Relationship between austenite dislocation density introduced during thermal cycling and Ms temperature in an Fe-17 Wt Pct Mn alloy

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Abstract

The reason why thermal cycling decreases the martensite start (Ms) temperature of an Fe-17 wt pct Mn alloy was quantitatively investigated, based on the nucleation model of ε martensite and a thermodynamic model for a martensitie transformation. The Ms temperature decreased by about 22 K after nine cycles between 303 and 573 K, due to the increase in shear-strata energy (ΔGsh) required to advance the transformation dislocations through dislocation forests formed in austenite during thermal cycling. The ΔGsh value increased from 19.3 to 28.8 MJ/m3 due to the increase in austenite dislocation density from 1.5 × 1012 to 3.8 × 1013/m2 with the number of thermal cycles (in this case, up to nine cycles). The austenite dislocation density increased rapidly for up to five thermal cycles and then increased gradually with further thermal cycles, showing a good agreement with the increase in austenite hardness with the number of thermal cycles.

Original languageEnglish
Pages (from-to)1913-1917
Number of pages5
JournalMetallurgical and Materials Transactions A: Physical Metallurgy and Materials Science
Volume33
Issue number7
DOIs
Publication statusPublished - 2002 Jan 1

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Thermal cycling
austenite
martensite
Martensite
Austenite
cycles
Temperature
temperature
Nucleation
Hardness
Thermodynamics
Hot Temperature
strata
hardness
nucleation
shear
thermodynamics

All Science Journal Classification (ASJC) codes

  • Condensed Matter Physics
  • Mechanics of Materials
  • Metals and Alloys

Cite this

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abstract = "The reason why thermal cycling decreases the martensite start (Ms) temperature of an Fe-17 wt pct Mn alloy was quantitatively investigated, based on the nucleation model of ε martensite and a thermodynamic model for a martensitie transformation. The Ms temperature decreased by about 22 K after nine cycles between 303 and 573 K, due to the increase in shear-strata energy (ΔGsh) required to advance the transformation dislocations through dislocation forests formed in austenite during thermal cycling. The ΔGsh value increased from 19.3 to 28.8 MJ/m3 due to the increase in austenite dislocation density from 1.5 × 1012 to 3.8 × 1013/m2 with the number of thermal cycles (in this case, up to nine cycles). The austenite dislocation density increased rapidly for up to five thermal cycles and then increased gradually with further thermal cycles, showing a good agreement with the increase in austenite hardness with the number of thermal cycles.",
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N2 - The reason why thermal cycling decreases the martensite start (Ms) temperature of an Fe-17 wt pct Mn alloy was quantitatively investigated, based on the nucleation model of ε martensite and a thermodynamic model for a martensitie transformation. The Ms temperature decreased by about 22 K after nine cycles between 303 and 573 K, due to the increase in shear-strata energy (ΔGsh) required to advance the transformation dislocations through dislocation forests formed in austenite during thermal cycling. The ΔGsh value increased from 19.3 to 28.8 MJ/m3 due to the increase in austenite dislocation density from 1.5 × 1012 to 3.8 × 1013/m2 with the number of thermal cycles (in this case, up to nine cycles). The austenite dislocation density increased rapidly for up to five thermal cycles and then increased gradually with further thermal cycles, showing a good agreement with the increase in austenite hardness with the number of thermal cycles.

AB - The reason why thermal cycling decreases the martensite start (Ms) temperature of an Fe-17 wt pct Mn alloy was quantitatively investigated, based on the nucleation model of ε martensite and a thermodynamic model for a martensitie transformation. The Ms temperature decreased by about 22 K after nine cycles between 303 and 573 K, due to the increase in shear-strata energy (ΔGsh) required to advance the transformation dislocations through dislocation forests formed in austenite during thermal cycling. The ΔGsh value increased from 19.3 to 28.8 MJ/m3 due to the increase in austenite dislocation density from 1.5 × 1012 to 3.8 × 1013/m2 with the number of thermal cycles (in this case, up to nine cycles). The austenite dislocation density increased rapidly for up to five thermal cycles and then increased gradually with further thermal cycles, showing a good agreement with the increase in austenite hardness with the number of thermal cycles.

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