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Pinus also caused a major shift in soil nutrient cycling as indicated by increased bacterial dominance, NO3-N (17-fold increase) and available phosphorus (3.2-fold increase) in soils, which in turn promoted increased growth of graminoids.
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Regarding a decreased PEF, a per-IQR increase in soil Cs was associated with increased odds of having decreased PEF (OR = 2.33; 95% CI, 1.41 3.86).
Repellency index decreased sharply with increase in soil moisture.
In addition, WC and NV displayed an increase in soil microbial activity as a result of greater soil respiration.
Increase in soil carbon pools through the additions of organic matter to soils and residues from larger root systems.
This is comparable to contemporary patterns in which δ15N in surface soils rise with increasing distance from a glacier front, due to an increase in soil development41.
One analysis published in the journal Global Change Biology showed a 19percentt increase in soil carbon after land changed from cropland to pasture.
Similarity was increased at different scales with increase in soil depth owing to strong buffering capacity.
Subsequently, the increase in soil richness resulted in reduction (≤ 5%) in surface runoff.
Water addition resulted in a significant increase in soil pH and electric conductivity.
However, the associated increase in soil pH may result in potentially greater N losses over time.
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