森林土壤氧化亚氮排放对大气氮沉降增加的响应研究进展

被引:18
作者
方华军 [1 ]
程淑兰 [2 ]
于贵瑞 [1 ]
王永生 [1 ]
徐敏杰 [2 ]
党旭升 [1 ]
李林森 [2 ]
王磊 [1 ]
李晓玉 [1 ]
司高月 [2 ]
机构
[1] 中国科学院地理科学与资源研究所生态系统观测与模拟重点实验室
[2] 不详
关键词
大气氮沉降; 氧化亚氮排放; 硝化细菌; 反硝化细菌; 同位素标记; 分子生物学;
D O I
暂无
中图分类号
S714 [森林土壤学];
学科分类号
0903 ; 090301 ;
摘要
森林土壤N2O来源于土壤氮素的氧化还原反应,硝化、反硝化、硝化细菌反硝化以及化学反硝化是其产生的四个关键过程。当前,氮素富集条件下森林土壤N2O排放存在硝化和反硝化主导作用之争,对大气氮沉降增加的响应模式以及微生物驱动机制尚不清楚。综述了森林土壤N2O来源的稳定性同位素拆分,森林土壤总氮转化和N2O排放对增氮的响应规律,增氮对N2O产生菌群落活性和组成的影响,并指出研究的薄弱环节与未来的研究重点。总体而言,森林土壤N2O排放对大气氮沉降增加的响应呈现非线性,包括初期无明显响应、中期缓慢增加和后期急剧增加三个阶段,取决于森林生态系统"氮饱和"程度。施氮会引起森林土壤有效氮由贫氮向富氮的转变,相应地改变了土壤硝化细菌和反硝化细菌群落丰度与组成,进而影响土壤N2O排放。由于森林土壤N2O排放监测、土壤总氮转化和N2O产生菌群落动态研究多为独立进行的,难以阐明微生物功能群与N2O排放之间的耦合关系。未来研究应该有机结合15N-18O标记和分子生物学技术,准确量化森林土壤N2O的来源,揭示森林土壤N2O排放对增氮的非线性响应机理。
引用
收藏
页码:262 / 271
页数:10
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