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Pedological and hydropedological characteristics of soils
retention is preferential water flow in the soil. Sometimes, water flows throughIn the chapter there is an overview of opinions on preferential flow of water in soil, on retenti...
Hydrology
- 2018 •
- C
Rok uplatnění
C - Kapitola v odborné knize
Effect of soil fauna and flora on water infiltration and flow in a soil.
The results of tracer studies gave evidence that water flow is very often realised through preferential paths defined as vertically oriented flow paths that are usually wetter and carry more water per unit area tha...
DA - Hydrologie a limnologie
- 2003 •
- D
Rok uplatnění
D - Stať ve sborníku
Soil water regime in head water regions - observation, assessment and modelling.
alternative types of soil water movement: the diffusion type flow (DTF) in drier soilsand phase, the infiltrating rain water flows through the soil without causing any rain water accumul...
DA - Hydrologie a limnologie
- 2001 •
- Jx
Rok uplatnění
Jx - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
Visualization and quantification of water movement in the soil profile
Visualization of the flow of water in the soil and knowledge of preferential flow in the soil profile is currently considered as an important factor for describing the course of water infiltration...
GD - Hnojení, závlahy, zpracování půdy
- 2014 •
- Jx
Rok uplatnění
Jx - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
Hydromorphic soils and transport processes on slopes of Bohemian forest.
The occurence of slope water springs, occurence of less permeable layers, lateral water flow in different depth of profiles, transport of substancec with flowing water, occurence of inverse soil c...
DF - Pedologie
- 2005 •
- D
Rok uplatnění
D - Stať ve sborníku
Preferential Flow and Water Balance in the Vadose Zone
and of entrapped air significantly affects the water balance within the soil profile. Flow of preferential flow in the vadose zone, dual permeability soil water flow and solutePreferenti...
DA - Hydrologie a limnologie
- 2006 •
- D
Rok uplatnění
D - Stať ve sborníku
Capillary, Film, and Vapor Flow in Transient Bare Soil Evaporation (1): Identifiability Analysis of Hydraulic Conductivity in the Medium to Dry Moisture Range
conductivity caused by film flow on evaporation rate, cumulative water loss, soil temperature, and soil water pressure head during evaporation. Film flow extends, conductivity in this moisture ra...
Soil science
- 2021 •
- Jimp •
- Link
Rok uplatnění
Jimp - Článek v periodiku v databázi Web of Science
Výsledek na webu
Runoff from a small mountain basin due to soil water oversaturation
of old (soil) and new (rain) water in various stages of runoff is evaluated in the flowing water. The aim is to distinguish between old and new water flow in the closing with the soil on...
DA - Hydrologie a limnologie
- 2011 •
- D
Rok uplatnění
D - Stať ve sborníku
Estimation of vineyard soil structure and preferential flow using dye tracer, X-ray tomography, and numerical simulations
on water flow and solute transport in the soil vadose zone. The pore system is highly was to assess the porous system and preferential flow pathways in a vineyard soil using could reveal more information ...
Soil science
- 2020 •
- Jimp •
- Link
Rok uplatnění
Jimp - Článek v periodiku v databázi Web of Science
Výsledek na webu
Mesoscopic aspects of root water uptake modeling – hydraulic resistances and root geometry interpretations in plant transpiration analysis
In the context of soil water flow modeling, root water uptake is often evaluated based on water potential difference between the soil and the plant (the water. Insignificance of their dif...
DA - Hydrologie a limnologie
- 2016 •
- Jx •
- Link
Rok uplatnění
Jx - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
Výsledek na webu
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