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Eriksson, Erik (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
In view of a recent work by Begemann & Libby (1957) their postulate on rapid mixing inside a groundwater body is examined. It is found that there are no possible processes which can accomplish such a mixing. Their observations can, however, be readily explained from a simple model of groundwater flow, assuming no mixing. Possible methods of using tracers like tritium for estimating groundwater storage are also discussed.DOI: 10.1111/j.2153-3490.1958.tb02035.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • 13EGEMANN, F., LIBBY, W. F., 1<)57: Continental water balance, groundwater inventory and storage times, surface ocean mixing rates and world-wide water circulation patterns from cosmic-ray and bomb tritium. Geochimica GIld Cosmochimica Acta. 12, pp 277-2<)6.
    • BOLIN, B., 195<): On the use of tritium as a tracer for water in nature. Proceedings Second U.N. Intern. Conf. on the Peaceful Uses of Atomic Energy Genopa. Vol 18.
    • VON BUTTLAR, H. & LIBBY, W. F., 1955: Natural distribution of cosmic-ray produced tritium. II. j. Inorg. Nucl. Chern. I, pp. 75-91.
    • ERIKSSON, E., 1<)5R: A note on the dispersion of a saltwater boundary ad vancing through saturated sand. to be published in Trans. Am. Geophys. Union.
    • GUSTAFSON, Y., 1<)46: Die Strornungsverhaltnisse in Gedranten Boden. Acta Agrie. Suet, II, 1-157.
    • KAUFMAN, W. j., ORLOB, G. T., 1<)56: An evaluation of groundwater tracers. Trans. Am. Geophys. Union. 37. pp 2'!7-301i.
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