Sentence examples for measuring soil redistribution from inspiring English sources

The use of rapidly acquired magnetic measurements represents a relatively new potential means of mapping and measuring soil redistribution.

137Cs is the most commonly used anthropogenic radioisotope used to assess soil redistribution rates.

Models have been developed to equate differences of radioisotope inventories with rates of soil redistribution and these models have been employed globally to assess soil redistribution on agricultural and natural landscapes.

Empirical approaches rely on measurements of soil redistribution, which may be interpolated in space and time using (geo)statistical methods.

Fortunately, the random variation can be overcome statistically by increasing independent sample numbers on both reference and measuring sites and by interpreting soil redistribution rates in terms of mean value for a uniform landform unit or contour transect (slope position) because the random errors tend to cancel out if averaged over a uniform area.

Measurements of cumulative soil redistribution from 1963 to 2000 were derived using Cesium-137 as a tracer.

The soil redistribution measurements differed meaningfully from the deterministic model predictions (R2 = 0.389), causing the Kalman filter to make a marked adjustment to the soil redistribution map.

The objectives of this study are to (1) perform sophisticated sensitivity and uncertainty analyses for the three widely-used models to characterize the potential sources of uncertainty including spatial variations on both reference and measuring sites and (2) explore ways to minimize uncertainty and to improve soil redistribution estimation.

Erosion rates, detachment and deposition areas were measured by the pole height method which allowed mapping of the soil redistribution.

The soil redistribution operation should prevent excess compaction.

Predicted soil redistribution rates for different slope locations varied.