Lyell Collection

Geological Society, London, Engineering Geology Special Publications

Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help


Keywords:
Author:
Advanced search>>
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
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 Request Permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Broholm, K.
Right arrow Articles by Fredericia, J.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Geological Society, London, Engineering Geology Special Publications; 1998; v. 14; p. 197-204;
DOI: 10.1144/GSL.ENG.1998.014.01.23
© 1998 Geological Society of London

Section 5: Research on pollutant behaviour

Transport of dissolved creosote compounds through fractured clay: column and field experiments

K. Broholm1, P. J. Jørgensen2, A. B. Hansen3, B. Nilsson4, R. C. Sidle4, E. Arvin1 & J. Fredericia4

1 Institute of Environmental Science and Engineering, Technical University of Denmark, Building 115, DK-2800 Lyngby, Denmark
2 Danish Geotechnical Institute, Maglebjergvej 1 DK-2800 Lyngby, Denmark
3 National Environmental Research Institute, Frederiksborgvej 399, Postbox 358, DK-4000 Roskilde, Denmark
4 Danish and Greenland Geological Survey, Thoravej 8 DK-2400 Copenhagen NV, Denmark

Transport of selected creosote compounds and tracers in two column experiments and a field study in fractured clayey till are presented. Twenty-five organic compounds were used in the column experiments and 12 in the field experiment. This paper focuses on three organic compounds: phenol, naphthalene and dibenzofuran. One column was biologically inactive, and the other was biologically active with denitrifying conditions in the beginning and aerobic/denitrifying conditions later on in the experiment. The infiltration water at the field site was aerobic in the beginning and anaerobic (no oxygen, very little nitrate, and some sulphate) later. The results showed very rapid transport through clayey till of the tracers and the organic compounds. Despite the rapid transport through fractures, biodegradation may be an important process in fractured media at least for the easily degradable organic compounds.