Titlebook: Applied Soil Hydrology; Viliam Novák,Hana Hlaváčiková Book 2019 Springer Nature Switzerland AG 2019 Soil moisture.Soil Water.Soil Water Mo

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https://doi.org/10.1007/1-4020-3776-7o water flow and water-potential distribution for various configurations of soil samples is described. The Darcian approach to saturated soil-water movement assumes the porous space is fully saturated with water; the soil pores do not change their dimensions, and soil temperature is constant. Hydrau

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https://doi.org/10.1007/1-4020-3776-7water can significantly improve the supply to plants of water and nutrients. A groundwater depth of about two metres below the soil surface is assumed to be the critical depth that contributes markedly to the supply of water to the plant canopy. In this chapter, the vertical transport of water from

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Springer Tracts in Civil Engineeringthods for evapotranspiration estimation, as well as the calculation methods to estimate its structural components: evaporation and transpiration. The basic equations of potential evapotranspiration calculation (the Penman equation) and actual evapotranspiration calculation (the Penman–Monteith equat