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Assessment of Leachate From Blended Waste Rock Material at the Pasminco Century Mine - Initial Results From a Two-Year Study

机译:在Pasminco Century Mine的混合废岩材料中评估渗滤液 - 来自两年的研究结果

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The Pasminco Century Mine (PCML) is located 250 kilometres north-north-west of Mt Isa in Queensland. As one of the world's largest zinc mines. PCML comprises mining and milling operations at Lawn Hill concentrate filtering and shipping facilities at Karumba in the Gulf of Carpentaria, and a 304 km slurry pipeline connecting the two operations. Mineralisation at Century occurs in the upper part of the Lawn Hill formation and is comprised of siltstones, shale and sandstone. Pyrite occurs immediately above the mineralised sequence, and throughout the footwall carbonaceous shale forming the lower proportion of the deposit. Zinc predominantly occurs as sphalerite (ZnS) and lead as galena (PbS). These sulfides are very fine-grained and may oxidise rapidly upon exposure. The pyrite, sphalerite and galena are the main potential sources of acid rock drainage (ARD) or heavy metal leachate at the mine site. To minimise the generation of ARD in the waste rock dumps, they are constructed in a specific manner and waste rock is classified into the following three classes based on competence and acid forming/consuming capabilities: · Class 1 Competent rock, non-acid forming or acid-consuming material. · Class 2 Non-competent, non-acid forming or acid-consuming material. · Class 3 Acid-forming material. The generalised Waste Rock Dump Design for current operations comprises an outer zone of Class 1 material and inner zone with Class 2 and 3 material. Limestone is the Class 1 material used for both its structural support and acid neutralising capacity. Reserves of limestone at the mine site are limited. Net acid generation (NAG) tests confirm that a mix of limestone and shales can be net acid consuming. Field based and laboratory based trials have been established at PCML to quantify blending levels of limestone and shale that will produce leachates both neutral in pH and low in metal/salt concentrations. This paper will discuss the first six months results (of a two-year sampling program) from the trials.
机译:该帕斯明克Century矿山(PCML)位于250公里伊萨山昆士兰州北部西北部。作为世界最大锌矿之一。 PCML包括草坪山精矿过滤并在卡奔塔利亚湾和304公里矿浆管道连接两个操作在Karumba航运设施采矿和选矿作业。矿化在世纪在草坪山形成的上部发生,并且是由粉砂岩,页岩和砂岩。黄铁矿发生立即矿化序列的上方,并在整个下盘碳质页岩形成沉积物的比例较低。锌主要发生如闪锌矿(硫化锌)和铅作为方铅矿(硫化铅)。这些硫化物是非常细粒度和可能暴露快速氧化。黄铁矿,闪锌矿和方铅矿是酸岩排水(ARD)或重金属渗滤液在矿场的主要潜在来源。为了最小化ARD在矸石堆放的生成,它们被构造以特定的方式和废石被分类成基于能力和酸下面三个等级形成/消耗的功能:·第1类主管岩石,非酸形成或酸消耗材料。 ·级别2非胜任的,非酸形成或酸消耗材料。 ·3级酸形成材料。广义废石转储设计当前操作包括第1类材料和内区的具有2级和3材料外区。石灰石是用于两个其结构支撑和酸中和能力的第1类材料。在矿区石灰石的储量是有限的。净酸代(NAG)测试证实石灰石和页岩的混合可以是净酸消耗。基于现场和实验室根据试验已经在PCML建立量化石灰石和页岩,将产生沥滤液pH和低两个中性金属/盐浓度的混合水平。本文将从试验讨论前六个月的结果(一个为期两年的抽样程序)。

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