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

污穢

珊瑚

匍匐

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

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

索賠

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

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

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

豐富

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.