XPS Reference Pages
Advanced XPS Analysis of Zinc
Figure 1 and Table 1 summarize reported literature positions for the Zn 2p3/2 peak, presenting mean values as well as their associated standard deviations. Although the Zn 2p3/2 signal is free from complications such as multiplet splitting, chemical analysis remains challenging due to significant signal overlap among different compounds. The situation is further complicated by factors such as natural line widths, variations in peak shapes, and the uncertainties introduced during charge referencing, all of which make reliable chemical‑state interpretation increasingly difficult.
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| Table 3. Summary of experimentally measured Zn L3M4,5M4,5 kinetic energies, modified Auger parameter (α’), as well as their respective standard deviations. [1] |
[1] J.D. Henderson, S.D.C. Buchanan, L.H. Grey, M.C. Biesinger, Appl. Surf. Sci., 730 (2026) 166284.
[2] J. Duchoslav, R. Steinberger, M. Arndt, D. Stifter, Corros. Sci. 82 (2014) 356-361.
Common XPS Questions - Insights from Workshop Participants
1️⃣ Reliable Peak Fitting & Deconvolution
How to perform defensible, physically meaningful peak fitting — avoiding overfitting while properly handling multiplets, satellites, asymmetry, and constraints.
2️⃣ Overlapping Peaks in Complex Systems
Strategies for separating overlapping core levels (e.g., Fe/Co, Ba–Co, Cr/Te, C 1s overlaps) and mixed-phase materials.
3️⃣ Oxidation State Identification
How to confidently distinguish oxidation states (e.g., Fe²⁺/Fe³⁺, Mn multivalency, Ag⁰ vs Ag⁺) and interpret satellite structures.
4️⃣ Quantitative Accuracy
How to correctly calculate atomic percentages, apply RSFs, account for transmission functions, and interpret stoichiometry mismatches.
5️⃣ Energy Referencing & Carbon Correction
Reliability of C 1s calibration, handling adventitious carbon, alternatives to carbon referencing, and the impact of improper calibration.
6️⃣ Background Selection & Fitting Parameters
Correct choice of inelastic background (Shirley vs Tougaard), FWHM constraints, peak shapes, spin–orbit rules, and acceptable χ² values.
7️⃣ Charging Effects (Especially Insulators & Operando Work)
How to detect, correct, and minimize charging in powders, polymers, biological materials, and electrochemical systems.
8️⃣ Oxygen Peak Interpretation
Deconvoluting O 1s spectra in mixed oxides, identifying oxygen vacancies, and resolving oxygen contributions in multi-metal systems.
9️⃣ Publication Standards & Reviewer Expectations
How many components are acceptable? Is peak fitting mandatory? What are common reviewer criticisms? How should survey and HR spectra be presented?
🔟 Surface Sensitivity & Depth Information
Understanding probing depth, interaction volume, oxide thickness estimation, surface vs subsurface contributions, and when XPS truly represents “surface-only” chemistry.
Magnesium 2p and Auger Parameter Values
Magnesium 2p binding energy and modified Auger parameter values are shown in Table 1. It is worth noting that accounting for the difference between charge referencing procedures is vital for correct analysis of magnesium compounds (especially for MgO and Mg(OH)2) [1]. For MgO, the peak position for the Mg 2p transition is 49.4 eV when charge referenced to adventitious carbon at 284.8 eV, and 50.8 when referenced to the Mg 2p metal peak at 49.73 eV (or grounded). This has led to a lot of confusion regarding the Mg 2p peak positions to use for analysis. The results from a consistently analyzed dataset are shown in Table 1 together with compiled literature values [1]. Since the chemical sensitivity of the Mg 2p transition is low for magnesium the Auger parameter and anion signals are particularly important to consider for improved speciation.
The anion fitting parameters—binding energy, peak width, and line shape—obtained from fitting reference samples are reported in Table 2 from a consistently analyzed data set [1]. The O 1s signal can be used to separate MgO and Mg(OH)2 despite their overlapping Mg 2p signals. The O 1s peak position of Mg(OH)2 is +1.6 eV with respect to the main lattice peak of MgO. However, the peak position for Mg(OH)2 can overlap with other environments such as the MgO defective oxide and adventitious carbon, which may need to be accounted for in the analysis.
Magnesium Induced Ghost Peaks
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| Figure 1. Survey spectrum of Mg(OH)2 powder where the O 1s ghost peak is clearly visible at 765.7 eV. The figure is reproduced from reference [1]. |
XPS Detection Limits
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| XPS detection limits using Al K(alpha) radiation [1]. |
[1] A.G. Shard, Surf. Interface Anal. 46 (2014) 175-185.
Carbon 1s for Organic Compounds
The seminal work of Graham Beamson and Dave Briggs in their "High Resolution XPS of Organic Polymers – The Scienta ESCA300 Database" has been utilized since 1992 as an invaluable resource for the XPS analysis of polymers and organic materials. A summary of carbon 1s binding energies for organic functional groups from this work are presented here. The original work calibrates the binding energy scale to 285.0 eV for aliphatic carbon C 1s. The values presented here are now calibrated to 284.8 eV for aliphatic carbon, in line with recent results [2].
Figure 1. Summary of the mean, maximum, and minimum carbon 1s binding energies for different organic functionalities according to the work of Beamson and Briggs [1]. Binding energy calibration presented here have been adjusted to the main aliphatic C 1s peak at 284.8 eV.Table 1. Summary of the mean, maximum, and minimum carbon 1s binding energies for different organic functionalities according to the work of Beamson and Briggs [1]. Binding energy calibration presented here have been adjusted to the main aliphatic C 1s peak at 284.8 eV.
The effects of various functional groups on beta carbon binding energies can be significant (Table 2). Note that, in this context, the alpha carbon is the carbon directly attached to the functional group, and the beta carbon is attached to the alpha carbon. These effects have been included in the refinement of the binding energy value for the aliphatic carbon component in adventitious carbon [2].
[1] G. Beamson, D. Briggs, High Resolution XPS of Organic Polymers - The Scienta ESCA300 Database, Wiley Interscience, 1992, Appendices 1 and 2.
[2] L.H. Grey, H.-Y. Nie, M.C. Biesinger, Appl. Surf. Sci. 653 (2024) 159319.
Oxygen 1s for Organic Compounds
Additional Notes:
C-OH (aliphatic) Ref to C 1s at 284.8 eV: Average 532.7 eV, Min. 532.5 eV, Max. 532.9 eV
C-OH (aromatic) Ref to C 1s at 285.0 eV: 533.6 eV
Also note that Si 2p3/2 for PDMS (silicone) is at 101.79 eV (Si 2p = 102.0 eV) with the C 1s at 284.38 eV and O 1s at 532.00 eV (referenced to aliphatic C at 285.0 eV). If we shift the C 1s to 285.0 eV then Si 2p3/2 is at 102.41 eV (Si 2p = 102.6 eV) and O 1s is at 532.62 eV for silicone. If we then shift the C 1s to 284.8 eV then Si 2p3/2 is at 102.21 eV (Si 2p = 102.4 eV) and O 1s is at 532.42 eV for silicone.
References:
[1] G. Beamson, D. Briggs, High Resolution XPS of Organic Polymers - The Scienta ESCA300 Database, Wiley Interscience, 1992, Appendices 3.1 and 3.2.
Calculating Oxygen Content from Adventitious Carbon 1s Spectra
(Note: you must download the file to Excel to use it - it is locked in Google Docs).
















