Abstract

The initial quantification of data quality is an important step in seismic data acquisition design, including the choice of sensing strategy. The signal-to-noise ratio (SNR) often drives the choice of distributed acoustic sensing (DAS) parameters in vertical seismic profiling (VSP). We compare this established approach for data quality assessment with metrics comparing DAS data products to available well logs. First, we create kinematic and dynamic data products derived from original seismic data, such as the interval velocity and amplitude of P-wave arrivals. Next, we quantify the quality of derived data products using well log data by calculating various statistical metrics. Using a large dataset of 220 different VSP experiments with a fixed source location and various DAS acquisition parameters, such as gauge length (GL), conveyance type, and lead-in length, we analyzed the statistical distribution of various metrics. The results indicate the decoupling between seismic-based and log-based metrics as well as between the quality of dynamic and kinematic data-products for the same record. Therefore, we propose using fit-for-purpose metrics to optimize the acquisition cost. In particular, for ray-based tomographic processing, it is sufficient to use traveltime-based metrics. On the other hand, for advanced dynamic analysis, amplitude-based metrics define the quality of final processing products. Hence, it is crucial to use fit-for-purpose metrics to optimize DAS VSP acquisition.

Highlights

  • Vertical seismic profiling (VSP) is a geophysical method for estimating the elastic properties of subsurface layers using seismic waves generated by a source located at the surface and receivers located in a borehole

  • We have calculated data-based and log-based metrics for 220 distributed acoustic sensing (DAS) vertical seismic profiling (VSP) records acquired into fiber optic cables installed in our test well

  • Data-based signal-to-noise ratio (SNR) metrics calculated in time or frequency domains depend on various hyperparameters

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Summary

Introduction

Vertical seismic profiling (VSP) is a geophysical method for estimating the elastic properties of subsurface layers using seismic waves generated by a source located at the surface and receivers located in a borehole. Spacing between geophones (channel spacing) is usually more than 10 m (for some applications could be less), the length of the array is limited by a few hundred meters, and the tool is typically moved 6–8 times to cover the entire length of the well, which can be logistically difficult. To overcome these limitations, VSP acquisition based on distributed acoustic sensing (DAS) [2,3,4] is emerging as an alternative technology to acquire borehole seismic data. DAS covers all the length of the well with very small (about 1 m, for GL of 10 m) channel spacing [10,11], which prevents spatial aliasing in seismic records and reduces acquisition costs

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