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On the residence time distribution in idealized groundwatersheds
Journal of Hydrology, 1995The relative cumulative frequency distribution of residence times F(T) is calculated for an entire groundwatershed under steady-state conditions and assuming Dupuit-Forchheimer flow. It appears that F(T) is always the same: F(T) = 1 -exp(−TT), provided that the aquifer recharge rate and T are constant over the groundwatershed.
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INTERNAL AND EXTERNAL RESIDENCE-TIME DISTRIBUTIONS
Chemical Engineering Communications, 1983(1983). INTERNAL AND EXTERNAL RESIDENCE-TIME DISTRIBUTIONS. Chemical Engineering Communications: Vol. 22, No. 1-2, pp. 105-107.
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VARIATIONS IN RESIDENCE-TIME DISTRIBUTIONS
1971ALAN D. RANDOLPH, MAURICE A. LARSON
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The role of topography on catchment-scale water residence time
Water Resources Research, 2005Brian Mcglynn +2 more
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Residence time distribution studies using radiotracers in chemical industry—A review
Chemical Engineering Communications, 2018Avinash Chandra +2 more
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