1) matrix stress
基岩应力;基体应力
2) matrix stress
基体应力
1.
The mean matrix stress from the thermal misfit between NiTi matrix and β Nb particle is too small to induce disloca.
应用修正的Eshelby方法计算了NiTiNb基记忆合金的热失配应力场,结果表明在含有βNb粒子的合金中,NiTi基体应力场呈各向同性,在[111]B2方向没有优先拉应力存在,而热失配应力太小又不能诱发位错的形成,因此在含有βNb粒子的NiTiNb基记忆合金中R相变难以发生。
4) rockmass stress
岩体应力
1.
This paper describes the fundamental theory Of controlled fracturing technique forrockmass stress measurement,the equipment employed and the test procedure,Some resultsobtained from modelling experiment of controlled fracturing and their analysis are presented,Thevalidity of controlled fracturing theory is proved.
本文阐明了控制致裂岩体应力量测的基本原理、试验方法。
5) rock stress
岩体应力
1.
To search a simple low cost method of rock stresses measurement, a improved parallel boreholes method of rock stress determination with use of controlled fracturing technique is proposed.
为了寻求一种操作简单、低成本的岩体应力测试方法，本文提出了一个依据控制致裂钻孔应力变化的量测推算原岩应力的改进平行钻孔法。
6) horizontal matrix stress
基岩水平应力
补充资料：轧辊残余应力(见轧辊应力)
轧辊残余应力(见轧辊应力)
residual stresses in roll
zhagun eanyu yingli轧辊残余应力(residual stresses in roll)见礼辐应力。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条