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Characterization of rotary-percussion drilling as a seismic-while-drilling source

机译:旋转冲击钻井作为地震钻孔源的特征

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This paper focuses on an evaluation of rotary-percussion drilling (RPD) as a seismic source. Two field experiments were conducted to characterize seismic sources from different rocks with different strengths, i.e. weak shale and hard arkose. Characterization of RPD sources consist of spectral analysis and mean power measurements, along with field measurements of the source radiation patterns. Spectral analysis shows that increase of rock strength increases peak frequency and widens bandwidth, which makes harder rock more viable for seismic-while-drilling purposes. Mean power analysis infers higher magnitude of body waves in RPD than in conventional drillings. Within the horizontal plane, the observed P-wave energy radiation pattern partially confirms the theoretical radiation pattern under a single vertical bit vibration. However a horizontal lobe of energy is observed close to orthogonal to the axial bit vibration. From analysis, this lobe is attributed to lateral bit vibration, which is not documented elsewhere during RPD. Within the horizontal plane, the observed radiation pattern of P-waves is generally consistent with a spherically-symmetric distribution of energy. In addition, polarization analysis is conducted on P-waves recorded at surface geophones for understanding the particle motions. P-wave particle motions are predominantly in the vertical direction showing the interference of the free-surface. (C) 2018 Elsevier B.V. All rights reserved.
机译:本文重点介绍旋转打击钻井(RPD)作为地震源的评估。进行了两种田间实验,以表征来自不同强度的不同岩石的地震源,即弱页岩和硬树脂。 RPD源的表征包括光谱分析和平均功率测量,以及源辐射模式的场测量。光谱分析表明,岩石强度的增加会增加峰值频率并扩大带宽,这使得更加可行的岩石对地震钻孔的目的更加可行。平均功率分析在RPD中的较高幅度比传统钻孔更高。在水平平面内,观察到的P波能量辐射图案部分地确认在单个垂直比特振动下的理论辐射图案。然而,观察到与轴向钻头振动接近正交的水平叶。根据分析,该叶片归因于横向位振动,在RPD期间没有记录在其他地方。在水平平面内,观察到的p波的辐射图案通常与能量的球形对称分布一致。此外,在磁性区域在表面地震镜记录的p波上进行偏振分析,以理解粒子运动。 P波粒子运动主要在垂直方向上显示出自由表面的干涉。 (c)2018 Elsevier B.v.保留所有权利。

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