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微地震震源地震波能量的計算方法

Calculation method for the seismic wave energy of microseismic hypocenters

  • 摘要: 由工程爆破中普遍采用的質點峰值振動速度與炸藥量和震源距關系的經驗公式推導出質點峰值振動速度與震源能量和震源距關系的經驗公式,并作為微震地震波能量衰減公式.在公式中引入地震波能量特征系數K1描述震源能量與震源峰值振動速度之間的比例關系,并認為K1主要與震源場地介質特征有關,而與爆破參數無關.通過校驗炮數據的回歸分析獲取監測區域能量特征系數K1.采用能量衰減模型,以微震事件各測點的峰值振動速度、震源距及K1為已知量,以震源能量及衰減系數為回歸參數進行回歸計算,直接反演出震源能量.本文方法為震源能量計算提供了新的思路和方法.

     

    Abstract: An empirical formula to describe the relation of particle vibration velocity to explosive's quantity and distance from the explosion center is used in the blasting engineering field. Based on this formula, a new empirical equation to characterize the relation of particle vibration velocity to hypocenter energy and distance to the hypocenter is presented in this article, which is considered as the attenuation formula of seismic wave energy. In the new equation, the coefficient of seismic wave energy, K1, is introduced to describe the relationship between hypocenter energy and particle vibration velocity. It is thought that K1 has strong relationship with the locale medium characteristic of the hypocenter, nothing to do with the blasting parameters. According to the energy data of check points, K1 is calculated by regression analysis. By using the energy attenuation model, taking particle vibration velocity, distance to the hypocenter and K1 of each mieroseismic incident as the known parameters, hypocenter energy and attenuation coefficient as the regression parameters, the hypocenter energy can be obtained by inverse calculation. This method provides a new idea to calculate the hypocenter energy.

     

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