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The swelling of clayey soil when it is subjected to moisture increase is a complicated process found to be influenced by several factors.
The cracks, associated often to moisture increase and higher values of the dielectric constant, produce a not negligible increase of the signal amplitude.
The moisture increase inside a HDPE bottle with the drug formulation was simulated with the sorption desorption moisture transfer model, which, in turn, allowed an accurate prediction of the drug degradation kinetics.
For example, the estimated soil moisture increase from April to May 2010 is attenuated by a half at depths between 25 30 cm and by a quarter between 95 100 cm, and the time of the first moisture peak is delayed by 1.3 and 6.5 days, respectively.
Furthermore, gobs(t) increases quickly by a few microgals during precipitation events, in line with the soil moisture increase and water height rise (as seen for March 2009, October 2009, March 2010 and July 2010), suggesting that changes in the gravity signal are associated with corresponding changes in the land-water distribution.
However, increased temperatures and moisture increase decay rates.
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One of the basic properties of the atmosphere is that moisture increases with temperature.
Toward the south, moisture increases from 18 inches (460 mm) to a maximum of 80 inches (2,000 mm) annually, and the scrub forest gives way to tall trees.
WPC and feed moisture increased redness, yellowness and decreased luminosity.
In addition, higher simulated soil moisture increases estimated E/ET.
As temperature and moisture increased, loss of crystalline structure and degree of gelatinization also increased.
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