Characteristics of iron-manganese nodules containing nickel and cobalt in chromite deposits in Co Dinh, Thanh Hoa province

Tien Dung Le, Van Duc Tran, Huu Trong Nguyen, Khac Giang Nguyen, Xuan Ban To, Thi Ly Ly Nguyen
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Abstract

Along with the chromite ore bodies, very early on, geologists recorded the presence of cobalt (Co) and nickel (Ni) metal. The resource of cobalt and nickel is forecasted with over 3 million tons of Ni and over 260 thousand tons of Co metals. Until now, however, knowledge about the existence form and distribution of Ni and Co in chromite ore bodies is very limited. Researching the sludge in the chromite mines and in comparison with manganese nodules found in the ocean floor helps to detect the presence of particles of iron and manganese (Fe-Mn nodules) in granular sewage sludges and in primary chromite ore bodies. Fe-Mn hydroxides, including todorokite mineral, are believed to be the adsorption medium and forming of Ni and Co in the Co Dinh placer chromite. Determining the existence form and distribution of Ni and Co in chromite placer deposits has scientific and practical significance in sampling orientation, sample processing, geological exploration, and reserve and resource estimations, sorting and recovering technology of Co and Ni metals.
清化省高定铬铁矿床中含镍和钴的铁锰结核的特征
除了铬铁矿体,地质学家很早就发现了钴(Co)和镍(Ni)金属。据预测,钴和镍的资源量分别为 300 多万吨镍金属和 26 万多吨钴金属。然而,迄今为止,有关铬铁矿体中镍和钴的存在形式和分布的知识非常有限。对铬铁矿矿井中的污泥进行研究,并与海底发现的锰结核进行比较,有助于发现颗粒状污水污泥和原生铬铁矿矿体中存在铁和锰颗粒(铁锰结核)。铁锰氢氧化物,包括沱沱矿,被认为是科定块状铬铁矿中镍(Ni)和钴(Co)的吸附介质和形成物。确定铬铁矿块矿床中 Ni 和 Co 的存在形式和分布,对取样定位、样品处理、地质勘探、储量和资源估算、Co 和 Ni 金属的分选和回收技术具有科学和现实意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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