Hostname: page-component-cd9895bd7-gvvz8 Total loading time: 0 Render date: 2024-12-23T16:28:00.805Z Has data issue: false hasContentIssue false
  • English
  • Français

The inifiltration rate into an aquifer determined from the dissolution of carbonate

Published online by Cambridge University Press:  01 May 2009

D. A. Spears  and
M. J. Reeves
D. A. Spears
Affiliation:
Department of GeologyUniversity of SheffieldSheffieldS1 3JD
M. J. Reeves
Affiliation:
Central Water Planning UnitReading Bridge HouseReadingRG1 8PS
Get access Rights & Permissions [Opens in a new window]

Summary

Changes attributable to weathering have been detected in Quaternary sediments overlying an important aquifer in the Vale of York. Solution of carbonates is quantitatively the most important effect of weathering. The amount of carbonate dissolved can be estimated from whole rock analyses. The length of time of weathering is known and an equivalent surface lowering rate for limestone can be calculated which is consistent with rates obtained by other workers.The volume of water required to give the observed compositional changes is calculated from porewater analyses. The time period is known and hence the rate of infiltration and the average recharge rate of the aquifer can be determined. The calculated rate of recharge is consistent with rates determined using other methods.

Type
Articles
Information
Geological Magazine , Volume 112 , Issue 6 , November 1975 , pp. 585 - 591
Copyright
Copyright © Cambridge University Press 1975

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Garrels, R. M. & Christ, C. L. 1965. Solutions, Minerals and equilibria. 450 pp. Harper & Row.Google Scholar
Gaunt, G. D., Jarvis, R. A. & Matthews, B. 1971. The late Weichselian sequence in the Vale of York. Proc. Yorks. geol. Soc. 38, 281–4.CrossRefGoogle Scholar
Goodchild, J. G. 1890. The weathering of limestones. Geol. Mag. 7, 463–6.CrossRefGoogle Scholar
Hughes, T., McK, . 1886. On some perched blocks and associated phenomena. Q. Jl geol. Soc. Lond. 42, 527–39.CrossRefGoogle Scholar
Krauskopf, K. B. 1967. Introduction to Geochemistry. McGraw-Hill.Google Scholar
Lamb, H. H., Lewis, R. P. W. & Woodroffe, A. 1966. Atmospheric circulation 8000–0 B.C. Proc. int. Symp. on World Climate 8000–0 B.C. R. met. Soc., Lond. 174–217.Google Scholar
Paces, T. 1973. Steady-state kinetics and equilibrium between groundwater and granitic rock. Geochim. cosmochim. Acta 37, 2641–63.CrossRefGoogle Scholar
Penny, L. F. 1974. Ch. 9, Quaternary. In Rayner, D. H. & Hemmingway, J. E. (Eds): The Geology and Mineral Resources of Yorkshire. pp. 405. Yorkshire Geological Society.Google Scholar
Piggott, G. D. 1965. The structure of limestone surfaces in Derbyshire, in ‘Denudation in Limestone Regions: A Symposium’. Geogrl J. 131, 41–4.CrossRefGoogle Scholar
Spears, D. A. & Reeves, M. J. (in press). The influence of superficial deposits on groundwater quality in the Vale of York. Q. Jl Engng Geol.Google Scholar
Sweeting, M. M. 1965. Introduction, in ‘Denudation in Limestone Regions: A Symposium’. Geogrl J. 131, 34–7.CrossRefGoogle Scholar
Turc, L. 1958. Le bilan d'eau des sols: relations entre les précipitations, l'évaporation et I'écoulement. C. r. des troisièmes journées de l'hydraulique, Soc. hydrotech. de France: Algiers, 36–44. Paris.Google Scholar
Water Resources Board (in the press). Groundwater Resources of the Vale of York.Google Scholar