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Acoustic Prediction and Risk Evaluation of Shallow Gas in Deep-Water Areas

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Abstract

Shallow gas is a potential risk in deep-water drilling that must not be ignored, as it may cause major safety problems, such as well kicks and blowouts. Thus, the pre-drilling prediction of shallow gas is important. For this reason, this paper conducted deep-water shallow gas acoustic simulation experiments based on the characteristics of deep-water shallow soil properties and the theory of sound wave speed propagation. The results indicate that the propagation speed of sound waves in shallow gas increases with an increase in pressure and decreases with increasing porosity. Pressure and sound wave speed are basically functions of the power exponent. Combined with the theory of sound wave propagation in a saturated medium, this paper establishes a multivariate functional relationship between sound wave speed and formation pressure and porosity. The numerical simulation method is adopted to simulate shallow gas eruptions under different pressure conditions. Shallow gas pressure coefficients that fall within the ranges of 1.0–1.1, 1.1–1.2, and exceeding 1.2 are defined as low-, medium-, and high-risk, respectively, based on actual operations. This risk assessment method has been successfully applied to more than 20 deep-water wells in the South China Sea, with a prediction accuracy of over 90%.

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Acknowledgements

The study is supported by the National Natural Science Foundation Project ‘Research on the Evolution Mechanism of Bearing Capacity of Deep-Water Oil and Gas Well Conduit’ (No. 51774301) and CNOOC Joint Research Project ‘Geotechnical Engineering Parameters Prediction Experiment Based on Acoustic Characteristics of Shallow Layer in the South China Sea’ (No. CCL2020RCPS0120 XNN).

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Correspondence to Gang Tong.

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Yang, J., Wu, S., Tong, G. et al. Acoustic Prediction and Risk Evaluation of Shallow Gas in Deep-Water Areas. J. Ocean Univ. China 21, 1147–1153 (2022). https://doi.org/10.1007/s11802-022-4790-z

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  • DOI: https://doi.org/10.1007/s11802-022-4790-z

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