利用含 Freundlich 参数的有限元模型对越南北宁省传统金属回收工艺村含水层重金属污染的研究

IF 0.9 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Russian Journal of Pacific Geology Pub Date : 2024-08-09 DOI:10.1134/s1819714024700155
Nguyen Bach Thao, Renat Shakirov, Nadezhda Syrbu, Tran Vu Long, Trinh Hoai Thu, Dao Duc Bang, Tran Quang Tuan, Duong Thi Thanh Thuy, Kieu Thi Van Anh, Vu Thu Hien, Natalia Lee
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引用次数: 0

摘要

摘要 越南,特别是北宁省的传统工艺村落对环境造成了许多负面影响。在金属回收和金属铸造领域,金属回收铸造工艺村产生的富含重金属的废物不仅对空气、土壤和沉积物造成严重的重金属污染,还对地下水资源造成污染。在越南北宁省 Tu Son 镇 Chau Khe 区的 Da Hoi 钢铁回收工艺村,全新世含水层暴露在受重金属铅、镉、镍和锌污染的 Ngu Huyen Khe 河沉积物中。在建立重金属迁移有限元模型时,选择了全新世含水层的 Freundlich 等温线参数,并采用了高时空变化延迟因子,以获得可靠的重金属在深度和时间上的定量分布。对初始条件和边界条件进行了改进。在全新世含水层中,重金属铅、锌、镉和镍的平流和扩散迁移的延迟因子是高度非线性的,并且在时间和空间上变化很大:铅为 8.7-66.4,锌为 2.0-12,镉为 1.7-4.8,镍为 1.1-5.9。数值模拟结果表明,重金属在全新世含水层中的迁移速度非常快,在整个含水层厚度内,镉和镍在 2-2.5 年左右、锌在 4 年左右、铅在 27 年左右就达到了含水层形成和含水层水体重金属浓度的平衡。从全新世含水层到更新世含水层的重金属通量是最大的,并且与平衡时间基本恒定,这将对更新世含水层造成严重污染。
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Study on Aquifer Contamination by Heavy Metals Using Finite Element Modeling with Freundlich Parameters in Traditional Metal Recycling Craft Village in Bac Ninh Province, Vietnam

Abstract

The traditional craft villages in Vietnam in general and in Bac Ninh province in particular have been exposing many negative impacts on the environment. The heavy metal-rich wastes from the metal recycling casting craft villages in the field of metal recycling and metal casting are causing severe heavy metal pollution not only to the air, soils, and sediments but also to the groundwater resources. In Da Hoi iron recycling craft village in Chau Khe ward, Tu Son town, Bac Ninh province, Vietnam, the Holocene aquifer is exposed to the Ngu Huyen Khe River’s sediments contaminated with heavy metals Lead, Cadmium, Nickel, and Zinc. Freundlich isotherm parameters of the Holocene aquifer have been selected for finite element modeling of heavy metal transport with high temporal and spatial varying retardation factors to get reliable quantitative heavy metals’ distribution in depth and time. Initial and boundary conditions have been augmented to be established. The retardation factors of the advection and dispersion transport in the Holocene aquifer for heavy metals Pb, Zn, Cd, and Ni are very highly none-linear and very much varying in time and space: 8.7–66.4 for Pb, 2.0–12 for Zn, 1.7–4.8 for Cd and 1.1–5.9 for Ni. The results of the numerical modeling show that heavy metal transport in the Holocene aquifer is very fast and the entire aquifer thickness has equilibrium aquifer formation and aquifer water heavy concentrations after around 2–2.5 years for Cd and Ni, around 4 years for Zn and around 27 years for Pb. The heavy metals’ fluxes from the Holocene aquifer to the Pleistocene aquifer are maximal and more or less constant from the equilibrium time and would cause severe contamination of the Pleistocene aquifer.

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来源期刊
Russian Journal of Pacific Geology
Russian Journal of Pacific Geology 地学-地球科学综合
CiteScore
1.30
自引率
37.50%
发文量
34
审稿时长
>12 weeks
期刊介绍: Russian Journal of Pacific Geology publishes the results of research on the Earth crust and mantle composition and provides articles on the geological structure and patterns of distribution of mineral deposits in the Pacific Ocean, marginal seas and continental margins. It discusses the topics of stratigraphy, sedimentology, magmatic activity, and seismicity. The journal deals with the problems of lithosphere plates tectonics, and offers the results of neotectonic, geomorphological, geodesic, environmental and mining studies in the Pacific region. The journal accepts theoretical, methodical and philosophical articles covering general issues of geology, geophysics, geochemistry, geoecology and mining. The journal also publishes critical notes and comments, and reviews.
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