Ghandi Khashayar, Landry Cody, Du Tait, Lainé Maxime, Saul Andres, Le Caër Sophie
University of Guelph, Department of chemistry, Guelph, ON, N1G 2W1, Canada.
Université de Sherbrooke, Faculté de médecine, Sherbrooke, QC, J1H 5N4, Canada.
Sci Rep. 2019 Nov 20;9(1):17165. doi: 10.1038/s41598-019-52662-z.
The purpose of the present work was to study how chemical reactions and the electronic structure of atoms are affected by confinement at the sub-nanometer scale. To reach this goal, we studied the H atom in talc, a layered clay mineral. Talc is a highly 2D-confining material with the width of its interlayer space close to angstrom. We investigated talc with a particle accelerator-based spectroscopic method that uses elementary particles. This technique generates an exotic atom, muonium (Mu), which can be considered as an isotope of the H atom. Moreover, the technique allows us to probe a single atom (H atom) at any time and explore the effects of the layered clay on a single ion (proton) or atom. The cation/electron recombination happens in two time windows: one faster than a nanosecond and the other one at longer than microseconds. This result suggests that two types of electron transfer processes take place in these clay minerals. Calculations demonstrated that the interlayer space acts as a catalytic surface and is the primary location of cation/electron recombination in talc. Moreover, the studies of the temperature dependence of Mu decay rates, due to the formation of the surrogate of H, is suggestive of an "H" formation reaction that is thermally activated above 25 K, but governed by quantum diffusion below 25 K. The experimental and computational studies of the hyperfine coupling constant of Mu suggest that it is formed in the interlayer space of talc and that its electronic structure is extremely changed due to confinement. All these results imply that the chemistry could be strongly affected by confinement in the interlayer space of clays.
本工作的目的是研究化学反应和原子的电子结构如何受到亚纳米尺度限制的影响。为实现这一目标,我们研究了滑石(一种层状粘土矿物)中的氢原子。滑石是一种高度二维限制材料,其层间空间宽度接近埃。我们用一种基于粒子加速器的光谱方法研究滑石,该方法使用基本粒子。这项技术产生一种奇异原子——μ子素(Mu),它可被视为氢原子的一种同位素。此外,该技术使我们能够随时探测单个原子(氢原子),并探索层状粘土对单个离子(质子)或原子的影响。阳离子/电子复合发生在两个时间窗口:一个快于纳秒,另一个长于微秒。这一结果表明在这些粘土矿物中发生了两种类型的电子转移过程。计算表明,层间空间起到催化表面的作用,是滑石中阳离子/电子复合的主要位置。此外,对由于形成氢的替代物而导致的μ子素衰变率的温度依赖性研究表明,存在一种“氢”形成反应,该反应在25 K以上是热激活的,但在25 K以下受量子扩散控制。对μ子素超精细耦合常数的实验和计算研究表明,它在滑石的层间空间中形成,并且由于限制其电子结构发生了极大变化。所有这些结果都意味着,粘土的层间空间限制可能会对化学过程产生强烈影响。