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应用生态学报 ›› 2026, Vol. 37 ›› Issue (9): 3141-3150.doi: 10.13287/j.1001-9332.202609.043

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闽江河口短叶茳芏湿地围垦为养殖塘对土壤反硝化潜势的影响

曾钰航1,2,3, 朱倩1,2,3, 杨平1,2,3*, 刘文静1,2,3, 仝川1,2,3, 林永新1,2, 杨洪4   

  1. 1福建省亚热带资源与环境重点实验室, 福建师范大学, 福州 350117;
    2福建师范大学地理科学学院, 福州 350117;
    3福建师范大学亚热带湿地研究中心, 福州 350117;
    4Department of Geography and Environmental Science, University of Reading, Reading RG6 6AB, UK
  • 收稿日期:2026-06-09 接受日期:2026-07-20 出版日期:2026-09-18 发布日期:2026-10-12
  • 通讯作者: *E-mail: geo_pingyang@fjnu.edu.cn
  • 作者简介:曾钰航, 女, 2002年生, 硕士研究生。主要从事湿地生物地球化学循环研究。E-mail: 734825736@qq.com
  • 基金资助:
    国家自然科学基金项目(42371100, 41801070)和福建省杰出青年科学基金项目(2025J010028)

Impact of reclamation of Cyperus malaccensis wetland into aquaculture ponds on soil denitrification potential in the Minjiang River Estuary

ZENG Yuhang1,2,3, ZHU Qian1,2,3, YANG Ping1,2,3*, LIU Wenjing1,2,3, TONG Chuan1,2,3, LIN Yongxin1,2, YANG Hong4   

  1. 1Fujian Provincial Key Laboratory for Subtropical Resources and Environment, Fujian Normal University, Fuzhou 350117, China;
    2School of Geographical Sciences, Fujian Normal University, Fuzhou 350117, China;
    3Research Centre of Wetlands in Subtropical Region, Fujian Normal University, Fuzhou 350117, China;
    4Department of Geography and Environmental Science, University of Reading, Reading RG6 6AB, UK
  • Received:2026-06-09 Accepted:2026-07-20 Online:2026-09-18 Published:2026-10-12

摘要: 围垦养殖作为滨海湿地退化与丧失的主要驱动力,显著影响了滨海地区氮生物地球化学循环过程。本研究以闽江河口短叶茳芏盐沼湿地及其围垦成的陆基养殖塘为对象,采用乙炔抑制法,分析了盐沼湿地围垦为养殖塘对土壤反硝化潜势特征的影响。结果表明:与短叶茳芏湿地相比,滨海湿地转化为养殖塘使土壤反硝化潜势显著降低61.2%~71.7%。土壤总碳、总氮、孔隙水中NO3--N与NH4+-N分别显著降低5.1%、62.3%、64.8%和53.6%,4种反硝化功能基因丰度(nirK、nirS、nosZⅠ和nosZⅡ)分别显著降低85.7%、92.6%、91.6%和94.1%,而土壤碳氮比显著提高170.4%。随机森林分析表明,土壤总氮、孔隙水NO3--N、NH4+-N及土壤nirK和nirS基因丰度是驱动湿地转变过程中土壤反硝化潜势变化的主要环境因子。综上,围垦养殖活动显著抑制了土壤的反硝化潜势,进而削弱了滨海湿地的自然脱氮能力,降低系统对外源氮负荷的净化缓冲能力,在同等氮输入水平下增加了氮素滞留与水体富营养化的潜在风险。

关键词: 反硝化潜势, 反硝化微生物, 碳氮底物, 围垦养殖, 河口湿地

Abstract: Land reclamation for aquaculture, a major driver of coastal wetland degradation and loss, may influence nitrogen biogeochemical cycling at the region scale. Using acetylene inhibition method, we measured soil denitrification potential (SDP) of a Cyperus malaccensis marsh and the converted earthen aquaculture pond in the Shanyutan wetland of the Miniiang River Estuary, southeastern China. Results showed that, compared with the C. malaccensis marsh, the conversion of coastal wetlands into aquaculture ponds significantly reduced SDP by 61.2% to 71.7%. Total soil carbon, total nitrogen, NO3--N, and NH4+-N in pore water significantly decreased by 5.1%, 62.3%, 64.8%, and 53.6%, respectively. The abundances of four denitrification functional genes (nirK, nirS, nosZⅠ, and nosZⅡ) significantly decreased by 85.7%, 92.6%, 91.6%, and 94.1%, respectively, while soil carbon-to-nitrogen ratio significantly increased by 170.4%. Random forest analysis identified soil total nitrogen, porewater NO3--N and NH4+-N, and the abundances of nirK and nirS genes as the main factors driving the variation in SDP following the wetland conversion. Overall, reclamation for aquaculture markedly suppressed soil denitrification potential, which in turn diminished the coastal wetland’s natural nitrogen removal and its buffering capacity against exogenous nitrogen loading, consequently raising the risks of nitrogen retention and eutrophication under equivalent nitrogen inputs.

Key words: denitrification potential, denitrifier, carbon-nitrogen substrate, aquaculture reclamation, estuarine wetland