The influence of stoniness and canopy properties on soil water content distribution: simulation of water movement in forest stony soil

Mountainous forest soils usually contain a large number of rock fragments (particle diameter >2 mm), which influence soil properties. Data characterizing hydraulic properties of these soils usually describe only the fine soil fraction (particle diameter

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Bibliographic Details
Published in:European journal of forest research 2012-11, Vol.131 (6), p.1727-1735
Main Authors: Novak, Viliam, Kava, Karol
Format: Article
Language:English
Subjects:
Biomedical and Life Sciences
Canopies
Climate change
Forest management
Forest soils
Forestry
Forests
Hydraulic properties
Interception
Life Sciences
Moisture content
Original Paper
Plant Ecology
Plant Sciences
Retention
Retention capacity
Rocks
Simulation
Soil dynamics
Soil formation
Soil properties
Soil types
Soil water movement
Soils
Stony soils
Water
Water content
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Description
Summary:Mountainous forest soils usually contain a large number of rock fragments (particle diameter >2 mm), which influence soil properties. Data characterizing hydraulic properties of these soils usually describe only the fine soil fraction (particle diameter
ISSN:1612-4669
1612-4677
DOI:10.1007/s10342-011-0589-y