College of Agriculture, Guizhou University, Guiyang, 550025, China.
Key Laboratory of Karst Georesources and Environment of Ministry of Education, Guizhou University, Guiyang, 550025, China.
Environ Geochem Health. 2023 Nov;45(11):7585-7601. doi: 10.1007/s10653-023-01676-8. Epub 2023 Jul 2.
As important place for water storage and supply, drinking-water reservoirs in karst mountain areas play a key role in ensuring human well-being, and its water quality safety has attracted much attention. Source apportionment and ecological risks of heavy metal(loid)s in sediments of drinking-water reservoir are important for water security, public health, and regional water resources management, especially in karst mountain areas where water resources are scarce. To expound the accumulation, potential ecological risks, and sources of heavy metal(loid)s in a drinking-water reservoir in Northwest Guizhou, China, the surface sediments were collected and analyzed based on the combined use of the geo-accumulation index (I), sequential extraction (BCR), ratios of secondary phase and primary phase (RSP), risk assessment code (RAC), modified potential ecological risk index (MRI), as well as the positive matrix factorization methods. The results indicated that the accumulation of Cd in sediments was obvious, with approximately 61.9% of the samples showing moderate to high accumulation levels, followed by Pb, Cu, Ni, and Zn, whereas the As and Cr were at low levels. A large proportion of BCR-extracted acid extractable and reducible fraction were found in Cd (72.5%) and Pb (40.3%), suggesting high bioavailability. The combined results of RSP, RAC, and MRI showed that Cd was the major pollutant in sediments with high potential ecological risk, while the risk of other elements was low. Source apportionment results of heavy metal(loid)s indicated that Cd (75.76%) and Zn (23.1%) mainly originated from agricultural activities; As (69.82%), Cr (50.05%), Cu (33.47%), and Ni (31.87%) were associated with domestic sources related to residents' lives; Cu (52.36%), Ni (44.57%), Cr (34.33%), As (26.51%), Pb (24.77%), and Zn (23.80%) primarily came from natural geological sources; and Pb (47.56%), Zn (22.46%) and Cr (13.92%) might be introduced by mixed sources of traffic and domestic. The contribution ratios of the four sources were 18.41%, 36.67%, 29.48%, and 15.44%, respectively. Overall, priority control factors for pollution in relation to agricultural sources included Cd, while domestic sources are primarily associated with As. It is crucial to place special emphasis on the impacts of human activities when formulating pollution prevention and control measures. The results of this study can provide valuable reference and insights for water resources management and pollution prevention and control strategies in karst mountainous areas.
作为储水和供水的重要场所,喀斯特山区饮用水水库对保障人类福祉起着关键作用,其水质安全备受关注。水库沉积物中重金属(类)的来源解析和生态风险评估对于水安全、公众健康和区域水资源管理至关重要,特别是在水资源匮乏的喀斯特山区。为了阐明中国贵州西北部饮用水水库重金属(类)的积累、潜在生态风险和来源,本研究采用地积累指数(I)、连续提取(BCR)、次生相与原生相比值(RSP)、风险评估代码(RAC)、修正潜在生态风险指数(MRI)以及正矩阵因子分析(PMF)等方法,对水库沉积物进行了综合分析。结果表明,Cd 在沉积物中具有明显的积累,约 61.9%的样品表现出中到高的积累水平,其次是 Pb、Cu、Ni 和 Zn,而 As 和 Cr 则处于较低水平。BCR 提取的酸可提取和可还原部分中 Cd(72.5%)和 Pb(40.3%)的比例较大,表明其生物可利用性较高。RSP、RAC 和 MRI 的综合结果表明,Cd 是沉积物中主要的污染因子,具有较高的潜在生态风险,而其他元素的风险较低。重金属(类)的来源解析结果表明,Cd(75.76%)和 Zn(23.1%)主要来源于农业活动;As(69.82%)、Cr(50.05%)、Cu(33.47%)和 Ni(31.87%)与居民生活相关的生活源有关;Cu(52.36%)、Ni(44.57%)、Cr(34.33%)、As(26.51%)、Pb(24.77%)和 Zn(23.80%)主要来源于自然地质源;而 Pb(47.56%)、Zn(22.46%)和 Cr(13.92%)可能来自交通和生活混合源。四个源的贡献比例分别为 18.41%、36.67%、29.48%和 15.44%。总体而言,农业源污染的优先控制因子包括 Cd,而生活源主要与 As 有关。在制定污染防治措施时,应特别关注人类活动的影响。本研究结果可为喀斯特山区水资源管理和污染防治策略提供有价值的参考和启示。