2014
DOI: 10.3923/ijss.2015.37.44
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Carbon-Nitrogen Stocks and Structural Stability of a Tropical Loamy Sand Soil as Influenced by Tithonia diversifolia (L.) and Other Fertilizers

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Cited by 4 publications
(4 citation statements)
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“…However, storing carbon in soil benefits everyone. According to Kumar et al (2009), Adesodun and Odejim (2010), and others, it boosts soil quality, improves agronomic production, advances food security, and mitigates climate change by offsetting anthropogenic emissions. Programs for conservation and reforestation have been implemented in this scenario throughout the past three decades (Tamirat and Mekides, 2020).…”
Section: Climate Change Adaptation and Mitigation Measuresmentioning
confidence: 99%
“…However, storing carbon in soil benefits everyone. According to Kumar et al (2009), Adesodun and Odejim (2010), and others, it boosts soil quality, improves agronomic production, advances food security, and mitigates climate change by offsetting anthropogenic emissions. Programs for conservation and reforestation have been implemented in this scenario throughout the past three decades (Tamirat and Mekides, 2020).…”
Section: Climate Change Adaptation and Mitigation Measuresmentioning
confidence: 99%
“…Soil aggregation is a good indicator of soil quality influenced by different land uses [42][43][44]. SSI below 5% indicates high impact, between 5 and 7% indicates a high risk of structural degradation, and above 7% indicates low risk of degradation [45]. Only the NF had an SSI greater than 7%, indicating that the soils of the areas under reclamation, and even the RF, present high risk of loss organic carbon and susceptibility of soil erosion.…”
Section: Soil Aggregate Stabilitymentioning
confidence: 99%
“…The SOC stock up to the deepest layer (60-90 cm) was found highest in horticultural lands while those values of croplands and uncultivated lands exhibited similarities which are in conformity with the findings of Vikas-Sharma et al (2014). Low vegetation cover, erosion, and overgrazing could be the main cause for lower SOC stock in the upper layers under uncultivated lands (Adesodun et al 2005) whereas increased SOC stock in the deeper layers might be due to long-term accumulation of OC through deposition of root derivatives of grasses, shrubs, and other patches of natural vegetation. The variation of C sequestration also caused by qualities of C inputs where more positive responses could be observed under fruit trees (Jia et al 2015).…”
Section: Effect Of Land-uses On Sequestered Soc and Its Poolsmentioning
confidence: 99%