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 Soulsby, R. L.
Right arrow Articles by Wild, B. R.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Geological Society, London, Special Publications; 2007; v. 274; p. 65-72;
DOI: 10.1144/GSL.SP.2007.274.01.08
© 2007 Geological Society of London

A model for simulating the dispersal tracks of sand grains in coastal areas: ‘SandTrack’

R. L. Soulsby, C. T. Mead & B. R. Wild

HR Wallingford, Howbery Park, Wallingford, Oxon OX10 8BA, UK (email: rls{at}hrwallingford.co.uk)

A new model is described that simulates the paths taken by a large number of identified (‘tagged’) sand grains in coastal areas in response to waves and currents. A number of practical applications require such a Lagrangian approach, as distinct from the more traditional Eulerian calculations of the transport rates of bulk quantities of identical, non-tagged, grains. Such applications might include studies on the dispersal of dredged spoil, or on the release of contaminated particulate material.

The particle-tracking algorithm determining the movement of tagged grains takes account of the following processes:

A novel method of simulating these processes has been devised, by formulating functions to parameterize each of them, and then specifying a grain speed as the product of the functions. The particle-tracking algorithm is implemented within HR Wallingford's SEDPLUME-RW model, originally devised to track the dispersal of muddy sediments. This in turn is driven by currents and waves computed by the hydrodynamic model TELEMAC. A validation exercise simulating dispersal of radioactive sand tracer measured in the 1960s in Morecambe Bay is described.