| Literature DB >> 32249770 |
Tomohito Tsuru1,2,3, Kazuyuki Shimizu4, Masatake Yamaguchi5,6, Mitsuhiro Itakura6, Kenichi Ebihara6, Artenis Bendo7, Kenji Matsuda7, Hiroyuki Toda4.
Abstract
Aluminium alloys are re-evaluated as most feasible way to satisfy the industrial needs of light-weight structural materials. However, unlike conventional structural metals such as iron and titanium, aluminium does not have easily accessible secondary phases, which means that aluminium-based alloys cannot be strengthened by harnessing multiple phases. This leaves age hardening as the only feasible strengthening approach. Highly concentrated precipitates generated by age hardening generally play a dominant role in shaping the mechanical properties of aluminium alloys. In such precipitates, it is commonly believed that the coherent interface between the matrix and precipitate does not contribute to crack initiation and embrittlement. Here, we show that this is not the case. We report an unexpected spontaneous fracture process associated with hydrogen embrittlement. The origin of this quasi-cleavage fracture involves hydrogen partitioning, which we comprehensively investigate through experiment, theory and first-principles calculations. Despite completely coherent interface, we show that the aluminium-precipitate interface is a more preferable trap site than void, dislocation and grain boundary. The cohesivity of the interface deteriorates significantly with increasing occupancy, while hydrogen atoms are stably trapped up to an extremely high occupancy over the possible trap site. Our insights indicate that controlling the hydrogen distribution plays a key role to design further high-strength and high-toughness aluminium alloys.Entities:
Year: 2020 PMID: 32249770 PMCID: PMC7136220 DOI: 10.1038/s41598-020-58834-6
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.379
Figure 1Experimental observation of the fracture surface of an Al-Zn-Mg alloy. (a) Three-dimensional tomographic images of fractured Al-Zn-Mg alloy samples captured by synchrotron X-ray tomography. Two fracture modes – intergranular fracture (IGF) and quasi-cleavage fracture (QCF) – can be observed on the fracture surface. Crack propagation can be also captured by tomographic image on the right, where the image was obrained at ε = 11% (near τUTS). The crack is found to propagate gradually and undulatory along various quasi-cleavage facets at which hydrogen atoms are sufficiently trapped. (b) Low-voltage SEM images of this fracture surface, in which very dense white and black dots correspond to an MgZn2 precipitate and the crater of the precipitate, respectively. (c) EDS mapping of Zn and Mg on the fracture surface, indicating a clear region of precipitate.
Figure 2Schematic image of possible trap sites of hydrogen and their binding energy. (a) Schematic showing various defect structures as trap sites of hydrogen in Al alloys. Atomic models of these defect structures used for DFT calculations, where T-site corresponds tetragonal site. (b) Binding energy per atom between hydrogen and defect structures such as vacancy, edge/screw dislocations, grain boundary, and η-MgZn2 precipitate evaluated by first-principles calculations.
Figure 3Hydrogen partitioning behaviour in Al-Zn-Mg alloys. Theoretically-derived estimates of (a) H occupancy and (b) hydrogen partitioning at various defect sites including all contributions of the binding energy shown in Fig. 2(b) and the trap site density for various sites. Site occupancy and actual concentration were derived based on thermodynamic equilibrium condition and first-principles calculations.
Figure 4Mechanism of spontaneous cleavage induced by hydrogen segregation at the Al–MgZn2 interface. (a) Binding energy per atom and interfacial cohesive energy as a function of occupancy. (b) The most stable configurations of hydrogen at the interface associated with specific occupancies. Spontaneous cleavage occurs when the concentration of hydrogen atom reaches 22.7 H atoms/nm2 according to negative value of the cohesive energy in (a). Additionally, the cleavage surface becomes more stable by forming H2 molecules at the fracture surface while maintaining hydrogen segregation and spontaneous cleavage.