Threshold water content beyond which hydrophobic soils become hydrophilic: The role of soil texture and organic matter content

Geoderma

Volumn 209-210, Issue , 2013, Pages 177-187

  Vogelmann, E S ^a   Reichert, J M ^a   Prevedello, J ^a   Consensa, C O B ^a   Oliveira, A É ^a   Awe, G O ^b   Mataix Solera, J ^c  

^a FEDERAL UNIVERSITY OF SANTA MARIA   (Brazil)

^b EKITI STATE UNIVERSITY   (Nigeria)

^c MIGUEL HERNÁNDEZ UNIVERSITY   (Spain)

Author keywords

Granulometric composition; Organic carbon; Soil moisture; Sorptivity; Water repellency

Indexed keywords

GRANULOMETRIC COMPOSITIONS; INCREASE IN WATER CONTENT; ORGANIC MATTER CONTENT; SOIL WATER REPELLENCY; SORPTIVITY; VOLUMETRIC WATER CONTENT; WATER REPELLENCY; WATER RETENTION CURVE;

BIOGEOCHEMISTRY; BIOLOGICAL MATERIALS; CONTACT ANGLE; HYDROPHILICITY; ORGANIC CARBON; ORGANIC COMPOUNDS; SOIL MOISTURE; SOIL SURVEYS; TEXTURES;

HYDROPHOBICITY;

BULK DENSITY; GRANULOMETRY; HYDROPHOBICITY; INFILTROMETER; ORGANIC MATTER; POROSITY; SOIL ORGANIC MATTER; SOIL TEXTURE; SOIL TYPE; SOIL WATER; SORPTION; THRESHOLD; WATER CONTENT; WATER RETENTION;

BRAZIL;

EID: 84880363731     PISSN: 00167061     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.geoderma.2013.06.019     Document Type: Article

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