2020
DOI: 10.1007/s12517-020-05898-3
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Well hydraulics of temporally varying artificial recharge with well clogging in confined aquifers

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Cited by 2 publications
(4 citation statements)
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“…The choices of an exponentially decayed K function above and the associated parameter values are based on previous experiment of Bianchi et al 14 . A similar K ‐ t function has also been adopted in some previous studies, 16–19 which can be regarded as a special case of the present study when K ∞ is equal to zero. The exponentially decayed K ‐ t function is also generally supported in laboratory and field tests 14,15,41,42 .…”
Section: Results Analysismentioning
confidence: 99%
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“…The choices of an exponentially decayed K function above and the associated parameter values are based on previous experiment of Bianchi et al 14 . A similar K ‐ t function has also been adopted in some previous studies, 16–19 which can be regarded as a special case of the present study when K ∞ is equal to zero. The exponentially decayed K ‐ t function is also generally supported in laboratory and field tests 14,15,41,42 .…”
Section: Results Analysismentioning
confidence: 99%
“…where K 0 and K ∞ are respectively the initial and asymptotic hydraulic conductivities [LT −1 ], λ is an adjustable parameter that denotes the reduction rate of permeability [T −1 ]. The choices of an exponentially decayed K function above and the associated parameter values are based on previous experiment of Bianchi et al 14 A similar K-t function has also been adopted in some previous studies, [16][17][18][19] which can be regarded as a special case of the present study when K ∞ is equal to zero. The exponentially decayed K-t function is also generally supported in laboratory and field tests.…”
Section: Solution Verificationmentioning
confidence: 99%
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