1) apparent stress
视应力
1.
A brief discussion on the relationship between apparent stress and slip-weakening law based on the energy partition criteria
由能量分配原理探讨滑移弱化与视应力的关系
2.
The apparent stress and apparent strain,actual stress and actual strain of skeleton for porous medium are defined.
首先给出了孔隙介质的视应力、视应变、骨架实际应力和骨架实际应变的定义,并在理想孔隙介质的物质模型假定下讨论了理想孔隙介质的本构关系,表明即使孔隙介质的骨架结构满足虎克弹性体本构关系的假定,即假定骨架的实际应力与实际应变之间呈现线性关系,但由于孔隙的存在,孔隙介质的视应力与视应变之间还是呈现非线性,说明应力与变形之间的非线性是孔隙介质的固有特性。
3.
Firstly,we get the average apparent stress and its range of global shallow events and the different types of earthquake by liner regression fitting,and validated the predecessors conclusion that the apparent stress of strike-slip earthquake great than that of dip-slip earthquake.
首先,拟合得到全球浅源地震和不同类型地震平均视应力的大小和范围,验证了前人得到的"走滑型视应力大于倾滑型视应力"的结论;其次,对折合能量和地震矩关系分析得到:正断层型地震的折合能量随着地震矩增大而减小,而对于走滑型和逆冲型地震未得到前人给出的明确结论;对主震视应力和余震视应力的分析比较表明,它们在量值上没有规律性,必须要结合实际的地震事件,才能反映出它们之间大小关系的真正物理内涵,因为不同的主震可能对震源区的应力场有不同的影响——造成震源区应力场的应力集中(障碍体模式),大部分余震的视应力高于主震视应力;或使应力场更加均匀(凹凸体模式),大部分余震视应力低于主震视应力。
2) Apparent stress drop
视应力降
3) apparent stress
视在应力
4) seismic apparent stress
地震视应力
1.
The average seismic apparent stress and its distribution in Chinese mainland are presented by use of data of medium-strong earthquake from 1900 to 2005.
研究表明:利用地震震级计算的中国大陆地震视应力大小与利用数字地震波资料测定结果相差不大,其空间分布基本一致。
5) Average apparent stress
平均视应力
6) apparent stress
地震视应力
1.
Based on different types of data of these events including earthquake sequences, stress drop and seismic moment, we discussed the intensity of apparent stresses of different earthquakes classified into two classes according to earthquake fault characteristics and earthquake types.
0地震的震型、发震断层性质等资料,分不同发震断层性质和不同震型两种情况,比较了不同地震视应力的大小关系。
2.
The authors calculate the apparent stresses of several strong earthquakes, relate the intensity of apparent stresses of the strong earthquakes with the magnitude of the successive earthquakes following the strong earthquakes to seek for the relationship between them, and point out the possibility of applying apparent stresses to seismic tendency prediction after strong earthquakes.
对多次强震的地震视应力进行了计算,将各次强震的地震视应力的高低与强震发生后的后续地震的强度进行联系,探索它们之间的关系,进而提出将地震视应力用于强震震后趋势预测的可能性。
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