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The consistent ranking of soil enzyme activities was also significantly increased by afforestation.
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Our feeling is that, since the concept of soil chiefly bases on the occurrence of weathering and internal differentiation – both induced by biotic and/or abiotic processes – in an incoherent mass of mineral matter, the clearly altered surfaces of Venus, Mars, and our moon deserve the rank of soils.
The ranking of the soils and correlation analysis (p < 0.05) indicated that aggregate stability as determined by wet sieving, infiltration rate, runoff and soil loss under laboratory and field conditions was effective in predicting seal formation among smectitic-rich loam to kaolinitic-rich clayey soils.
Classical statistics revealed a characteristic ranking in the variability of soil properties.
The scaling heterogeneity of water losses among treatments increased as: BT < CT < MT < NT, while that <span class="lh">of soil losses ranked as: BT ≈ MT < CT ≈ NT.
The change in the interseasonal patterns of TS SM is tightly related to plant phenology and the control of vegetation on the ranking of mean relative difference (MRD) of soil moisture significantly weakens during non-growing seasons due to diminished root water uptake.
Based on this principle of soil productivity processes, ranking of inherent productivity of soil was performed separately for the major climatic areas.
Overall, our findings indicate that the present integrated risk assessment tool with readily available input data can be used to rank farm fields according to risk of soil erosion and losses of P and N.
The new farm is built on grade three agricultural land – the middle ranking out of the 1-5 scale for quality of soil – which the company says has a history of not draining well and therefore not good for growing crops.
There were high Spearman's rank correlation coefficients between any two-measurement series, indicating strong time stability of the spatial pattern of soil water storage.
Spearman rank correlation and wavelet coherency analyzes were used to determine overall and scale-dependent similarities of temporal patterns of soil moisture, respectively.
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