污秽
发表于 2025-3-26 23:54:28
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珊瑚
发表于 2025-3-27 01:52:28
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匍匐
发表于 2025-3-27 08:37:58
Swelling and Shrinking Soils,ration into dry, heavy soils; they significantly increase the retention volume of such soils and the infiltration surface of water-filling soil cracks. The importance of water infiltration into the soil matrix from cracks surface is demonstrated.
Autobiography
发表于 2025-3-27 09:32:25
Water Repellent Soils,llency: contact angle, severity of water repellency, persistence of soil water repellency and index of water repellency. It also presents the hydrophobic compounds in soils and the influence of soil-water repellency on hydrological processes in soil (infiltration, preferential flow, evaporation).
Arb853
发表于 2025-3-27 16:26:12
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索赔
发表于 2025-3-27 19:18:13
Redistribution of Water in Homogeneous Soil,ary/initial conditions on the rate of redistribution. The quantification of the redistribution process by the solution of the Richards equation assuming constant hydraulic conductivity of soil demonstrates the logarithmic decrease of soil-water movement during redistribution, thus preserving soil water for plants.
Abrade
发表于 2025-3-27 23:18:48
Stony Soils,o contains links to the latest literature in this area. An illustrative example of the evaluation of effective stony-soil parameters for particular stony soil from the Western High Tatra Mts. (Slovakia) and results of the illustrative water-flow modelling in the stony soil (a case study) are presented and discussed.
致敬
发表于 2025-3-28 03:17:55
Soil Air and Its Dynamics,ith 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.
obnoxious
发表于 2025-3-28 10:07:00
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丰富
发表于 2025-3-28 10:51:42
https://doi.org/10.1007/1-4020-3776-7ary/initial conditions on the rate of redistribution. The quantification of the redistribution process by the solution of the Richards equation assuming constant hydraulic conductivity of soil demonstrates the logarithmic decrease of soil-water movement during redistribution, thus preserving soil water for plants.