Experimental Investigation of Texture Gradients in Aluminium/Copper Plates Bonded through Explosive Welding Process

Henryk Paul; M. Miszczyk; M. Prażmowski

doi:10.4028/www.scientific.net/MSF.702-703.603

Paper Titles

Abnormal Growth Mechanisms of Goss Grains in Grain-Oriented Electrical Steels
p.585

The Effect of Cold Rolling Direction on the Secondary Recrystallization in Fe-3%Si Steel
p.591

Texture and Microstructure Evolution during Box Annealing of a Non-Oriented-Grain Electrical Steel
p.595

Modeling of the Particles Pinning Effect on Grain Growth
p.599

Experimental Investigation of Texture Gradients in Aluminium/Copper Plates Bonded through Explosive Welding Process
p.603

Facilitated Recrystalization of the Hard-to-Recrystalize Structure in 16% Cr Steel Sheets by one-Pass ECAP Prior to Cold Rolling
p.607

Recrystallization Textures in Aluminum Alloys: Experimental Study and Modelling
p.611

Cellular Automata Simulation of Textural Evolution during Primary Static Recrystallization of IF Steel
p.615

Influence of Nb-Ti Composition on Recrystallization of Ferritic Stainless Steel
p.619

HomeMaterials Science ForumMaterials Science Forum Vols. 702-703Experimental Investigation of Texture Gradients in...

Experimental Investigation of Texture Gradients in Aluminium/Copper Plates Bonded through Explosive Welding Process

Abstract:

In this study, the commercial purity Al/Cu plates were bonded through the explosive welding process. The SEM/EBSD local orientation measurements were conducted to consider the changes in the microstructure and the development of texture gradients for the applied explosive loading. A particular attention was paid to the texture changes across the interface. The detailed local orientation measurements show that the ultra-fine grained layers are formed close to the bonding zone. The layers were characterized by the copper-type rolling texture components. The interface was outlined by a characteristic sharp transition between the two materials. However, in some places, local melted zones were also encountered, mainly in the front slope of the waves.