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岩溶碳循环
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岩溶碳循环
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岩溶(喀斯特)碳循环
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karst-related carbon cycle
岩溶碳循环
通过岩溶作用(碳酸盐溶解和沉积作用)由大气回收(碳酸盐溶解时)或向大气释放CO2(碳酸盐沉淀时),从而调节大气温室气体浓度影响气候变化的过程。又称喀斯特碳循环。
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