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长白山风倒区自然恢复26年后土壤碳、氮含量特征

孟莹莹1,2,包也1,2,郭焱1,2,王晓雨1,2,于大炮1,周莉1**,代力民1   

  1. 1中国科学院沈阳应用生态研究所, 沈阳 110016; 2中国科学院大学, 北京 100049)
  • 出版日期:2014-07-10 发布日期:2014-07-10

Soil carbon and nitrogen content in windthrow area on Changbai Mountain after 26 years’ natural recovery.

MENG Ying-ying1,2, BAO Ye1,2, GUO Yan1,2, WANG Xiao-yu1,2, YU Da-pao1, ZHOU Li1**, DAI Li-min1   

  1. (1Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; 2University of Chinese Academy of Sciences, Beijing 100049, China)
  • Online:2014-07-10 Published:2014-07-10

摘要:

植物群落的变迁会引起土壤碳/氮分布格局的变化。本文在长白山1986年风倒区和对照区(未受风干扰的原始植被分布区)沿海拔梯度选择阔叶红树林、云冷杉林和岳桦林,采集0~10(表层)和10~20 cm(下层)土壤,分析其碳、氮含量,研究长白山西坡风倒区植被恢复以来土壤理化性质的变化。结果表明:土壤有机碳、全氮含量在对照区和风倒区均表现为表层显著高于下层。对3个林型来说,风倒区与对照区土壤有机碳、全氮含量无显著性差异,但对照区和风倒区2个土层的碳、氮含量及储量随海拔增加有上升的趋势;同时,3个林型表层土壤中有机碳、全氮的含量有显著性差异,而下层土壤中差异不明显。在阔叶红松林和云冷杉林表层土壤中,对照区土壤C/N显著高于风倒区。随着海拔的升高,对照区和风倒区2个土层的碳氮比都有降低的趋势。总的来说,长白山风倒区经过26年的自然恢复,其土壤有机碳、全氮含量及储量与原始植被区已无明显的差异,但碳氮比差异性显著,说明自然恢复26年后风倒区土壤质量已经基本恢复,但由于植被类型的差异导致碳/氮输入等差异依然存在,因而,用碳氮比可以更准确地反映植被变化对土壤的影响。
 
 

关键词: 底栖动物群落, 生物指数, 澜沧江流域, 功能摄食群

Abstract: Changes in the structure and composition of vegetation communities often determine the organic carbon and nitrogen cycles in the soil. In order to explore the soil characteristics of forests on Changbai Mountain naturally recovered 26 years after wind damage, we selected three typical forest types―Korean pine and broadleaved mixed forest, sprucesfir forest and Erman’s birch forest along an altitudinal gradient, and compared the contents of soil organic carbon (SOC) and total nitrogen (TN) in the wind damaged area with those in the undamaged area (control area). Regardless of wind damage, SOC and TN contents were significantly higher in topsoil (0-10 cm) than in subsoil (10-20 cm). Within each forest type, no significant differences were found in SOC and TN contents between the damaged and control area. However, SOC and TN contents of both topsoil and subsoil increased with elevation. SOC and TN contents in topsoil significantly differed among the three forest types, while no differences observed in subsoil. Moreover, in Korean pine and broadleaved mixed forest and sprucefir forest, SOC and TN contents in topsoil were higher in the control area than  in the damaged area. With rising elevation, C/N in both topsoil and subsoil displayed a decrease trend regardless of wind damage. Overall, after 26 years’ natural recovery since the wind damage, the contents of SOC and TN did not differ significantly between the damaged area and the control area, but the ratio of C/N did. Our results suggested that soil quality was largely recovered, but the types of SOC input differed between the damaged area and the control area due to differences in the structure and composition of vegetation communities. Therefore, soil C/N may reflect the effects of vegetation changes on soil better than the contents of SOC and TN.

Key words: functional feeding group, biotic index, Lancang River basin, benthic macroinvertebrate assemblages