Projections of depth-specific SIC change rates under different climatic conditions by the end of the 21st century (IMAGE)

Science China Press

Projections of depth-specific SIC change rates under different climatic conditions by the end of the 21st century

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SIC change rates of soil depths are shown, attributed to vertical leaching and lateral export via subsurface water movement. The Black and red numbers indicate SIC loss and SIC accumulation in specific layers, respectively.

 

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