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Inorganic carbon (C) comprises approximately a third of the total C pool in soils worldwide, largely in the form of pedogenic calcite. Pedogenic calcite occurs in semi-arid and arid regions in the form of calcareous, calcic, and petrocalcic horizons. Understanding the processes governing the storage and flux of this inorganic C pool is crucial to the development of accurate regional and global C budgets...
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