废弃矿区锑污染源和锑矿相的蚀变途径:次生莫蓬石[NaSb(OH)6]的作用

IF 3.1 3区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Dario Fancello , Elisabetta Dore , Daniela Medas , Nicola Rigonat , Carlo Meneghini , Marilena Moroni , Stefano Naitza , Patrizia Onnis , Giovanni De Giudici
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引用次数: 0

摘要

采矿活动造成的锑污染是当前的一个环境问题。本文研究了意大利撒丁岛东南部苏苏尔吉乌(Su Suergiu)废弃锑矿中锑的释放和迁移过程。利用x射线粉末衍射、扫描电镜-能量色散光谱和电子探针-波长色散光谱对露头岩石、矿山废弃物和冶炼渣进行了分析,提供了矿物学和成分数据,有助于探讨Sb相的氧化途径。锑的主要来源是金属锑和Sb2O3 (valentinite/ senarmonite),作为冶炼过程的残留物倾倒在冶炼渣堆中,以及天然露头和矿山废物中发现的原生辉锑矿(Sb2S3)。这些矿物经过风化作用,在溶液中释放出Sb,在溶液中被氧化并以溶解的Sb(OH)6−的形式存在。碳酸盐和钠相,如冶金过程中产生的水合钠硅酸盐,影响冶炼渣堆的地球化学平衡,其中已经观察到稀有的钼辉石Na[Sb(OH)6]的沉淀。在Su Suergiu,钼辉石起源于溶解沉淀过程,作为氧化途径的最后形成矿物,通过结合Sb(OH)6−in溶液来限制Sb的迁移率。在检测到的Sb次级相(例如Sb-氧化物、fsb -氧化物等)中,尽管由于其稳定性受水文状况、溶解度和水的物理化学参数的影响,其作为临时汇的作用,但钼辉石是主要的Sb粘合剂。次生含锑矿物可控制锑在污染区内的分散。在苏苏尔久,由于与冶金活动有关的特定地球化学条件,含铁化合物对Sb迁移的作用低于钼辉石。这项研究的相关性源于Sb的已知毒性及其在世界范围内的漫漫性开采,这导致Sb冶炼厂产生的富含na - Sb的残留物广泛存在。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Antimony contamination sources and alteration pathways of Sb mineral phases in an abandoned mining area: The role of secondary mopungite [NaSb(OH)6]

Antimony pollution caused by mining activities is a current environmental concern. This study investigates the processes involved in the Sb release and mobility in the abandoned Sb mine of Su Suergiu (SE Sardinia, Italy). Analyses of outcropping rocks, mine wastes and smelting slags by means of X-Ray Powder Diffraction, Scanning Electron Microscopy - Energy Dispersive Spectroscopy and Electron Microprobe – Wavelength Dispersive Spectroscopy provided mineralogical and compositional data which contributed to the discussion about the oxidation pathways of Sb phases. The main Sb sources are metallic Sb and Sb2O3 (valentinite/senarmontite), dumped in the smelting slag heaps as residues of metallurgical processes, and primary stibnite (Sb2S3) found in natural outcrops and mine wastes. These minerals, subjected to weathering processes, release Sb in solution where it is oxidized and remains as dissolved Sb(OH)6. Carbonates and Na phases, like hydrate NaAl-silicate derived from metallurgical processes, influence the geochemical equilibria of the smelting slag heaps, where the precipitation of the rare mopungite, Na[Sb(OH)6], has been observed. At Su Suergiu, mopungite originates from a dissolution-precipitation process as the last forming mineral of the oxidation pathways, limiting the Sb mobility by bonding the Sb(OH)6 in solution. Among the detected Sb secondary phases (e.g., Sb-oxides, FeSb-oxides, etc.), mopungite is the prevalent Sb binder although it acts as a temporary sink because its stability is influenced by the hydrological regime, its solubility, and the water physicochemical parameters. Secondary Sb-bearing minerals can control the dispersion of Sb in contaminated area. At Su Suergiu the role of Fe-bearing compounds on Sb mobility is subordinate to that of mopungite due to the specific geochemical conditions related to the metallurgical activities. The relevance of this study arises from the known toxicity of Sb and from its worldwide diffuse mining, that results in the widespread occurrence of Na–Sb-rich residues produced by Sb smelting plants.

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来源期刊
Applied Geochemistry
Applied Geochemistry 地学-地球化学与地球物理
CiteScore
6.10
自引率
8.80%
发文量
272
审稿时长
65 days
期刊介绍: Applied Geochemistry is an international journal devoted to publication of original research papers, rapid research communications and selected review papers in geochemistry and urban geochemistry which have some practical application to an aspect of human endeavour, such as the preservation of the environment, health, waste disposal and the search for resources. Papers on applications of inorganic, organic and isotope geochemistry and geochemical processes are therefore welcome provided they meet the main criterion. Spatial and temporal monitoring case studies are only of interest to our international readership if they present new ideas of broad application. Topics covered include: (1) Environmental geochemistry (including natural and anthropogenic aspects, and protection and remediation strategies); (2) Hydrogeochemistry (surface and groundwater); (3) Medical (urban) geochemistry; (4) The search for energy resources (in particular unconventional oil and gas or emerging metal resources); (5) Energy exploitation (in particular geothermal energy and CCS); (6) Upgrading of energy and mineral resources where there is a direct geochemical application; and (7) Waste disposal, including nuclear waste disposal.
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