A constitutive model of twin nucleation and deformation twinning in high-Mn austenitic TWIP steels
📄 Viewing lite version
Full site ›
Book Details
Author(s)David Richard Steinmetz
PublisherBooks On Demand
ISBN / ASIN3732253449
ISBN-139783732253449
AvailabilityUsually ships in 24 hours
Sales Rank99,999,999
CategoryScience
MarketplaceUnited States 🇺🇸
Description ▲
In this dissertation, a multiscale dislocation density-based constitutive model for the strain-hardening behavior in twinning-induced plasticity(TWIP) steels is presented. The approach is a physics-based strain rate- and temperature-sensitive model which reflects microstructural investigations of twins and dislocation structures in TWIP steels. One distinct advantage of the approach is that the model parameters, some of which are derived by ab initio predictions, are physics-based and known within an order of magnitude. This allows more complex microstructural information to be included in the model without losing the ability to identify reasonable initial values and bounds for all parameters. Dislocation cells, grain size and twin volume fraction evolution are included. Particular attention is placed on the mechanism by which new deformation twins are nucleated, and a new formulation for the critical twinning stress is presented. Various temperatures were included in the parameter optimization process. Dissipative heating is also considered. The use of physically justified parameters enables the identification of a universal parameter set for the example of an Fe-22wt%Mn-0.6wt%C TWIP steel.
More Books in Science
Impingement Jet Cooling in Gas Turbines (Developments …
View
Hierarchic Electrodynamics and Free Electron Lasers: C…
View
Numerical Combustion: Proceedings of the Third Interna…
View
Laser and Plasma Applications in Materials Science: Fi…
View
GENOME INFORMATICS 2010: GENOME INFORMATICS SERIES VOL…
View
Galaxy Collisions: Forging New Worlds from Cosmic Cras…
View
The Self-Aware Universe: How Consciousness Creates the…
View
Essentials of Geochemistry: .
View