Effect of surface area of grain boundaries on stress relaxation behavior in pure copper over wide range of grain sizes
Effect of surface area of grain boundaries on stress relaxation behavior in pure copper over wide range of grain sizes
复制标题
晶界表面积对宽范围晶粒尺寸纯铜应力松弛行为的影响
DOI:
10.1016/j.msea.2020.139585
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发表时间:
2020
期刊:
影响因子:
--
通讯作者:
Suzuki Shinsuke
中科院分区:
文献类型:
--
作者:
Suzuki Yurina;Ueno Kota;Murasawa Kodai;Kusuda Yoshinori;Takamura Masato;Hakoyama Tomoyuki;Hama Takayuki;Suzuki Shinsuke
The objective of this study was to investigate the effect of the surface area of grain boundaries on the stress relaxation behavior over a wide range of grain sizes. Stress relaxation tests were performed using single crystal (SC), coarse grained (CG), and ultra-fine grained (UFG) samples. Additionally, pure copper was used to eliminate the effects of the solid solution and precipitates. The initial stress relaxation behavior was investigated using the stress relaxation rate at 0.2 s after the beginning of strain holding. Furthermore, the internal stress was investigated as the end of the stress relaxation behavior. The stress relaxation rate increased with the surface area of the grain boundaries per unit volume (SV). Although the activation volume of the UFG sample was smaller than that of the CG samples, the stress relaxation rate was higher. This suggested that the grain boundary sliding contributed to the stress reduction of the UFG sample. Therefore, the stress relaxation rate increased withSVeven if grain boundary sliding occurred. The internal stress increased withSV, except for the SC sample. Furthermore, in the CG range, the internal stress could be approximated by the Hall-Petch (H-P) relation with a coefficient almost equal to that of the flow stress. This behavior of internal stress inherently explains the dislocation pile-up model assumed in the H-P relation. The internal stress of the UFG sample decreased below the expected value based on the H-P relation. It is suggested that the depletion of dislocation sources prevented the internal stress from increasing.
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影响因子:
6.2
作者:
M. Z. Butt;M. S. Khiliji
通讯作者:
M. S. Khiliji
DOI:
10.2465/gkk1952.19.141
发表时间:
1990
期刊:
Journal of the Mineralogical Society of Japan
影响因子:
--
作者:
K. Sumino
通讯作者:
K. Sumino
影响因子:
1.2
作者:
T. Okada;Mitsuyoshi Utani;Atsushi Osue;N. Fujii;M. Tagami;F. Inoko
通讯作者:
F. Inoko
DOI:
10.2355/tetsutohagane.99.366
发表时间:
2013
影响因子:
0.3
作者:
M. Kumagai;T. Kikuchi;M. Imafuku;S. Ohya
通讯作者:
S. Ohya
影响因子:
--
作者:
文哉 西嶋;幸矢 野村;千尋 渡邊;亮一 門前
通讯作者:
亮一 門前