地震预报中的跨断层牛顿力测量

Manchao He , Shulin Ren , Zhigang Tao
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引用次数: 3

摘要

地震预测是全球学术界共同面临的科学挑战。这种困境的根源在于缺乏满足地震发生充分必要条件的前兆指标,这可能是地震预报失败的根本原因。基于此,本文提出了基于断层间牛顿力测量的双块地震灾变力学理论。在此理论基础上,结合地震牛顿力监测的实验室物理模型试验,提出了“地震发生的充分必要条件是牛顿力的变化,断层表面牛顿力的突然下降可以作为地震灾害的预测指标”的新理论思路。自主开发了多个设备系统,该技术已成功应用于工程实践。这一概念目前已在小规模双块灾难性事件(如滑坡)中得到证实。根据双块体灾变力学理论,滑坡与地震性质相似,但规模不同。通过对滑坡的现场监测,验证了牛顿力的突然下降可以作为滑坡灾害的预报指标,成功地解决了滑坡的短期预报问题。跨断层牛顿力测量技术和思想的引入,为提高国际地震监测的方法和水平,解决世界一流的地震短期预报科学难题奠定了基础。
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Cross-fault Newton force measurement for Earthquake prediction

Earthquake prediction is a common scientific challenge for academics worldwide. This dilemma originates from the lack of precursory indicators that meet the sufficient and necessary conditions of earthquake occurrence, which may be the root cause of the failure of earthquake prediction. In light of this, a double-block catastrophic mechanics theory for earthquakes based on cross-fault Newton force measurement is proposed herein. Based on this theory and laboratory physical model tests of seismic Newton force monitoring, a new academic thought is envisioned “the sufficient and necessary condition for earthquake occurrence is the change of Newton force, and the sudden drop of Newton force on the fault surface can be used as a predictor of earthquake disaster.” Several equipment systems have been independently developed, and the technology has been successfully applied to engineering practice. This concept has currently been proven in small-scale double-block catastrophic events such as landslides. Based on the double-block catastrophic mechanics theory, landslides and earthquakes have the similar nature but different scales. According to the on-site monitoring of landslides, it is verified that the sudden drop of Newton force can be used as a predictor of landslide disaster which successfully solves the problem of short-term landslide prediction. The introduction of cross-fault Newton force measurement technology and idea has laid a foundation for improving the method and level of international earthquake monitoring and solving the world-class scientific problem of short-term earthquake prediction.

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