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The flow mechanism in the Chalk based on radio-isotope analyses of groundwater in the London Basin

Journal of Hydrology

By:
, , and

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Abstract

14C analyses of groundwaters from the Chalk of the London Basin are re-interpreted and the age of the groundwater is revised. Radio-isotope analyses are used to examine the flow mechanism in the aquifer. The evidence supports the view that a network of micro-fissures and larger intergranular pores in the matrix provides a significant part of the water pumped from Chalk wells and the major fissures distribute the water to the wells. Most of the matrix is fine-grained and contains a very old water. This diffuses into the micro-fissures and larger pores and is carried to the wells by the major fissures. ?? 1979.

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
The flow mechanism in the Chalk based on radio-isotope analyses of groundwater in the London Basin
Series title:
Journal of Hydrology
Volume
40
Issue:
1-2
Year Published:
1979
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Journal of Hydrology
First page:
67
Last page:
83
Number of Pages:
17