Mn2+ 浓度对酸性条件下 δ-MnO2 晶体生长的影响

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
Liyan Bi, Haoran Hu, Lei Wang, Zuran Li, Fangdong Zhan, Yongmei He, Yanqun Zu, Yuan Li, Xinran Liang
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引用次数: 0

摘要

δ-MnO2 是环境矿物的重要组成部分,也是最强的吸附剂和氧化剂之一。δ-MnO2 的结晶形态是影响其反应活性的关键因素之一。在这项研究中,最初合成的 δ-MnO2 被置于酸性环境中,与 Mn2+ 发生反应并发生结晶转变。在结晶δ-MnO2 的转化过程中,进行了动力学取样,然后分析了样品的结构和形态。结果表明,在 pH 值为 2.5 和 4 时,δ-MnO2 纳米片在初始阶段通过边对边组装自发地自组装成纳米带。随后,这些纳米带通过沿 c 轴的面对面组装相互连接形成初级纳米棒。然后,这些原生纳米棒沿 (001) 平面和侧表面组装,实现了进一步的生长和增厚。由于较低的 pH 值更有利于在 δ-MnO2 中形成空位,因此 δ-MnO2 可以快速地将 Mn2+ 直接吸附到空位上,形成隧道壁。同时,隧道壁的快速形成还能使相邻纳米带之间迅速建立氢键,从而使这些纳米带组装成原生纳米棒。因此,在具有相同 Mn2+ 浓度的溶液中,pH 值为 2.5 时,δ-MnO2 向 α-MnO2 的结构转变和形态演变比 pH 值为 4 时更快。 这些发现有助于深入了解从层基到隧道基纳米棒的晶体生长机制,以及高效、可控地合成纳米材料的方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effect of Mn2+ concentration on the growth of δ-MnO2 crystals under acidic conditions

δ-MnO2 is an important component of environmental minerals and is among the strongest sorbents and oxidants. The crystalline morphology of δ-MnO2 is one of the key factors affecting its reactivity. In this work, δ-MnO2 was initially synthesized and placed in an acidic environment to react with Mn2+ and undergo a crystalline transformation. During the transformation of crystalline δ-MnO2, kinetic sampling was conducted, followed by analyses of the structures and morphologies of the samples. The results showed that at pH 2.5 and 4, δ-MnO2 nanoflakes spontaneously self-assembled into nanoribbons via edge-to-edge assembly in the initial stage. Subsequently, these nanoribbons attached to each other to form primary nanorods through a face-to-face assembly along the c-axis. These primary nanorods then assembled along the (001) planes and lateral surfaces, achieving further growth and thickening. Since a lower pH is more favorable for the formation of vacancies in δ-MnO2, δ-MnO2 can rapidly adsorb Mn2+ directly onto the vacancies to form tunnel walls. At the same time, the rapid formation of the tunnel walls leads to a quick establishment of hydrogen bonding between adjacent nanoribbons, enabling the assembly of these nanoribbons into primary nanorods. Therefore, in a solution with the same concentration of Mn2+, the structure transformation and morphology evolution of δ-MnO2 to α-MnO2 occur faster at pH 2.5 than at pH 4. These findings provide insights into the mechanism for crystal growth from layer-based to tunnel-based nanorods and methods for efficient and controlled syntheses of nanomaterials.

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来源期刊
Geochemical Transactions
Geochemical Transactions 地学-地球化学与地球物理
CiteScore
3.70
自引率
4.30%
发文量
2
审稿时长
>12 weeks
期刊介绍: Geochemical Transactions publishes high-quality research in all areas of chemistry as it relates to materials and processes occurring in terrestrial and extraterrestrial systems.
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