Micro-Raman mapping of critical metals (Li, Co, Ni) in a rhythmically laminated deep-ocean ferromanganese deposit

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Simone Bernardini , Giancarlo Della Ventura , Armida Sodo , Mariana Benites , Luigi Jovane , James R. Hein , Federico Lucci
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引用次数: 0

Abstract

Deep-ocean ferromanganese deposits represent one of the most important strategic reservoirs for rare and critical metals. In particular, Mn-oxyhydroxides, such as asbolane and lithiophorite, concentrate large amounts of Li, Ni, and Co into polymetallic nodules and crusts. However, because of their poor crystallinity and the presence of finely intermixed additional phases, these minerals cannot be unambiguously identified by standard X-ray powder diffraction methods. In addition, Li cannot be routinely detected by standard X-ray spectroscopy techniques.

In this work we show how the spatial distribution of asbolane (the Ni-Co-rich Mn-oxide) and lithiophorite (the Li-rich Mn-oxide) across strongly inhomogeneous ferromanganese mineralizations can be investigated at high-resolution (∼ 1 μm) via fast and easily accessible Raman scattering measurements. Because of the strong selectivity of these minerals to the incorporation of critical metals, the obtained micro-Raman maps provide also an indirect map of the Co and Ni vs. Li distribution in the crusts. The described results thus show that our spectroscopic approach could represent an efficient and valuable in situ tool for mineral chemistry and resource evaluation of these elements in ferromanganese deposits from deep-ocean environments. This research opens a new frontier for the application of Raman spectroscopy in ore prospecting for critical minerals and metals.

节律层状深海锰铁矿床中临界金属(锂、钴、镍)的显微拉曼图谱
深海锰铁矿床是稀有金属和关键金属最重要的战略储藏地之一。特别是锰氧氢氧化物,如asbolane和石硫磷矿,将大量的锂、镍和钴富集到多金属结核和结壳中。然而,由于这些矿物的结晶度较低,且存在细微的混合附加相,因此无法通过标准的 X 射线粉末衍射方法来明确识别。在这项工作中,我们展示了如何通过快速、便捷的拉曼散射测量,以高分辨率(1 ∼ 1 μm)研究强烈不均匀的铁锰矿化中asbolane(富含镍-铜的氧化锰)和lithiophorite(富含锂的氧化锰)的空间分布。由于这些矿物对临界金属的掺入具有很强的选择性,因此所获得的微拉曼图还可以间接地绘制地壳中钴、镍和锂的分布图。因此,所述结果表明,我们的光谱分析方法是一种高效、有价值的原位工具,可用于矿物化学和深海环境中铁锰矿床中这些元素的资源评估。这项研究为拉曼光谱在关键矿物和金属矿石勘探中的应用开辟了新的领域。
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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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