向海自然保护区湿地地表水氟化物分布特征及相关性分析
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1.吉林农业大学;2.白城市机动车排气污染防治技术服务中心;3.张家港港务集团有限公司港埠分公司

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X52,X142

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吉林省2020年省级污染防治专项资金白城市水环境区域补偿资金项目(吉财资环指﹝2020﹞544号);吉林省2023年省级污染防治专项资金白城市水环境断面达标奖励资金项目(吉财资环指﹝2022﹞995号)


Characterization and correlation analysis of fluoride distribution in wetland surface water of Xianghai Nature Reserve
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    摘要:

    [目的]本研究旨在揭示向海国家级自然保护区湿地水体中氟化物的时空分布规律及其驱动机制,明确水质超标原因,为科学制定向海湿地生态治理措施提供理论支撑,为区域水环境治理、流域水质改善提供经验。[方法]根据向海自然保护区湿地地表水国控断面2012—2021年十年间的长期监测数据,对比分析氟化物在丰水期、平水期和枯水期的不同浓度特征,阐明氟化物的年际和季节变化特征。运用Pearson相关性分析探寻各项水质指标间的关联性,并结合Gibbs图分析地表水水化学特征,解析氟化物的自然来源。[结果]①2012—2021年间,向海水库地表水氟化物年均浓度为2.02~3.87 mg/L,长期超过地表Ⅴ类水质标准(GB3838-2002)限值,年均超标倍数达0.36~1.61倍。②时间变化上,氟化物浓度在枯水期较高3.54~3.66 mg/L,丰水期较低2.76~2.87 mg/L,呈现出先下降后回升再下降的趋势,具有较强的季节性波动;空间上,2022年一场泡氟化物浓度1.56~3.2 mg/L显著高于二场泡1.16~2.48 mg/L。③底泥沉积物中总氟化物含量呈现明显空间分异,一场泡均值576 mg/kg远高于二场泡113 mg/kg,且与水溶性氟分布趋势一致,周边区域土壤中总氟化物含量高。④向海水库地表水主要水化学类型为HCO3?—Na?Mg和HCO3?—Na型,地表水水化学的成因以及氟化物富集与区域蒸发浓缩作用、溶解沉淀作用、离子交换作用等均有密切关联。[结论]向海水库地表水氟化物主要污染途径是内源释放,建议着手于内源污染和水文调控进行治理。

    Abstract:

    [Objective] This study aims to reveal the spatio-temporal distribution patterns and driving mechanisms of fluoride in the wetland water of Xianghai National Nature Reserve, clarify the reasons for water quality exceeding standards, and provide theoretical support for the scientific formulation of ecological governance measures for Xianghai Wetland, as well as offer experience for regional water environment governance and improvement of water quality in the basin. [Methods] Based on the long-term monitoring data of the national control section of surface water in Xianghai Nature Reserve from 2012 to 2021, the different concentration characteristics of fluoride in the flood season, normal water season and dry season were compared and analyzed to clarify the inter-annual and seasonal variation characteristics of fluoride. Pearson correlation analysis was used to explore the correlations among various water quality indicators, and Gibbs diagram was combined to analyze the water chemical characteristics of surface water and interpret the natural sources of fluoride. [Results]① From 2012 to 2021, the annual average fluoride concentration in the surface water of Xianghai Reservoir ranged from 2.02 to 3.87 mg/L, chronically exceeding the Class V surface water quality standard (GB3838-2002) by 0.36–1.61 times annually.② Temporally, fluoride concentrations were higher in the dry season (3.54–3.66 mg/L) and lower in the wet season (2.76–2.87 mg/L), exhibiting an initial decline, subsequent rebound, and final decline with pronounced seasonal fluctuations. Spatially, concentrations at Yichangpao (1.56–3.2 mg/L, 2022) significantly exceeded those at Erchangpao (1.16–2.48 mg/L).③ Sediment total fluoride content showed distinct spatial heterogeneity, with mean values at Yichangpao (576 mg/kg) far exceeding Erchangpao (113 mg/kg), aligning with water-soluble fluoride distribution trends. Surrounding soil exhibited high total fluoride levels.④ The dominant hydrochemical types of surface water were HCO??—Na?Mg and HCO??—Na, with fluoride enrichment closely linked to regional evaporation concentration, dissolution-precipitation, and ion exchange processes. [Conclusion] Endogenous release is the primary pollution pathway for fluoride in Xianghai Reservoir’s surface water. Control measures should focus on endogenous pollution management and hydrological regulation.

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  • 收稿日期:2025-03-17
  • 最后修改日期:2025-06-09
  • 录用日期:2025-06-12
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