A methodology for the measurement of the interfacial excess of solute at a grain boundary
Creators
Description
Segregation of solutes on grain boundaries is usually quantified by the peak value of the concentration profile measured across the grain boundary. This procedure is inadequate both from the theoretical and from the practical point of view. Instead, we put forward the concept of interfacial excess of solute, as having a thermodynamic background and being of operative efficiency. Our analyses reveal carbon and boron co-segregation at a martensite lath boundary of a Dual Phase steel. - Highlights: • Quantifying the amount of segregation by the peak concentration is not an adequate procedure. • The excess of solute is a proper thermodynamic variable and is of operative efficiency. • Co-segregation of boron and carbon at a martensitic lath boundary suggests an atomic-scale layer of cementite.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.scriptamat.2016.04.005Additional details
Identifiers
- DOI
- 10.1016/j.scriptamat.2016.04.005;
- PII
- S1359-6462(16)30125-7;
Publishing Information
- Journal Title
- Scripta Materialia
- Journal Volume
- 120
- Journal Page Range
- p. 90-93
- ISSN
- 1359-6462
- CODEN
- SCMAF7
INIS
- Country of Publication
- United Kingdom
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 48012791
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- ABUNDANCE; BORON; CARBON; CEMENTITE; CONCENTRATION RATIO; GRAIN BOUNDARIES; INTERFACES; LAYERS; MARTENSITE; MARTENSITIC STEELS; PROBES; SEGREGATION; SOLUTES
- Descriptors DEC
- ALLOYS; CARBIDES; CARBON ADDITIONS; CARBON COMPOUNDS; DIMENSIONLESS NUMBERS; ELEMENTS; INTERMETALLIC COMPOUNDS; IRON ALLOYS; IRON BASE ALLOYS; IRON CARBIDES; IRON COMPOUNDS; MICROSTRUCTURE; NONMETALS; SEMIMETALS; STEELS; TRANSITION ELEMENT ALLOYS; TRANSITION ELEMENT COMPOUNDS
Optional Information
- Copyright
- Copyright (c) 2016 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.