Center for High Pressure Science and Technology Advanced Research, Beijing, China.
State Key Laboratory of Physical Chemistry of Solid Surfaces, College of Materials, Xiamen University, Xiamen, China.
Nature. 2021 Nov;599(7886):605-610. doi: 10.1038/s41586-021-04122-w. Epub 2021 Nov 24.
Solids in nature can be generally classified into crystalline and non-crystalline states, depending on whether long-range lattice periodicity is present in the material. The differentiation of the two states, however, could face fundamental challenges if the degree of long-range order in crystals is significantly reduced. Here we report a paracrystalline state of diamond that is distinct from either crystalline or amorphous diamond. The paracrystalline diamond reported in this work, consisting of sub-nanometre-sized paracrystallites that possess a well-defined crystalline medium-range order up to a few atomic shells, was synthesized in high-pressure high-temperature conditions (for example, 30 GPa and 1,600 K) employing face-centred cubic C as a precursor. The structural characteristics of the paracrystalline diamond were identified through a combination of X-ray diffraction, high-resolution transmission microscopy and advanced molecular dynamics simulation. The formation of paracrystalline diamond is a result of densely distributed nucleation sites developed in compressed C as well as pronounced second-nearest-neighbour short-range order in amorphous diamond due to strong sp bonding. The discovery of paracrystalline diamond adds an unusual diamond form to the enriched carbon family, which exhibits distinguishing physical properties and can be furthered exploited to develop new materials. Furthermore, this work reveals the missing link in the length scale between amorphous and crystalline states across the structural landscape, having profound implications for recognizing complex structures arising from amorphous materials.
自然界中的固体通常可以分为晶体和非晶体状态,这取决于材料中是否存在长程晶格周期性。然而,如果晶体的长程有序度显著降低,这两种状态的区分可能会面临根本性的挑战。在这里,我们报告了一种不同于晶体或非晶态金刚石的准晶态金刚石。本文报道的准晶态金刚石由亚纳米级的准晶纳米颗粒组成,这些准晶纳米颗粒具有明确的结晶中程有序,直至几个原子壳层,是在高压高温条件下(例如 30 GPa 和 1600 K)使用面心立方 C 作为前体制备的。通过 X 射线衍射、高分辨率透射显微镜和先进的分子动力学模拟相结合,确定了准晶态金刚石的结构特征。准晶态金刚石的形成是由于压缩 C 中密集分布的成核点以及由于强 sp 键合导致非晶态金刚石中明显的第二近邻短程有序所致。准晶态金刚石的发现为丰富的碳家族增添了一种不寻常的金刚石形式,它具有独特的物理性质,可以进一步开发新材料。此外,这项工作揭示了在结构景观中,从非晶态到晶态的长度尺度上缺失的一环,这对识别由非晶材料产生的复杂结构具有深远的意义。