Effect of the rolling parameters on the structure and mechanical properties of the beryllium sheets
Vestnik Tomskogo gosudarstvennogo universiteta. Matematika i mehanika, no. 4 (2016), pp. 123-132

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In this work, a molding material of three grades was used: grade A (99.95% of beryllium), grade B (99.87% of beryllium), and grade C (99.2% of beryllium). The workpieces, casted in vacuum, initially were extruded at 850$^\circ$С and then swaged. The rolling temperature was 500, 700, and 900$^\circ$С. For all grades, the tensile strength $\sigma$B in flex test increases with a decrease of the rolling temperature. With an increase in the total compression degree from 20 to 90% at the temperature of 900$^\circ$С, the size of subgrains in the beryllium sheets of grade B does not essentially change and remains about 10 $\mu$m. After 30 minutes of the annealing at the temperature 700$^\circ$С the structure of the beryllium sheets of grade A becomes recrystallized with an average grain size of 29 $\mu$m. After recrystallization, the tensile strength $\sigma$B decreases by 15% and the values of the elongation and transverse contraction decrease by two times. The temperature of 850–900$^\circ$С and a single compression up to 30% are the optimum rolling conditions. Thus, the appropriate combination of structural behavior and paste-forming properties can be obtained in material with subgrained structure in conditions of a high deformation temperature and high material purity.
Keywords: beryllium, rolling of beryllium, beryllium sheet, mechanical properties.
Mots-clés : structure
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     title = {Effect of the rolling parameters on the structure and mechanical properties of the beryllium sheets},
     journal = {Vestnik Tomskogo gosudarstvennogo universiteta. Matematika i mehanika},
     pages = {123--132},
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Yu. V. Tuzov; I. I. Papirov. Effect of the rolling parameters on the structure and mechanical properties of the beryllium sheets. Vestnik Tomskogo gosudarstvennogo universiteta. Matematika i mehanika, no. 4 (2016), pp. 123-132. http://geodesic.mathdoc.fr/item/VTGU_2016_4_a10/