Abstract
Infiltration is the process of water entry into soil; it is the basic process supplying the soil root zone with water. Infiltration as a process can be divided into two basic types: rain infiltration and ponding infiltration (infiltration from ponds on the soil surface). Infiltration (and cumulative infiltration) curves of both types of infiltration are described and expressed by empirical and analytical functions proposed by Philip. Special attention is devoted to the Green and Ampt approach to quantify infiltration because of its simplicity and clear physical interpretation of the process. The influences of the rain rate, entrapped air, initial soil-water content and layered soil profile on infiltration dynamics are discussed. Methods for the estimation of the soil hydraulic conductivity using the infiltration process in the field are described as well.
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Novák, V., Hlaváčiková, H. (2019). Infiltration of Water into Soil. In: Applied Soil Hydrology. Theory and Applications of Transport in Porous Media, vol 32. Springer, Cham. https://doi.org/10.1007/978-3-030-01806-1_10
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DOI: https://doi.org/10.1007/978-3-030-01806-1_10
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