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"May soil be as soft as down".
(In May soil moisture was nearly significant in the mass-standardized DEA model).
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Soil fauna may affect soil organic matter (SOM) dynamics not only by assimilating litter but also by modifying the soil environment at many spatiotemporal scales.
In addition to naturally occurring acid soils, agricultural practices may decrease soil pH, leading to yield losses due to Al toxicity.
This study demonstrates that herbicide application and cultivation may decrease soil organic matter and soil health.
Likewise, differences and diversity in root morphology may allow soil biota to populate the soil profile more completely than in simply structured environments.
Finally, land cover change may affect soil moisture alternation toward different transformation directions.
Harvesting traffic may alter soil properties and reduce forest productivity if soil disturbances are not mitigated.
Biochar may increase soil fertility and crop yield by enhancing soil organic carbon (SOC), nutrient availability and water retention.
Newman et al. (1997) reported that over-drainage of peat soils may lead to soil compaction and phosphorus nutrient accumulation.
Aeolian deposits record palaeoenvironmental conditions and may coin soil properties.
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