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生态学杂志 ›› 2025, Vol. 44 ›› Issue (9): 2966-2975.doi: 10.13292/j.1000-4890.202509.031

• 研究报告 • 上一篇    下一篇

滨海湿地沉积物中不同形态无机硫分布特征及其影响因素

乔曼容1,郎赟超1,2,3,韩晓昆1,2,3*,剌伟4,丁虎1,2,3,刘丛强1,2,3
  

  1. 1天津大学地球系统科学学院, 表层地球系统科学研究院, 天津 300072; 2天津市环渤海地球关键带科学与可持续发展重点实验室, 天津 300072; 3天津环渤海滨海地球关键带国家野外科学观测研究站, 天津 300072; 4山西大学环境与资源学院, 太原 030031)

  • 出版日期:2025-09-10 发布日期:2025-09-03

Spatial distribution and influencing factors of inorganic sulfur species in coastal wetland sediments.

QIAO Manrong1, LANG Yunchao1,2,3, HAN Xiaokun1,2,3*, LA Wei4, DING Hu1,2,3, LIU Congqiang1,2,3   

  1. (1Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, China; 2Tianjin Key Laboratory of Earth Critical Zone Science and Sustainable Development in Bohai Rim, Tianjin 300072, China; 3Tianjin Bohai Rim Coastal Earth Critical Zone National Observation and Research Station, Tianjin 300072, China; 4School of Environmental & Resource Science, Shanxi University, Taiyuan 030031, China).

  • Online:2025-09-10 Published:2025-09-03

摘要: 硫(S)循环是生物地球化学循环的重要环节,深刻影响着碳、铁、磷等元素循环和滨海湿地生态功能。为了深入理解滨海湿地沉积物中硫的迁移转化过程,本研究通过采集天津北大港湿地沉积柱样品,分析了不同盐度湿地沉积物中酸可挥发性硫(AVS)、元素硫(ES)、黄铁矿硫(FeS2)、有机碳和活性铁含量,阐明了不同盐度湿地沉积物剖面中不同形态硫、活性铁和有机碳的垂向分布特征,探讨了不同形态硫迁移转化的影响因素。结果显示,中盐湿地和多盐湿地沉积物中还原性无机硫以AVS为主,分别占还原性无机硫的71.45%±18.97%和58.96%±28.88%,其次是FeS2及其少量ES,而在寡盐的水库湿地中FeS2含量最高,其平均含量为83.41±33.03 μmol·g-1,占还原性无机硫的71.98%±13.01%,说明不同盐度湿地沉积物中还原性无机硫的分布情况具有明显差异。研究表明,中高盐度湿地水体中硫酸盐浓度较高,导致沉积物中甲烷和有机质驱动的硫酸盐还原作用较强烈,产生较多的AVS,其黄铁矿生成主要受到活性铁和ES含量限制,而寡盐水库湿地沉积物中FeS2的累积可能主要受到水库滞留效应和颗粒输入以及元素硫较高等因素的影响。研究结果有助于湿地生态环境的修复和管理。


关键词: 滨海湿地, 沉积物, 还原性无机硫, 酸可挥发性硫, 元素硫, 黄铁矿, 活性铁

Abstract: Sulfur cycle is an important component of fundamental biogeochemical cycles, which deeply affects the cycles of carbon, iron, phosphorus and other elements as well as the ecological function of coastal wetlands. In this study, we measured the content of acid volatile sulfide (AVS), elemental sulfur (ES), pyrite sulfur (FeS2), organic carbon, and active iron in the sediment cores collected from the Beidagang wetland (in Tianjin) with different salinity, to better understand the migration and transformation processes of sulfur in coastal wetland sediments. The vertical distribution characteristics of sulfur species, active iron, and organic carbon in the wetlands with different salinity were clarified. The influencing factors of sulfur migration and transformation in different forms were examined. The results showed that AVS was the main reduced inorganic sulfur in the sediments of mesohaline and polyhaline wetlands, followed by FeS2 and ES. The relative contributions of AVS to reduced inorganic sulfur (RIS) were 71.45% ± 18.97% and 58.96% ± 28.88% for the mesohaline and polyhaline wetland sediments, respectively. However, the content of FeS2 was the highest inorganic sulfur in the sediments of oligohaline wetland, with an average content of 83.41 ± 33.03 μmol·g-1, which accounted for 71.98% ± 13.01% of RIS in the sediments. These results indicated that the spatial distribution of reduced inorganic sulfur species in wetland sediments highly depended on salinity. Furthermore, the high sulfate concentration in the water of mesohaline and polyhaline wetlands led to an enhanced sulfate reduction driven by methane and organic matter in the sediments, producing more AVS. The formation of pyrite in the mesohaline and polyhaline wetlands was mainly limited by the content of active iron and ES, while the accumulation of FeS2 in the sediments of oligohaline wetland may be mainly affected by the reservoir retention effect, particle input, and high sulfur content. Our results contribute to the restoration and management of ecological environment in wetlands.


Key words: coastal wetland, sediment, reduced inorganic sulfur, acid volatile sulfide, elemental sulfur, pyrite, active iron