2019
DOI: 10.1038/s41598-018-37518-2
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Unusual oxidation-induced core-level shifts at the HfO2/InP interface

Abstract: X-ray photoelectron spectroscopy (XPS) is one of the most used methods in a diverse field of materials science and engineering. The elemental core-level binding energies (BE) and core-level shifts (CLS) are determined and interpreted in the XPS. Oxidation is commonly considered to increase the BE of the core electrons of metal and semiconductor elements (i.e., positive BE shift due to O bonds), because valence electron charge density moves toward electronegative O atoms in the intuitive charge-transfer model. … Show more

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Cited by 12 publications
(14 citation statements)
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“…The two components at 444.4 and 445.3 eV are assigned as the bondings of In-P and In-O, respectively. [22][23][24][25][26][27][28] These results demonstrate that more indium atoms on the surface of #1b were oxidized than #1a. The P 2p XP spectra also deconvoluted into two components assigned as P-In and P-O bondings.…”
Section: Resultsmentioning
confidence: 74%
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“…The two components at 444.4 and 445.3 eV are assigned as the bondings of In-P and In-O, respectively. [22][23][24][25][26][27][28] These results demonstrate that more indium atoms on the surface of #1b were oxidized than #1a. The P 2p XP spectra also deconvoluted into two components assigned as P-In and P-O bondings.…”
Section: Resultsmentioning
confidence: 74%
“…As there was no report about P 1s spectra from InP materials, it was attempted to presume the origins of the two sub peaks recognized in the P 1s spectra, considering from the XPS studies about P 2p. [22][23][24][25][26][27][28] As shown in Fig. 3, the chemical shifts of the sub peaks from the P-In main peak were approximately 5.5 and 1.6 eV.…”
Section: Discussionmentioning
confidence: 84%
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“…The sharing of the elements with their neighbor atoms in the bond arrangement can cause a shift in the core-level binding energy. 35 The binding energy values at 398.4, 399.9, and 401 eV are attributed to pyridinic-N, pyrrolic-N, and graphitic-N species, respectively. 36 It revealed that all samples contained relatively large amounts of graphitic-N species, especially Fe@NC-900(5h) contained a little higher pyridinic species (Figure 2c).…”
Section: Resultsmentioning
confidence: 93%
“…3). Слой естественного окисла на поверхности InP(100) содержит оксиды In 2 O, а также фосфаты, InPO 4 , и гидрофосфаты, In x (HPO 4 ) y , индия [82,83,86].…”
Section: Gapunclassified