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浅论湖南蓝山地区氧化锰铁矿的矿床成因及综合利用
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作者 刘森荣 骆新光 叶锋 《冶金管理》 2023年第9期88-89,共2页
湖南蓝山地处南岭山系,区内地层岩性以泥盆系碳酸盐岩为主,地表多被第四系残坡积物覆盖。受气候和地貌条件的影响,并在长期强烈的表生风化作用下,在第四系残坡积物中形成了分布广、展布面积大、蕴藏量丰富的锰铁多金属矿。铁、锰矿是涉... 湖南蓝山地处南岭山系,区内地层岩性以泥盆系碳酸盐岩为主,地表多被第四系残坡积物覆盖。受气候和地貌条件的影响,并在长期强烈的表生风化作用下,在第四系残坡积物中形成了分布广、展布面积大、蕴藏量丰富的锰铁多金属矿。铁、锰矿是涉及国家资源安全的大宗紧缺战略性矿产,蓝山地区的氧化铁锰矿具有储量丰富、经济价值高、易开采的特点,且能综合利用矿区内的粘土岩、白云岩和灰岩,若能积极开发该处的锰铁多金属矿资源,对进一步促进地方发展、健全和完善我国产业链和供应链具有重要的示范效应。 展开更多
关键词 蓝山 氧化锰铁矿 矿床
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Enhancement of bio-oxidation of refractory arsenopyritic gold ore by adding pyrolusite in bioleaching system 被引量:5
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作者 张旭 冯雅丽 李浩然 《Transactions of Nonferrous Metals Society of China》 SCIE EI CAS CSCD 2016年第9期2479-2484,共6页
Pyrolusite was added in the bioleaching process to enhance the bio-oxidation process. Bioleaching tests at different dosages of pyrolusite ore, pH and inoculation amounts of Acidithiobacillus ferrooxidans were studied... Pyrolusite was added in the bioleaching process to enhance the bio-oxidation process. Bioleaching tests at different dosages of pyrolusite ore, pH and inoculation amounts of Acidithiobacillus ferrooxidans were studied. The results showed that the time of the bio-oxidation process was decreased obviously and the arsenic leaching rate reached 94.4% after the bioleaching. The bio-oxidation of arsenopyrite and the effective extraction of manganese from pyrolusite were achieved by the bioleaching process. After bioleaching, the leaching rate of gold from the reaction residues reached 95.8% by cyanide leaching. In the bio-oxidation process, pyrolusite increased the redox potential of the solution to accelerate the bioleaching rate. The experiment showed that there were two reaction modes in the bioleaching process. 展开更多
关键词 arsenopyritic gold ore PYROLUSITE BIO-OXIDATION Acidithiobacillus ferrooxidans
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Combined Chemical and Mineralogical Evidence for Heavy Metal Binding in Mining- and Smelting-Affected Alluvial Soils 被引量:8
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作者 A. VANEK V. ETTLER +3 位作者 T. GRYGAR L. BORUVKA O. EBEK O. DRBEK 《Pedosphere》 SCIE CAS CSCD 2008年第4期464-478,共15页
The binding of metallic contaminants (Pb, Cd, and Zn) and As on soil constituents was studied on four highly contaxninated alluvial soil profiles from the mining/smelting district of Pribram (Czech Republic) using... The binding of metallic contaminants (Pb, Cd, and Zn) and As on soil constituents was studied on four highly contaxninated alluvial soil profiles from the mining/smelting district of Pribram (Czech Republic) using a combination of mineralogical and chemical methods. Sequential extraction analysis (SEA) was supplemented by mineralogical investigation of both bulk samples and heavy mineral fractions using X-ray diffraction analysis (XRD) and scanning electron microscopy with an energy dispersive X-ray spectrometer (SEM/EDS). The mineralogy of Fe and Mn oxides was studied by voltammetry of microparticles (VMP) and diffuse reflectance spectrometry (DRS). Zinc and Pb were predominantly bound in the reducible fraction attributed to Fe oxides and Mn oxides (mainly birnessite, Na4Mn14O27.9H2O), which were detected in soils by XRD and SEM/EDS. In contrast, Cd was the most mobile contaminant and was predominantly present in the exchangeable fraction. Arsenic was bound to the residual and reducible fractions (corresponding to Fe oxides or to unidentified Fe-Pb arsenates). SEM/EDS observations indicate the predominant affinity of Pb for Mn oxides, and to a lesser extent, for Fe oxides. Thus, a more suitable SEA procedure should be used for these mining-affected soils to distinguish between the contaminant fraction bound to Mn oxides and Fe oxides. 展开更多
关键词 alluvial soil Fe and Mn oxides heavy metals MINERALOGY mining
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Coexistence of antiferromagnetic and ferromagnetic in Mn-doped anatase TiO_2 nanowires
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作者 李红梅 刘敏 +1 位作者 曾阳素 黄同成 《Journal of Central South University》 SCIE EI CAS 2010年第2期239-243,共5页
A series of Mn-doped TiO2 nanowires(NWs) were prepared by hydrothermal method at the mole fraction of Mn changing from 0 to 12.0%.X-ray powder diffraction(XRD) analysis shows that all the samples have pure anatase str... A series of Mn-doped TiO2 nanowires(NWs) were prepared by hydrothermal method at the mole fraction of Mn changing from 0 to 12.0%.X-ray powder diffraction(XRD) analysis shows that all the samples have pure anatase structure.SEM and TEM studies show that the diameter and the length of the Mn-doped TiO2 NWs are larger than those of the undoped TiO2 NWs.Energy dispersive X-ray spectroscopy(EDX) reveals that the samples are composed of Ti,Mn and O.According to magnetization measurements,all samples show ferromagnetic behavior,but only the undoped TiO2 NWs are completely ferromagnetic with a saturated magnetization about 1.0 mA·m2/kg.Mn-doped TiO2 samples exhibit antiferromagnetic and ferromagnetic(AF-FM) behaviors simultaneously.Photoluminescence(PL) spectra demonstrate the existence of MnO2 sublattice.These observations indicate that an AF-WF crossover is induced by the coexistence of TiO2 sublattice and MnO2 sublattice. 展开更多
关键词 TiO2 NANOWIRES Mn ANTIFERROMAGNETISM FERROMAGNETISM
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