Pressure Solution at the Molecular Scale

Edgar Alejandro Pachon-Rodriguez, Agnès Piednoir, and Jean Colombani
Phys. Rev. Lett. 107, 146102 – Published 30 September 2011

Abstract

The topological evolution of the cleavage surface of a gypsum single crystal during its dissolution in a flowing undersaturated aqueous solution has been observed with an atomic force microscope. The matter transfer from solid to liquid proceeds through the migration of atomic steps. The step velocity has been measured and appears to depend on the force applied by the tip on the surface. Whereas the high force velocity enhancement is likely to stem from corrosive wear, the speed behavior at low force (<10nN) differs drastically and can be interpreted as a consequence of the pressure solution of the crystal induced by the tip force. The step velocity evolution with the force obeys the known kinetic law of pressure solution. Hence these experiments enable us to evidence a first atomic mechanism at the origin of pressure solution.

  • Figure
  • Figure
  • Figure
  • Figure
  • Received 26 May 2011

DOI:https://doi.org/10.1103/PhysRevLett.107.146102

© 2011 American Physical Society

Authors & Affiliations

Edgar Alejandro Pachon-Rodriguez, Agnès Piednoir, and Jean Colombani*

  • Laboratoire de Physique de la Matière Condensée et Nanostructures; Université de Lyon; Université Claude Bernard Lyon 1; CNRS, UMR 5586; Domaine scientifique de la Doua, F-69622 Villeurbanne cedex, France

  • *Jean.Colombani@univ-lyon1.fr

Article Text (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 107, Iss. 14 — 30 September 2011

Reuse & Permissions
Access Options
Author publication services for translation and copyediting assistance advertisement

Authorization Required


×
×

Images

×

Sign up to receive regular email alerts from Physical Review Letters

Log In

Cancel
×

Search


Article Lookup

Paste a citation or DOI

Enter a citation
×