草地学报

草地学报 ›› 2019, Vol. 27 ›› Issue (2): 320-325.DOI: 10.11733/j.issn.1007-0435.2019.02.007

• 研究论文 • 上一篇    下一篇

衡阳紫色土丘陵坡地植被恢复过程中土壤可矿化碳库特征

杨宁1, 杨满元1, 姜琳1, 万丽1, 吴磊1, 邹冬生2   

  1. 1. 湖南环境生物职业技术学院园林学院, 湖南 衡阳 421005;
    2. 湖南农业大学生物科学技术学院, 湖南 长沙 410128
  • 收稿日期:2018-11-08 修回日期:2019-03-04 出版日期:2019-04-15 发布日期:2019-05-30
  • 通讯作者: 邹冬生
  • 作者简介:杨宁(1974-),男(苗族),湖南绥宁人,博士,教授,主要从事植物生态学与恢复生态学的教学与研究,E-mail:yangning8787@sina.com
  • 基金资助:
    湖南省科技厅项目（S2006N332）；湖南省教育厅科学研究项目（16C0559）；湖南环境生物职业技术学院南岳学者基金项目资助

Properties of Mineralizable Carbon(MC) Pool during Re-vegetation on Sloping-land with Purple Soils in Hengyang, Hunan Province

YANG Ning1, YANG Man-yuan1, JIANG Lin1, WAN Li1, WU Lei1, ZOU Dong-sheng2   

  1. 1. College of Landscape Architecture, Hunan Environmental-Biological Polytechnic College, Hengyang, Hunan Province 421005, China;
    2. College of Bioscience and Biotechnology, Hunan Agricultural University, Changsha, Hunan Province 410128, China
  • Received:2018-11-08 Revised:2019-03-04 Online:2019-04-15 Published:2019-05-30

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摘要： 本研究采用空间序列代替时间序列方法，研究衡阳紫色土丘陵坡地植被恢复过程0～10、10～20与20～40 cm土层土壤可矿化碳库特征。结果表明：恢复过程中土壤有机碳含量、可矿化碳含量和矿化速率随土层加深而减少，随恢复进程而增加；矿化率随恢复进程增加，随土层加深先减后增再分布均匀；累积矿化排放量及其速率随恢复进程增加，其速率随培养时间延长而减小；qCO2值随恢复进程和土层加深而递减；土壤可矿化碳含量与凋落物现存量、质量损失率的相关系数r分别为—0.698*和0.915**（*P<0.05，**P<0.01）。研究表明，随着植被恢复进行，土壤生境由早期干扰强烈转向中后期日趋稳定，土壤固碳能力由早期差、潜力大转向中后期强、潜力小。

关键词: 碳库特征, 可矿化碳, 植被恢复, 紫色土, 有机碳

Abstract: By using the spatial series to replace time series,a test was conducted to study the properties of mineralizable carbon (MC) pool in 0～10,10～20 and 20～40 cm soil layers during re-vegetation on sloping-land with purple soils in Hengyang,Hunan Province. It observed that the contents of soil organic carbon (SOC) and MC as well as the carbon mineralization rate (MR) decreased with increasing soil depth but increased with the process of re-vegetation;MC/SOC increased with the re-vegetation process but decreased then increased and finally distributed evenly with increasing soil depth;The amount of cumulative released carbon and the carbon release rate increased with the process of re-vegetation,but the release rate decreased with increasing incubation time;qCO2 decreased with increasing soil depth and the process of re-vegetation;The soil MC contents had a negative correlation with the litter existing biomass(r=-0.698*) but positive correlation with the mass loss rate(r=0.915**)(*P<0.05,**P<0.01). All the results indicated that soil habitat changed from strong interference at early stages to relative stability at late stages,and the soil carbon sequestration ability changed from small capacity and strong potential at early stages to large capacity and weak potential at late stages.

Key words: Carbon pool properties, Mineralizable carbon (MC), Re-vegetation, Purple soils, Soil organic carbon(SOC)

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