长江科学院院报 ›› 2020, Vol. 37 ›› Issue (5): 50-58.DOI: 10.11988/ckyyb.20190170

• 水土保持与生态建设 • 上一篇    下一篇

鄱阳湖典型洲滩湿地植被叶片和土壤δ15N特征分析

肖洋1, 张翔2, 王孟1, 邓志民1, 林玉茹3   

  1. 1.长江水利委员会 长江水资源保护科学研究所, 武汉 430051;
    2.武汉大学 水资源与水电工程科学国家重点实验室, 武汉 430072;
    3.长江科学院 水资源综合利用研究所, 武汉 430010
  • 收稿日期:2019-02-25 出版日期:2020-05-01 发布日期:2020-06-10
  • 作者简介:肖 洋(1989-),男,湖北荆州人,工程师,博士,研究方向为生态水文学。E-mail:xiaoyang198990@outlook.com
  • 基金资助:
    国家重点研发计划项目(2017YFC0405300);国家自然科学基金项目(41601043);中央级公益性科研院所基本科研业务费项目(CKSF2017061/SZ)

Characteristics of δ15N of Foliage and Soil at Typical IsletWetland in Poyang Lake

XIAO Yang1, ZHANG Xiang2, WANG Meng1, DENG Zhi-min1, LIN Yu-ru3   

  1. 1. Changjiang Water Resources Protection Institute, Changjiang Water Resources Commission,Wuhan 430051,China;
    2. State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University,Wuhan 430072, China;
    3. Water Resources Department, Yangtze River Scientific Research Institute,Wuhan 430010, China
  • Received:2019-02-25 Published:2020-05-01 Online:2020-06-10

摘要: 为研究鄱阳湖典型洲滩湿地植被叶片和土壤δ15N特征,以蚌湖和修水之间的洲滩作为研究对象,选取典型断面研究2015年10—12月和2016年4月植被叶片和土壤δ15N的相关关系,探讨土壤含水量和无机氮(铵态氮和硝态氮)对植被叶片和土壤δ15N的影响。结果表明:大部分C3植被的叶片δ15N大于C4植被;湿润时期植被叶片和土壤δ15N大于干旱时期,但湿润时期和干旱时期植被叶片均较土壤富集15N。铵态氮在湿地土壤中占比高达87.43%,是土壤主要的无机氮,但湿地植被主要吸收硝态氮。研究区氮循环开度较小,土壤δ15N随着可利用氮素的增加而降低,而随着土壤含水量的增加而增加。植被叶片δ15N与土壤δ15N呈显著的正相关关系,植被叶片δ15N主要受土壤氮素变化和氮同位素分馏的影响。

关键词: 洲滩湿地, 植被叶片, δ15N, 氮循环, 氮素含量, 土壤含水量, 铵态氮, 硝态氮, 鄱阳湖

Abstract: To study the characteristics of δ15N of foliage and soil at typical islet wetland in Poyang Lake, we took the islet wetland between Benghu Lake and Xiushui River as the research object. We analyzed the relation between foliar δ15N and soil δ15N at typical section from October to December, 2015 and in April, 2016. We also examined the influence of moisture content of soil and inorganic nitrogen (ammonium nitrogen and nitrate nitrogen) content on foliar δ15N and soil δ15N. Results demonstrated that foliar δ15N of most C3 plants were larger than that of C4 plants. The foliar δ15N and soil δ15N in wet period were larger than those in drought period; however, in both wet and dry periods, the 15N was more enriched in foliage than in soil. Ammonium nitrogen is the major inorganic nitrogen in the wetland soil, accounting for 87.43%, whereas in wetland plants, nitrate nitrogen was dominantly adsorbed. The opening degree of nitrogen cycle in the study area is small, and the soil δ15N decreased with the increase of available nitrogen but increased with the rising of soil water content. There is a significant positive correlation between foliar δ15N and soil δ15N, and foliar δ15N is mainly affected by soil’s nitrogen content and nitrogen isotope fractionation.

Key words: islet wetland, plant foliage, δ15N, nitrogen cycle, nitrogen content, water content in soil, ammonium nitrogen, nitrate nitrogen, Poyang Lake

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