4.8 Article

Vacancy driven surface disorder catalyzes anisotropic evaporation of ZnO (0001) polar surface

Journal

NATURE COMMUNICATIONS
Volume 13, Issue 1, Pages -

Publisher

NATURE PORTFOLIO
DOI: 10.1038/s41467-022-33353-2

Keywords

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Funding

  1. Samsung Research Funding & Incubation Center of Samsung Electronics [SRFC- MA1702-01]
  2. National Research Foundation of Korea (NRF) - Korea government (MSIT) [NRF-2020R1A2C2101735, NRF-2018R1A2B6004394, 2018R1D1A1B07044564]
  3. Advanced Facility Center for Quantum Technology, Sungkyunkwan University (SKKU)
  4. National Research Foundation of Korea [2018R1D1A1B07044564] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)

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This study investigates the characteristics of ZnO polar surfaces and their influence on the evaporation and crystal growth of ZnO nanostructures. The results demonstrate that the evaporation and crystal growth rates of ZnO vary significantly on different surfaces, with the Zn-terminated ZnO (0001) polar surface exhibiting the fastest rates. The evaporation process on the polar surface accelerates dramatically at approximately 300 degrees C, resulting in the formation of a few nanometer-thick quasi-liquid layer. This quasi-liquid layer controls the dissociative evaporation of ZnO by reacting with Zn and O-2 vapors and the underlying ZnO crystal, and facilitates the desorption of O-2 molecules by catalyzing the disordering of the ZnO lattice.
Evaporation and crystal growth occur at different rates on different surfaces. Here authors show dissociative evaporation from ZnO (0001) polar surfaces is accelerated by the formation of a Zn-deficient quasi-liquid layer derived from the formation and inward diffusion of Zn vacancies that stabilize the polar surface. The evaporation and crystal growth rates of ZnO are highly anisotropic and are fastest on the Zn-terminated ZnO (0001) polar surface. Herein, we study this behavior by direct atomic-scale observations and simulations of the dynamic processes of the ZnO (0001) polar surface during evaporation. The evaporation of the (0001) polar surface is accelerated dramatically at around 300 degrees C with the spontaneous formation of a few nanometer-thick quasi-liquid layer. This structurally disordered and chemically Zn-deficient quasi-liquid is derived from the formation and inward diffusion of Zn vacancies that stabilize the (0001) polar surface. The quasi-liquid controls the dissociative evaporation of ZnO with establishing steady state reactions with Zn and O-2 vapors and the underlying ZnO crystal; while the quasi-liquid catalyzes the disordering of ZnO lattice by injecting Zn vacancies, it facilitates the desorption of O-2 molecules. This study reveals that the polarity-driven surface disorder is the key structural feature driving the fast anisotropic evaporation and crystal growth of ZnO nanostructures along the [0001] direction.

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