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氮沉降对长白山森林土壤团聚体内碳、氮含量的影响

Effects of nitrogen deposition on carbon and nitrogen contents in soil aggregates in temperate forests of Changbai Mountain, Northeast China

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【作者】 周学雅陈志杰耿世聪张军辉韩士杰

【Author】 ZHOU Xue-ya;CHEN Zhi-jie;GENG Shi-cong;ZHANG Jun-hui;HAN Shi-jie;Ministry of Education Key Laboratory of Geospatial Technology for the Middle and Lower Yellow River Regions, College of Environment and Planning, Henan University;Tan Kah Kee College, Xiamen University;College of Life Science, Henan University;Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences;

【通讯作者】 韩士杰;

【机构】 河南大学环境与规划学院教育部黄河中下游数字地理重点实验室厦门大学嘉庚学院河南大学生命科学学院中国科学院沈阳应用生态研究所森林生态与管理重点实验室

【摘要】 氮沉降是影响陆地生态系统碳、氮循环的最重要因素之一.为了解土壤团聚体碳、氮组分对氮沉降的响应,本研究在长白山选取次生杨桦林(YHL)与原始阔叶红松林(HSL)两种林型进行为期6年的氮添加试验,采集土壤样品并分析氮沉降对不同粒径土壤团聚体中可溶性有机碳、氮(DOC和DON)、微生物生物量碳、氮(MBC和MBN)、颗粒有机碳、氮(POC和PON)的影响.结果表明:除POC和PON外,两林分土壤团聚体碳、氮组分含量均随团聚体粒径的减小而增加;氮添加处理显著降低了HSL土壤团聚体中POC和PON含量,降幅分别达20.7%和22.6%,显著增加了DOC含量,增幅达11.6%;氮添加处理对YHL土壤团聚体的碳、氮组分均无显著影响,其中,对DOC和MBC的影响接近于显著(0.05<P<0.1).皮尔森相关分析结果表明,土壤团聚体中总碳或总氮与碳、氮活性组分之间有良好的相关性,其中,HSL土壤的POC与DOC之间呈极显著负相关(r=-0.503),DOC又与MBC呈显著正相关关系(r=0.462).氮添加处理降低阔叶红松林土壤团聚体中POC和PON含量、增加DOC含量的主要原因是其促进了微生物对POM的分解,进而导致DOC的释放.阔叶红松林土壤碳、氮库对氮沉降的响应比次生杨桦林更加敏感.

【Abstract】 Nitrogen deposition is one of the most important factors affecting carbon(C) and nitrogen(N) cycling in terrestrial ecosystem. A six-year N addition experiment was carried out to explore how N deposition affected C and N fractions in soil aggregates in the secondary aspen forest(YHL) and primary Korean pine broad-leaved forest(HSL). We investigagted the effects of N addition on dissolved organic carbon and nitrogen(DOC and DON), microbial biomass carbon and nitrogen(MBC and MBN), particulate organic carbon and nitrogen(POC and PON) in soil aggregates with different particle sizes. The results showed that the contents of carbon and nitrogen fractions generally increased with the decrease of particle sizes of soil aggregates except for POC and PON. In soil aggregates of HSL, POC and PON significantly decreased by 20.7% and 22.6% in N treatment, respectively, but DOC increased by 11.6%. In YHL, N addition treatment had no signi-ficant effect on C and N fractions in soil aggregates. Total carbon or nitrogen correlated well with the active C and N fractions in soil aggregates, with a great significant negative correlation between POC and DOC in HSL(r=-0.503) and a significant positive correlation between DOC and MBC(r=0.462). In HSL, the negative effect of N treatment on POC and PON and the positive effect on DOC was mainly attributed to the accelerated decomposition of POM by stimulating microbial activity. Soil C and N pools in HSL were more vulnerable to N deposition than that in YHL.

【基金】 福建省教育厅科技项目(JAT170832);国家自然科学基金项目(41330530,41430639,41575153,41807330,31800413);中原学者项目(182101510005)资助~~
  • 【文献出处】 应用生态学报 ,Chinese Journal of Applied Ecology , 编辑部邮箱 ,2019年05期
  • 【分类号】S714.2
  • 【网络出版时间】2019-05-06 09:48
  • 【被引频次】11
  • 【下载频次】804
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