Enhanced Oxidative Bioleaching for Nickel and Metal Recovery from Arsenic Ores Moves Toward Efficient and Sustainable Extraction.

Zohreh Boroumand, Hadi Abdollahi, Shabnam Najafi Asli Pashaki, Mirsaleh Mirmohammadi, Yousef Ghorbani
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Abstract

The research focuses on extracting nickel and other valuable elements through oxidative bioleaching from two distinct arsenic-rich ores of varying grades. This process involved utilizing a mix of mesophilic and moderately thermophilic bacteria in shake flasks with different pulp density levels to bio-leach nickeline. Mesophilic bacteria achieved over 99% nickel dissolution from both low- and high-grade ores within 10 and 28 days, respectively, at pulp densities of 0.5% and 1%. In contrast, abiotic control and chemical tests showed significantly lower nickel dissolution rates (approximately 6.9% and 26.1% for low-grade; 10.3% and 45% for high-grade samples). Moderately thermophilic bacteria achieved complete nickel dissolution from the low-grade ore at a 0.5% pulp density, while dissolution from the high-grade ore reached approximately 63%. In comparison, abiotic controls and chemical achieved only 19% and 39% dissolution for the high-grade ore, and 21.9% and 45% for the low-grade ore, respectively. X-ray diffraction (XRD) analysis confirmed the formation of scorodite as a secondary phase due to arsenic solubilization from primary minerals in the presence of iron. Kinetic modelling revealed that the bioleaching of the low-grade ore was predominantly controlled by a mixed reaction mechanism, whereas chemical factors limited the bioleaching rate of the high-grade ore. This research underscores the efficacy of oxidative bioleaching using mixed bacterial cultures and highlights its potential for efficiently extracting nickel and other valuable metals (cobalt and copper) from arsenic-bearing ores under controlled pulp density conditions.

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增强氧化生物浸出法从砷矿石中回收镍和金属,向高效和可持续提取迈进。
研究重点是通过氧化生物浸出法从两种不同品位的富砷矿石中提取镍和其他有价元素。这一过程包括在具有不同矿浆密度水平的摇瓶中混合使用中嗜热细菌和中度嗜热细菌,对镍线进行生物浸出。在纸浆密度为 0.5% 和 1% 的情况下,中嗜热细菌分别在 10 天和 28 天内从低品位和高品位矿石中实现了 99% 以上的镍溶出。相比之下,非生物对照和化学测试显示的镍溶解率要低得多(低品位样本约为 6.9% 和 26.1%;高品位样本约为 10.3% 和 45%)。中度嗜热细菌在 0.5% 的矿浆密度下实现了低品位矿石中镍的完全溶解,而高品位矿石中的溶解度则达到了约 63%。相比之下,非生物控制和化学方法对高品位矿石的溶解度分别仅为 19% 和 39%,对低品位矿石的溶解度分别为 21.9% 和 45%。X 射线衍射(XRD)分析证实,在铁存在的情况下,由于原生矿物中砷的溶解,形成了作为次生相的蝎尾石。动力学模型显示,低品位矿石的生物浸出主要受混合反应机制控制,而化学因素则限制了高品位矿石的生物浸出率。这项研究强调了使用混合细菌培养物进行氧化生物浸出的功效,并突出了其在受控矿浆密度条件下从含砷矿石中高效提取镍和其他有价金属(钴和铜)的潜力。
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