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应用生态学报 ›› 2025, Vol. 36 ›› Issue (10): 2945-2955.doi: 10.13287/j.1001-9332.202510.017

• 生态系统碳氮生物地球化学循环过程专栏(专栏策划: 林永新、郑棉海、倪祥银) • 上一篇    下一篇

滨海湿地转为养殖塘对土壤溶解性有机质的影响

王慧1, 吴限2, 袁俊吉2, 丁维新2, 郑丛语2, 徐向华1*   

  1. 1南京信息工程大学生态与应用气象学院, 南京 210044;
    2中国科学院南京土壤研究所, 南京 210008
  • 收稿日期:2025-02-26 修回日期:2025-08-27 发布日期:2026-05-04
  • 通讯作者: *E-mail: xuxianghua@nuist.edu.cn
  • 作者简介:王 慧, 女, 1999年生, 硕士研究生。主要从事湿地土壤碳氮循环研究。E-mail: 2305608683@qq.com
  • 基金资助:
    江苏省碳达峰碳中和科技创新专项资金(BK20220020)、江苏省杰出青年基金项目(BK20230050)和国家自然科学基金项目(U24A20628)

Impacts of converting coastal natural wetlands to mariculture ponds on soil dissolved organic matter

WANG Hui1, WU Xian2, YUAN Junji2, DING Weixin2, ZHENG Congyu2, XU Xianghua1*   

  1. 1School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing 210044, China;
    2Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China
  • Received:2025-02-26 Revised:2025-08-27 Published:2026-05-04

摘要: 滨海湿地是缓解气候变化的重要“蓝色”碳汇,但水产养殖业的快速发展驱动滨海湿地不断被转化为养殖池塘。本研究以江苏盐城滨海自然湿地和由湿地转变的不同养殖年限(7、10、12和15年)海水养殖塘为对象,利用紫外光谱和三维荧光光谱技术并结合平行因子分析法,分析了滨海湿地转化为养殖塘对土壤溶解性有机质(DOM)组分和来源特征的影响。结果表明:与自然湿地相比,滨海湿地转变为养殖塘导致DOM含量降低,且随着养殖年限增加DOM含量逐渐降低。DOM主要有4个有效荧光组分,包括3种类腐殖质物质(C1、C2、C3)和1种类蛋白质物质(C4),其中,陆源类腐殖质组分(C1和C3)在DOM中占主导地位,占比达58.7%~60.0%;随着养殖年限增加,4种组分含量均降低,其中C1和C3分别显著降低26.2%~51.7%和26.6%~61.9%。湿地转变为养殖塘7年后DOM稳定性显著降低,随后呈现上升趋势。冗余分析表明,土壤有机碳含量、电导率和含水量是驱动湿地转变过程中DOM变化的关键因素。综上,滨海湿地转变为养殖塘降低了土壤DOM含量,威胁滨海湿地碳汇功能,未来发展水产养殖业应尽量避免破坏滨海自然湿地。

关键词: 滨海湿地, 水产养殖, 溶解性有机质, 紫外光谱, 三维荧光光谱, 平行因子分析

Abstract: Coastal wetlands are important “blue carbon” ecosystems for mitigating climate change. The rapid expansion of mariculture has driven extensive conversion of coastal wetlands into aquaculture ponds. We investigated the impacts of such conversion on soil dissolved organic matter (DOM) by collecting soil samples from a Spartina alterniflora saltmarsh and four saltmarsh-converted mariculture ponds with the cultivation ages of 7, 10, 12, and 15 years in Yancheng, Jiangsu Province. The sources and components of DOM were characterized using ultraviolet-visible spectroscopy and three-dimensional excitation-emission matrix fluorescence spectroscopy combined with parallel factor analysis. Results showed that DOM concentrations in the ponds were lower than that in S. alterniflora saltmarsh and declined progressively with increasing pond age. Four fluorescence components were identified, including three humic-like substances (C1, C2, C3) and one protein-like substance (C4). Terrestrial humic-like components (C1 and C3) dominated the DOM pool (58.7%-60.0%) but declined most sharply following the cultivation age (26.2%-51.7% for C1 and 26.6%-61.9% for C3). After seven years of conversion, DOM stability significantly decreased, and then exhibited an upward trend. Redundancy analysis revealed that soil organic carbon content, electrical conductivity, and water content were the main factors driving DOM changes during the conversion. In conclusion, the conversion of coastal wetlands to mariculture ponds reduced soil DOM content and stability, thereby threatening their carbon sink function. Future mariculture development should minimize the conversion of natural coastal wetlands.

Key words: coastal wetland, mariculture, dissolved organic matter, ultraviolet-visible spectroscopy, three-dimensional excitation-emission matrix fluorescence spectroscopy, parallel factor analysis