欢迎访问《应用生态学报》官方网站,今天是 分享到:

应用生态学报 ›› 2011, Vol. 22 ›› Issue (07): 1675-1681.

• 研究报告 • 上一篇    下一篇

庐山不同海拔森林土壤有机碳密度及分布特征

杜有新1,吴从建3,周赛霞1,黄良3,韩世明1,徐雪峰1,丁园2**   

  1. 1江西省-中国科学院庐山植物园, 江西庐山 332900; 2南昌航空大学环境与化学工程学院, 南昌 330063;3九江市林业局, 江西九江 332000
  • 出版日期:2011-07-18 发布日期:2011-07-18

Forest soil organic carbon density and its distribution characteristics along an altitudinal gradient in Lushan Mountains of China.

DU You-xin1, WU Cong-jian3, ZHOU Sai-xia1, HUANG Liang3,  HAN Shi-ming1,XU Xue-feng1, DING Yuan2   

  1. 1Lushan Botanical Garden, Jiangxi Province &Chinese Academy of Sciences, Lushan 332900, Jiangxi, China; 2College of Envioronmental Chemistry Engineering,Nanchang Hang Kong University, Nanchang 330063, China;3Jiujiang Forestry Bureau, Jiujiang 332000, Jiangxi, China
  • Online:2011-07-18 Published:2011-07-18

摘要: 为阐明地处中亚热带北部的庐山森林土壤有机碳沿海拔梯度的分布特征,2010年7—8月,分别在庐山的南、北坡按200 m的高差选择6个和5个不同海拔采样点,分层(0~10、10~20、20~30、30~40和>40 cm)采集土样,测定土壤容重、有机碳含量及有机碳密度.结果表明:海拔和坡向显著影响森林土壤有机碳密度.在北坡,随海拔升高, 土壤有机碳呈逐渐增加趋势,土壤有机碳含量与土壤容重和pH值呈显著负相关关系;在南坡则没有明显规律.随土层加深,土壤有机碳逐渐下降.北坡和南坡土壤有机碳密度分别为7.07~10.34 kg·m-2和6.03~12.89 kg·m-2.南坡土壤有机碳密度随海拔梯度和土层深度变化的变异性较大,原始植被的破坏和人工林的建立可能是影响土壤有机碳空间分布的重要因素之一.

关键词: 庐山, 海拔梯度, 森林土壤, 有机碳密度, 枯落物, 生态化学计量学, 土壤, 林龄, 叶片, 沙地樟子松

Abstract: To understand the spatial distribution characteristics of organic carbon in northern subtropical forest soils along an altitudinal gradient in Lushan Mountains of China, six and five sampling plots with a 200-m interval of elevation and covered by different vegetation types were installed on the southern and northern slopes, respectively in July-August in 2010 to collect soil profiles, with the soil thickness, bulk density, organic carbon content, and organic carbon density of 0-10 cm, 10-20 cm, 20-30 cm, 30-40 cm, and >40 cm layers measured. The soil organic carbon density was significantly affected by altitude and slope. On northern slope, soil organic carbon content increased with increasing altitude, and had significant negative correlations with soil bulk density and pH value. On southern slope, soil organic carbon content had no obvious variation pattern along the altitudinal gradient and had less correlation with soil bulk density and pH value, but soil organic carbon density decreased with increasing soil depth. The soil organic carbon density on northern and southern slopes was within the range of 7.07-10.34 kg·m-2 and 6.03-12.89 kg · m-2, respectively. The larger variation of soil organic carbon density along altitudinal gradient and soil depth on southern slope suggested that the destruction of original vegetation and the establishment of forest plantation could be one of the important factors affecting the spatial distribution of soil organic carbon.

Key words: Lushan, altitudinal gradient, forest soil, organic carbon density, litter, ecological stoichiometry, soil, stand age, leaf, Pinus sylvestris var. mongolica