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应用生态学报 ›› 2025, Vol. 36 ›› Issue (6): 1859-1870.doi: 10.13287/j.1001-9332.202506.035

• 研究论文 • 上一篇    下一篇

氮添加下夏季闽江河口短叶茳芏湿地土壤无机硫形态赋存特征

李尔恒1,2, 孙志高1,2,3*, 武慧慧1,2, 方冠荣1,2, 姚钦予1,2, 李亚瑾1,2, 钟小瑛1,2   

  1. 1福建师范大学福建省亚热带资源与环境重点实验室, 福州 350117;
    2福建师范大学湿润亚热带生态地理过程教育部重点实验室, 福州 350117;
    3福建闽江河口湿地生态系统国家定位观测研究站, 国家林业和草原局, 福州 350215
  • 收稿日期:2025-01-12 接受日期:2025-04-06 出版日期:2025-06-18 发布日期:2025-12-18
  • 通讯作者: *E-mail: zhigaosun@163.com
  • 作者简介:李尔恒, 男, 2001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: erhengLi01@163.com
  • 基金资助:
    福建省自然科学基金重点项目(2023J02012)、国家自然科学基金面上项目(42371105,41971128)和福建省“闽江学者奖励计划”

Impacts of nitrogen addition on variations of inorganic sulfur forms in soils of Cyperus malaccensis marsh in the Minjiang estuary during summer

LI Erheng1,2, SUN Zhigao1,2,3*, WU Huihui1,2, FANG Guanrong1,2, YAO Qinyu1,2, LI Yajin1,2, ZHONG Xiaoying1,2   

  1. 1Fujian Provincial Key Laboratory for Subtropical Resources and Environment, Fujian Normal University, Fuzhou 350117, China;
    2Ministry of Education Key Laboratory of Humid Subtropical Eco-geographical Process, Fujian Normal University, Fuzhou 350117, China;
    3Fujian Minjiang Estuary Wetland Ecosystem National Observation and Research Station, National Forestry and Grassland Administration, Fuzhou 350215, China
  • Received:2025-01-12 Accepted:2025-04-06 Online:2025-06-18 Published:2025-12-18

摘要: 选择闽江河口鳝鱼滩的短叶茳芏湿地为研究对象,基于野外氮添加模拟试验,对比研究了不同氮添加水平下(对照N0,0 g N·m-2·a-1;低氮NL,12.5 g N·m-2·a-1;中氮NM,25.0 g N·m-2·a-1;高氮NH,75.0 g N·m-2·a-1)湿地土壤无机硫形态的赋存特征。结果表明: 各氮处理湿地土壤中的水溶性硫(H2O-S)和盐酸溶解性硫(HCl-soluble-S)含量与对照相比均呈增加趋势,其值在NL、NM、NH处理下分别增加了36.0%、11.6%、7.5%和66.0%、29.4%、71.8%;而吸附性硫(Adsorbed-S)和盐酸挥发性硫(HCl-volatile-S)含量均呈降低趋势,降幅分别为45.8%、37.0%、4.0%和6.1%、1.7%、3.3%。氮添加整体提高了湿地土壤的总无机硫(TIS)含量和储量,且相较于N0处理,NL、NM、NH处理下的TIS含量分别增加了29.1%、8.2%、25.6%,储量分别增加了23.1%、13.7%、25.6%。不同氮处理下的TIS储量增幅主要取决于H2O-S和HCl-soluble-S的贡献。氮添加下湿地土壤不同形态无机硫含量变化主要取决于氮养分(尤其是NH4+-N/NO3--N)和pH的变化,并可能与植物-土壤系统之间的硫养分联系密切相关。氮添加下湿地土壤中的TIS含量及储量均明显升高,说明可供给植物吸收利用的有效硫养分整体增加,且该增加趋势在高氮处理(NH)下尤为明显。

关键词: 无机硫形态, 氮输入, 湿地土壤, 短叶茳芏, 闽江河口

Abstract: We investigated the distribution of inorganic sulfur forms in the typical Cyperus malaccensis marsh in the Minjiang estuary by conducting a field nitrogen (N) addition experiment with four N addition levels (no N treatment, N0, 0 g N·m-2·a-1; low N treatment, NL, 12.5 g N·m-2·a-1; medium N treatment, NM, 25.0 g N·m-2·a-1; and high N treatment, NH, 75.0 g N·m-2·a-1) . Results showed that the contents of water-soluble-sulfur (H2O-S) and HCl-soluble-sulfur (HCl-soluble-S) in marsh soil increased with N addition levels, and the values in the NL, NM and NH treatments increased by 36.0%, 11.6%, 7.5% (H2O-S) and 12.8%, 4.8%, 9.0% (HCl-soluble-S), respectively. The contents of adsorbed-sulfur (Adsorbed-S) and HCl-volatile-sulfur (HCl-volatile-S) decreased by 45.8%, 37.0%, 4.0% and 6.1%, 1.7% and 3.3%. N addition generally increased the contents and stocks of total inorganic sulfur (TIS). Compared with the N0 treatment, the TIS content in the NL, NM and NH treatments increased by 29.1%, 8.2% and 25.6%, while its stock increased by 23.1%, 13.7% and 25.6%, respectively. The elevation of TIS stock mainly rested with the contributions of H2O-S and HCl-soluble-S. The variations of inorganic sulfur forms were mainly dependent on the alterations of N nutrient (especially NH4+-N/NO3--N) and pH, and the relationships of S nutrient between plants and soils. Under N enrichment, the content and stock of TIS showed an increasing trend, indicating that the available S absorbed and utilized by plants was elevated and the increasing trend was particularly evident in the high N addition treatment (NH).

Key words: inorganic sulfur form, nitrogen addition, marsh soil, Cyperus malaccensis, Minjiang estuary