A short history of muddy floods
β Scribed by J. Boardman
- Book ID
- 102453435
- Publisher
- John Wiley and Sons
- Year
- 2010
- Tongue
- English
- Weight
- 88 KB
- Volume
- 21
- Category
- Article
- ISSN
- 1085-3278
- DOI
- 10.1002/ldr.1007
No coin nor oath required. For personal study only.
β¦ Synopsis
Abstract
The term βmuddy floodβ has been used widely in the lowland, arable areas of western and central Europe to describe muddy runoff from arable fields that causes damage to property. There is some evidence that muddy floods are much more frequent in the last two decades than previously. It is clear though that there is very substantial underβreporting of the phenomena even in areas where they have been recognised for 20 years e.g. UK and France. Reconstructions based on questionnaires, news media and local authority records have had some success in historical analysis of muddy flood frequency but there is still a huge data deficiency. Records from some countries are woefully lacking e.g. Germany, Spain and Italy.
Costs of muddy flooding are substantial especially in the loess belt of Belgium. The number of properties flooded in France suggests also that costs are high; similarly in England (UK) where costs for case studies are known but not for the country as a whole.
There are two quite different solutions to the problem of muddy flooding. Protection can be provided by engineering devices: retention ponds, dams, trenches. This is an βend of pipeβ solution with severe cost implications and risks with regard to the design return period. Alternatively, land use change on relatively small areas of catchments, can be shown to be effective at reducing floodβrisk hazard. A combination of the two has proved most effective at several sites in Europe. Copyright Β© 2010 John Wiley & Sons, Ltd.
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## Abstract Muddy floods, i.e. water flowing from agricultural fields and carrying large quantities of soil, affect routinely numerous municipalities of central Belgium, northern France and southern England. A comparison of flood frequency between different European regions is difficult, because of