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

R.A. Downing; F.J. Pearson; D. B. Smith

doi:10.1016/0022-1694(79)90088-x

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

R.A. Downing·F.J. Pearson·D. B. Smith

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Abstract

14 C 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.

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Journal of Hydrology Article

Source-reported bounding extent: 51.5027068477811° to 51.789943291380695° latitude; -0.2450492943921745° to 1.0281677944668104° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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R.A. Downing, F.J. Pearson, D. B. Smith. 1979. The flow mechanism in the Chalk based on radio-isotope analyses of groundwater in the London Basin. https://doi.org/10.1016/0022-1694(79)90088-x

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