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黄土地区不同覆被下土壤无机碳分布及同位素组成特征

崔丽峰1,2,刘丛强1,涂成龙1**,李龙波1,2,丁虎1   

  1. (1中国科学院地球化学研究所环境地球化学国家重点实验室, 贵阳 550002; 2中国科学院大学, 北京 100049)
  • 出版日期:2013-05-10 发布日期:2013-05-10

Soil inorganic carbon and its isotopic composition under different vegetation types in Loess Plateau of Northwest China. 

CUI Li-feng1,2, LIU Cong-qiang1, TU Cheng-long1**, LI Long-bo1,2, DING Hu1   

  1. (1 State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China; 2 University of Chinese Academy of Sciences, Beijing 100049, China)
  • Online:2013-05-10 Published:2013-05-10

摘要: 土壤无机碳在剖面上的分布在评估区域碳库储量、陆地碳循环以及全球变化的研究中具有重要作用。本文通过测定黄土地区不同植被类型覆盖下土壤pH值、碳酸盐含量、δ13C和δ18O值,探讨了黄土地区植被类型对碳酸盐在土壤剖面中分布和同位素组成特征的影响。结果表明:各剖面碳酸盐含量为5.7%~14.1%,其均值大小为荒地>草地>林地;林地中,阔叶林>灌木林>针叶林,针叶林变化最明显;受成土母质影响,各剖面土壤pH值在7~8,呈弱碱性;土壤碳酸盐δ13C值分布为-6.2‰~-1.8‰,各剖面δ13C均值大小为荒地>灌木林>针叶林>草地>阔叶林;植被类型主要是通过向土壤输入有机质来影响土壤无机碳同位素组成;不同覆被下土壤剖面碳酸盐δ18O值差异明显,其可能受土壤物理性质如孔隙度、湿度等影响;黄土地区不同覆被下土壤无机碳含量和δ13C、δ18O值明显不同,因此,在植被演替过程中,植被类型的改变会影响到土壤无机碳库的储量和区域碳循环过程。

关键词: 棉秆炭, Biolog, DGGE, 根际, 连作棉花

Abstract: The distribution of inorganic carbon in soil profile is crucial for assessing regional soil inorganic carbon storage, terrestrial carbon cycle, and global climate change. In this paper, the pH value, carbonate content, and its δ13C and δ18O values in five soil profiles under different vegetation types in the Loess Plateau were measured, aimed to explore the effects of vegetation type on the distribution and isotopic composition of inorganic carbon in the soil profiles. In the five 0-130 cm soil profiles, carbonate content varied from 5.7% to 14.1%, and its average value was in the sequence of wasteland > grassland > broadleaf forestland > shrub forestland > coniferous forestland. As affected by the parent material loess, the soil was weakly alkaline, with pH value 7-8. The δ13C value of the soil carbonate varied from -6.2‰ to -1.8‰, with the order of wasteland > shrub forestland > coniferous forestland > grassland > broadleaf forestland. Vegetation type affected the δ13C value of the soil carbonate mainly through the input of organic carbon. The δ18O value of the carbonate in the soil profiles under different vegetation types had significant distinction, which was possibly affected by the soil physical properties such as porosity and humidity. In the Loess Plateau, there was a significant difference in the vertical distribution of soil inorganic carbon content and its δ13C and δ18O values under different vegetation types, and thus, the vegetation type change during vegetation succession could affect the storage of soil inorganic carbon and the process of regional carbon cycle.

Key words: cotton stalk biochar, Biolog, DGGE, rhizosphere, continuous cropping cotton.