Wu Jian-Guo
Chinese Research Academy of Environmental Sciences, Beijing 100012, China.
Ying Yong Sheng Tai Xue Bao. 2007 Dec;18(12):2896-904.
In this paper, the researches about the relationships of soil carbon and nitrogen storage with temperature, and the responses of soil carbon and nitrogen decomposition to the spatiotemporal differentiation of temperature, increasing air temperature, and soil freezing-thawing were summarized, and the uncertainty and determination errors of related research methods were discussed. Climate warming could promote soil carbon and nitrogen decomposition and soil CO2 emission within a short period, but not always accelerate the decomposition of soil carbon and nitrogen in a long-term. Therefore, to give a reasonable interpretation on the discrepancies of previous studies, a systematic analysis on the mechanisms about the effects of changing temperature on the decomposition of soil carbon and nitrogen should be made, and the differences about the long-term and short-term responses of soil carbon and nitrogen decomposition to the changing temperature, as well as the influences of research method, vegetation, soil, and climate conditions on the research results should also be fully understood.
本文综述了土壤碳氮储量与温度关系,以及土壤碳氮分解对温度时空分异、气温升高和土壤冻融的响应,并讨论了相关研究方法的不确定性和测定误差。气候变暖在短期内可促进土壤碳氮分解及土壤CO₂排放,但长期未必总能加速土壤碳氮分解。因此,为合理解释以往研究的差异,应系统分析温度变化对土壤碳氮分解影响的机制,充分认识土壤碳氮分解对温度变化的长期和短期响应差异,以及研究方法、植被、土壤和气候条件对研究结果的影响。