Mineralogical and leaching characteristics of sulfur concentrate and hot filter residue from zinc–oxygen-pressure leaching

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Pu Sun , Guomu Chen , Dongfeng Zhou , Chang Wei , Xingbin Li , Zhigan Deng , Minting Li
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引用次数: 0

Abstract

The mineralogical properties and environmental impact of sulfur concentrate and hot filter residue produced from the zinc–oxygen-pressure leaching were studied through a series of characterization, including X-ray fluorescence (XRF), inductively coupled plasma optical emission spectroscopy (ICP–OES), X-ray diffraction (XRD), scanning electron microscopy-energy dispersive X-ray spectroscopy (SEM–EDS), particle size distribution (PSD), Fourier transform infrared spectroscopy (FT-IR), X-ray photoelectron spectroscopy (XPS), and thermogravimetry and differential thermal analysis (TG–DTA). Furthermore, short-term environmental activity was assessed using the toxic leaching procedure (TCLP). The results indicated that the sulfur concentrate exhibited a coarser particle size compared with the hot filter residue, primarily appearing as spindle-shaped element sulfur (S0). The hot filter residue contained spindle-shaped S0 and rod gypsum, alongside phases of sphalerite, pyrite, and copper–silver-containing phases encapsulated by S0, recovering valuable metals first requires the removal of S0. The surfaces of both sulfur concentrate and hot filter residue were composed of S, ZnS, Al-O, PbSO4, and SiO2. They exhibited thermal instability and some degree of water absorption, with vigorous burning observed at temperatures ranging from 200 °C to 380 °C. The leachates from these materials exhibited increased concentrations of elements such as zinc, lead, and cadmium surpassing permissible limits, highlighting the importance of their safe disposal for the stable production of zinc–oxygen-pressure systems.
锌氧压浸硫精矿和热滤渣矿物学及浸出特性研究
通过x射线荧光(XRF)、电感耦合等离子体发射光谱(ICP-OES)、x射线衍射(XRD)、扫描电镜-能量色散x射线能谱(SEM-EDS)、粒度分布(PSD)、傅里叶变换红外光谱(FT-IR)等一系列表征手段,研究了锌氧压浸硫精矿和热滤渣的矿物学性质和环境影响。x射线光电子能谱(XPS),热重和差热分析(TG-DTA)。此外,使用毒性浸出程序(TCLP)评估了短期环境活动。结果表明:硫精矿粒度较热滤渣粗,主要表现为梭形元素硫(S0);热滤渣中含有纺锤形的S0和棒状石膏,以及由S0包裹的闪锌矿、黄铁矿和含铜银相,回收有价金属首先需要去除S0。硫精矿和热滤渣表面均由S、ZnS、Al-O、PbSO4和SiO2组成。它们表现出热不稳定性和一定程度的吸水性,在200°C至380°C的温度范围内观察到剧烈燃烧。这些材料的渗滤液中锌、铅和镉等元素的浓度增加,超过了允许的限度,突出了安全处理这些元素对锌氧压系统稳定生产的重要性。
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来源期刊
Chemie Der Erde-Geochemistry
Chemie Der Erde-Geochemistry 地学-地球化学与地球物理
CiteScore
7.10
自引率
0.00%
发文量
40
审稿时长
3.0 months
期刊介绍: GEOCHEMISTRY was founded as Chemie der Erde 1914 in Jena, and, hence, is one of the oldest journals for geochemistry-related topics. GEOCHEMISTRY (formerly Chemie der Erde / Geochemistry) publishes original research papers, short communications, reviews of selected topics, and high-class invited review articles addressed at broad geosciences audience. Publications dealing with interdisciplinary questions are particularly welcome. Young scientists are especially encouraged to submit their work. Contributions will be published exclusively in English. The journal, through very personalized consultation and its worldwide distribution, offers entry into the world of international scientific communication, and promotes interdisciplinary discussion on chemical problems in a broad spectrum of geosciences. The following topics are covered by the expertise of the members of the editorial board (see below): -cosmochemistry, meteoritics- igneous, metamorphic, and sedimentary petrology- volcanology- low & high temperature geochemistry- experimental - theoretical - field related studies- mineralogy - crystallography- environmental geosciences- archaeometry
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