Published July 15, 2004 | Version v1
Journal article

Deriving the bulk modulus of a single-phase powder from the March preferred orientation parameter

Description

This study has examined the validity of the March model using extensive suites of uniaxially pressed powders of molybdite and calcite neutron powder diffraction data, for which the compression was systematically varied. It is clear from the various Rietveld refinements that the model becomes increasingly unsatisfactory as the uniaxially applied compaction pressure (and, therefore, the level of preferred orientation) increase. The model has been tested with a physical relationship which links the March r-parameter to the compaction pressure via the powder bulk modulus, B. The agreement between the results obtained from directly measured values of B and from Rietveld analysis with the March model is promising in terms of deducing the powder bulk modulus from the March r-parameter

Additional details

Identifiers

DOI
10.1016/j.physb.2004.03.155;
PII
S0921452604003709;

Publishing Information

Journal Title
Physica. B, Condensed Matter
Journal Volume
350
Journal Issue
1-3
Journal Page Range
p. E577-E580
ISSN
0921-4526
CODEN
PHYBE3

Conference

Title
3. European conference on neutron scattering
Dates
3-6 Sep 2003
Place
Montpellier (France)

INIS

Country of Publication
Netherlands
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
36054412
Subject category
S75: CONDENSED MATTER PHYSICS, SUPERCONDUCTIVITY AND SUPERFLUIDITY;
Resource subtype / Literary indicator
Conference
Descriptors DEI
CALCITE; COMPRESSION; GRAIN ORIENTATION; MECHANICAL PROPERTIES; MOLYBDATES; NEUTRON DIFFRACTION; POWDERS
Descriptors DEC
CARBONATE MINERALS; COHERENT SCATTERING; DIFFRACTION; MICROSTRUCTURE; MINERALS; MOLYBDENUM COMPOUNDS; ORIENTATION; OXYGEN COMPOUNDS; REFRACTORY METAL COMPOUNDS; SCATTERING; TRANSITION ELEMENT COMPOUNDS

Optional Information

Copyright
Copyright (c) 2004 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.