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Using linear regressions we obtained the degree of soil sealing to be the best predictor of LST-variations.
Apron deposits were described and subsequently correlated based on their internal stratigraphy and their relative degree of soil development.
Soil morphological characteristics were quantified as a profile development index (PDI) to determine the degree of soil development.
Erosion was highly dependent on runoff, bulk density, soil organic C, and the degree of soil surface covered.
This case study illustrates that the degree of soil heterogeneity in this patchy system may change with disturbance.
The proposed method can predict the degree of soil plugging and the inner skin friction of open-ended piles and be selected as convenient option in engineering field.
The purpose of this study was to determine the degree of soil heterogeneity and to check if K-entropy would be a good measure of soil evolution.
This paper presents a new design approach for predicting the degree of soil plugging and the inner skin friction of axial-loaded open-ended piles.
In addition, our results reveal both the high degree of soil mixing over millennial timescales and the local variability of mixing in forested landscapes.
Taken together, our results were inconclusive in determining whether the degree of soil nutrient limitation alters canopy exchange of plant growth-limiting nutrients.
Based on the degree of soil development, surface deposits on terrace flights form the post-incisive soil chronosequence, supporting the hypothesis of terrace formation by fluvial processes.
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