Changes of carbon stocks in alpine grassland soils from 2002 to 2011 on the Tibetan Plateau and their climatic causes
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文摘
SOC changes in alpine grasslands were estimated using repeated soil inventory. Alpine meadows showed a markedly C gain, alpine steppes exhibited a slight C loss. SOC changes were apparently related to the original SOC stocks in alpine steppes. SOC changes were correlated with March–April precipitation in alpine meadows. SOC changes were associated with MAP in alpine steppes.

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