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首页> 外文期刊>Journal of African earth sciences >Characterization of brines and evaporite deposits for their lithium contents in the northern part of the Danakil Depression and in some selected areas of the Main Ethiopian Rift lakes
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Characterization of brines and evaporite deposits for their lithium contents in the northern part of the Danakil Depression and in some selected areas of the Main Ethiopian Rift lakes

机译:盐水和蒸发岩沉积物在达坎普尔坳陷北部的锂含量和一些选定地区的主要埃塞俄比亚裂痕湖泊

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摘要

Lithium is a metal with increasing demand on the global market mainly for its application in lithium ion batteries for electric vehicles. Ethiopia has potential for lithium resources related to pegmatites and to rift-bound brine deposits.The current research focused on known brine lakes and hot springs in the Danakil Depression and the Main Ethiopian Rift. Lithium contents in water samples from rift-bound lakes like Abijata, Shala, Chamo, Abaya, and Chew Bahir show low concentrations consistent with background values for surface waters. Lithium concentrations are elevated in brine lakes, brine ponds, and hot springs of the Danakil Depression. Hot springs in the Dallol contain up to 20 ppm lithium. Lithium enrichment was also noted in residual brines from multi-stage solar evaporation pans during soda-ash production. However, brines produced during precipitation of trona and halite contain about 0.009 ppm lithium, which is well below economically extractable concentrations. Core samples from the Danakil Depression potash exploration reported up to 20-40 ppm in the carnallite and bischofite layers of the evaporite sequence.At least three potential sources for lithium are noted in the Danakil Depression. For example, lithium is leached and mobilized during water rock interactions by deeply circulating and cycling hot meteoric and possibly juvenile geothermal fluids related to the intense volcano-tectonic processes. The current hydrological condition also suggest the possibility of lithium mobilization during surface run off from the basement and Mesozoic sedimentary rocks exposed along the western rift margin of the Danakil Depression. Moreover, variable lithium contents in the different layers of the evaporite sequence suggests, that lithium originated from sea water evaporation before the Danakil Depression became a closed basin. The current research strongly indicates that more detailed investigation is required to evaluate the lithium resources as a primary product and/or as a secondary byproduct during potash mining.
机译:锂电池是一种金属,随着全球市场需求越来越大,主要用于其在电动车辆锂离子电池中的应用。埃塞俄比亚有可能与佩格麦特有关的锂资源和裂缝盐水沉积物。目前的研究侧重于达坎尼尔抑郁症和主要埃塞俄比亚裂缝中的已知盐水湖泊和温泉。水样中的锂含量来自裂缝湖泊,如阿比皮亚,Shala,Chamo,Abaya和Chew Bahir等浓度与表面水域的背景值一致。锂浓度在盐水湖泊,盐水池塘和达达纳坳陷的温泉升高。达尔洛中的热弹簧含有最多20 ppm的锂。在苏打水生产过程中,来自多级太阳蒸发平底锅的残留盐水中还注意到锂富集。然而,在沉淀到ronona和Harite期间产生的盐水含有约0.009ppm的锂,其远低于经济可萃取的浓度。来自Danakil抑郁钾的核心样本在碳铝酸盐序列的碳铝酸盐和双壳层中报告了20-40ppm。在Danakil抑郁症中注意到至少有三个潜在的锂源来源。例如,通过深入循环和循环与激烈的火山构造过程相关的少年地热流体,在水岩相互作用期间浸出和动员锂。目前的水文条件还表明,在沿着达克尼亚抑郁症的西部裂隙边缘暴露的地下室和中生代沉积岩中,锂动员的可能性。此外,蒸发丁胺序列的不同层中的可变锂含量表明,锂源于海水蒸发之前,在Danakil凹陷成为闭孔盆之前。目前的研究强烈表明,需要更详细的调查来评估锂资源作为初级产品和/或钾矿物挖掘期间的二级副产品。

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