuous gas-phase growth above a 1,1,1-trichloroethane pool in a two-dimensional flow cell packed with 1.1-mm diameter sand. In contrast to the behavior observed in coarse glass beads, these visualization results show that the gas phase evolves as a collection of macroscopic fingers, composed of multiple trapped and disconnected gas clusters, and that the growth rate of these fingers is faster at the leading edge of the DNAPL pool due to the stripping of dissolved gases. These results provide valuable information for the incorporation of discontinuous gas phases in our evolving conceptual models of DNAPL source zones.

Abbreviations: DNAPL, dense nonaqueous phase liquid • REV scale, representative elementary volume scale • 1,1,1-TCA, 1,1,1-trichloroethane • TCE, trichloroethene







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2009 by the Soil Science Society of America.