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Thermal groundwater movement and radionuclide transport in SW England

Published online by Cambridge University Press:  05 July 2018

E. M. Durrance
Affiliation:
Department of Geology, University of Exeter, Devon, UK
M. J. Heath
Affiliation:
Department of Geology, University of Exeter, Devon, UK

Abstract

Heat flow in SW England is well above average for the UK as a whole, but northwards towards Bath and Bristol the values decrease rapidly. However, hot springs occur both in the Bath-Bristol area and in mines in Cornwall. The development of hydrothermal circulation systems is thus not controlled entirely by geothermal gradient: the presence of a suitable fracture permeability is the main requirement. The thermal ‘head’ produced, which nevertheless depends upon the temperature and volume of water in the system, theoretically can exceed local topographic heads even in areas of low geothermal gradient.

Thermal groundwaters usually carry above average quantities of radioelements in solution because of the long residence times involved. 222Rn values are often particularly high. High concentrations of 222Rn in surface waters arise from the discharge of groundwater. The results of a survey of 222Rn in streams in SW England have established areas of high values which are interpreted as rising limbs of convection cells with dimensions in the order of 5–10 km.

In SE Devon γ-ray spectrometry of soils shows two E.-W. belts of high activity. The northern is coincident with the faulted southern margin of the Crediton Trough, while the southern is coincident with the westerly extension of the Abbotsbury fault system. Groundwater movement along deep-seated fracture systems is considered to be the explanation of these features. The horizontal scale of the area involved suggests that a thermal rather than local topographic head is the driving force. Groundwater circulation within fractures, driven by a thermal head, may therefore occur even in areas of low geothermal gradient and should be considered when selecting waste disposal sites.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1985

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References

Adams, J. A. S., and Gasparini, P. (1970) Gamma ray Spectrometry of Rocks. Elsevier, Amsterdam.Google Scholar
Alderton, D., and Sheppard, S. (1977) Trans. Inst. Mining. Metall. 86B, 191-4.Google Scholar
Andrews, J. N., Burgess, W. G., Edmunds, W. M., Kay, R. L. F., and Lee, D. J. (1982) Nature, 298, 339-43.CrossRefGoogle Scholar
Batchelor, A. S. (1980) Unpubl. summary of informal workshop on the Cornubian batholith. Camborne School of Mines, Cornwall.Google Scholar
Bristow, C. M. (1977) A review of the evidence for the origin of the kaolin deposits in S.W. England. Proc. 8th International Kaolin Symposium and Meeting on Alunite, MadridRome.Google Scholar
Cassidy, J. (1982) A gamma-radiometric survey of the northern units of the Leinster granite. Geological Survey of Ireland Report 82/1.Google Scholar
Cermak, V. (1979) In Terrestrial Heat Flow in Europe (Cermak, V. and Rybach, L., eds.). Springer-Verlag, Berlin, 340.CrossRefGoogle Scholar
Dearman, W. R. (1963) Proc. Geol. Assoc. Lond. 74, 265-87.CrossRefGoogle Scholar
Donaldson, I. G. (1968) Proc. Third Annual Conference on Hydraulics and Fluid Mechanics, 200-4.Google Scholar
Duncan, J. M., Witherspoon, P. A., Mitchell, J. K., Watkins, D. J., Hardcastle, J. H., and Chen, J. C. (1972) Seepage and groundwater effects associated with explosive cratering. Univ. California, Berkeley, Report TE-72.2.Google Scholar
Durrance, E. M. (1978) Proc. Ussher Soc. 4, 220-8.Google Scholar
Durrance, E. M. (1983) Radiological indications of hydrothermal circulation in South East Devon. Ph.D. Thesis, Univ. Exeter.Google Scholar
Durrance, E. M. (1984) Uranium in the New Red Sandstone of South East Devon. Proc. Ussher Soc. (in press).Google Scholar
Bromley, A. V., Bristow, C. M., Heath, M. J., and Penman, J. M. (1982) Ibid. 5, 304-20.Google Scholar
Elder, J. (1981) Geothermal Systems. Academic Press, London.Google Scholar
Fehn, U., Cathles, L. M., and Holland, H. D. (1978) Econ. Geol. 73, 1556-66.CrossRefGoogle Scholar
Garg, S. K., and Kassoy, D. R. (1981) In Geothermal Systems (Ryback, L. and Muffler, L. J. P., eds.). Wiley, Chichester.Google Scholar
Garnish, J. D. (1976) Geothermal Energy: the case for research in the United Kingdom, Energy Paper 9, HMSO London.Google Scholar
Goyal, K. P. (1978) Heat and mass transfer in a saturated porous medium with application to geothermal reservoirs. Ph.D. Thesis, Univ. of Colorado, Boulder, Colorado.Google Scholar
Goyal, K. P. and Kassoy, D. R. (1977) A fault controlled model of the Mesa anomaly. Proc. Third Workshop on Geo-thermal Reservoir Engineering, Stanford University, Stanford, California, 209-13.Google Scholar
Haenal, R. (1980) Atlas of Subsurface Temperatures in the European Community. Commission of the European Communities. Directorate for Research, Science and Education, Brussels.Google Scholar
Heath, M. J. (1982) Uranium in the Dartmoor granite: Geochemical and Radiogeologicat investigations in relation to the South West England Geothermal Anomaly. Ph.D. Thesis, Univ. Exeter.Google Scholar
Heath, M. J. (1985) Mineral. Mag. 49, 233-44.CrossRefGoogle Scholar
Kassoy, D. R., and Zebib, A. (1978) J. Fluid Mech. 88, 769-92.CrossRefGoogle Scholar
Louis, C. (1970) Water flows in fissured rock and their effects on the stability of rock massifs. Lawrence Liver-more Laboratory, Livermore, California. Report UCRL TRANS 10469 (English translation of dissertation, Univ. Karlsruhe, Germany, 1967).Google Scholar
Lovhorg, L. (1972) In Uranium Prospecting Handbook. Inst. Ming. MetalL London (Bowie, S. H. U., Davis, M., and Ostle, D., eds.). 157-73.Google Scholar
Lovhorg, L., Wollenberg, H., Sorensen, P., and Hansen, J. (1971) Econ. Geol. 66, 368-84.Google Scholar
Melville, R. V., and Freshney, E. C. (1982) British Regional Geology: The Hampshire Basin and adjoining areas. HMSO, London.Google Scholar
Mogro-Campero, A., and Fleischer, R. L. (1977) Earth Planet. Sci. Lett. 34, 321-5.CrossRefGoogle Scholar
Richardson, S. W., and Oxhurgh, E. R. (1979) Nature, 282, 565-7.CrossRefGoogle Scholar
Rybach, L. (1981) In Geothermal Systems (Ryback, L. and Muffler, L. J. P., eds.). Wiley, Chichester, 336.Google Scholar
Sheppard, S. M. F. (1977) J. geol. Soc. Lond. 133, 573-91.CrossRefGoogle Scholar
Wheildon, J., Fracis, M. F., Ellis, J. R. L., and Thomas-Betts, A. (1980) Explanation and Interpretation of the S.W. England geothermal anomaly. Preprint. Seminar on Geothermal Energy, Strasbourg.CrossRefGoogle Scholar
Wittke, W. (1973) Intern. Assoc. Eng. Geol. 7, 3-28.CrossRefGoogle Scholar