Lyell Collection

Geological Society, London, 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 Walling, D. E.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Geological Society, London, Special Publications; 1999; v. 163; p. 41-59;
DOI: 10.1144/GSL.SP.1999.163.01.04
© 1999 Geological Society of London

Contemporary Floodplain Process

Using fallout radionuclides in investigations of contemporary overbank sedimentation on the floodplains of British rivers

D. E. Walling

Department of Geography, University of Exeter, Exeter EX4 4RJ, UK

Increased interest in the functioning of river floodplains has generated the need for more information on rates and patterns of contemporary overbank sedimentation. Traditional approaches to documenting rates of overbank sedimentation on floodplains face many practical difficulties, but recent advances in the application of the fallout radionuclides 137Cs and unsupported 210Pb afford greatly increased potential for assembling such information. The potential for using these two radionuclides to investigate contemporary overbank sedimentation is demonstrated by considering examples drawn from recent work undertaken by the author and his co-workers on the floodplains of British rivers. These examples are used to illustrate (1) establishment of recent chronologies for sediment cores collected from river floodplains, (2) documentation of the spatial pattern of overbank sedimentation rates, (3) quantification of conveyance losses associated with overbank sedimentation, and (4) investigation of changing rates of overbank sedimentation over the past 100 years.