Integrating test device and method for creep failure and ultrasonic response of methane hydrate-bearing sediments

Clarifying the creep behaviors of hydrate-bearing sediment (HBS) under long-term loading is crucial for evaluating reservoir stability during hydrate exploitation. Figuring out a way of characterizing deformation behaviors and their geophysical responses to HBS is the basis for modeling creep behaviors. In this study, we propose a novel device to test time-dependent deformation and the ultrasonic response of HBS under high-pressure and low-temperature. The experimental device consists of a high-pressure chamber, an axial-load control system, a confining pressure system, a pore pressure system, a back-pressure system, and a data collection system. This testing assembly allows temperature regulation and independent control of four pressures, e.g., confining pressure, pore pressure, back pressure, and axial loading. Columned artificial HBS samples, with a diameter of 39 mm and a height of 120 mm, can be synthesized in this device. Afterward, in situ creep experiments can be achieved by applying stable confining pressure and axial load, together with geophysical signals acquisition. During loading, the stress-strain relationships and ultrasonic data can be obtained simultaneously. Through analyzing the stress-strain relationship and ultrasonic data, the macroscopical failure and microcosmical creep deformation law of the samples can be figured out. Preliminary experiments verified the applicability of the device. The method provides some significance for field observation of reservoir failure via geophysical techniques during hydrate exploitation.

Automated summary

In this study, a novel device is proposed to test the time-dependent deformation and ultrasonic response of hydrate-bearing sediment (HBS) under high-pressure and low-temperature conditions. The device allows control of four pressures and analysis of stress-strain relationships and ultrasonic data to determine the macroscopical failure and microcosmical creep deformation law of the samples. Preliminary experiments have verified the applicability of the device. This method is significant for field observation of reservoir failure during hydrate exploitation using geophysical techniques.