Synthesis of jadarite in the Li2O–Na2O–B2O3–SiO2–NaCl–H2O system: FTIR, Raman, and Li and B K-edge XANES characterizations and theoretical calculations

Xiuzhen Xie, H. Kuang, Eli Wiens, Reza Deevsalar, Ayetullah Tunc, Sarah Purdy, Lucia Zuin, John S. Tse, Jin-Xiao Mi, Yuanming Pan
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Abstract

Abstract. The occurrence of jadarite (LiNaSiB3O7OH) as a major ore mineral in the world-class lithium–boron deposit of the Miocene Jadar lacustrine basin (western Serbia) raises interesting questions about its formation conditions and potential associations for lithium mineralization in other sedimentary basins. This contribution reports on the first successful synthesis of jadarite in the Li2O–Na2O–B2O3–SiO2–NaCl–H2O system at temperatures from 180 to 230 ∘C and pH values from 6 to 12. Synthetic jadarite has been characterized by powder X-ray diffraction (PXRD), Fourier transform infrared (FTIR) spectroscopy, laser Raman spectroscopy, and synchrotron Li and B K-edge X-ray absorption near-edge structure (XANES). First-principles theoretical calculations reproduce the measured FTIR and Raman spectra and allow definitive assignments of vibration modes. Similarly, the measured Li and B K-edge XANES spectra are reasonably reproduced by first-principles theoretical calculations. Our synthesis results, together with its association with searlesite in the Jadar basin, suggest jadarite forms in deep sediments derived from Li-rich alkaline brines under high-temperature diagenetic conditions.
在 Li2O-Na2O-B2O3-SiO2-NaCl-H2O 体系中合成玹石:傅立叶变换红外光谱、拉曼光谱、Li 和 B K 边 XANES 表征及理论计算
摘要。在中新世亚达尔湖相盆地(塞尔维亚西部)的世界级锂硼矿床中,作为一种主要矿石矿物出现的角闪石(LiNaSiB3O7OH)提出了有关其形成条件以及与其他沉积盆地锂矿化的潜在关联的有趣问题。本文报告了在 Li2O-Na2O-B2O3-SiO2-NaCl-H2O 体系中,在 180 至 230 ∘C 温度和 6 至 12 pH 值条件下首次成功合成玹石的情况。通过粉末 X 射线衍射 (PXRD)、傅立叶变换红外光谱 (FTIR)、激光拉曼光谱以及同步辐射 Li 和 B K 边 X 射线吸收近边结构 (XANES) 对合成玹石进行了表征。第一原理理论计算再现了测量到的傅立叶变换红外光谱和拉曼光谱,并确定了振动模式。同样,第一原理理论计算也合理地再现了测量到的 Li 和 B K 边 XANES 光谱。我们的合成结果,以及它与贾达尔盆地中的海泡石的关联,表明玹石形成于高温成岩条件下富锂碱性盐水的深层沉积物中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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