微地震监测的第一性原理
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北京京援伟达技术有限公司

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P631

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应主编 刘少华 邀请写稿


The First Principle of Microseismic Monitoring
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GeoImage LLC

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    摘要:

    任何监测,需先明确目标及其监测特性。微震的两个重要特性是:微小、与破裂以剪切错动机制为主。由此得到的监测特性是:常常几百米外信噪比(S/N)<1,传统定位失效;震源向空间辐射出纵波与横波,且波动振幅与极性随方向变化。此即微地震监测的本质,或第一性原理。据此发现很多人:(1)坚持S/N>1的传统定位,如代价高昂的临近监测、或持续但效果有限地去噪、或束手无策,而未能有效去噪后与残余噪声共存,实施偏移叠加来提取微震信息;(2)使用了偏移叠加,但未(正确地)从3分量记录中,利用剪切错动力偶源产生的远场位移解提取地震波向量,特别是振幅大、衰减慢、传播远的直达横波或旋转波向量SV与SH;(3)未考虑地震波到达时的振幅与极性是来震方向的函数;即,未使用被动或天然地震的震源机制、弹性力学中的应力应变本构关系、以及构造地质学或岩石力学中的Anderson讨论等,指导偏移叠加与地震活动性解释。这些问题明显地存在于很多地面、井中、矿山安全、反演速度模型、以及破坏性地震前的小微震前兆的监测中。本文以向量叠加监测的研发为例,说明如何使用第一性原理解决上述问题;以及为保证微震监测大概率可靠,应遵循众多必要条件。

    Abstract:

    Any monitoring must first clarify the objective and its monitoring characteristics. The two important characteristics of microseismic are: tiny, and rupture with mainly shear dislocation mechanism. The monitoring characteristics obtained by the features are: often the signal-to-noise ratio (S/N) is <1 from a few hundred meters away, and the traditional location fails; One hypocenter radiates longitudinal and transverse waves into space, and the amplitude and polarity of the waves change with different directions. This is the essence or first principle of microseismic monitoring. Based on this, it is found that many people: (1) adhere to the traditional relocation with S/N>1, such as costly proximity monitoring, or continuously but effectively-limited denoising, or helplessness; But cannot coexist with residual noise after effective denoise, extract microseismic information through data migration and stacking (DMS); (2) have used DMS, but the seismic wave vectors are not (correctly) extracted from the 3-C records by using the far-field displacement solution generated by the shear couple source, especially the direct transverse or rotation wave vectors SV and SH with large amplitude, slow attenuation, and long propagation; And (3) The amplitude and polarity of the arrival seismic wave are not considered to be a function of the direction of the incoming earthquake; That is, the focal mechanism of passive or natural earthquakes, the stress-strain constitutive relationship in elastic mechanics, and the Anderson discussion in structural geology or rock mechanics are not used to guide the DMS and explanation of microseismicity. These problems are evident in many detections of surface, well, mine safety, inversion for velocity models, and micro/small earthquake precursors before destructive earthquakes. This paper takes VS (Vector Stacking) R D as example to illustrate how to solve the above problems using the first principle; and in order to ensure reliable microseismic monitoring in the sense of high probability, many necessary conditions should be strictly followed.

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梁北援. 微地震监测的第一性原理[J]. 科学技术与工程, , ():

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  • 收稿日期:2026-02-09
  • 最后修改日期:2026-05-06
  • 录用日期:2026-05-10
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