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In all countries, a very small fraction of the population is at work before 8.00 a.m. and the fraction is highest between 9.00 a.m. and 16.00 p.m.
At these three sites, cyanolichen coverage is well below 5%% and the amount of the bare soil fraction is highest at the Swedish Öland site, followed by the Tabernas site (Fig. 6a).
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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.
Solar fraction is high in summer and autumn for the relative high radiation and high ambient temperature.
Thus, a completely amorphous copolymer is obtained if the molar fraction is high enough.
As seen earlier, particle migration is not significant when particle fraction is higher and thus, higher particle fraction composites could exhibit higher heat transfer rate for longer period.
It should be mentioned that the superiority of microparticles composites in reducing the melting time is more pronounced if the particle fraction is higher.
During this period, the difference between exergy efficiencies of micro and nanocomposites is more significant, if the particle fraction is higher.
We deduce that the rate of overgrowth volume fraction is higher for fine grains and decreases as the grain size increases.
While the overall amorphous fraction is higher for melt crystallization, the mobile amorphous fraction (wa) is found to be higher for cold crystallization.
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