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首页> 外文期刊>Journal of Applied Geophysics >Frequency-dependent near-surface Q factor measurements via a cross-hole survey
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Frequency-dependent near-surface Q factor measurements via a cross-hole survey

机译:通过跨孔测量测量频率相关的近地表Q因子

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We have measured near-surface absorption in a site of Daqing Oilfield, China, by using a cross-hole survey. The near-surface was divided into two layers according to the water table depth, the weathering and sub-weathering layers. The seismic attenuation for each layer was analysed in detail to estimate the quality factor Q and investigate its dependency on frequency. The absorption model was estimated using tomographic absorption inversion without source effect. The inverse Q factor for the weathering layer is much smaller than that for the sub-weathering layer, indicating that absorption decreases when the near-surface is saturated with water. The Q(-1) factors for the two layers vary with frequency in a similar way, increasing with frequency at the low frequency end, reaching its maximum value at a characteristic frequency and then decreasing with increasing frequency. The results closely match theoretical predictions and laboratory measurements and therefore can be treated as reliable evidence of frequency-dependent Q factor. (C) 2015 Elsevier By. All rights reserved.
机译:我们使用跨孔测量法测量了中国大庆油田某地的近地表吸收。根据地下水位深度将近地表分为两层,即风化层和次风化层。详细分析了每一层的地震衰减,以估计品质因数Q并研究其对频率的依赖性。使用断层摄影吸收反演来估算吸收模型,而没有源效应。风化层的反Q因子远小于亚风化层的Q因子,这表明当近表面被水饱和时,吸收会降低。两层的Q(-1)因子以类似的方式随频率变化,在低频端随频率增加,在特征频率处达到最大值,然后随频率增加而减小。结果与理论预测和实验室测量值非常吻合,因此可以将其视为频率相关Q因子的可靠证据。 (C)2015 Elsevier By。版权所有。

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