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首页> 外文期刊>Minerals Engineering >The leaching behavior of minerals from a pyrrhotite-rich pentlandite ore during heap leaching
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The leaching behavior of minerals from a pyrrhotite-rich pentlandite ore during heap leaching

机译:堆浸浸料中富含Pyrlotite的PETLONDITE ORE矿物的浸出行为

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Due to decreasing ore grades and increasingly complex ore bodies, the heap leaching of sulfide ores is of increasing interest. In this research, the heap leaching phenomena of a pyrrhotite-rich pentlandite ore was investigated for the first 150 days of operation in order to understand the phenomena taking place in the early phase of leaching in an industrial scale heap. The ore investigated originates from Terrafame (Finland) and contains approximately 20 wt% metal sulfides, the majority of which are pyrrhotite and pyrite. The nickel and zinc minerals of interest, pentlandite and sphalerite, are minor constituents of the ore. The oxidative leaching behavior of sulfidic minerals was shown to follow for the most part the order of nobility of sulfides. In the heap leaching investigated, pyrrhotite especially was shown to be far more reactive than pentlandite and sphalerite and thus the recovery of valuable metals can occur only after pyrrhotite dissolution. It was found that the nickel, zinc, and copper present in the irrigation solution can partially precipitate into the heap where more reductive metal sulfides, such as pyrrhotite and alabandite, are present, a metathesis phenomenon postulated elsewhere for copper and now confirmed in industrial scale operation. Pyrrhotite was also shown to create the majority of the reagent (acid and oxygen) demand and the majority of the reagent demand variation during the early days of heap leaching. In addition, the height of the heap was shown have an important role in determining the leaching time, due to physical, chemical, and practical limitations on acid feed. The acid demand for pyrrhotite leaching in low-oxygen consuming reactions was found to be higher (approx. 62 kg/tonne of ore) than the possibility to feed acid on a tall heap (23 kg/tonne of ore at maximum). This was shown to result in heavy precipitation of iron compounds, such as goethite. The results give more clarity for the initial stages of leaching at Terrafame and thereby enable clearer strategies to be formulated for solution circulation management according to heap age.
机译:由于矿石等级和越来越复杂的矿体,硫化物矿石的堆浸出越来越感兴趣。在这项研究中,研究了富含Pyrrhotite的PETLONDITE ORE的堆浸出现象,以便在工业规模堆中浸出早期阶段进行的现象。研究矿石来自Terrafame(芬兰),含有约20wt%的金属硫化物,其中大部分是烟草酸盐和黄铁矿。感兴趣的镍和锌矿物质,五翼石和荆大石,是矿石的次要成分。显示亚硫酸矿物的氧化浸出行为遵循硫化物的高度阶段。在研究的堆浸出中,特别是Pyrrhotite特别是比PENTLONE和闪锌矿更具反应性,因此只有在Pyrhotite溶解后才能恢复有价值的金属。发现灌溉溶液中存在的镍,锌和铜可以部分地沉淀到堆中,其中还有更新的金属硫化物,例如Pyrlothite和Alabandite,在其他地方为铜发出的复分解现象,现在以工业规模证实手术。也显示出在堆浸出的早期试用剂(酸和氧气)需求和大部分试剂需求变化的烟草酸盐。此外,由于物理,化学和酸进料的实际限制,显示堆的高度在确定浸出时间方面具有重要作用。发现对低氧消费反应中的胃肠酸浸出的酸性需求更高(约62kg /吨矿石),而不是在高堆上喂酸(最大23kg / tonne的矿石)的可能性。这显示出导致铁化合物的重沉淀,例如霉菌。结果对Terrafame浸出的初始阶段提供了更多的清晰度,从而使根据堆时代的解决方案循环管理能够制定更清晰的策略。

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