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Further, our research illustrates the need to consider varying responses among different tree species when predicting future consequences of N inputs on soil C storage.
We conducted an outdoor mesocosm experiment to investigate the relative impact of above and belowground tree inputs on soil nematode trophic composition, and examine whether tree-driven impacts differed between contrasting species (birch and pine).
The effects of nutrient and organic inputs on soil organic carbon (SOC) and total nitrogen (TN) stocks were studied in three 23 25-year-old 23 25-year-old 23 25-year-olde fertility experiments (LTFEs) in the Nepal terai.
In this study we investigated historical charcoal production sites in Germany that have not been in use for > 60 years, and evaluated the effects of the former charcoal inputs on soil and vegetation parameters relative to those of adjacent, unamended areas.
However, as it was beyond the scope of this study to assess the impacts of high intermediate inputs on soil, water, and air quality, we lack full understanding about potential environmental trade-offs, particularly at the field level.
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The vegetation transition at treeline provides an opportunity to test the effects of vegetation, topography, and external inputs on soils at three spatial scales.
The model accounts for the cumulative effect of successive rainfall events and wastewater input on soil moisture status and depth to water table.
Therefore, further study on the long-term application of organic inputs effect on soil fertility and peanut production would be suggested.
However, there is still uncertainty about the role and magnitude of the effect of chronic N inputs on forest soil C sequestration and how different tree species can modulate this effect.
Concentration of Cd was higher in S-5 followed by S-4, S-3, and S-2 (0.2 ± 0.03 μg g−1) showing the ranking order of S-5 > S-4 > S-3 > S-1 > S-2, which is attributable to spatial difference in fertilizer broadcasting and consequential input on the soil surface.
However, research on forest/plantation and associated soil carbon sink still remain scarce [ 47], some potential carbon pools under SRC/VSRC plantation might have been overlooked, e.g. weed root C inputs to soil [ 48].
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CEO of Professional Science Editing for Scientists @ prosciediting.com