Published January 2013 | Version v1
Journal article

Microstress partitioning in porous and microcracked synthetic cordierite

  • 1. Corning Incorporated, S and T, CMP-SP-FR06, Corning, NY 14831 (United States)
  • 2. Los Alamos National Laboratory, LANSCE-LC, Los Alamos, NM 87545 (United States)
  • 3. Los Alamos National Laboratory, MST-8, Los Alamos, NM 87545 (United States)

Description

As a continuation of earlier work on thermal expansion in extruded porous cordierite honeycombs, high-temperature neutron diffraction allowed us to observe lattice strains as a function of temperature. The transfer of grain microstrain (and stress) between the main (orthorhombic) cordierite phase and the minority spinel phase could be experimentally captured and rationalized by simple stress balance equations.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.scriptamat.2012.09.015

Additional details

Identifiers

DOI
10.1016/j.scriptamat.2012.09.015;
PII
S1359-6462(12)00595-7;

Publishing Information

Journal Title
Scripta Materialia
Journal Volume
68
Journal Issue
2
Journal Page Range
p. 100-103
ISSN
1359-6462
CODEN
SCMAF7

INIS

Country of Publication
United Kingdom
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
45025176
Subject category
S36: MATERIALS SCIENCE;
Descriptors DEI
ANISOTROPY; CUBIC LATTICES; NEUTRON DIFFRACTION; ORTHORHOMBIC LATTICES; PARTITION; PHASE STABILITY; POROUS MATERIALS; SPINELS; STRAINS; STRESSES; TEMPERATURE DEPENDENCE; THERMAL EXPANSION
Descriptors DEC
COHERENT SCATTERING; CRYSTAL LATTICES; CRYSTAL STRUCTURE; DIFFRACTION; EXPANSION; MATERIALS; MINERALS; OXIDE MINERALS; SCATTERING; STABILITY

Optional Information

Copyright
Copyright (c) 2012 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.