摘要
按照震源地震波能量辐射原理,在断层面上任意一点由破裂或滑动而产生的地震波能量ES、地震矩M0及相应的视应力σa都应大于零.在近期研究中发现Poldo等在震源参数反演求取断层面上临界滑动弱化距离Dc所采用的视应力约束方程出现了"视应力取值小于零"的情形,其负值被解释为对地震波辐射能无贡献的耗散能,可合并至破裂能部分.数学上的表述并未影响到反演结果,但从能量守恒观点上讲,这样的表述是不准确的.进一步讲,由此表述所求得的辐射能量ES大于由能量分配原理所得结果.根据能量分配准则,指出出现负值视应力是不合适的,并给出了表述视应力随断层滑移过程变化的替代方法,同时提供了求解临界滑动弱化距离Dc的正确途径.
According to the representation theorem of seismic energy radiation, we know that, at any point on the fault, the instantaneous seismic radiation energy Es, the seismic moment Mo, and the apparent stress σa =μEs/Mo (μ is the shear modulus on the fault plane) should be positive at any time during an earthquake faulting. However, we have noticed that, in recent source parame- ter study in deriving the critical slip-weakening distance, the apparent stress used as a constrained condition on the fault plane could be less than zero, and the negative value was considered as the dissipation energy and incorporated to the fracture energy. Although the mathematical formula in such case has no influence to the final resolution, the source process violates the basic physical law, resulting in the overestimate of radiated seismic energy. In this study, we have proposed an alternative way to take account of the apparent stress expression based on the energy partition principle, and at the same time, we have suggested that an additional constraint including the radiation energy conservation on the fault could add to the inversion for source parameters in order to estimate the critical slip-weakening distance Dc.
出处
《地震学报》
CSCD
北大核心
2009年第1期13-18,共6页
Acta Seismologica Sinica
基金
中国科学院百人计划
国家基金委(40574022)资助项目
关键词
视应力
地震波辐射能
破裂能
临界滑动弱化距离
apparent stress
seismic slip-weakening distance radiation energy
fracture energy
critical