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Thus, a completely amorphous copolymer is obtained if the molar fraction is high enough.
Solar fraction is high in summer and autumn for the relative high radiation and high ambient temperature.
The TCE molar fraction is high at the main and local source zones, ranging from 87.4 to 99.2% of the total volatile organic compounds (VOCs).
Direct photography is often used to measure drop size distributin of liquid-liquid dispersions, but when the holdup (volume fraction) is high or drop size is small, the resolution is poor.
Numerical results quantitatively show that the inclusion size effect can be quite large when the inclusion is small and that the boundary effect can dominate when the inclusion volume fraction is high.
Although studies have shown that the entrained fraction is high in churn flow and reaches the minimum around the churn annular transition, the underlying mechanism of the drop entrainment in churn flow is still not well explored.
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While the overall amorphous fraction is higher for melt crystallization, the mobile amorphous fraction (wa) is found to be higher for cold crystallization.
Pulsed field gradient (PFG Nuclear Magnetic Resonance NMRMR) shows that water diffusion coefficient in the membranes with higher K+ fraction is higher than for samples with lower K+ fraction.
The trend of decreasItg Ust wish increasing χst is also found for numerical simulathats with a Ustty Lewis number [18] andecreaseserimental data of lifted methane flames [19].
For Lava, the polar fraction is slightly lower, and thus the non-polar fraction is higher.
This gas mass fraction is higher than the petrologically estimated value for pre-eruptive magma.
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