Crack-arresting compression layers produced by ion implantation
Introduction
Ion implantation is known to produce lattice expansion in a number of ceramic materials which is attributed to injection of ions, production of point defects, structural change, charge accumulation and other factors [1], [2]. Such expansion is constrained by the bulk of a sample, thus resulting in compressive stresses in the implanted layer. The compressive stress is beneficial for suppressing crack propagation in particular in brittle ceramic materials easily fractured under dynamic loading. The efficiency of crack arrest depends on the distribution and magnitude of the implantation-induced compressive stress as well as the tensile stress that causes the crack propagation. The high-energy low-mass ions have a long ion range and thus produce the compressive stress layer relatively deep below the surface. It is expected to be particularly efficient in crack arresting in cases where the applied tensile stress reduces from the surface to the sample interior.
This work aims at investigating the distribution of the implantation-induced compressive stress within the implanted layer using a high resolution Raman probe and analysing its interaction with cracks propagating under thermal shock.The efficiency of the compressive stress barrier in arresting propagating cracks is explored.
Section snippets
Experiment
The () and (0 0 1) faces of sapphire and magnesium oxide single crystals, respectively, are uniformly implanted with 3.0 MeV H+ ions to a fluence of 3.3 × 1017 cm−2 at room temperature. The samples used are ∼10 mm thick with the implanted surface area of ∼15 × 30 mm2. The ion range under these conditions is 50 μm for sapphire and 60 μm for magnesium oxide crystals as determined by SRIM calculations and verified by optical microscopy. Following implantation, the cross sectional planes of sapphire are
Results and discussion
Direct evidence of crack arrest is demonstrated in the optical photographs presented in Fig. 1(a) for MgO and in (b) for sapphire. The photographs are taken from cross sections made perpendicular to the ion implanted faces of the crystals. Both photographs show that the thermal shock-initiated cracks are effectively stopped within the implanted layer. Fig. 1(a) indicates that in the unimplanted region of the MgO crystal, cracks propagate to the depth of ∼360 μm and deeper, while in the adjacent
Conclusion
Compressive stress layers are produced in sapphire and magnesium oxide crystals using 3.0 MeV H+ ion implantation. The layers are observed to represent effective crack-arresting barriers. The implantation-induced compressive stress distribution and its effect on crack closure are considered. The analysis is used to evaluate the range of crack propagation and the efficiency with which cracks are arrested in the implanted magnesium oxide and sapphire crystals subjected thermal shock loading.
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