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四川安宁河地表水及表层沉积物氟元素分布特征OACSTPCD

Distribution of Fluorine in Surface Water and Sediment of Anning River Basin

中文摘要英文摘要

为探明四川省安宁河地表水及表层沉积物中氟的分布特征,于2022年对安宁河干流及其主要支流14个点位的地表水和表层沉积物进行采样,采用离子色谱法、熔碱-离子选择电极法等方法分别测定水体和表层沉积物中的氟含量,分析氟的分布特征及影响因素.结果表明:安宁河水体仅稀土矿区支流存在一定程度的氟污染,水中氟化物均值含量区间为0.14~1.33mg/L.沉积物中氟化物99%以残渣态存在,不易与其余物质发生化学反应从而析出,对生物的毒性风险较小.水体F-与REE3+、Ba2+、Pb2+、SO42-呈极显著相关(P<0.01).主成分分析源向讨论表明水体F-的来源与稀土矿的开采冶炼有关,同时其含量也受到岩石风化等自然因素的影响.

In order to examine the distribution characteristics of fluorine in the surface water and sediment samples of the Anning River,samples were collected from 14 locations along the main river and its tributaries in 2022.The fluorine content in both the surface water and the sediment were determined through the use of ion chromatography and molten alkali-ion selective electrode techniques,to evaluate the distribution patterns and factors that contribute to the presence of fluorine in the Anning River.The results indicated that fluorine contamination was confined to the tributaries of rare earth mining areas along the Anning River,and the average fluoride concentration in the water samples ranged from 0.14 to 1.33 mg/L.The majority(99%)of fluoride in sediment was found to be in a residual state,limiting its reactivity with other compounds and reducing the risk of toxicity to organisms.Additionally,a significant correlation was observed between water fluoride levels and the presence of rare earth elements(REE),barium(Ba),lead(Pb),and sulfate ions(SO42-)(P<0.01).Principal component analysis indicated that the presence of water fluoride levels can be linked to the extraction and processing of rare earth minerals,with its chemical composition also being influenced by natural processes like rock erosion.

陈俊尧;刘瑶;王洪波;张健峰;童敏;罗鹏;王雪梅

四川省凉山生态环境监测中心站,四川西昌 615000四川省凉山生态环境监测中心站,四川西昌 615000四川省凉山生态环境监测中心站,四川西昌 615000西昌学院资源与环境学院,四川西昌 615000西昌学院资源与环境学院,四川西昌 615000西昌学院资源与环境学院,四川西昌 615000西昌学院资源与环境学院,四川西昌 615000

环境科学

安宁河氟元素地表水表层沉积物

Anning Riverfluorinesurface watersediment

《四川环境》 2024 (6)

17-22,6

10.14034/j.cnki.schj.2024.06.003

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