A combined atomic nitrogen‑oxygen OES line-ratios method to determine the low-energy and high-energy electron temperature in non-equilibrium atmospheric pressure air glide arc plasmas

  • Xi Ming Zhu
  • , Lu Wang
  • , Wei Cui
  • , Yun Wu
  • , Min Jia
  • , Yang Zhao
  • , Bang Dou Huang

Research output: Contribution to journalArticlepeer-review

3 Scopus citations

Abstract

Atmospheric pressure air plasma is widely used in material processing, plasma-assisted combustion, life science and agriculture. The active-particle density is considered a key factor in monitoring the plasma states, and it is related to the electron temperature. However, there is a lack of an efficient optical emission spectroscopy (OES) method to obtain the electron temperature in atmospheric pressure non-equilibrium air plasma, especially when the electron energy distribution deviates from the Maxwellian distribution. So, in this work, we propose a novel combined OES line-ratios method to determine the high/low-energy electron temperature. This method is based on two summarized excited-state systems, the “N(2p3 4So) excited-state system” and “O(2p3(4So)3s 5So) excited-state system”, which are presented to find key excited-states sensitive to the high/low-energy electron temperature, respectively. Besides, a collisional-radiative model, considering the atomic nitrogen and oxygen including their excited states, is built to provide the mapping relation and verify the kinetic properties from the above excited-state systems. Our combined line-ratio method has been applied in an air glide arc plasma igniter.

Original languageEnglish
Article number106998
JournalSpectrochimica Acta - Part B Atomic Spectroscopy
Volume218
DOIs
StatePublished - Aug 2024
Externally publishedYes

Keywords

  • Air glide arc plasma
  • CR model
  • High/low-energy electron temperature
  • Line-ratio method

Fingerprint

Dive into the research topics of 'A combined atomic nitrogen‑oxygen OES line-ratios method to determine the low-energy and high-energy electron temperature in non-equilibrium atmospheric pressure air glide arc plasmas'. Together they form a unique fingerprint.

Cite this