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首页> 外文期刊>Minerals Engineering >EVALUATION OF A DIAGNOSTIC LEACHING TECHNIQUE FOR GOLD IN NATIVE GOLD AND GOLD +- SILVER TELLURIDES
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EVALUATION OF A DIAGNOSTIC LEACHING TECHNIQUE FOR GOLD IN NATIVE GOLD AND GOLD +- SILVER TELLURIDES

机译:天然金和金+-银碲化物中金的诊断浸出技术的评估

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A detailed investigation of the stability in cyanide solutions of native gold and gold +- silver tellurides in a flotation concentrate from the Golden Mile, Kalgoorlie, has been undertaken to assess whether leaching under different conditions can be used to quantify the distribution of Au between native gold and gold +- silver tellurides, as suggested by, for example, Chryssoulis and Cabri (1990).The leaching was carried out on +20 #mu#m native gold and gold +- silver tellurides separated from a high-grade flotation concentrate and then diluted with barren quartz. The material leached assayed 270 ppm Au and 118 ppm Te. About 77 percent of the Au was present as native gold (largely liberated) and about 23 percent was in gold -+ silver tellurides (predominantly calaverite with trace petzite and Au-bearing hessite, also largely liberated). The grainsize of the gold-bearing minerals was mainly in the range 20 #mu#m to 100 #mu#m. The leach conditions used were:- Stage 1: Leaching in dilute cyanide (0.1 percent) at pH 9.5 for 24 hours to dissolve native gold but not gold +- silver tellurides.Stage 2: Leaching the residue from Stage 1 in strong cyanide (2 percent) at pH 12.5 for 96 hours to dissolve gold +- silver tellurides.Extractions of native gold and gold +- silver tellurides in the two stages of leaching were found to be as follows:The results showed that the bulk of the native gold dissolved in the Stage 1 leach (weak cyanide, moderate pH), along with about half the hessite and petzite but hardly any of the calaverite. The estimate of Au in native gold from the Stage J leach corresponded fairly closely to the native gold content as the hessite/petzite concentrations were low. However although the Stage 2 leach (strong cyanide, high pH) dissolved almost all the remaining hessite/petzite, only a small proportion of the calaverite dissolved.The main conclusions of the investigation are that calaverite is very refractory to cyanidation, much more so than hessite/petzite, and that the diagnostic leaching procedure studied did not provide a good estimate of Au in gold +- silver tellurides. For the diagnostic leach procedure to be effective, a treatment, such as chlorination, which breaks down calaverite prior to the Stage 2 cyanidation is required.
机译:已对卡尔古利(Golden Mile)浮选精矿中天然金和碲化金和金+-碲化银在氰化物溶液中的稳定性进行了详细研究,以评估在不同条件下的浸出是否可用于量化金在天然矿之间的分布。金和金+-碲化银,例如Chryssoulis和Cabri(1990)所提出的。浸出是在+20#μ#m天然金和金+-银的碲化物中进行的,该天然金和银从高级浮选精矿中分离出来。然后用贫瘠的石英稀释。浸出的材料测得270 ppm Au和118 ppm Te。大约77%的Au以天然金的形式存在(被大量释放),大约23%的存在于金+-碲化银中(主要是具有钙钛矿和钙钛矿和含Au的黑铁矿,也被大量释放了)。含金矿物的粒度主要在20#μm至100#μm的范围内。使用的浸出条件为:-阶段1:在pH 9.5的稀氰化物(0.1%)中浸提24小时,以溶解天然金,但不溶解金+-碲化银。阶段2:将阶段1的残留物浸入强氰化物中(2在12.5的pH值下96小时溶解金+-碲化银。在两个浸出阶段中提取天然金和金+-碲化银的结果如下:结果表明大部分天然金溶解了在第1阶段浸出(弱氰化物,中等pH值)中,约有一半的黑铁矿和水钠钙石,但几乎没有钙铝石。 J浸出过程中天然金中Au的估算值与天然金含量相当接近,因为he石/蓬松石的浓度较低。然而,尽管阶段2浸出(氰化度高,pH高)几乎溶解了所有剩余的黑铁矿/蓬松石,但只有小部分的钙霞石溶解了。研究的主要结论是,钙霞石对氰化作用非常难熔,比Hessite / petzite,并且研究的诊断性浸出程序不能很好地估计金+-碲化银中的Au。为了使诊断浸出程序有效,需要进行诸如氯化之类的处理,该处理在阶段2氰化之前分解钙铁矿。

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