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作 者:方熊[1,2] 刘菊秀[1] 张德强[1] 刘世忠[1] 褚国伟[1] 赵亮[1,2]
机构地区:[1]中国科学院华南植物园,广州510650 [2]中国科学院研究生院,北京100049
出 处:《应用与环境生物学报》2012年第4期531-538,共8页Chinese Journal of Applied and Environmental Biology
基 金:中国科学院知识创新工程重要方向项目(No.KSCX2-EW-Q-8);国家自然科学基金项目(No.31070439);国家科技支撑计划项目(No.2009BADC6B002)联合资助~~
摘 要:全球变化对土壤有机碳(SOC)存贮与分解的影响在全球碳(C)循环中具有重要地位.分别通过室内土壤培养法和氯仿熏蒸法,研究了降水变化和氮(N)添加处理对鼎湖山3种不同演替阶段的季风常绿阔叶林、针阔混交林和马尾松针叶林SOC矿化和土壤微生物量碳(SMBC)的影响.结果表明:1)降水量增加能够提高森林演替晚期SOC累积矿化量和矿化速率,而对森林演替早期SOC累积矿化量和矿化速率没有显著影响(P>0.05).2)干旱条件(降水量减少)降低森林SMBC含量,且在鼎湖山季风林表层土壤(0~10 cm)中SMBC的减少达到显著水平(P<0.05).3)N添加处理对鼎湖山3种森林类型SOC累积矿化量、矿化速率以及SMBC都没有显著影响(P>0.05).未来关于SOC矿化对全球变化响应的研究,要综合考虑土壤有机质质量、C/N比例、外源性氮输入等因素的作用.Soil organic carbon (SOC) mineralization and soil microbial carbon (SMBC) play an important role in global C cycle. With method of incubation and chloroform fumigation extraction, the effects of precipitation change and nitrogen (N) addition on the SOC mineralization and SMBC were studied along a forest succession series including pine forest (PF), mixed pine and broadleaved forest (MF) and monsoon evergreen broadleaved forest (MEBF) at Dinghushan, Southestern China. The results showed that: (1) Increased precipitation could improve the mineralization of SOC in the late-successional forest plots, but the effect in the early-successional forest plots were not significant (P〉0.05). (2) Less precipitation (drought) resulted in lower content of SMBC in the monsoon forest soil (0~10 cm), while the doubled precipitation treatment had no significant effect on the SMBC content. (3) N deposition did not affect SMBC mineralization and SMBC in all of the three forests. It is important to take the quality of organic matter, C/N ratio, exogenous nitrogen and many other combined effects into consideration in the future studies on the responses of SOC mineralization and SMBC to climate change. Fig 4, Tab 2, Ref 37
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