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首页> 外文期刊>International Journal of Mineral Processing >Mineralogical signature of nonsulfide zinc ores at Accha (Peru): A key for recovery
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Mineralogical signature of nonsulfide zinc ores at Accha (Peru): A key for recovery

机译:Accha(秘鲁)非硫化锌矿石的矿物学特征:回收的关键

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摘要

The Accha deposit in Southern Peru is the first case in which an integrated study between mineralogy, petrography and metallurgical characteristics of a nonsulfide Zn orebody has been carried out. The Accha-Yanque Zinc Belt is located in a major zinc-rich metallogenic province hosting a number of economic mineral deposits, which extends in a zone peripheral to the edge of the Oligocene-Miocene Yauri-Apurimac granite batholith. This belt is comprised of a number of weathering-derived nonsulfides occurrences, showings and mineral deposits. A thorough mineralogical and petrographic study has been carried out on the MET 1, MET 2, MET 3 and MET 4 cores, drilled between 2006 and 2007 for metallurgical purposes. The nonsulfides mineral association in the deposit consists mainly of smithsonite and hemimorphite replacing both primary ore minerals and carbonate host rocks. Smithsonite occurs in zoned concretions with goethite, Mn(hydr) oxides and Zn-clays. One of the most peculiar nonsulfide Zn mineral at Accha is a sauconite-like Zn-smectite, which can be locally very abundant (up to 30 percent ). Differences in mineralogy of the ore and gangue minerals, as well as the composition of the host rock can have a profound impact on zinc recovery and reagent consumption in any extraction process. The Accha nonsulfide ore minerals are intimately intergrown with the limestone host and therefore difficult to separate with traditional methods, this rendering the economic recovery of the metal through the acid leaching process difficult. This is further complicated by the abundance of sauconite in the deposit. It was therefore necessary to envisage a flowsheet development, derived from a thorough metallurgical test work program on various ore types, which could result in an economically viable treatment route in the light of both the carbonate host rock and the peculiar mineralogical association. Several careful processing steps comprised of comminution, dense media separation and flotation before acid leaching, and including precise acid leaching conditions to prevent the formation of deleterious 'gels' that would interfere with subsequent solid-liquid separation processes, have been tested for Accha as part of the development of an economic processing flowsheet.
机译:秘鲁南部的Accha矿床是首次对非硫化锌矿体的矿物学,岩石学和冶金特性进行综合研究的案例。 Accha-Yanque锌带位于富锌的主要成矿省,拥有许多经济矿藏,该矿床在渐新世-中新世Yauri-Apurimac花岗岩基岩边缘的外围延伸。该带包括许多风化衍生的非硫化物矿床,矿床和矿床。在2006年至2007年之间为冶金目的对MET 1,MET 2,MET 3和MET 4岩心进行了彻底的矿物学和岩石学研究。该矿床中的非硫化物矿物联合体主要由铁矿石和半变质岩组成,取代了主要的矿石矿物和碳酸盐基质岩。钙钛矿存在于带针铁矿,Mn(水)氧化物和Zn-粘土的分区混凝土中。阿查(Accha)中最奇特的非硫化锌矿产之一是类似锌铁矿的锌蒙脱石,其局部含量非常高(高达30%)。矿石和脉石矿物的矿物学差异以及基质岩石的组成会对任何提取过程中的锌回收和试剂消耗产生深远影响。阿查非硫化物矿物与石灰石基质紧密共生,因此很难用传统方法分离,这使得通过酸浸工艺进行金属的经济回收变得困难。矿床中大量的锌铁矿使这一情况更加复杂。因此,有必要设想一种流程图,该流程图的开发源于针对各种矿石类型的详尽的冶金测试工作程序,根据碳酸盐基质岩和特殊的矿物学组合,这可能导致经济可行的处理途径。作为Accha的一部分,已经对几个仔细的处理步骤进行了测试,包括粉碎,稠密的介质分离和酸浸之前的浮选,以及包括精确的酸浸条件以防止形成有害的“凝胶”,这些凝胶会干扰随后的固液分离过程。经济处理流程图的开发。

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