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1)  strain accumulation and release
应变积累和释放
2)  strain accumulating and releasing
应变积累释放
1.
According to the deficiency of the strain accumulating and releasing curves and the previous models, the strain-accumulating rate of the strain accumulating and releasing model has been deduced based on the G-R relation and the empirical formula between energy release and earthquake magnitude, where the strain-accumulating rate is relative independent of the strain-releasing rate.
针对过去应变积累释放曲线或模型存在的不足,根据GR关系以及能量震级经验关系,推导出一个相对独立的应变积累速率公式。
3)  Strain accumulating and releasing model
应变积累释放模型
4)  accumulated release
累积释放度
5)  release percent
累积释放量
1.
Methods:The collagen burn pellicle of compound sulfadiazine sliver was prepared by initator method,the release percent was determined by paddle method.
3mL ,交联时间为 3h ,交联温度为 37℃ ,恒温 3h时 ,胶原蛋白膜的累积释放量最大。
6)  strain accumulation
应变积累
1.
By use of horizontal velocity data observed by GPS during 2001—2004 and 2004—2007 in the northeastern margin of Qinghai-Tibet block,aided by the negative dislocation model,the characteristics of horizontal crustal movement and the status of strain accumulation of this area are researched and following conclusion are drawn.
利用青藏块体东北缘2001—2004年、2004—2007年GPS水平运动速度场结果,借助负位错模型,研究该区当前的地壳水平运动特征与应变积累状况。
2.
By use of the regional leveling and GPS observations in Sichuan-Yunnan area during 1994-2006,aided by the negative dislocation model for the elastic block boundaries,combining with the total characteristics of deformation cross-fault,the recent status and intensity of strain accumulation of tectonic blocks and their boundary faults in Sichuan-Yunnan area are studied.
利用1994~2006年川滇地区GPS和区域水准观测资料,借助弹性块体边界负位错模型,结合近年来跨断层形变总体特征,研究了川滇地区构造块体及其边界断裂的应变积累状况与强度。
补充资料:应变能释放速率
分子式:
CAS号:

性质:在线性弹性断裂力学中,把裂纹增加单位长度所需的能量。以符号G表示。对于张开型裂纹,通常用G1表示,当G1达某一临界值G1C时,材料断裂。

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