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犀牛湖高氟化物成因分析及控制对策研究OA

Study on causes and control countermeasures of high fluoride content in Xiniu Lake

中文摘要英文摘要

针对我国北方干旱半干旱地区闭口型湖泊犀牛湖氟化物浓度超标问题,研究通过解析氟化物的空间分布特征、来源及其迁移路径,提出针对性治理策略.基于历史监测数据与加密布点采样(覆盖湖体、入湖水体、土壤及底泥).结果表明:犀牛湖氟化物浓度存在显著南北梯度差异,两次采样湖水氟化物浓度均是北湖采样点浓度大于南部采样点,主要受西大沟低氟补水的局部稀释作用影响.全湖平均浓度 1.34 mg/L.周边表层土壤总氟平均含量(241.17 mg/kg)低于全国均值(436 mg/kg),但水溶性氟占比高(6.15 mg/kg),且含量随深度递增;底泥总氟平均 357.4 mg/kg,湖区底泥氟含量(399~532 mg/kg)显著高于湖岸(233~356 mg/kg),表明由于地表径流或地下水补给持续释放至水体.溯源分析表明,历史工业源影响目前已不存在,当前氟富集以内源累积为主,入湖河流(西大沟、芦花沟)仅能短期稀释.针对犀牛湖浅水特征(平均水深 2 m),提出以水体置换为核心,通过西大沟引入低氟水分批或连续置换,结合动态水质监测优化水量与周期,同步辅以化学沉淀和生态修复抑制底泥氟再悬浮.为干旱区高氟湖泊治理提供了兼顾效率、经济性与生态安全的综合方案.

Aiming at the excessive fluoride pollution in Xiniu Lake,a closed lake located in the arid and semi-arid regions of northern China,targeted governance strategies were proposed in this research after the spatial distribution characteristics,sources and migration pathways of fluoride were analyzed.Historical monitoring data and intensive site sampling covering the lake water,inflow water,soil and sediment were adopted for the research.The results showed that obvious north-south gradient differences in fluoride pollution were detected in Xiniu Lake.Higher fluoride values were measured at sampling sites in the northern lake area rather than the southern area during two sampling campaigns,which were primarily affected by localized dilution triggered by low-fluoride water replenishment from Xida Ditch.The average fluoride pollution across the whole lake was calculated as 1.34 mg/L.The average total fluorine content in surrounding topsoil was determined to be 241.17 mg/kg,lower than the national average value of 436 mg/kg.Nevertheless,a high proportion of water-soluble fluorine(6.15 mg/kg)was recorded,and fluorine content was found to rise with increasing soil depth.The average total fluorine content of sediments was measured at 357.4 mg/kg.Significantly higher fluorine pollution(399~532 mg/kg)were quantified in lake sediments compared with lakeshore sediments(233~356 mg/kg),which indicated continuous fluorine release into water bodies via surface runoff or groundwater recharge.According to source apportionment analysis,impacts from historical industrial sources were verified to have disappeared.Current fluorine enrichment was dominated by endogenous accumulation,and inflow rivers(Xida Ditch and Luhua Ditch)were only capable of short-term dilution.In consideration of the shallow-water feature of Xiniu Lake with an average water depth of 2 m,comprehensive countermeasures centered on water replacement were put forward.Low-fluoride water diverted from Xida Ditch was suggested to replace lake water in batches or continuously.Water volume and replacement cycles were optimized on the basis of dynamic water quality monitoring.Chemical precipitation and ecological restoration were supplemented simultaneously to restrain the resuspension of sediment fluorine.An integrated scheme balancing efficiency,cost-effectiveness and ecological safety was provided for the remediation of high-fluoride lakes in arid zones.

张浩静;郝艳;洪坤钰;祁迹;马敬敬;马云龙

宁夏大学生态环境学院,银川 750021宁夏大学生态环境学院,银川 750021||宁夏环境科学研究院(有限责任公司),银川 750021宁夏环境科学研究院(有限责任公司),银川 750021宁夏大学生态环境学院,银川 750021宁夏大学生态环境学院,银川 750021银川市生态环境监测站,银川 750021

资源环境

氟化物污染闭口型湖泊水体置换生态修复

fluoride pollutionclosed lakeswater replacementecological restoration

《环境保护科学》 2026 (4)

59-66,8

黄河流域生态保护和高质量发展联合研究项目(2022-YRUC-01-050204-011-03)

10.16803/j.cnki.issn.1004-6216.202512010

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