Evidence of Deep Water Penetration in Silica during Stress Corrosion Fracture

F. Lechenault, C. L. Rountree, F. Cousin, J.-P. Bouchaud, L. Ponson, and E. Bouchaud
Phys. Rev. Lett. 106, 165504 – Published 21 April 2011

Abstract

We measure the thickness of the heavy water layer trapped under the stress corrosion fracture surface of silica using neutron reflectivity experiments. We show that the penetration depth is 6585   Å, suggesting the presence of a damaged zone of 100   Å extending ahead of the crack tip during its propagation. This estimate of the size of the damaged zone is compatible with other recent results.

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  • Received 28 November 2010

DOI:https://doi.org/10.1103/PhysRevLett.106.165504

© 2011 American Physical Society

Authors & Affiliations

F. Lechenault1, C. L. Rountree2, F. Cousin3, J.-P. Bouchaud4, L. Ponson5, and E. Bouchaud1,6

  • 1CEA-Saclay, IRAMIS, SPEC, F-91191 Gif-sur-Yvette, France
  • 2CEA-Saclay, IRAMIS, SPCSI, F-91191 Gif-sur-Yvette, France
  • 3CEA-Saclay, IRAMIS, Laboratoire Léon Brillouin, UMR12, F-91191 Gif-sur-Yvette, France
  • 4Science and Finance, Capital Fund Management, 6 Boulevard Haussmann, 75009 Paris, France
  • 5Graduate Aerospace Laboratories (GALCIT), California Institute of Technology, Pasadena, California 91125, USA
  • 6Department of Physics, Norwegian University of Science and Technology, Hogskoleringen 5, N-7491 Trondheim, Norway

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Issue

Vol. 106, Iss. 16 — 22 April 2011

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