TY - JOUR
T1 - Soil-Gas Phase Transport and Structure Parameters for a Soil Under Different Management Regimes and at Two Moisture Levels
AU - Eden, Marie
AU - Møldrup, Per
AU - Schjønning, Per
AU - Scow, Kate M.
AU - de Jonge, Lis Wollesen
PY - 2012/9
Y1 - 2012/9
N2 - Measurements of diffusive and convective gas transport parameters can be used to describe soil functional architecture and reveal key factors for soil structure development. Undisturbed 100-cm(3) soil samples were sampled at the Long-term Research on Agricultural Systems experiment located at the University of California, Davis. The 18 plots used in this study represented fairly wide ranges in organic carbon (0. 0072-0.0153 kg kg(-1)) and clay (0.30-0.44 kg kg(-1)). Soil-air permeability, k(a), and soil-gas diffusivity, D-P/D-0, were determined at field-moist conditions (fin) and, subsequently, after saturation and drainage to - 100 cm of matric potential (pF2). Gas diffusivity in intact samples at fm conditions exhibited a general, linear relationship with air-filled porosity (epsilon), independent of soil texture and treatment. Comparing intact and repacked samples drained to pF2, repacked soil displayed markedly lower D-P/D-0 values at similar air-filled porosity, illustrating soil structure effects on D-P/D-0. The Currie tortuosity-connectivity parameter, X=Log(D-P/D-0)/Log(epsilon), decreased with increasing bulk density in the intact samples at both moisture conditions, suggesting less tortuous and well-connected pathways for gas diffusion at higher bulk density. Pore organization, PO = k(a) / epsilon, showed a treatment effect with typically higher values for the organic plots, implying that an improved possibility for formation of organomineral soil aggregates resulted in better-connected macropore networks. Fitting a linear model to D-P/D-0 versus epsilon measurements revealed different slopes at the two moisture conditions, suggesting short-term nonsingularity (hysteretic) effects after rewetting and drainage.
AB - Measurements of diffusive and convective gas transport parameters can be used to describe soil functional architecture and reveal key factors for soil structure development. Undisturbed 100-cm(3) soil samples were sampled at the Long-term Research on Agricultural Systems experiment located at the University of California, Davis. The 18 plots used in this study represented fairly wide ranges in organic carbon (0. 0072-0.0153 kg kg(-1)) and clay (0.30-0.44 kg kg(-1)). Soil-air permeability, k(a), and soil-gas diffusivity, D-P/D-0, were determined at field-moist conditions (fin) and, subsequently, after saturation and drainage to - 100 cm of matric potential (pF2). Gas diffusivity in intact samples at fm conditions exhibited a general, linear relationship with air-filled porosity (epsilon), independent of soil texture and treatment. Comparing intact and repacked samples drained to pF2, repacked soil displayed markedly lower D-P/D-0 values at similar air-filled porosity, illustrating soil structure effects on D-P/D-0. The Currie tortuosity-connectivity parameter, X=Log(D-P/D-0)/Log(epsilon), decreased with increasing bulk density in the intact samples at both moisture conditions, suggesting less tortuous and well-connected pathways for gas diffusion at higher bulk density. Pore organization, PO = k(a) / epsilon, showed a treatment effect with typically higher values for the organic plots, implying that an improved possibility for formation of organomineral soil aggregates resulted in better-connected macropore networks. Fitting a linear model to D-P/D-0 versus epsilon measurements revealed different slopes at the two moisture conditions, suggesting short-term nonsingularity (hysteretic) effects after rewetting and drainage.
KW - ORGANIC-MATTER CONTENT
KW - PHYSICAL-PROPERTIES
UR - http://www.scopus.com/inward/record.url?scp=84866886316&partnerID=8YFLogxK
U2 - 10.1097/SS.0b013e318267ec85
DO - 10.1097/SS.0b013e318267ec85
M3 - Journal article
SN - 0038-075X
VL - 177
SP - 527
EP - 534
JO - Soil Science
JF - Soil Science
IS - 9
ER -