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Elemental distribution on grain surfaces.
Electron energy loss spectroscopy (EELS) mapping was used to further reveal the elemental distribution (Fig. S4).
Additional chemical data regarding elemental distribution between the minerals is necessary to verify this assumption.
We then quantified the elemental distribution at the same referenced interface using point analyses and elemental maps produced by scanning electron microscopy.
Coupling the superior imaging capabilities of HIM with established methods for measuring elemental distribution using SEM can help resolve complex weathering processes found in natural soil environments.
This supports the presence of 2D PVSK at grain boundaries, which was further confirmed by elemental distribution (EDS) analysis (Supplementary Fig. 24).
With an in-house MATLAB® script quantitative imaging of the elemental distribution was possible.
The coexistence of bcc and fcc phases appears with the change of elemental distribution.
Energy dispersive spectroscopy was employed to investigate elemental distribution on the coating surfaces and cross-sections.
The elemental distribution was measured using Rutherford Backscattering Spectrometry (RBS) at each step of Si bombardment.
The elemental distribution in the coatings was characterized by electron probe microanalysis.
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