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Molecular Self-Assembly Versus Surface Restructuring During Calcite Dissolution.

Martin Nalbach1, Stefanie Klassen1, Ralf Bechstein1

  • 1Institute of Physical Chemistry, Johannes Gutenberg University Mainz , Duesbergweg 10-14, 55099 Mainz, Germany.

Langmuir : the ACS Journal of Surfaces and Colloids
|September 8, 2016
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Summary
This summary is machine-generated.

Organic azo dyes significantly alter calcite surfaces, causing restructuring independent of pH. Ordered molecular structures form only under specific conditions, unlike the robust surface restructuring.

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Area of Science:

  • Geochemistry
  • Materials Science
  • Physical Chemistry

Background:

  • Organic additives influence mineral-water interfaces by self-assembly or surface restructuring.
  • Calcium-complexing azo dyes are known to interact with mineral surfaces.

Purpose of the Study:

  • Investigate the impact of azo dyes on calcite dissolution and surface morphology.
  • Compare the effects of Eriochrome Black T and Eriochrome Black A on calcite (10.4).

Main Methods:

  • High-resolution atomic force microscopy (AFM) in aqueous solution.
  • Controlled experiments varying pH and dye isomers.

Main Results:

  • Pronounced surface restructuring of calcite observed with both azo dye isomers, irrespective of pH.
  • Restructuring involves stabilization of step edges, altering interface morphology.
  • Ordered molecular stripe formation occurred only with Eriochrome Black A within a narrow pH window (~3.6).

Conclusions:

  • Surface restructuring induced by azo dyes is robust against pH and molecular conformation changes.
  • Ordered molecular self-assembly requires precise control over molecular properties like conformation and deprotonation state.
  • Calcite surface morphology is significantly altered by calcium-complexing azo dyes.