The spatial distribution of groundwater flooding in a chalk catchment in southern England

Groundwater flooding occurred in the upper parts of many chalk rivers in the UK during the exceptionally wet winter of 2000–01. This provided a rare opportunity to investigate the spatial distribution of groundwater discharge and flooding along the normally dry intermittent headwaters of a chalk cat...

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Bibliographic Details
Published inHydrological processes Vol. 18; no. 5; pp. 959 - 971
Main Authors Finch, J. W., Bradford, R. B., Hudson, J. A.
Format Journal Article
LanguageEnglish
Published Chichester, UK John Wiley & Sons, Ltd 15.04.2004
Wiley
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Summary:Groundwater flooding occurred in the upper parts of many chalk rivers in the UK during the exceptionally wet winter of 2000–01. This provided a rare opportunity to investigate the spatial distribution of groundwater discharge and flooding along the normally dry intermittent headwaters of a chalk catchment. The extent of flooding along the River Pang, upstream of the seasonal head, was mapped using aerial photography, and point measurements of flow and water temperature were used to identify the contributing reaches of the river. The results are discussed in the context of the geological and groundwater conditions. The occurrence of flooding can largely be explained by the regional groundwater flow directions, but increased flow in some locations may be as a result of preferential groundwater flow along lines of geological structure. Published by John Wiley & Sons, Ltd.
Bibliography:istex:DE260520E4AB928083C163D049E3BF2988D9DAE4
ArticleID:HYP1340
ark:/67375/WNG-JRM0WCFS-3
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0885-6087
1099-1085
DOI:10.1002/hyp.1340