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The electrochemical activity of the basal plane and edge plane of graphite has long been a subject of an extensive debate. While significant advances have been made, several gaps still exist in our understanding of this issue, namely, the relative differences in the electrochemical activity of the perfect basal plane and perfect edge plane and the dependence of measurable electrochemical quantities on the edge/defect density of the basal plane. In this work, we employ a microdroplet electrochemical cell technique and atomic force microscopy to measure localized electrochemical properties of the graphitic surface with known edge coverage. The electron transfer rate, capacitance, and density of electronic states of the perfect basal plane and perfect edge plane are estimated, and a qualitative model is proposed for the dependence of the electrochemical quantities on the defect density of the basal plane.
Graphene is just one example of a large class of two-dimensional crystals. These crystals can either be extracted from layered three-dimensional materials or grown artificially by several different methods. Furthermore, they present physical properties that are unique because of the low dimensionality and their special crystal structure. They have potential for semiconducting behavior, magnetism, superconductivity, and even more complex many-body phenomena. Two-dimensional crystals can also be assembled in three-dimensional heterostructures that do not exist in nature and have tailored properties, opening an entirely new chapter in condensed matter research.
The Bi mineralization is described in quartz-sulfde veins of the Nazarovskoe gold polymetallic deposit (Western Transbaikalia), which is localized within the Eravnino volcano-tectonic structure and is confned to the Nazarovskoe fault zone and the contact with a granodiorite pluton intruding volcanosedimentary rocks. The Bi minerals include Ag-Bi, Cu-Bi, Pb-Bi, and Ag-Pb-Bi sulfosalts, Bi sulfotellurides, aikinite, and native bismuth in assemblage with chalcopyrite and galena. Most Bi minerals are described for the frst time both for the Nazarovskoe deposit and the entire Ozerninsky ore cluster.
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No abstract is provided for this article.
The article contains the results of a mineralogical study of sulfide ores of the Samolazovskoe deposit (Aldan Shield) and the products of their experimental bacterial oxidation in a heap. Pyrite and marcasite are the major minerals of primary ores. They form fine-grained crystalline and micrometer-grained to cryptocrystalline aggregates. Sphalerite, galena, chalcopyrite, pyrrhotite, fahlore, luzonite, bournonite and other Sb sulfosalts, antimonite, arsenopyrite are minor minerals. Tiemannite, coloradoite, calaverite, hessite, petzite and native gold are rare. The ores in the experimental biooxidation heap are mostly altered in its upper parts. The secondary products of the alteration of ores include fine-grained Mg- and S-bearing calcite, smectites after feldspars, and films of Fe3+oxyhydroxides on the surface and in fractures of ore. In the lower part of the heap, technogenic processes are weak and mainly include the formation of gypsum . The sulfides are preserved throughout the heap vertical profile including very fine crystalline, colloform and botryoidal aggregates with a nonstoichiometric ratio of cations and anions and the presence of As, Ni and Cu. The botryoidal aggregates of the Fe disulfides contain galena, which forms a “microseptary” structure, which was not found in primary ores. The high-fineness native gold was found in assemblage with coloradoite and calaverite as inclusions in fine-grained aggregates of Fe disulfides. The conclusion is made on an insufficient impact of the bioleaching of refractory ores in the irrigation regime used, and forming of the secondary minerals that prevent the extraction of gold. Keywords: Samolazovskoe deposit, Aldan Shield, coloradoite, calaverite, native gold, refractory ores, bio-oxidation.
Рассмотрены минералогические и геохимические особенности оолитовых железняков Синаро-Течен-ского месторождения (Зауралье, Курганская обл.). Рудный горизонт локализован в нижней части мощной толщи морских мезо-кайнозойских отложений Западно-Сибирского бассейна под известкови-стыми глинами, выше которых залегают слои, обогащенные глауконитом и клиноптилолитом. В составе железняков преобладают ооиды гетита в смектит-опаловом цементе. Акцессорные минералы представлены пиритом, галенитом, сфалеритом, монацитом. Текстурно-структурные особенности позволяют предположить образование обогащенных железом осадков в результате коагуляции коллоида. Наиболее вероятным источником железа является материковый снос; осаждение железа происходило в эстуариях субтропических рек при смешении коллоидного раствора речной воды с электролитом морской воды. Химические особенности пород определяются составом адсорбированного комплекса окси/гидроксида железа.
Research subject . In morphological terms, the Bakayskoe gold occurrence comprises an area of fracture and crushing of sublatitudinal strike in the granitoids of the Turgoyak massif (C1-2), which contains quartz veins with sulfide mineralization. The vein zone is about 1.5 km in length. The Turgoyak massif is located on the border of the Magnitogorsk and Central Ural areas, being a satellite of the Syrostan massif. Materials and methods . Samples collected in old workings and ore stockpiles were studied by optical and SEM microscopy. Fluid inclusions in vein quartz were studied by thermoscryometry. Results. The predominant ore minerals were found to be pyrite and galena; rarely, the ores contain chalcopyrite, tetrahedrite, sphalerite, sulfosalts, and bismuth sulfotellurides. In the studied samples, gold is present as both native gold (primary and supergene), and tellurides and sulfides. Ores are partly oxidized. The average and median values of the homogenization temperature (Tg) of primary and primary-secondary inclusions from ore quartz are about 242– 247°C. The average and median Tg of quartz from shale is slightly lower (222 and 215°C, respectively), with a significant scatter of values. The concentration of salts in NaCl equivalent, determined by the melting point of the last ice crystal, varies from 1.4 to 13.0 wt % in FI from the host shales and 0.2–5.6 wt % in ore quartz. Such wide variations in salinity in all the studied cases may indicate changes in FI by secondary processes.