FIELD DETERMINED VARIATION OF THE UNSATURATED HYDRAULIC CONDUCTIVITY FUNCTIONS USING SIMPLIFIED ANALYSIS OF INTERNAL DRAINAGE EXPERIMENTS

The probability of attending school four our group of interest in this region increased by 6.5 percentage points after the expansion of the Bolsa Família program in 2007 and

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Persistent seed banks are composed of seeds that have more than one year of age and reserves of seeds remain in the soil year after year,generally buried into the soil..

Since the calculation of the irrigation water depth involves the knowledge of the actual soil water content before irrigation, of the soil water content at field capacity, and of

The estimated costs of soil erosion vary from the 5 dollars spent to remove each ton of sediment to keep navigation activities in operation, to 45.4 billion dollars a year in

The purpose of this study was to analyze the estimated percolation of soil water using the Darcy- Buckingham equation with K( θ ) functions determined by direct field and

With the simultaneous measurement of soil moisture obtained by the sensors, and the total soil water potential from the soil water retention curve, it was possible to determine

Estimating unsaturated hydraulic conductivity of Brazilian soils using soil water retention data. Pedotransfer functions for the estimation of soil water retention in