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应用生态学报 ›› 2016, Vol. 27 ›› Issue (9): 2761-2770.doi: 10.13287/j.1001-9332.201609.006

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凋落物中水溶性有机物和残渣对亚热带森林土壤氮素转化的影响

马芬1,2, 裴广廷1,2, 马红亮1,2*, 高人1,2, 尹云锋1,2, 杨柳明1,2   

  1. 1湿润亚热带山地生态国家重点实验室培育基地, 福州 350007;
    2福建师范大学地理科学学院, 福州 350007
  • 收稿日期:2016-03-21 发布日期:2016-09-18
  • 通讯作者: * E-mail: mhl936@163.com
  • 作者简介:马 芬,女,1990年生,硕士研究生. 主要从事陆地生态系统土壤碳氮循环和生态环境研究. E-mail: fenma8487@163.com
  • 基金资助:
    国家自然科学基金项目(41271282,31170578)和教育部创新团队项目(IRT0960)资助

Effects of water-soluble organic matter and residue of litter on nitrogen transformation in subtropical forest soil.

MA Fen1,2, PEI Guang-ting1,2, MA Hong-liang1,2*, GAO Ren1,2, YIN Yun-feng1,2, YANG Liu-ming1,2   

  1. 1Cultivation Base of State Key Laboratory of Humid Subtropical Mountain Ecology, Fuzhou 350007, China;
    2College of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China
  • Received:2016-03-21 Published:2016-09-18
  • Contact: * E-mail: mhl936@163.com
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (41271282, 31170578) and the Project for Innovation Team of Ministry of Education (IRT0960)

摘要: 设置60%和90%WHC两种土壤水分条件,并添加凋落物过滤液、剩余残渣和丙氨酸,进行为期36 d的室内培养(25 ℃),研究了凋落物中水溶性有机物和残渣对土壤氮素转化的影响.结果表明: 在60%和90%WHC条件下,丙氨酸在土壤中迅速矿化,该处理的土壤铵态氮(NH4+-N)含量分别比对照显著提高5.4%~44.7%和16.1%~41.3%,净氮矿化和氨化速率在培养前期也高于对照,而凋落物过滤液和残渣添加处理则降低了土壤NH4+-N含量,且残渣的降幅大于过滤液.试验期间,土壤硝态氮(NO3--N)含量呈直线增长趋势,培养结束时60%WHC条件下NO3--N含量显著高于90%WHC.土壤水分含量增多不利于土壤有机质的矿化;90%WHC条件下可溶性有机碳(SOC)含量明显低于60%WHC,而土壤氧化亚氮(N2O)排放量比60%WHC提高1.5~63.0倍,且在60%WHC条件下凋落物残渣添加处理显著促进了土壤N2O的排放.凋落物在分解过程中的可溶性物质和剩余物对土壤氮的影响存在差异,且这种差异随分解而发生动态变化.

Abstract: An incubation experiment was carried out with the addition of litter filtrate, litter residue and alanine at 25 ℃ for 36 days under 60% and 90%WHC (water holding capacity) conditions. The results showed that alanine was rapidly mineralized in soil, and soil NH4+-N content significantly increased by 5.4%-44.7% and 16.1%-41.3%, respectively under 60% and 90%WHC conditions compared with the control. The soil net nitrogen mineralization and ammonification rates in the two treatments were also higher than those in the control at the early stage of incubation. However, the soil NH4+-N content was reduced by the addition of filtrate and residue, and the reduction degree of residue was greater. During the incubation, soil NO3--N content showed a linear increasing trend with the incubation time, and it was significantly higher under the 60%WHC condition than that under 90%WHC condition at the end of incubation. The mineralization of soil organic matter was limited by higher soil moisture. Therefore, the soil soluble organic carbon (SOC) content under 90%WHC condition was obviously lower than that under 60%WHC, but nitrous oxide (N2O) emission was 1.5-63.0 times higher than that under 60%WHC. Furthermore, N2O emission was induced significantly by the addition of litter residue under 60%WHC condition. These results indicated that there were different effects of soluble matter and litter residue on soil nitrogen transformation, and these differences would change dynamically in the decomposition process.