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黄土高原植被演替对土壤碳库及δ13C的影响

万,昊1,2**,刘卫国1,3,魏杰1   

  1. (1中国科学院地球环境研究所黄土与第四纪地质国家重点实验室, 西安 710075; 2中国科学院大学, 北京 100049; 3西安交通大学人居与环境学院, 西安 710049)
  • 出版日期:2015-01-10 发布日期:2015-01-10

Effects of vegetation succession on carbon stock and δ13C in Loess Plateau.

WAN Hao1,2**, LIU Wei-guo1,3, WEI Jie1   

  1. (1State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, China; 2University of Chinese Academy of Sciences, Beijing 100049, China; 3School of Human Settlement and Civil Engineering, Xi’an Jiaotong University, Xi’an 710049, China)
  • Online:2015-01-10 Published:2015-01-10

摘要: 采集宁夏云雾山草原植被演替阶段的土壤和植物样品,测定土壤容重(BD)、土壤含水量(WC)、土壤有机碳(SOC)含量、以及土壤和植物优势种稳定碳同位素组成(δ13C),并比较了它们之间的差异,分析其反映的环境信息。结果表明:在表层0~10 cm深度,灌木地SOC含量为71.7 g·kg-1,显著高于草地的54.6 g·kg-1;灌木地0~20 cm深度SOC含量占1 m深SOC含量的58.1%,而草地在0~40 cm深度的SOC含量占1 m深的34.1%;短期植被演替(约10 a)对土壤剖面0~20 cm层的δ13C值有显著影响,其中对0~10 cm层δ13C影响最大;草地演替为灌木地后δ13C偏负1.4‰,30 cm以下土壤δ13C值对短期植被变化不敏感;通过δ13C在C3植被的短期演替过程中的响应关系发现,δ13C值作为土壤碳库更替和碳循环的研究工具有很好的辨识力;灌木的δ13C值从叶子到根系存在明显差异,逐渐偏正,变化为2.2‰,草地为1.9‰;通过对0~40 cm深度植物根系δ13C值的测定发现,灌木地由表层的-28.15‰变为-26.11‰,偏正了2.04‰,草地根系δ13C值从表层的-27.08‰变为-27.57‰,偏负了0.49‰。

关键词: 氮素效率, 氮肥, 管理模式, 光能利用率

Abstract: In this study, we investigated the bulk density (BD), water content (WC), organic carbon (SOC), and stable carbon isotope composition (δ13C) of soils collected from different successional stages of steppe vegetation in Yunwu Mountain, Ningxia Province. The δ13C values of the dominant plants in the vegetation were also analyzed. Our aims were to compare the differences in these variables between different vegetation types and to understand the related environmental information. Results showed that the SOC in the surface layer (0-10 cm layer) was 71.7 g·kg-1 in shrub land, being significantly higher than that in grassland (54.6 g·kg-1). The SOC for the 0-20 cm layer in shrub land accounted for 58.1% of the SOC above 1 m, whereas in grassland the SOC in the 0-40 cm layer only accounted for 34.1% of the SOC above 1 m. The shortterm vegetation succession had a significant influence on the δ13C values of SOC in the 0-20 cm layer, particularly in the 0-10 cm layer. The vegetation succession from grassland to shrub land led to a negative shift of 1.4‰ in δ13C values, but there was no significant change below soil depth of 30 cm. Therefore, δ13C might be a useful tool for studying the changes of soil carbon stock and carbon cycle during shortterm vegetation succession of C3 plants. The δ13C values became less negative from leaves to roots, with the deviation being 2.2‰ for shrubs and 1.9‰ for grass. Moreover, for plant roots from 0 to 40 cm depth, the δ13C values changed from -28.15‰ to -26.11‰ in shrub land and from -27.08‰ to -27.57‰ in grassland.

Key words: nitrogen efficiency, nitrogen fertilizer, management mode, light use efficiency