Dissolved inorganic carbon and stable carbon isotopic evolution of neutral mine drainage interacting with atmospheric CO2(g)
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文摘

We assess the δ13C in a neutral mine drainage

The DIC evolved sequentially by kinetic and equilibrium processes

The δ13C of the carbonate was enriched by 0.7‰

Carbon was released into the atmosphere and precipitated as carbonate

20% of the carbon was outgassed and 12% was sequestered in sediments

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