The little seasonal change of colloidal organic carbon, nitrogen and phosphorus indicated that a balance is maintained between the input and output of colloid matter in the water.
胶体有机碳、氮、磷季节变化幅度并不很大,表明胶体物质在水体中输入和输出大体处于平衡状态。
Soil organic carbon (SOC) is an important component of the global carbon cycle, and it has direct effects on the global carbon balance.
土壤有机碳(SOC)是全球碳循环的重要组成部分,它具有直接影响全球碳平衡。
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