Abstract
The presence of organic C in soil is a key determinant for soil quality and productivity. Soil, being the largest C sinks, also controls the global warming. In this regard, this review focused onto the soil C dynamics, C sequestration potential of soil and related C pools. Detailed discussion of several researches depicted that, C sequestration depends onto soil C saturation deficit, presence of biochemically protected recalcitrant C fractions, aggregation and aggregate associated physically shielded C. On the other hand, labile organic C is the soil nutrient reservoir and is closely related with diversified soil biology. For the sustainable and holistic soil resource management and to mitigate climate change, this study also highlighted the possible management practices towards longer residence time of C in soil.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
