Sediment nitrate dissimilatory reduction processes in the river-lake ecotone of Poyang Lake, China: Mechanisms and environmental implications

IF 2.8 3区 农林科学 Q3 ENVIRONMENTAL SCIENCES Journal of Soils and Sediments Pub Date : 2024-08-28 DOI:10.1007/s11368-024-03890-y
Yinghui Jiang, Zhenglei Xie, Mingjun Ding, Hua Zhang, Gaoxiang Huang, Yun Cao, Guoyu Yin
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Abstract

Purpose

The river-lake ecotone in lake ecosystems can strongly influence sediment nitrate dissimilatory reduction processes. However, the mechanisms underlying these processes in river-lake ecotone ecosystems are still poorly understood. This study aims to investigate the rates of sediment nitrate dissimilatory reduction processes in Poyang Lake and clarify the mechanisms and environmental implications of these processes.

Materials and methods

Sediment samples from five river-lake ecotones and lake ecosystems were collected from Poyang Lake, China. Sediment nitrate reduction and N2O production rates were measured using 15N isotope tracing experiments. The abundance of denitrifiers, anammox 16S rRNA bacteria, and nrfA genes was quantified using the polymerase chain reaction method. Correlation analysis, redundancy analysis, and stepwise linear regression were used to evaluate the mechanisms of sediment nitrate reduction processes.

Results and discussion

Sediments in the river-lake ecotone showed significantly higher denitrification (DEN), N2O production, dissimilatory nitrate reduction to ammonium (DNRA), and anammox rates compared to lake ecosystems. DEN was the dominant process contributing to nitrate reduction, accounting for 73.36% and 74.13% in the river-lake ecotone and lake ecosystem, respectively. DEN, N2O, and DNRA rates were significantly positively correlated with TOC, sulfide, and Fe2+ contents, which control the abundance of denitrifying and nrfA genes, ultimately increasing these rates.

Conclusion

The annual input of reactive N to the lake from the watershed is almost equivalent to the annual N removal. However, higher DNRA and N2O production rates indicate that approximately 23.59% of the annual N input to the lake may be transformed to NH4+ or N2O. N retention and N2O production in the river-lake ecotone significantly exceed those in the lake ecosystem, highlighting the ecotone as a hotspot for eutrophication risk and N2O emissions.

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中国鄱阳湖河湖生态区沉积物硝酸盐分解还原过程:机理与环境影响
目的 湖泊生态系统中的河湖生态带可对沉积物硝酸盐异化作用还原过程产生强烈影响。然而,人们对河湖生态带生态系统中硝酸盐还原过程的机理还知之甚少。本研究旨在调查鄱阳湖沉积物硝酸盐异嗜还原过程的速率,并阐明这些过程的机理及其对环境的影响。采用 15N 同位素追踪实验测量了沉积物硝酸盐还原率和 N2O 生成率。采用聚合酶链式反应方法量化了反硝化菌、厌氧 16S rRNA 细菌和 nrfA 基因的丰度。结果与讨论与湖泊生态系统相比,河流-湖泊生态区沉积物的反硝化作用(DEN)、N2O产生量、硝酸盐还原成氨的异氨还原作用(DNRA)和anammox速率都明显较高。反硝化作用是硝酸盐还原的主要过程,在河湖生态带和湖泊生态系统中分别占 73.36% 和 74.13%。DEN、N2O和DNRA速率与总有机碳、硫化物和Fe2+含量呈显著正相关,而总有机碳、硫化物和Fe2+含量可控制反硝化基因和nrfA基因的丰度,最终提高这些速率。然而,较高的 DNRA 和 N2O 生成率表明,每年输入湖泊的氮中约有 23.59% 可能转化为 NH4+ 或 N2O。河流-湖泊生态带的氮滞留量和 N2O 生成量明显超过湖泊生态系统,突出表明生态带是富营养化风险和 N2O 排放的热点地区。
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来源期刊
Journal of Soils and Sediments
Journal of Soils and Sediments 环境科学-土壤科学
CiteScore
7.00
自引率
5.60%
发文量
256
审稿时长
3.5 months
期刊介绍: The Journal of Soils and Sediments (JSS) is devoted to soils and sediments; it deals with contaminated, intact and disturbed soils and sediments. JSS explores both the common aspects and the differences between these two environmental compartments. Inter-linkages at the catchment scale and with the Earth’s system (inter-compartment) are an important topic in JSS. The range of research coverage includes the effects of disturbances and contamination; research, strategies and technologies for prediction, prevention, and protection; identification and characterization; treatment, remediation and reuse; risk assessment and management; creation and implementation of quality standards; international regulation and legislation.
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