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Based on the results very large solar fractions can be achieved with optimized passive solar design.
So numerical models with different volume fractions can be obtained easily.
Via selective detection, the chemical composition drift of the different fractions can be determined.
Zimmermann, M., Leifeld, J., Schmidt, M. W. I., Smith, P. & Fuhrer, J. Measured soil organic matter fractions can be related to pools in the RothC model.
It is demonstrated that the braiding angles and fibre volume fractions can be represented as functions of this key parameter.
With method 5 only two different fractions can be discerned, i.e. a labile one and a stable one.
The samples complexity was reduced and the sample-loading amount for the rest low-level fractions can be considerably increased.
Therefore, these fractions can be considered indicators of changes in restoration-induced soil quality and sensitivity to environmental factors and restoration practices.
The numerical evidence indicates that undefined petroleum fractions can be highly represented in phase equilibria calculations by a properly selected set of components.
The variation in emission intensities of the selected lines and in metastable fractions can be related with electron densities in various parts of the EEPFs.
Carbon isotope ratios of individual compound are not affected, while variations in isotope ratios of fractions can be explained by changes in the fraction compositions.
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