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三嵌段Janus粒子自组装成三维开放晶格的途径。

Self-Assembly Pathways of Triblock Janus Particles into 3D Open Lattices.

作者信息

Eslami Hossein, Müller-Plathe Florian

机构信息

Department of Chemistry, College of Sciences, Persian Gulf University, Boushehr, 75168, Iran.

Eduard-Zintl-Institut für Anorganische und Physikalische Chemie, Technische Universität Darmstadt, Peter-Grünberg-Straße 8, 64287, Darmstadt, Germany.

出版信息

Small. 2024 Apr;20(14):e2306337. doi: 10.1002/smll.202306337. Epub 2023 Nov 22.

Abstract

The self-assembly of triblock Janus particles is simulated from a fluid to 3D open lattices: pyrochlore, perovskite, and diamond. The coarse-grained model explicitly takes into account the chemical details of the Janus particles (attractive patches at the poles and repulsion around the equator) and it contains explicit solvent particles. Hydrodynamic interactions are accounted for by dissipative particle dynamics. The relative stability of the crystals depends on the patch width. Narrow, intermediate, and wide patches stabilize the pyrochlore-, the perovskite-, and the diamond-lattice, respectively. The nucleation of all three lattices follows a two-step mechanism: the particles first agglomerate into a compact and disordered liquid cluster, which does not crystallize until it has grown to a threshold size. Second, the particles reorient inside this cluster to form crystalline nuclei. The free-energy barriers for the nucleation of pyrochlore and perovskite are ≈10 kT, which are close to the nucleation barriers of previously studied 2D kagome lattices. The barrier height for the nucleation of diamond, however, is much larger (>20 kT), as the symmetry of the triblock Janus particles is not perfect for a diamond structure. The large barrier is associated with the reorientation of particles, i.e., the second step of the nucleation mechanism.

摘要

三嵌段Janus粒子的自组装过程从流体状态模拟到三维开放晶格:烧绿石晶格、钙钛矿晶格和金刚石晶格。粗粒化模型明确考虑了Janus粒子的化学细节(两极处有吸引性斑块,赤道周围有排斥力),并且包含明确的溶剂粒子。通过耗散粒子动力学来考虑流体动力学相互作用。晶体的相对稳定性取决于斑块宽度。窄斑块、中等宽度斑块和宽斑块分别使烧绿石晶格、钙钛矿晶格和金刚石晶格稳定。所有这三种晶格的成核过程遵循两步机制:粒子首先聚集成一个紧密且无序的液体团簇,直到它生长到阈值尺寸才会结晶。其次,粒子在这个团簇内部重新定向以形成晶核。烧绿石晶格和钙钛矿晶格成核的自由能垒约为10kT,这与之前研究的二维 Kagome 晶格的成核垒相近。然而,金刚石晶格成核的垒高度要大得多(>20kT),因为三嵌段Janus粒子的对称性对于金刚石结构来说并不完美。这个大的垒与粒子的重新定向有关,即成核机制的第二步。

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