Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Effect of acidic environment on subcritical crack growth in alumina ceramics

Journal Article · · Scripta Materialia
; ; ; ;  [1]
  1. Russian Academy of Sciences, Moscow (Russian Federation). High Tech Ceramics Research Centre

Alumina ceramics are good candidates for applications involving corrosion-active media, e.g. in seal-rings, bearings and impellers in pumps. However, their strength is susceptible to deterioration in chemical environments. This phenomenon is believed to result primarily from a stress-enhanced chemical reaction between the environment and the bonds at the tips of microstructural stress concentrators, such as microcracks, pores and grain boundaries. As a consequence, alumina ceramics exhibit subcritical crack growth prior to catastrophic failure, and their strength and fracture are dependent on time or stressing rate. In the alumina ceramics processing, sintering additives are often utilized which are forming the grain-boundary phase. The behavior of such a phase may control the slow crack growth processes. In this context, the present study is aimed at investigation of the influence of acidic environment on crack velocity exponent for aluminas sintered with different additives.

OSTI ID:
616239
Journal Information:
Scripta Materialia, Journal Name: Scripta Materialia Journal Issue: 6 Vol. 38; ISSN 1359-6462; ISSN SCMAF7
Country of Publication:
United States
Language:
English

Similar Records

Effects of chemical environments on slow crack growth in glasses and ceramics
Journal Article · Sun Jun 10 00:00:00 EDT 1984 · J. Geophys. Res.; (United States) · OSTI ID:6474167

Fracture and subcritical crack-growth behavior of Y-Si-Al-O-N glasses and Si{sub 3}N{sub 4} ceramics
Journal Article · Tue Feb 29 23:00:00 EST 2000 · Journal of the American Ceramic Society · OSTI ID:20020619

Subcritical crack growth and other time- and environment-dependent behavior in crustal rocks
Journal Article · Sun Jun 10 00:00:00 EDT 1984 · J. Geophys. Res.; (United States) · OSTI ID:6369453