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Updated: May 25, 2026

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Sub-nanometer Resolution Imaging with Amplitude-modulation Atomic Force Microscopy in Liquid
Published on: December 20, 2016
NC-AFM contrast formation on the calcite (1014) surface
Philipp Rahe1, Jens Schütte, Angelika Kühnle
1Johannes Gutenberg-Universität Mainz, Institut für Physikalische Chemie, Mainz, Germany. rahe@uni-mainz.de
Summary
This study uses non-contact atomic force microscopy (NC-AFM) to investigate calcite surface reconstructions. It clarifies the existence of the row-pairing reconstruction and explains varied experimental observations.
Area of Science:
- Geochemistry
- Surface Science
- Materials Science
Background:
- Calcite (calcium carbonate) is abundant, with its (1014) cleavage plane extensively studied.
- Two surface reconstructions, (2 × 1) and row-pairing, have been proposed for calcite.
- The (2 × 1) reconstruction is confirmed, but the row-pairing reconstruction's existence remains debated.
Purpose of the Study:
- To investigate the (1014) calcite surface using non-contact atomic force microscopy (NC-AFM).
- To analyze and classify different NC-AFM contrast modes observed on the calcite surface.
- To provide experimental evidence for surface reconstructions and clarify the existence of the row-pairing reconstruction.
Main Methods:
- Non-contact atomic force microscopy (NC-AFM) in ultra-high vacuum.
- Systematic study of various NC-AFM contrast modes.
- Analysis of tip termination and interaction regimes.
Main Results:
- A classification scheme for 12 different NC-AFM contrast modes was developed.
- Experimental evidence was obtained for 10 contrast modes.
- Specific contrast modes allowed for the identification of surface reconstructions, explaining conflicting literature data.
- The study provides detailed analysis supporting the existence of the row-pairing reconstruction.
Conclusions:
- NC-AFM is a powerful tool for characterizing calcite surface reconstructions.
- The observed variety in NC-AFM contrasts explains discrepancies in previous studies.
- The existence of the row-pairing reconstruction on the (1014) calcite surface is supported by experimental evidence.
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