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Use of Phosphate Solubilizing Bacteria to Leach Rare Earth Elements from Monazite-Bearing Ore

机译:磷酸盐增溶细菌从含独居石矿石中浸出稀土元素的应用

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In the present study, the feasibility to use phosphate solubilizing bacteria (PSB) to develop a biological leaching process of rare earth elements (REE) from monazite-bearing ore was determined. To predict the REE leaching capacity of bacteria, the phosphate solubilizing abilities of 10 species of PSB were determined by halo zone formation on Reyes minimal agar media supplemented with bromo cresol green together with a phosphate solubilization test in Reyes minimal liquid media as the screening studies. Calcium phosphate was used as a model mineral phosphate. Among the test PSB strains, Pseudomonas fluorescens, P. putida, P. rhizosphaerae, Mesorhizobium ciceri, Bacillus megaterium, and Acetobacter aceti formed halo zones, with the zone of A. aceti being the widest. In the phosphate solubilization test in liquid media, Azospirillum lipoferum, P. rhizosphaerae, B. megaterium, and A. aceti caused the leaching of 6.4%, 6.9%, 7.5%, and 32.5% of calcium, respectively. When PSB were used to leach REE from monazite-bearing ore, ~5.7 mg/L of cerium (0.13% of leaching efficiency) and ~2.8 mg/L of lanthanum (0.11%) were leached by A. aceti, and Azospirillum brasilense, A. lipoferum, P. rhizosphaerae and M. ciceri leached 0.5–1 mg/L of both cerium and lanthanum (0.005%–0.01%), as measured by concentrations in the leaching liquor. These results indicate that determination of halo zone formation was found as a useful method to select high-capacity bacteria in REE leaching. However, as the leaching efficiency determined in our experiments was low, even in the presence of A. aceti, further studies are now underway to enhance leaching efficiency by selecting other microorganisms based on halo zone formation.
机译:在本研究中,确定了使用磷酸盐增溶细菌(PSB)从含独居石的矿石中开发稀土元素(REE)的生物浸出过程的可行性。为了预测细菌的REE浸出能力,通过在补充有溴甲酚绿的Reyes最小琼脂培养基上形成卤素区域,并在Reyes最小液体培养基中进行磷酸盐增溶试验来确定10种PSB的磷酸盐溶解能力,作为筛选研究。磷酸钙用作模型无机磷酸盐。在测试的PSB菌株中,荧光假单胞菌,恶臭假单胞菌,球根假单胞菌,中型中生根瘤菌,巨大芽孢杆菌和醋酸醋杆菌形成了晕圈区域,其中醋酸杆菌菌的区域最宽。在液体介质中的磷酸盐增溶测试中,脂氮螺旋藻,根瘤菌,巨大芽孢杆菌和乙酰丙酮杆菌分别导致钙的浸出6.4%,6.9%,7.5%和32.5%。当使用PSB从含独居石的矿石中浸出REE时,乙曲霉和巴西偶氮螺旋藻分别浸出〜5.7 mg / L的铈(浸出效率的0.13%)和〜2.8 mg / L的镧(浸出效率的0.11%),用浸出液中的浓度测量,脂铁杆菌,根腐球菌和蝉菌浸出的铈和镧含量均为0.5-1 mg / L(0.005%-0.01%)。这些结果表明,发现晕圈区形成的确定是在REE浸出中选择高容量细菌的有用方法。然而,由于在我们的实验中确定的浸出效率很低,即使在存在乙酸曲霉的情况下,目前正在进行进一步的研究以通过基于晕圈区的形成选择其他微生物来提高浸出效率。

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