Ricardo Vidrio, Cesar Saucedo, Vincenzo Lordi, Shimon Kolkowitz, Keith G. Ray, Robert J. Hamers, Jennifer T. Choy
{"title":"Sub-nanometer-thick native sp2 carbon on oxidized diamond surfaces","authors":"Ricardo Vidrio, Cesar Saucedo, Vincenzo Lordi, Shimon Kolkowitz, Keith G. Ray, Robert J. Hamers, Jennifer T. Choy","doi":"arxiv-2409.06934","DOIUrl":null,"url":null,"abstract":"Oxygen-terminated diamond has a wide breadth of applications, which include\nstabilizing near-surface color centers, semiconductor devices, and biological\nsensors. Despite the vast literature on characterizing functionalization groups\non diamond, the chemical composition on the shallowest portion of the surface\n(< 1 nm) is challenging to probe with conventional techniques like XPS and\nFTIR. In this work, we demonstrate the use of angle-resolved XPS to probe the\nfirst ten nanometers of (100) single-crystalline diamond, showing the changes\nof the oxygen functional groups and the allotropes of carbon with respect to\ndepth. With the use of consistent peak-fitting methods, the peak identities and\nrelative peak binding energies were identified for sp2 carbon, ether, hydroxyl,\ncarbonyl, and C-H groups. For the oxygen-terminated sample, we also quantified\nthe thickness of the sp2 carbon layer situated on top of the bulk sp3 diamond\nbonded carbon to be 0.4 $\\pm$ 0.1 nm, based on the analysis of the Auger\nelectron spectra and D-parameter calculations. These results indicate that the\nmajority of the oxygen is bonded to the sp2 carbon layer on the diamond, and\nnot directly on the sp3 diamond bonded carbon.","PeriodicalId":501234,"journal":{"name":"arXiv - PHYS - Materials Science","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2024-09-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - PHYS - Materials Science","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2409.06934","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Oxygen-terminated diamond has a wide breadth of applications, which include
stabilizing near-surface color centers, semiconductor devices, and biological
sensors. Despite the vast literature on characterizing functionalization groups
on diamond, the chemical composition on the shallowest portion of the surface
(< 1 nm) is challenging to probe with conventional techniques like XPS and
FTIR. In this work, we demonstrate the use of angle-resolved XPS to probe the
first ten nanometers of (100) single-crystalline diamond, showing the changes
of the oxygen functional groups and the allotropes of carbon with respect to
depth. With the use of consistent peak-fitting methods, the peak identities and
relative peak binding energies were identified for sp2 carbon, ether, hydroxyl,
carbonyl, and C-H groups. For the oxygen-terminated sample, we also quantified
the thickness of the sp2 carbon layer situated on top of the bulk sp3 diamond
bonded carbon to be 0.4 $\pm$ 0.1 nm, based on the analysis of the Auger
electron spectra and D-parameter calculations. These results indicate that the
majority of the oxygen is bonded to the sp2 carbon layer on the diamond, and
not directly on the sp3 diamond bonded carbon.