Abstract

To investigate experimentally how ultra-fine bubbles (UFBs) may promote hydrate formation, we examined the formation of propane (C3H8) hydrate from UFB-infused water solution using two preparation methods. In one method, we used C3H8-hydrate dissociated water, and in the other, C3H8-UFB-included water prepared with a generator. In both solutions, the initial conditions had a UFB number density of up to 109 mL−1. This number density decreased by only about a half when stored at room temperature for 2 days, indicating that enough amount of UFBs were stably present at least during the formation experiments. Compared to the case without UFBs, the nucleation probabilities within 50 h were ~1.3 times higher with the UFBs, and the induction times, the time period required for the bulk hydrate formation, were significantly shortened. These results confirmed that UFB-containing water promotes C3H8-hydrate formation. Combined with the UFB-stability experiments, we conclude that a high number density of UFBs in water contributes to the hydrate promoting effect. Also, consistent with previous research, the present study on C3H8 hydrates showed that the promoting effect would occur even in water that had not experienced any hydrate structures. Applying these findings to the debate over the promoting (or “memory”) effect of gas hydrates, we argue that the gas dissolution hypothesis is the more likely explanation for the effect.

Highlights

  • Gas hydrates that exist below the deep sea floor are both an unconventional natural gas resource and a potential source of greenhouse gas

  • Some of the liquid sample used for the hydrate-formation experiment was set aside for analyzing its size distribution of ultra-fine bubble (UFB) by the laser-light scattering (LS) method, the particle tracking analysis (PTA) method, and the freeze-fractured replica observation via transmission electron microscope (FFT) method

  • Consistent with this image, we found that most UFBs are spherical or oval, and that their size distributions had similarities to those observed in other hydrocarbon-gas UFBs (Uchida et al, 2016a,b)

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Summary

Introduction

Gas hydrates that exist below the deep sea floor are both an unconventional natural gas resource and a potential source of greenhouse gas. Gas-hydrate formation can be a nuisance when it starts to plug gas pipelines in cold regions. Such interests have stimulated much research and development on gas hydrates (Kvenvolden, 1988; Sloan, 2004; Sloan and Koh, 2007; Masuda et al, 2016). With the gas pipeline issue, research has focused on suppressing the formation and growth of gas hydrate. As the hydrate form contains gas at relatively high density, gas hydrate is regarded as a promising medium for transporting and storing the gas (Gudmundsson and Borrehaug, 1996; Ida and Kohda, 2004; Horiguchi et al, 2011; Mimachi et al, 2014; Takeya et al, 2018).

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