Temperature dependence of the impact response of copper: erosion by melting
- 14 November 1982
- journal article
- Published by IOP Publishing in Journal of Physics D: Applied Physics
- Vol. 15 (11) , 2357-2367
- https://doi.org/10.1088/0022-3727/15/11/027
Abstract
Annealed copper targets were impacted by 5 mm diameter hardened steel spheres at a velocity of 130+or-20 m s-1 and at an impingement angle of 20+or-0.5 degrees . Target temperatures were varied over the range 70-1350K. Evidence for melting was found throughout the temperature range. At low temperatures melting was insufficient to produce detectable mass loss and was only found in localised shear bands. At temperatures within 200K of homogeneous melting, mass losses as great as 0.8% of the impacting sphere were measured. In this latter range, evidence of considerable melting was observed in craters, and deposits of copper were found attached to the spheres. The deposits were composed of unusually small crystallites (grain size approximately=10 mu m) and appeared to have been formed by melting followed by rapid quenching.Keywords
This publication has 19 references indexed in Scilit:
- Shadow Moire Contouring Of Impact CratersOptical Engineering, 1982
- An analysis of solid particle erosion mechanismsJournal of Physics D: Applied Physics, 1981
- Adiabatic shear localization and erosion of strong aluminum alloysWear, 1979
- Erosion of a strong aluminum alloyWear, 1979
- Phase transitions under shock-wave loadingReviews of Modern Physics, 1977
- Deformation of metal surfaces by the oblique impact of square platesInternational Journal of Mechanical Sciences, 1977
- The role of adiabatic shear in solid particle erosionWear, 1975
- Particle erosion of ductile metals: A mechanism of material removalWear, 1974
- An electron diffraction and resistivity study of non-crystalline thin films of gold and silverJournal of Non-Crystalline Solids, 1972
- Physical properties of surfaces IV—Polishing, surface flow and the formation of the beilby layerProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1937