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Ultrasonic Measurements of Seismic Anisotropy in Synthetic Silica Cemented Sandstones with Controlled Fracture Geometry

机译:合成二氧化硅泥浆砂岩抗震各向异性的超声波测量,具有控制骨折几何形状

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We present ultrasonic measurements on two sets of novel synthetic, porous, silica cemented sandstone samples with a controlled fracture geometry. X-Ray CT scanning was used to determine the fracture density of each sample.Asmaller block was cored and measured in the ultrasonic pulse-echo system and the results revealed that shear-wave splitting was 100 times fracture density and independent of pore fluid viscosity for wave propagation at 90° to the fracture normal.Alarger block was ground into an octagonal shape and measured at ambient pressures using a bench-top method. We collected P- and S-wave velocity and attenuation data for five angles relative to the fracture normal. These measurements showed evidence for fluid-dependent shear-wave splitting at 45° to the fracture normal associated with changes in fluid viscosity.
机译:我们在两套新型合成,多孔的二氧化硅粘液砂岩样品上呈现超声波测量,具有受控裂缝几何形状。使用X射线CT扫描来确定每个样品的断裂密度。氨莱块块被芯片并在超声波脉冲回波系统中测量,结果显示剪切波分裂是裂缝密度100倍并与孔隙流体粘度无关将裂缝正常的波形在90°处的波传播被研磨成八边形形状并使用台式方法在环境压力下测量。我们收集了P - 和S波速度和衰减数据,相对于裂缝正常。这些测量显示出在与流体粘度变化相关的裂缝正常的45°处的流体依赖性剪切波分裂的证据。

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