Wang, Yuecun, Wang, Xudong, Ding, Jun, Liang, Beiming, Zuo, Lingling, Zheng, Shaochuan, Huang, Longchao, Xu, Wei, Fan, Chuanwei, Duan, Zhanqiang, Jia, Chunde, Zheng, Rui, Liu, Zhang, Zhang, Wei, Li, Ju, Ma, En, and Shan, Zhiwei
In the absence of externally applied mechanical loading, it would seem counterintuitive that a solid particle sitting on the surface of another solid could not only sink into the latter, but also continue its rigid-body motion towards the interior, reaching a depth as distant as thousands of times the particle diameter. Here, we demonstrate such a case using in situ microscopic as well as bulk experiments, in which diamond nanoparticles ~100 nm in size move into iron up to millimeter depth, at a temperature about half of the melting point of iron. Each diamond nanoparticle is nudged as a whole, in a displacive motion towards the iron interior, due to a local stress induced by the accumulation of iron atoms diffusing around the particle via a short and easy interfacial channel. Our discovery underscores an unusual mass transport mode in solids, in addition to the familiar diffusion of individual atoms. It has long been believed that diffusion as individual atoms is the primary way for carbon to enter Fe crystals from outside. Here, the authors report an unusual mass transport way in solids, through which diamond nanoparticles can enter Fe spontaneously and translate inward for a long distance. [ABSTRACT FROM AUTHOR]