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

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發(fā)表于 2025-3-28 15:08:53 | 只看該作者
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發(fā)表于 2025-3-28 21:45:56 | 只看該作者
Eco-Efficiency in Industry and Scienceith an atmosphere. This chapter analyses the convection and diffusion of air in the soil and expresses them quantitatively. It also quantifies oxygen transport to the plant roots to cover respiration by solving the simplified transport equation. The influence of the oxygen diffusion rate on plant canopy growth is also presented.
43#
發(fā)表于 2025-3-29 01:13:01 | 只看該作者
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發(fā)表于 2025-3-29 04:05:58 | 只看該作者
978-3-030-13195-1Springer Nature Switzerland AG 2019
45#
發(fā)表于 2025-3-29 11:10:14 | 只看該作者
Applied Soil Hydrology978-3-030-01806-1Series ISSN 0924-6118 Series E-ISSN 2213-6940
46#
發(fā)表于 2025-3-29 13:17:03 | 只看該作者
Viliam Novák,Hana Hlavá?ikováPresents basic topics of soil hydrology clearly, making it suitable for a wide range of researchers and students.Extremely well illustrated and complemented with practical tables.Explores specific top
47#
發(fā)表于 2025-3-29 18:44:35 | 只看該作者
Theory and Applications of Transport in Porous Mediahttp://image.papertrans.cn/b/image/160141.jpg
48#
發(fā)表于 2025-3-29 20:11:22 | 只看該作者
https://doi.org/10.1007/1-4020-3776-7in the case of bare soil or the water table, the SPAC system is reduced to the Soil–Atmosphere Continuum (SAC) or to the Water-Table–Atmosphere Continuum (WAC). This chapter contains basic information about all three subsystems of SPAC. Conceptual approaches to the soil-water and energy transport ar
49#
發(fā)表于 2025-3-30 00:17:53 | 只看該作者
https://doi.org/10.1007/1-4020-3776-7s a three-phase system, composed of solid, liquid and gaseous components, the basic properties of all three phases are described and quantified. Definitions of soil porosity, specific bulk density, bulk density, aeration, soil water content and soil specific surface are presented. Soil texture is de
50#
發(fā)表于 2025-3-30 07:45:17 | 只看該作者
https://doi.org/10.1007/1-4020-3776-7imultaneously in all three phases: ice, liquid water and water vapour. Its dynamics are linked to the great expenditure of energy to keep in motion ‘the water cycle and thus stabilize Earth’s climatic conditions. Water’s occurrence and its movement are preconditions for biomass production. In this c
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