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Soil moisture was controlled by weighing each pot during the growth period.
Dentin moisture was controlled with absorbent paper until no surface water was observed.
The pots were incubated at 28°C under fluorescent light, and moisture was controlled daily at the level of 40% (w/w) for 25 days.
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Results indicate that spatial patterns in soil moisture are controlled by small-scale curvature features at fine resolutions and by larger-scale vegetation patches at coarser resolutions.
We focused on the dry end of the soil moisture range and found that the magnitude of soil moisture variability was controlled by the interplay of soil hydraulic properties and climate.
Under the experimental conditions of this study, it was found that the rate of moisture adsorption was controlled the surface exchange reaction.
The evolution of moisture content was controlled, and both methods were compared by means of a statistical analysis of the thickness, quality, porosity coefficient, color and compressive properties of the cork.
Plots were divided into bare soil and grass vegetation and upper surface soil moisture before rainfall events was controlled by the subsurface groundwater level.
The moisture content in the concrete specimens was controlled by massing the specimens.
A positive linear relationship was observed between mean soil moisture and its standard deviation and was controlled by the parameter defining the shape of soil water retention curves and the spatial variability of saturated hydraulic conductivity.
The influence of LAI time variation on the soil moisture simulations is controlled by the sensitivity of modelled soil moisture to the average LAI values over that period, and soil parameters affected the sensitivity of the model to LAI.
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