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The studied water content range was from 0 to 0.8 while temperature from 20 to 100 °C.
The transition stage from an increase to a decrease in c′ and ϕ′ values with soil water occurred in the soil water content range of 6 10%.
However, such criteria did not clearly demonstrate the model's ability to give accurate predictions over the whole analyzed water content range.
The compost was chosen because it has a very wide water content range and because it represents a wide range of porous media, including soils and biofilter media.
The fruit density, bulk density and porosity varied from 1224.34 to 1766.77 kg/cm3, 641.74 to 588.66 kg/cm3, and 0.469 to 0.637 kg/cm3, respectively for the same water content range.
In fact, the parallel between in situ profiles and the shrinkage curves in such a large water content range is difficult to obtain because of the lack of earth pressure in the laboratory tests and in situ limited water contents.
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Relative water content ranged from 73%to93%3%, indicating that some plants experienced a slight decrease in turgor.
The water content ranged between 30.0% and 68.9% but did not show a trend with depth.
After the treatment of the pulse electric field–hydrocyclone field coupling unit, the water content ranges from 5to6%6 %.
Temperatures examined ranged between 20 °C and 200 °C and water content ranged between sub 50 ppm and 10% by volume.
According to monthly field measurements, soil water content at TC was below 15% cm3 cm−3; however, data logger-recorded soil water content ranged between 3 and 34% cm3 cm33.
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