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超越离子交换:解析锂离子在HTiO上吸附的复杂性

Beyond Ion Exchange: Unraveling the Complexity of Lithium-Ion Adsorption on HTiO.

作者信息

Lu Binda, Wang Xinyang, Zhang Yufang, Wang Qiankun, Jiang Feng, Lin Wanran, Liu Lingfei, Ye Peiyuan, Lu Wang, Lu Zhouguang, Xu Zhenghe

机构信息

Shenzhen Key Laboratory of Interfacial Science and Engineering of Materials, Department of Materials Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China.

Advanced Materials Innovation Center, Jiaxing Research Institute of Southern University of Science and Technology, Jiaxing 314031, China.

出版信息

ACS Appl Mater Interfaces. 2025 Jul 9;17(27):39628-39641. doi: 10.1021/acsami.5c06231. Epub 2025 Jun 29.

Abstract

Layered titanium acid (HTiO or HTO) has been extensively utilized as a lithium-ion sieve in studies on lithium extraction from salt lake brines. However, the actual lithium uptake by layered HTO, commonly known through an ion exchange mechanism, is much lower than the theoretical value. The hypothesis is that there is a clear need to further elucidate the mechanism of lithium-ion adsorption for the purpose of guiding the design of a lithium ion sieve (LIS). In this study, lithium adsorption on layered HTO as a function of pH was investigated to gain deeper insight into its underlying adsorption mechanism. Lithium adsorption was found to increase significantly with pH, in particular, at pH 14. To comprehend this strong pH dependency, thermogravimetric analysis-differential scanning calorimetry (TG-DSC) techniques were used to analyze the state of HTO layers before and after lithium adsorption. Surprisingly, HTO surfaces at pH 14 exhibited fewer hydration layers and a higher abundance of hydroxyl groups compared with values at lower pH values. Characterization of HTO before and after lithium adsorption using X-ray diffraction (XRD) and transmission electron microscopy (TEM) revealed an anatase type of TiO in HTO at pH 14. Fourier transform infrared spectroscopy (FTIR) and solid-state nuclear magnetic resonance (SSNMR) measurements showed a significant alteration in the configuration of hydroxyl groups within HTO layers after Li adsorption at pH 14, distinguishing it from the behavior observed at other pH values. These findings demonstrate that lithium adsorption occurs predominantly through LiOH molecules, which displace interlayer water molecules. The results from density functional theory (DFT) calculations align well with our experimental findings. This research provides a more profound understanding of lithium adsorption in multilayer LIS materials and a scientific basis for the design of innovative multilayer structures for the extraction of lithium from salt lake brines.

摘要

层状钛酸(HTiO或HTO)在盐湖卤水提锂研究中被广泛用作锂离子筛。然而,通常通过离子交换机制得知的层状HTO的实际锂摄取量远低于理论值。假设是,为了指导锂离子筛(LIS)的设计,显然需要进一步阐明锂离子吸附机制。在本研究中,研究了层状HTO上锂吸附随pH的变化,以更深入地了解其潜在的吸附机制。发现锂吸附量随pH显著增加,特别是在pH 14时。为了理解这种强烈的pH依赖性,采用热重分析-差示扫描量热法(TG-DSC)技术分析锂吸附前后HTO层的状态。令人惊讶的是,与较低pH值相比,pH 14时的HTO表面水合层数更少,羟基丰度更高。使用X射线衍射(XRD)和透射电子显微镜(TEM)对锂吸附前后的HTO进行表征,发现在pH 14时HTO中存在锐钛矿型TiO。傅里叶变换红外光谱(FTIR)和固态核磁共振(SSNMR)测量表明,在pH 14时锂吸附后HTO层内羟基的构型发生了显著变化,这与在其他pH值下观察到的行为不同。这些发现表明,锂吸附主要通过LiOH分子发生,LiOH分子取代了层间水分子。密度泛函理论(DFT)计算结果与我们的实验结果吻合良好。本研究为多层LIS材料中的锂吸附提供了更深刻的理解,并为从盐湖卤水中提取锂的创新多层结构设计提供了科学依据。

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