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The impact of moisture distribution on maximum phenomenon is investigated from non-saturation degree (Snon) and relative humidity (RH).
This research mainly focuses on the impact of pore structure and moisture distribution on maximum phenomenon, specifically the two parameters of it.
In the present study, the moisture distribution on the wetting front during drainage and imbibition in a 2D sand chamber is studied thoroughly.
While as the imbibition rate increases from 5 ml/min to 400 ml/min, the moisture distribution on the wetting front becomes more uniform.
Incubation experiments were conducted to reveal the impact of non-uniform moisture distribution on soil N2O emissions under subsurface-drip-irrigation (SDI), with surface-irrigation (SI) as a control.
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The effect of random system properties, plate geometry, stacking sequences, support conditions, fiber volume fractions and temperature and moisture distributions on hygrothermomechanical post-buckling load of the laminated cylindrical shell panel are presented.
Multon and Toutlemonde (2006) investigated the effects of moisture distribution and stress state on the ASR-induced expansion in concrete.
Information on moisture distribution patterns under point-source trickle emitters is a pre-requisite for the design and operation of trickle-irrigation systems.
Capillary properties and atmospheric condition had significant impacts on subsurface moisture distribution and salt migration in response to the evaporation.
The results demonstrated that the effect of temperature gradient on the moisture distribution, i.e., heat-induced moisture movement, resulted in an accumulation of moisture at the interface, and induced interfacial stresses even in the absence of a moisture gradient.
Although rock check dams have been used for centuries to control erosion and support subsistence agriculture on western US rangelands, there is a lack of measured data to quantify their impact on soil moisture distribution.
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