The dependence of precipitate morphology on the grain boundary types in an aged Al–Cu binary alloy

2020 ◽  
Vol 56 (1) ◽  
pp. 781-791
Author(s):  
Ahua Du ◽  
Weiguo Wang ◽  
Xinfu Gu ◽  
Song Chen ◽  
Yunkai Cui ◽  
...  
2018 ◽  
Vol 941 ◽  
pp. 340-345
Author(s):  
Tetsuya Matsunaga ◽  
Maaouia Souissi ◽  
Ryoji Sahara ◽  
Hiromichi Hongo ◽  
Masaaki Tabuchi ◽  
...  

Although welding results in premature failure by type IV fracture under high temperature creep conditions, the alloy design of light elements such as boron addition and nitrogen reduction enhances the creep lifetime of 9Cr heat resistant steel. In particular, the simulated heat affected zone (SHAZ) sample of new 9Cr steel (called TA steel) shows about 10 times longer creep lifetime than that of the standard Gr. 91 steel. The welded TA steel is thus expected to exhibit good creep properties because its SHAZ sample has coarser grains and suppresses type IV fracture. The preservation of base metal’s microstructure after welding results from the precipitate morphology, such as high grain boundary coverage by precipitates and low amount of MX being nucleation sites of ferrite grains during the a-g phase transformation. In addition, the increase of stability of M23C6 affects high pinning pressure toward grain boundary migration upon rapid heating during welding. First-principles calculations confirm the increased stability when boron is absorbed by M23C6. Moreover, the calculations reveals that boron decreases the coherency between matrix and M23C6, suppressing grain coarsening during creep tests in TA steel. It is concluded that the increased microstructural stability during welding and long high temperature exposure generates the elongated creep lifetime in welded TA steel including about 0.01 wt% boron and less than 0.01 wt% nitrogen.


2006 ◽  
Vol 519-521 ◽  
pp. 425-430 ◽  
Author(s):  
Keiyu Nakagawa ◽  
Teruto Kanadani ◽  
Kenich Nakayama ◽  
Akira Sakakibara

In this study, we investigated the effects of a small addition of Cu (0.1%) or Ge (0.1%) on the microstructure and mechanical property of Al-Si alloys. The results are as follows. The size of precipitates in the Cu-added or Ge-added alloys is smaller than that in the binary alloy. The size of the precipitates at the grain boundary in the Cu-added or Ge-added alloys is larger than the size of the precipitates in the binary alloy. However, the number of the precipitates at the grain boundary in the Cu-added and Ge-added alloys is smaller than that in the binary alloy. It was found that a small addition of Cu or Ge has the effect of raising the fatigue strength under repeated tensile loading as well as the tensile strength.


2020 ◽  
Vol 790 ◽  
pp. 139705 ◽  
Author(s):  
Hidetoshi Somekawa ◽  
Daisuke Egusa ◽  
Eiji Abe

In this paper a crystallographic framework and methodology are presented that enable the derivation of the symmetry of any bicrystal comprising a planar interface between two crystals of the same or different form. If the crystals are different the interface is an interphase boundary, and if they are the same the interface is a grain boundary. Special cases of the latter, corresponding to special relative orientations of the adjacent crystals, are domain and inversion boundaries and stacking faults and crystallographic shear faults. All possible symmetry groups for bicrystals are tabulated, and generic relations between the symmetry exhibited by the different types of interfaces are discussed. The crystallographic framework used is that devised by Pond & Bollmann (1979), in which the starting point in the treatment of a given bicrystal is the dichromatic pattern, i. e. the pattern created by the two crystal lattices with one regarded as white and the other black. An additional step has been introduced in order to be able to extend the treatment to bicrystals in which one or both of the crystals are non-symmorphic and/or non-holosymmetric. This additional step is the creation of a dichromatic complex, which is the pattern created by the lattice complexes of the two crystals. The analytical determination of the symmetry of dichromatic patterns and complexes is presented. The symmetry of a particular bicrystal can be obtained from the corresponding dichromatic complex by cross-sectioning. The methodology employed in this treatment of bicrystal symmetry is to use the theory of the symmetry of composites. A composite is regarded here as an entity comprising two components, which may be crystal lattices, as in a dichromatic pattern, or lattice complexes, as in a dichro­matic complex, or crystals, as in a bicrystal. The components of a com­posite may be equivalent or different, corresponding to the investigation of a bicrystal containing a grain or interphase boundary respectively. In the latter case, the symmetry of the composite is given by the intersection of the symmetry of the components, whereas in the former case additional symmetry may be present corresponding to symmetry operations relating the two equivalent components. The existence and disposition of such symmetrizing operations is revealed particularly clearly by using the dichromatic framework. Since one component is considered to be black and the other to be white, symmetrizing operations correspond to antisymmetry (or colour-reversing) operations. The methodology used in this work also elucidates the significance of crystallographically equivalent variants of a composite, and enables the interrelation of variants to be established. Crystallographically equivalent variants arise as a consequence of dissymmetrization, and, in this respect, the idea of regarding a relaxed bicrystal as having been created from a dichromatic pattern by a squence of imaginary steps is most helpful. Each step in the procedure causes dissymmetrization and therefore leads to the existence of variants. Four types of variants arise, and these have been designated orientation, complex, morphological and relaxational variants. Morphological v̇ariants, for example, arise as a result of cross-sectioning a dichromatic complex; the variants correspond to bicrystals having iden­tical symmetry (except possibly for orientation of their elements) and identical orientation of the adjacent crystals but different interfacial planes. The number and mutual disposition of such variants constitute the crystallographic aspect of the symmetry of grain boundary facetting and precipitate morphology for example.


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