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生态学杂志 ›› 2011, Vol. 30 ›› Issue (06): 1119-1124.

• 研究报告 • 上一篇    下一篇

太湖湖滨带土壤活性有机碳沿水分梯度的变化特征

沈玉娟1,赵琦齐1,冯育青1,2,王琳菲1,陆华兵3,余杏生3,阮宏华1**   

  1. 1南京林业大学, 江苏省林业生态工程重点实验室, 南京 210037;2苏州市湿地保护与管理站, 江苏苏州 215000;3苏州市吴中区林业局, 江苏苏州 215128
  • 出版日期:2011-06-08 发布日期:2011-06-08

Variation characteristics of soil active organic carbon along a soil moisture gradient in a riparian zone of Taihu Lake.

SHEN Yu-juan1, ZHAO Qi-qi1, FENG Yu-qing2, WANG Lin-fei1, LU Hua-bing3, SHE Xing-sheng3, RUAN Hong-hua1**   

  1. 1Jiangsu Key Laboratory of Forestry and Ecological Engineering, Nanjing Forestry University, Nanjing 210037, China; 2The Office of Wetland Conservation and Management, Suzhou 215000, Jiangsu, China;3Juzhou Forestry Station, Suzhou 215128, Jiangsu, China
  • Online:2011-06-08 Published:2011-06-08

摘要: 湖滨带等水陆交错区土壤碳循环是全球碳循环的一个重要的组成部分,但相关方面的研究还相当缺乏。本研究选择位于苏州渔阳山保存较为良好的典型的太湖湖滨带作为实验地,并根据距离水体的远近,将湖滨带从近水体到高岗地分别设置3个实验区,对湖滨带湿地土壤水溶性有机碳(WSOC)、轻组有机碳(LFOC)2种活性有机碳进行研究,分析土壤活性有机碳与土壤因子的关系。结果表明:土壤水分明显影响土壤表层活性有机碳的含量,湖滨带土壤WSOC、LFOC在表层(0~10 cm)沿土壤水分梯度的降低而减小,表现为近水区>中水区>远水区,且下层土壤沿水分梯度的差异变小;表层土壤活性有机碳各组分显著高于下层土壤,这与土壤有机碳和氮素变化趋势一致;WSOC、LFOC均与土壤总有机碳、土壤全氮、土壤含水率呈显著或极显著正相关;沿水分梯度土壤有机碳、全氮和土壤湿度是调控土壤活性有机碳沿水分梯度变化的主要因子。

关键词: 小麦, 温光敏核雄不育系, 育性转换, 温度敏感期, 临界温度

Abstract: Soil carbon cycle in aquatic-terrestrial ecotone (e.g., riparian zone) is an important component of global carbon cycle, but few researches are made on it. Taking a typical riparian zone of Taihu Lake near Suzhou as the object, three experimental sites along a soil moisture gradient, i.e., from the near of water body to the high mound, were installed in this paper, with the soil water soluble organic carbon (WSOC) and light fraction organic carbon (LFOC) contents and their correlations with soil physical and chemical factors analyzed. Soil moisture had obvious effects on the surface soil (0-10 cm) active organic carbon. The surface soil WSOC and LFOC contents decreased along the soil moisture gradient, but the variation degree of these contents in deeper soil layers became smaller. The WSOC and LFOC contents were significantly higher in surface soil than in subsurface soil, which was in accordance with the variation trends of soil organic carbon and nitrogen. In different soil layers at each site, the WSOC and LFOC were all significantly positively correlated with soil total organic carbon, total nitrogen, and moisture, suggesting that the latter three parameters could be the main factors controlling soil active soil organic carbon.

Key words: Triticum aestivum, Thermo-photo-sensitive genic male sterile line, Fertility transition, Thermo-sensitive period, Critical temperature