Percolation theory generates a physically based description of tortuosity in saturated and unsaturated porous media

Soil Science Society of America Journal

Volumn 77, Issue 6, 2013, Pages 1920-1929

  Ghanbarian, Behzad ^a   Hunt, Allen G ^a   Sahimi, Muhammad ^b   Ewing, Robert P ^c   Skinner, Thomas E ^a  

^a WRIGHT STATE UNIVERSITY   (United States)

^b Univ of Southern California ^*  (United States)

^c IOWA STATE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CRITICAL WATER CONTENT; ELECTRICAL CONDUCTIVITY; FINITE SIZE SCALING; PERCOLATION THEORY; PHYSICAL MEANINGS; PORE CONNECTIVITY; POWER-LAW FUNCTIONS; UNSATURATED POROUS MEDIA;

FRACTAL DIMENSION; PERCOLATION (SOLID STATE);

POROUS MATERIALS;

HYDRAULIC CONDUCTIVITY; HYDROGEOLOGY; NUMERICAL MODEL; PERCOLATION; PHREATIC ZONE; POROUS MEDIUM; POWER LAW; SATURATION; TORTUOSITY; VADOSE ZONE; WATER CONTENT;

EID: 84891934837     PISSN: 03615995     EISSN: 14350661     Source Type: Journal    
DOI: 10.2136/sssaj2013.01.0089     Document Type: Article

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