Abstract

The natural gas hydrate (NGH) reservoir in China is mainly distributed in the continental shelf with water depths ranging from 600–1500 m, about 90% of which is stored in the shallow area of the deep sea, with weak cementation and non-diagenetic characteristics. In order to test and study this type of NGH, samples must be prepared in situ, in large quantities, and at fast speed. At present, there are problems with the common stirring, spraying, and bubbling preparation techniques available, such as slow generation rate, low gas storage density, and lack of rapid preparation. Therefore, the rapid preparation of large samples of non-diagenetic natural gas hydrate has received extensive attention at home and abroad. In view of this technical bottleneck, Southwest Petroleum University innovatively established a rapid preparation kettle of 1062 L. In this paper, the preparation experiment of natural gas hydrate in the South China Sea (the pressure of the preparation kettle was reduced from 7 MPa to 3.3 MPa) was carried out in the preparation method of the ‘three-in-one’ (stirring method, spraying method, bubbling method) and experimental test method. In the process of preparation of non-diagenetic gas hydrate, the data of dynamic image, temperature, pressure, electrical resistivity, and reaction time are tested. During the preparation of natural gas hydrate, temperature, pressure, and electrical resistivity curves in four preparation methods were made, respectively. Through the experimental data analysis of different preparation methods of natural gas hydrate, it has been found that the preparation time of natural gas hydrate using the stirring method, the spraying method, and the bubbling method alone require a longer preparation time. However, when the three-in-one method is used to prepare natural gas hydrate, the preparation cycle of natural gas hydrate is obviously shortened. The preparation time of the single method of stirring method, spraying method, and bubbling method is respectively about 5.13, 3.59, and 3.37 times as long as that of three-in-one method. The three-in-one method for preparing natural gas hydrate greatly improves the preparation efficiency, which has a great significance to the scientific and technological progress of experimental research and evaluation methods of natural gas hydrate.

Highlights

  • Natural gas hydrate is one of the most promising potential alternative energy sources after shale gas, coal bed gas, and tight gas

  • A unique marine non-diagenetic natural gas hydrate in situ preparation method and experimental research platform has been formed in China

  • As for the kind of non-diagenetic natural gas hydrate, it has no rock skeleton—the hydrate itself is the rock skeleton instead, and it has the characteristics of weak cementation, instability, easy collapse due to external influence, and disordered decomposition [3]

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Summary

Introduction

Natural gas hydrate (hereinafter referred to as hydrate) is one of the most promising potential alternative energy sources after shale gas, coal bed gas, and tight gas. Hydrate reservoirs in the South China Sea are mainly distributed in argillaceous silt with a depth of less than 220 m below the seafloor. Yang Qunfang et al [17] designed an experimental system for the preparation of natural gas hydrate by spraying, which enhanced the direct contact heat transfer between water in low temperature and natural gas. Tajima et al [19] set multiple helical structures in the middle of the static mixer to divide the cross section into two nearly semicircular channels They found that it can prolong the gas residence time and improve the synthesis rate of hydrate. A comparative experiment was carried out between the preparation of natural gas hydrate by stirring, bubbling, and spraying, and by the ‘three-in-one’ method. A unique marine non-diagenetic natural gas hydrate in situ preparation method and experimental research platform has been formed in China. As for the kind of non-diagenetic natural gas hydrate, it has no rock skeleton—the hydrate itself is the rock skeleton instead, and it has the characteristics of weak cementation, instability, easy collapse due to external influence, and disordered decomposition [3]

Experimental Equipment
Experimental Purpose
Experiment Steps
Equipment testing
Vacuum pumping
Experimental Phenomena and Data Processing
Resistivity
10. Preparation
12. Resistivity
15. Resistivity
Conclusions
Full Text
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