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The pore fraction slowly decreased as the rotation rate increased.
These two systems showed different pore fraction in N2 adsorption test, and displayed different mechanical behaviors in uniaxial tension test.
The thermal conductivity was found to be inversely related to the pore fraction.
While the model was consistent with the trends observed experimentally, the quantitative experimental results suggested that to attain an appreciable difference in release characteristics, both pore size and pore fraction should be changed for this system.
By introducing nano-sized hydrophilic acetylene black (HAB) powders into the HABPs, the porosity, hydrophilic pore fraction and wettability increase, while the tortuosity and hydrophilic pore size decrease, which results in higher permeated water flux.
Our modelling indicates that increasing the fraction of pores and/or crystals reduces the strength of volcanic rocks, and that increasing the pore fraction results in larger strength reductions than increasing the crystal fraction.
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When we express our numerical samples (more than 200 simulations spanning a wide range of crystal and pore fractions) in terms of ϕp′, we find that their strengths can be described by a single curve for a given pore diameter.
The macro-pore fraction was more sensitive than the micro-pore fraction to the application of organic amendments.
At higher PI (connected-pore fraction higher than 0.8), the DL/UL curve for POROS R1 showed double plateaus, whereas that for POROS R2 gave only one plateau.
Correlation analysis indicated that during the reclamation process higher levels of microbial respiration, SOC, water stable aggregates and macro-pore fraction were associated with greater soil hydraulic conductivity.
Higher microbial respiration and mineralization quotient (qmC) in the MSW-treated soils resulted in higher levels of water stable aggregates (WSA > 0.25 mm) and more macro-pore fraction, leading to greater hydraulic conductivity, with larger increases at the higher rate of application (i.e. 30 Mg ha− 1).
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