Determining the influence of stones on hydraulic conductivity of saturated soils using numerical method

Geoderma

Volumn 161, Issue 3-4, 2011, Pages 177-181

  Novák, Viliam ^a   Kňava, Karol ^a   Šimůnek, Jirka ^b  

^a INSTITUTE OF CHEMISTRY   (Slovakia)

^b UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

HYDRUS; Saturated hydraulic conductivity; Soil coarse fraction; Stony soil

Indexed keywords

DATA CHARACTERIZING; EMPIRICAL EQUATIONS; HYDRAULIC GRADIENTS; HYDRUS; NUMERICAL RESULTS; PARTICLE DIAMETERS; RETENTION PROPERTIES; ROCK FRAGMENTS; SATURATED HYDRAULIC CONDUCTIVITY; SATURATED SOILS; SOIL HYDRAULICS; SOIL WATER MOVEMENT; SPHERICAL SHAPE; STONY SOIL; TWO-DIMENSIONAL SIMULATIONS; WATER FLOWS;

COMPUTER SIMULATION; HYDRAULIC CONDUCTIVITY; NUMERICAL METHODS; PARTICLE SIZE; SOIL MOISTURE;

GEOLOGIC MODELS;

DIAMETER; HYDRAULIC CONDUCTIVITY; NUMERICAL MODEL; RETENTION; SATURATED MEDIUM; SOIL TEXTURE; STEADY-STATE EQUILIBRIUM; TWO-DIMENSIONAL MODELING;

CARPATHIANS; TATRA MOUNTAINS;

EID: 79951581165     PISSN: 00167061     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.geoderma.2010.12.016     Document Type: Article

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