Origin of the {h 1 1 }&lt;1/h,1,2&gt; Fiber in Single Phase Ferrite Steels

Patricia Gobernado; Roumen H. Petrov; Jaap Moerman; Carla Barbatti; Leo A.I. Kestens

doi:10.4028/www.scientific.net/MSF.715-716.134

Paper Titles

Stored Energy of Goss Grains in Fe-3%Si Steel after Cold Rolling
p.109

Characteristics of Dynamic Recrystallization during Hot Deformation for High Nitrogen Stainless Steels
p.115

Mechanism of Secondary Recrystallization in Grain-Oriented Si Steel
p.122

Directed Growth of Ferrite in Austenite and Kurdjumov-Sachs Orientation Relationship
p.128

Origin of the {h 1 1 }<1/h,1,2> Fiber in Single Phase Ferrite Steels
p.134

Dynamic Recrystallisation during Isothermal Hot Deformation in a Titanium Modified Austenitic Stainless Steel
p.140

Monte-Carlo Simulation of Goss Abnormal Grain Growth in Fe-3%Si Steel by Sub-Boundary Enhanced Solid-State Wetting
p.146

Dynamic Recrystallization in Similar 5182 Al/Al and Dissimilar Al/Fe Friction Stir Spot Welds
p.152

The Effect of Cold Rolling Reduction on Shear Band and Texture Formation in Fe-3%Si Alloy
p.158

HomeMaterials Science ForumMaterials Science Forum Vols. 715-716Origin of the {h 1 1 }<1/h,1,2> Fiber in...

Origin of the {h 1 1 }<1/h,1,2> Fiber in Single Phase Ferrite Steels

Abstract:

In the present work, the oriented nucleation origin of the recrystallized {h11}<1/h,1,2> fibre is characterized. Aiming to investigate the substructural evolution of <110>//RD fibre grains and {001}<110> grains in particular, a detailed microstructure and texture analysis is performed by high resolution orientation scanning microscopy on a cross-rolled sample. The reason to work with cross-rolled material is the increased incidence of rotated cube orientations after cross rolling. The present data have revealed the presence in the deformed substructure of a crystallite volume that has rotated towards the {311}<136> component in the interior of <110>//RD fibre grains as a result of a grain fragmentation process. Preliminary simulations of the deformation texture suggested that the observed orientation fragmentation might be produced by strain localizations of a shear band nature.