
ISSN: 2637-4676
*Corresponding author:
Bijan Azad, Department of Rehabilitation of Arid and Mountainous Regions, Faculty of Natural Resources, University of Tehran, Tehran 31587-77871, IranReceived:October 25, 2019; Published: October 31, 2019
DOI: 10.32474/CIACR.2019.07.000272
To view the Full Article Peer-reviewed Article PDF
Soils are the largest organic carbon pool in terrestrial ecosystems, the quantity of this pool is twice the amount of organic carbon in the atmosphere and three times more organic carbon than the biotic world [1]. Soils store an estimated 1500Pg organic carbon in the first meter of soil and 2500Pg of organic carbon to 2m; which is more organic carbon than is contained in the biotic world (500Pg of carbon) and twice as much organic carbon as the atmosphere (750Pg of carbon)
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