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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Extraction of soils above concealed lithium deposits for rare metal exploration in Jiajika area: A pilot study
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Extraction of soils above concealed lithium deposits for rare metal exploration in Jiajika area: A pilot study

机译:吉亚地区稀有金属勘探隐藏锂沉积物的土壤萃取:试验研究

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摘要

Jiajika in Sichuan, China, is an important mining area for lithium and other Group I and Group II elements. However, the weathered residual overburden makes it difficult to prospect using traditional soil geochemistry. Deep-penetrating geochemical theories provide new ideas and methods that can be used to explore for concealed ore bodies. In this study, topsoil samples were collected from 10 to 25 cm depth above two concealed lithium deposits, Vein 804 (V-804) and Vein X03 (V-X03). Lithium (Li), cesium (Cs), rubidium (Rb), beryllium (Be), and boron (B) were extracted from the soils using pure water and 0.2 mol/L potassium sulfate solutions (K2SO4). Anomalies were observed for water-extractable Li, Cs, and Rb, and K2SO4-extractable Li, Cs, and Be in samples from above both veins. The harmonic mean of the data for each element was used to calculate the response ratio. The highest response ratios are 1.2-2.5 times and 2 to 8 times higher than the response ratios for other samples from V-804 and V-X03, respectively. Linear correlations are observed between the water-extractable and K2SO4 extractable elements, and imply that unbound species of the elements were extracted by K2SO4. The extracted elements display single peak, double peak, and multi-peak anomaly patterns, which indicate that transfer of Li, Cs, Rb, Be, and B through the overburden may be through a combination of diffusion, capillarity, electrochemical forces, and redox gradients.
机译:嘉吉卡在中国四川,是锂电片和其他群体和第二次元素的重要矿区。然而,风化的剩余覆盖层使得难以使用传统土壤地球化学的展望。深入的地球化学理论提供了可用于探索隐藏矿石的新想法和方法。在该研究中,将另一种样品从10至25cm深度收集在两个隐藏的锂沉积物,静脉804(V-804)和静脉X03(V-X03)中。使用纯水和0.2mol / L硫酸钾溶液(K2SO4)从土壤中萃取锂(Li),铯(Cs),铷(RB),铍(B)和硼(B)。观察到用于可水中的Li,Cs和Rb,K2SO4-萃取的Li,Cs,以及在两个静脉上方的样品中的异常。每个元素的数据的谐波平均值用于计算响应比。最高反应比率为1.2-2.5倍,比V-804和V-X03的其他样品的响应比高出2至8倍。观察到可萃取的和K2SO4可提取的元件之间的线性相关性,暗示通过K 2 SO 4提取未结合的元素物​​种。提取的元件显示单峰,双峰和多峰异常模式,表明Li,Cs,Rb,Be和B通过覆盖层的转移可能是通过扩散,毛细管性,电化学力和氧化还原的组合渐变。

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