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Some models have already been developed to explain the effect of moisture content on the radon emanation fraction of soil.
Water-extractable organic matter (WEOM) is the most labile, dynamic, and bioavailable fraction of soil organic matter (SOM).
Particulate organic matter (POM) is a labile fraction of soil organic matter (SOM) that can contribute to nitrogen (N) mineralization.
Here the fraction of soil is fulfilling the role of aggregate in the material and low quantities of cement will act as a stabilizer.
The wind-erodible fraction of soil (EF) is one of the key parameters for estimating the susceptibility of soil to wind erosion.
As the crops grew, transpiration and interception became gradually dominated, while the fraction of soil evaporation dropped from 100% to less than 20%.
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The organic fraction of soils is critically important to soil health and optimal ecosystem functioning.
The mineralogy of the clay fraction of soils is a major determinant of the behavior of soil.
They further suggest that the concentration of light Si isotopes in the clay fraction of soils is partly due to H4SiO04 sorption onto secondary clay-sized iron oxides.
As a result it was recommended that source tracing with the < 32 μm fraction of soils and sediment should be treated separately from the 63 32 μm and larger particle size fractions.
Open image in new window Figure 4 X-ray diffraction spectrum of < 80 μ m samples fraction of soils in Mfou.
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