院报 ›› 2024, Vol. 41 ›› Issue (1): 59-65.DOI: 10.11988/ckyyb.20220852

• 水环境与水生态 • 上一篇    下一篇

都柳江上游水体中锑的矿山源贡献与健康风险评估

刘凤竹1, 张翅鹏1,2, 杨泽延1,3, 罗欢1, 罗江兰1   

  1. 1.贵州大学 资源与环境工程学院,贵阳 550025;
    2.贵州大学 贵州喀斯特环境生态系统教育部野外科学观测研究站,贵阳 550025;
    3.贵州大学 喀斯特地质资源与环境教育部重点实验室,贵阳 550025
  • 收稿日期:2022-07-19 修回日期:2022-09-07 出版日期:2024-01-01 发布日期:2024-01-15
  • 通讯作者: 张翅鹏(1983-),男,贵州贵阳人,副教授,博士,研究方向为土壤中重金属迁移转化与修复治理。E-mail: re.cpzhang@gzu.edu.cn
  • 作者简介:刘凤竹(1996-),男,贵州毕节人,硕士研究生,研究方向为环境重金属污染与防治。E-mail:3150152280@qq.com
  • 基金资助:
    国家自然科学基金委员会-贵州省人民政府喀斯特中心项目(U1612442)

Contribution Source and Health Risk Assessment of Antimony in Waters Upstream of Duliu River Polluted by Mining Activity

LIU Feng-zhu1, ZHANG Chi-peng1,2, YANG Ze-yan1,3, LUO Huan1, LUO Jiang-lan1   

  1. 1. College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China;
    2. Field Scientific Observation Station of Ministry of Education for Karst Environmental and Ecological System, Guizhou University,Guiyang 550025, China;
    3. Key Laboratory of Ministry of Education for Karst Geology Resources and Environment, Guizhou University, Guiyang 550025, China
  • Received:2022-07-19 Revised:2022-09-07 Online:2024-01-01 Published:2024-01-15

摘要: 以受锑矿开采污染的都柳江为研究对象,在上游河段采集水样和悬浮颗粒物样,利用切向超滤技术、S同位素技术及离子色谱法等获取相关理化数据,探究矿山活动对河流中锑(Sb)浓度的影响,以及不同水文条件下Sb形态转化与净化机制。研究表明:从上游初始污染点至三都县城段溶解态Sb浓度可由148.77 μg/L降至49.98 μg/L;受锑矿山影响干流 δ34S值升高,介于-0.58‰~1.21‰,且与Sb浓度呈显著正相关关系(r=0.71,p<0.05);生产和闭矿的两座矿山溪流下游混合后对干流水体Sb浓度贡献比为1.3:1;水体中溶解态Sb浓度包含真溶解态和胶体态,约为颗粒态Sb含量的170倍;真溶解态Sb占比80%以上,主要以迁移性较强的SbO-3形态存在;大坝拦截作用下水库中悬浮颗粒物浓度相对其他2个河段较低,但其Sb含量较高;水体中的Sb向胶体及颗粒态转化较少,不易被吸附团聚去除;3个河段Sb的健康风险评价结果显示HI和CR分别介于3.59~10.77和2.52×10-3~7.55×10-3,可能对人体产生致癌风险;真溶解态Sb是Sb污染水体中影响人体健康的主要形态。研究结果可为流域水环境Sb污染治理及生态保护提供科学依据。

关键词: 水环境, 矿山开采, Sb污染, S同位素, 健康风险评价

Abstract: This study focuses on the Duliu River, which has been contaminated due to antimony mining. Water and suspended particulate samples were collected from the upstream reaches and analyzed using tangential ultrafiltration, S isotope technology, and ion chromatography to obtain the physical and chemical properties. The aim is to investigate the effects of mining activities on the concentration of antimony (Sb) in rivers and the mechanisms behind the transformation and purification of Sb in different hydrological conditions. Results show that from the initial pollution point to the Sandu county section, the concentration of dissolved Sb decreased from 148.77 μg/L to 49.98 μg/L. Affected by antimony mining, the δ34S value in mainstream Duliu River increased, ranging from -0.58‰ to 1.21‰ and exhibiting a significant positive correlation with Sb concentration (r=0.71,p<0.05). The contribution ratio of producing and closed mines to the Sb concentration in the downstream section was 1.3:1. The concentration of dissolved Sb, including truly dissolved and colloidal Sb, was approximately 170 times that of particulate Sb, with truly dissolved Sb accounting for over 80%, mainly in the form of SbO-3. Despite lower concentration of suspended particulates in the reservoir compared to river sections, the Sb concentration in reservoir was higher. Sb was less likely to transform into colloid and particulate and was not easily removed through adsorption and agglomeration. Moreover, health risk assessment indicated that the HI and CR values were in the ranges of 3.59-10.77 and 2.52×10-3-7.55×10-3, respectively, implying possible carcinogenic risks to humans. In conclusion, truly dissolved Sb was the primary form posing a health hazard. This study provides a scientific basis for Sb pollution control and ecological protection in the contaminated Duliu River.

Key words: water environment, mining, Sb pollution, S isotope, health risk assessment

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