摘要
把概率论方法与Logistic方程结合起来,采用随机变量(X)分布的统计参量:即变异系数Cv、偏态系数γ1、峰态系数2γ、信息熵H(X)和h*量值以及分数维维数D0*和D1*等参量,探讨了定量描述"密集—平静"不均匀分布现象和判断系统处于平衡状态和非平衡状态的方法。研究认为:地震活动性异常的实质是X的概率分布由单峰型(平衡状态)转为双峰型或多峰型(非平衡状态)分布,可以由上述参量尤其是γ2和h*量值的综合分析来区分。对于"密集—平静"的前震序列和强余震发生前的序列,这种转变可以由"时间分支行为"来解释;并且提出了根据有震(X≥1)和无震(X=0)两种定态的时段之比,来判断前震序列的一种简易方法。中国大陆M≥7.0地震年频度分布存在双峰型分布特征,可能说明中国大陆M≥7.0地震活动处于远离力学平衡状态。一个大地震在其发生演化过程中,地震活动及前兆现象经历了从弹性应变积累阶段的无序状态(表现为单峰型的泊松过程)到非弹性应变中期阶段的有序状态(有序的自组织结构,表现为双峰或多峰型),再到短临阶段的无序状态。这时出现各种异常现象的同步变化被显著破坏为特征的混沌状态,系统不可逆转地被推向失稳状态;触发因素在这时起重要作用,将引发大地震发生,使系统进入应变能大释放和长期衰减的新状态,而后开始新一轮孕育过程。对于地震及其前兆所具有的这种现象,似乎不可能在纯力学的基础上探索研究,而应该视为在远离平衡条件下非线性动力学体系一般性问题的组成部分。这种认识本身的深化可能就是地震预报研究领域一个重要的突破点。
Combining the probability theory method with the Logistic equation, we explored methods trying to describe the swarm-equanimity phenomenon quantitatively and judge the system in equilibrium state or not by some statistical parameters of variant (X) distribution, i.e. the variation coefficient Cv, skewness coefficient y1, kurtosis coefficient y2, the information entropy H(X) and h" quantity value and fractal dimension Do , D1^*. It is believed that the substance of the earthquake activity anomaly is actually the statistical distribution of X transforming from single-peak distribution (equanimity state) to twoor more-peak distribution (non-equanimity state) which can be distinguished by integrat- edly analyzing the above described statistical parameters, especially the y2 and h^*. The transformation for fore earthquake sequence and ex-sequence of strong aftershock can be explained by "time branch behavior". We propose a simple method to estimate fore earthquake sequence type by the ratio of time period with earthquake (X≥1) to that without earthquake(X=0). The two-peak distribution characteristics of yearly frequency for M≥ 7.0 earthquake in China's Mainland may show that M≥7.0 earthquakes activity in the area is far from equanimity state. In the period of a strong earthquake evolvement, the seismic activity and precursor phenomenon undergo from disordered state at elastic strain accumulation step(shows single-peak Poison procedure) to ordered state at mid-term of non-elastic strain accumulation step( self-organize structure order, shows two or more peak distribu- tion), and then to disordered state at imminent step. At this step, the chaos appears which is characterized by that synchronal anomalies are being disrupted obviously, and the system is inevitable falling into unstable state. Trigger factor is very important at this time and would cause strong earthquake occurrence, which makes the system release strain en- ergy largely and long term attenuation. After that, it begins a new run for seismogenic period. The phenomenon of earthquake activity and its precursor seems impossible to study based on pure mechanics theory, it should be thought as a compositional part of non-linear geodynamics system that is far away from equilibrium state. The effort to deepen this cognition maybe is a breakthrough in earthquake prediction realm.
出处
《地震》
CSCD
北大核心
2007年第4期1-17,共17页
Earthquake
基金
国家自然科学基金项目(4050400)
关键词
“密集-平静”
概率分布质变
单峰型
多峰型
混沌
判断方法
"Swarm-Equanimity"
Quantitative change of the probability distribution
Single-peak type
Multi-peak type
Chaos
Judging method