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Statistical physics approach to earthquake occurrence and forecasting

机译:统计物理方法用于地震发生和预报

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There is striking evidence that the dynamics of the Earth crust is controlled by a wide variety of mutually dependent mechanisms acting at different spatial and temporal scales. The interplay of these mechanisms produces instabilities in the stress field, leading to abrupt energy releases, i.e., earthquakes. As a consequence, the evolution towards instability before a single event is very difficult to monitor. On the other hand, collective behavior in stress transfer and relaxation within the Earth crust leads to emergent properties described by stable phenomenological laws for a population of many earthquakes in size, time and space domains. This observation has stimulated a statistical mechanics approach to earthquake occurrence, applying ideas and methods as scaling laws, universality, fractal dimension, renormalization group, to characterize the physics of earthquakes. In this review we first present a description of the phenomenological laws of earthquake occurrence which represent the frame of reference for a variety of statistical mechanical models, ranging from the spring-block to more complex fault models. Next, we discuss the problem of seismic forecasting in the general framework of stochastic processes, where seismic occurrence can be described as a branching process implementing space time-energy correlations between earthquakes. In this context we show how correlations originate from dynamical scaling relations between time and energy, able to account for universality and provide a unifying description for the phenomenological power laws. Then we discuss how branching models can be implemented to forecast the temporal evolution of the earthquake occurrence probability and allow to discriminate among different physical mechanisms responsible for earthquake triggering. In particular, the forecasting problem will be presented in a rigorous mathematical framework, discussing the relevance of the processes acting at different temporal scales for different levels of prediction. In this review we also briefly discuss how the statistical mechanics approach can be applied to non-tectonic earthquakes and to other natural stochastic processes, such as volcanic eruptions and solar flares. (C) 2016 Elsevier B.V. All rights reserved.
机译:有惊人的证据表明,地壳的动力学受作用于不同时空尺度的各种相互依赖的机制控制。这些机制的相互作用在应力场中产生不稳定性,导致突然释放能量,即地震。结果,很难监测单个事件发生前向不稳定性的演变。另一方面,地壳内应力传递和松弛中的集体行为会导致出现稳定的现象学定律所描述的突然出现的特性,这些规律对于大小,时域和空间域的许多地震都是如此。这一观察结果激发了对地震发生的统计力学方法,应用了定标定律,普遍性,分形维数,重正态化组等思想和方法来表征地震的物理特征。在这篇综述中,我们首先介绍地震发生的现象学定律,它们代表了从弹簧块到更复杂的断层模型等各种统计力学模型的参考框架。接下来,我们在随机过程的一般框架中讨论地震预报问题,其中地震发生可以描述为实现地震之间时空-能量相关的分支过程。在这种情况下,我们展示了相关性如何源自时间和能量之间的动态比例关系,能够解释普遍性并为现象学幂律提供统一的描述。然后,我们讨论了如何实现分支模型来预测地震发生概率的时间演变并允许区分造成地震触发的不同物理机制。特别是,将在严格的数学框架中提出预测问题,讨论在不同时间尺度上作用的过程对于不同预测水平的相关性。在本文中,我们还将简要讨论如何将统计力学方法应用于非构造地震和其他自然随机过程,例如火山喷发和太阳耀斑。 (C)2016 Elsevier B.V.保留所有权利。

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