槽波物理模拟点接触低频窄脉冲超声换能器研制

Development of a point-contact low-frequency narrow-pulse ultrasonic transducer for in-seam wave physical simulation

  • 摘要: 超声换能器是槽波三维地震物理模拟数据采集系统中最关键的部件,其性能决定物理模拟是否成功。目前,常规地震物理模拟采用圆柱形换能器,直径1 cm左右,但对于槽波物理模拟固体采集来说直径太大,不能满足多种煤厚的槽波物理模拟数据采集需求。采用压电陶瓷方柱体轴向伸缩振动模式、阶梯型压电晶体结构+背衬层的整体思路,利用COMSOL Multiphysics开展了阶梯型方柱体压电晶体模态的有限元仿真分析,优化结构设计,增大辐射能量/接收灵敏度,实现换能器与模型点接触且不需要耦合剂;开展背衬层材料配比实验,配比了固体粉末+乙烯−醋酸乙烯共聚物混合物作为背衬层吸收余振,实现灵敏度损失较小情况下的窄脉冲,拓宽换能器带宽。研制出的大功率低频、点状、窄脉冲、干耦合超声换能器,主频32 kHz、频宽约20 kHz(−3 dB,23~43 kHz),前端尺寸2 mm。分别采用研制的点接触超声换能器与常规圆柱形超声换能器作为震源在物理模型上进行反射、透射观测系统数据采集、波场特征分析,结果发现研制的点接触超声换能器在能量方面优于圆柱形超声换能器,其信号衰减小、信噪比高,但其由于换能器高频截止频率为43 kHz,高频信号无法接收;圆柱形超声换能器能量小但频带宽,可接收高频槽波信号;在进行槽波三维地震物理模拟时可根据模型大小、煤层厚度等因素进行最优选择。

     

    Abstract: The ultrasonic transducer is recognized as the most critical component in the in-seam wave 3D seismic physical modeling data acquisition system, with its performance determining the success of physical simulations. Conventional seismic physical modeling currently employs cylindrical transducers with diameters around 1 cm, which are deemed unsuitable for solid data acquisition in in-seam wave physical modeling due to their excessive dimensions, thereby limiting applications across varying coal seam thicknesses. A novel design approach is introduced, incorporating the axial expansion-contraction vibration mode of a piezoelectric ceramic square column and a stepped piezoelectric crystal structure combined with a backing layer. Finite element simulations are conducted using COMSOL Multiphysics to analyze the modal characteristics of the stepped square-column piezoelectric crystal, with structural optimization implemented to enhance radiated energy and reception sensitivity. This design enables point contact between the transducer and the model, eliminating the need for coupling agents. Backing layer material formulations are experimentally developed, utilizing a mixture of solid powder and ethylene-vinyl acetate co-polymer to absorb residual vibrations. Consequently, narrow pulses are achieved with minimal sensitivity loss, and the transducer’s bandwidth is effectively broadened. The developed high-power, low-frequency, point-contact, narrow-pulse, dry-coupled ultrasonic transducer exhibits a dominant frequency of 32 kHz, a bandwidth of approximately 20 kHz (−3 dB from 23 kHz to 43 kHz), and a front-end dimension of 2 mm. Comparative evaluations are performed using both the developed point-contact transducer and conventional cylindrical transducers as seismic sources in physical model reflection/transmission observations. Results indicate that the point-contact transducer demonstrates superior energy characteristics, evidenced by reduced signal attenuation and improved signal-to-noise ratios. However, its high-frequency cutoff frequency of 43 kHz precludes the reception of high-frequency signals. Conversely, the cylindrical transducer, while exhibiting lower energy output, provides broader frequency coverage capable of capturing high-frequency in-seam wave components. Transducer selection for in-seam wave three-dimensional seismic physical modeling is recommended based on factors such as model dimensions and coal seam thickness.

     

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