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Автор Wiebenga, William A.
Автор Ellis, W. R.
Автор Kevi, L.
Дата выпуска 1970
dc.description During a laboratory investigation using radiotracers, empirical formulas were developed to replace the ambiguous or incorrect Dupuit‐Forchheimer assumption used in relationships governing the flow of water through porous, unconsolidated materials ranging from clay to coarse sands or fine gravels. The Dupuit‐Forchheimer assumption states that the ratio of specific flow rate to average flow velocity is equal to porosity, but it is not specified whether true porosity or void ratio or specific yield, also called effective porosity, is meant. The hydraulic conductivity shows a good correlation with the maximum 10% grain size, and the ratio of specific flow rate to average flow velocity shows good correlation with functions of specific yield and percentile sorting coefficient. From field measurements of specific flow rate and average flow velocity the specific yield can be computed.
Формат application.pdf
Копирайт Copyright 1970 by the American Geophysical Union.
Название Empirical Relations in Properties of Unconsolidated Quartz Sands and Silts Pertaining to Water Flow
Тип article
DOI 10.1029/WR006i004p01154
Electronic ISSN 1944-7973
Print ISSN 0043-1397
Журнал Water Resources Research
Том 6
Первая страница 1154
Последняя страница 1161
Выпуск 4
Библиографическая ссылка De Wiest, R. J. M., Geohydrology, 142, John Wiley, New York, 1965.
Библиографическая ссылка Ellis, W. R., L.Kevi, W. A.Wiebenga, The investigation of water flow through porous mediums by means of radio‐tracers, Water Resour. Res., 42, 413–416, 1968.
Библиографическая ссылка Guizerix, J., G.Grandclement, B.Gaillard, P.Ruby, Appareil pour la mesure des vitesses relatives des eaux souterraines par la méthode de dilution ponctuelle, Radioisotopes in hydrology, 25, International Atomic Energy Agency, Vienna, 1963.
Библиографическая ссылка Pettijohn, F. J., Sedimentary Rocks, 36–51, Harper, New York, 1957.
Библиографическая ссылка Scheidegger, A. E., The Physics of Flow through Porous Media, 313, University of Toronto Press, Toronto, 1963.
Библиографическая ссылка Swartzendruber, D., Non‐Darcy flow behavior, J. Geophys. Res., 6713 Fig. 2, 5208, 1962.
Библиографическая ссылка Todd, D. K., Groundwater Hydrology, 336, John Wiley, New York, 1959.
Библиографическая ссылка Wiebenga, W. A., W. R.Ellis, B. W.Seatonberry, J. T. G.Andrew, Radioisotopes as ground‐water tracers, J. Geophys. Res., 7216, 4081, 1967.
Библиографическая ссылка Young, H. D., Statistical Treatment of Experimental Data, 172, McGraw‐Hill, New York, 1962.

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