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生态学杂志 ›› 2011, Vol. 30 ›› Issue (06): 1083-1090.

• 研究报告 • 上一篇    下一篇

沙田湖人工湿地植物-土壤有机碳库

徐后涛1,王丽卿1**,沈杰2,季高华1,赵风斌1   

  1. 1上海海洋大学水产与生命学院, 上海 201306;2上海市青浦区水利管理署, 上海 201700
  • 出版日期:2011-06-08 发布日期:2011-06-08

Plant and soil organic carbon pools in a constructed wetland of Shatianhu River.

XU Hou-tao1, WANG Li-qing1**, SHEN Jie2, JI Gao-hua1, ZHAO Feng-bin1   

  1. 1College of Fisheries and Life Science, Shanghai Ocean University, Shanghai 201306, China; 2Qingpu Water Resources Management Department, Shanghai 201700, China
  • Online:2011-06-08 Published:2011-06-08

摘要: 在人工构建的用于处理水产养殖废水的表面流和水平潜流湿地复合系统中,对湿地植物各组织、湿地表层土壤(0~10 cm)、湿地植物根际土壤的有机碳含量季节变化规律进行研究,并对湿地植物表层土壤和湿地植物对有机碳的固定作用进行了分析。结果表明:湿地植物地上部分组织固定的有机碳含量表现为在生长期迅速增加,8月较高,进入成熟期(11月)后保持稳定,8月有机碳含量与5月有显著性差异、与11月差异不显著;湿地植物地下部分组织固定的有机碳含量低于地上部分,但季节变化与地上部分相似,5月含量最小,8月达到一个较高的值,11月与8月有机碳含量差异不大。植物进入生长期后,湿地表层土壤有机碳含量显著高于湿地上无植物时期,各湿地植物根际土有机碳含量均高于表层土,但差异不显著(睡莲除外)。湿地表层土壤有机碳密度介于0.96~1.67 kg·m-2,受植物种类、植物生长季节等因素的影响。根据湿地面积和表层土壤有机碳含量,估算出沙田湖人工湿地(表面流湿地部分面积为3592 m2)0~10 cm土壤有机碳总量为5.61 t,通过植物吸收每年固定的碳量为10.34 t。

关键词: 贡嘎山, 暗针叶林, 峨眉冷杉, 群落结构

Abstract: The artificially constructed wetland of Shatianhu River is a complex wetland system used for treating the surface flow and horizontal undercurrent of aquaculture wastewater. Taking this wetland as test object, this paper studied the seasonal variations of organic carbon concentration in plant organs, surface soil (0-10 cm), and rhizosphere soil, and assessed the carbon sequestration potential of the plant organs and surface soil. The fixed carbon in the aboveground parts of the wetland plants increased rapidly during growth period, being higher in August and kept stable at mature stage (November), and with significant difference between May and August and but less difference between August and November. The carbon fixed in underground parts of the plants was lower than that in aboveground parts, but its seasonal variation pattern was similar, being the lowest in May, relatively higher in August, and less difference between August and November. During the growth period of the plants, surface soil organic carbon content was significantly higher than that in the period with no plants in the wetland. The organic carbon content in surface soil was lower than that in rhizosphere soil, but less difference was observed (except for water lily). The surface soil organic carbon density was in the range of 0.96-1.67 kg·m-2, which was affected by the plant species, plant growth season, and others. Based on the wetland area (surface flow part was 3592 m2) and surface soil organic carbon content, it was estimated that the wetland surface soil organic carbon stock was 5.61 t, and the annual plant carbon sequestration was 10.34 t.

Key words: Gongga Mountains, Dark coniferous forest, Abies fabri, Community structure