不同林龄桉树人工林土壤有机碳的变化Changes of Soil Organic Carbon in Different-aged Eucalyptus Plantations
王纪杰,鲍爽,梁关峰,俞元春
WANG Ji-jie,BAO Shuang,LIANG Guan-feng,YU Yuan-chun
摘要(Abstract):
对不同林龄的桉树人工林土壤有机碳的剖面分布特征进行了研究。结果显示,桉树人工林土壤总有机碳、易氧化态有机碳和稳定态有机碳含量均随土层深度的增加而减小。随林龄的增加呈现先增加后减小的折线变化,土壤总有机碳和易氧化态有机碳含量4 a时最大,二者正相关性极强;稳定态有机碳在2 a最大,4 a时下降幅度最大,与p H值呈极显著负相关关系。说明4 a桉树林地土壤养分含量最高,根系对稳定态有机碳的转化量最大。桉树根系可伸入1 m的土层吸收利用稳定态有机碳,反应其较强的吸收利用养分的能力,同时也降低了土壤碳汇稳定性。
In this paper,studies were made of soil organic carbon in different-aged Eucalyptus plantations.The results showed that the content of soil organic carbon,readily oxidized organic carbon and chemical recalcitrant organic carbon decreased with the increase of soil depth. And along with the increase of the forest age,they first increased,and then decreased,displaying a broken-line change. The soil organic carbon and readily oxidized organic carbon had the maximum contents at the age of four,and had a very significantly positive correlation. Stable organic carbon reached the maximum at the age of two,and but had a maximum decrease extent at the age of four. This index had a highly significant negative correlation with p H. It meant that the soil quality aged 4 was the best in Eucalyptus plantations,and the maximum was the transformation amount of their stable organic carbon. Root systems of Eucalyptus could absorb chemical stable organic carbon under 1 m thick soil,exhibiting the root's great ability of absorbing nutrients,and also decreasing the stability of soil carbon sequestration at the same time.
关键词(KeyWords):
桉树人工林;土壤总有机碳;易氧化有机碳;稳定态有机碳;相关性
Eucalyptus plantations,Soil organic carbon,Readily oxidized organic carbon,Chemical stable organic carbon,relativity
基金项目(Foundation): 林业科技成果国家级推广项目;; 国家林业公益性行业科研专项(200804040)
作者(Author):
王纪杰,鲍爽,梁关峰,俞元春
WANG Ji-jie,BAO Shuang,LIANG Guan-feng,YU Yuan-chun
DOI: 10.16779/j.cnki.1003-5508.2015.04.002
参考文献(References):
- [1]任军,郭金瑞,边秀芝,等.土壤总有机碳研究进展[J].中国土壤与肥料,2009,27(6):1~7.
- [2]冯瑞芳,杨万勤,张健.人工林经营与全球变化减缓[J].生态学报,2006,26(11):3870~3877.
- [3]史军,刘纪远,高志强,等.造林对土壤碳储量影响的研究[J].生态学杂志,2005,24(4):410~416.
- [4]张苏峻,黎艳明,周毅,等.粤西桉树人工林土壤总有机碳密度及其影响因素[J].中南林业科技大学学报,2010,30(5):22~28.
- [5]鲁如坤.土壤农业化学分析方法[M].北京:中国农业科技出版社,1999.
- [6]Blair G J,Lefroy R D B.Soil C fraction based on their degree of oxidation and the development of a C management index for agriculture systems[J].Soil biology&biochemistry,1995,8(46):1459~1466.
- [7]Eusterhues K,Rumpel C,Kgel-Knabner I.Stabilization of soil organic matter by interactions with minerals as revealed by mineral dissolution and oxidative degradation[J].Organic Geochemistry,2003,34:1591~1600.
- [8]Lorenz K,Lal R,Preston C M,et al.Strengthening the soil organic carbon pool by increasing contributions from recalcitrant aliphatic bio(macro)molecules[J].Geoderma,2007,142:1~10.
- [9]Six J,Bossuyt H,Degryze S,et al.A history of research on the link between(micro)aggregates,soil biota,and soil organic matter dynamics[J].Soil&Tillage Research,2004,79:7~31.
- [10]樊后保,袁颖红,廖迎春等.闽南山区连续年龄序列桉树人工林土壤养分动态[J].应用与环境生物学报,2009,15(6):756~760.
- [11]姜培坤.不同林分下土壤活性有机碳库的研究[J].林业科学,2005,41(1):10~13.
- [12]王纪杰.桉树人工林土壤质量演变机制研究[D].南京林业大学博士论文,2011.
- 桉树人工林
- 土壤总有机碳
- 易氧化有机碳
- 稳定态有机碳
- 相关性
Eucalyptus plantations,Soil organic carbon,Readily oxidized organic carbon,Chemical stable organic carbon,relativity