Palacký University Olomouc, Faculty of Science, Joint Laboratory of Optics of Palacký University and Institute of Physics of the Czech Academy of Sciences, 17. listopadu 1192/12, 779 00 Olomouc, Czech Republic
Palacký University Olomouc, Faculty of Science, Joint Laboratory of Optics of Palacký University and Institute of Physics of the Czech Academy of Sciences, 17. listopadu 1192/12, 779 00 Olomouc, Czech Republic
Tomáš Fürst
Palacký University in Olomouc, Dpt. Mathematical Analysis and Applications of Mathematics, Faculty of Science, Olomouc 771 46, Czech Republic
Rostislav Vodák
Palacký University in Olomouc, Dpt. Mathematical Analysis and Applications of Mathematics, Faculty of Science, Olomouc 771 46, Czech Republic
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Total article views: 4,806 (including HTML, PDF, and XML)
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Total article views: 2,805 (including HTML, PDF, and XML)
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When rain falls on the ground, most of the water subsequently flows through the soil. The movement of water through the partially wet soil layer is surprisingly complicated. For decades, no mathematical model has been able to capture this process in its entire complexity. Here, we present a model that aims to solve this long-standing problem. In this paper, we show that the model correctly reproduces the transition between diffusion and preferential flow regimes.
When rain falls on the ground, most of the water subsequently flows through the soil. The...
