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Progresses on velocity dispersion and wave attenuation measurements at seismic frequency

机译:地震频率速度分散和波衰减测量的进展

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A low frequency measurement system has been designed and built at UH rock physics lab. From measured Young's modulus, Poisson ratio, and phase difference, the velocities and attenuation in rock samples can be obtained. Tests'with the system demonstrate it can successfully detect the fluid flow related velocity dispersion and wave attenuation. The random error and system error are evaluated to be within reasonable level. Limited by the strain gage techniques, the absolute values on modulus or velocity obtained from the current system may not be very accurate, in soft rock samples like heavy oil sand. But the attenuation and relative dispersion trend are still trustable.
机译:在UH岩石物理实验室设计和建造了低频测量系统。从测量的杨氏模量,泊松比和相位差,可以获得岩石样品中的速度和衰减。系统证明它可以成功地检测流体流量相关的速度分散和波衰减。随机错误和系统错误被评估为合理的级别。由应变计技术的限制,从当前系统获得的模量或速度的绝对值可能不是非常精确的,在柔软的岩石样本中,如重油砂。但衰减和相对色散趋势仍然可信赖。

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