An experimental study on microscopic characteristics of gas-bearing sediments under different gas reservoir pressures

被引:2
|
作者
Guo, Zhenqi [1 ,2 ]
Liu, Tao [1 ,2 ,3 ]
Guo, Lei [4 ]
Su, Xiuting [3 ]
Zhang, Yan [5 ]
Li, Sanpeng [1 ]
机构
[1] Ocean Univ China, Shandong Prov Key Lab Marine Environm & Geol Engn, Qingdao 266100, Peoples R China
[2] Ocean Univ China, Coll Environm Sci & Engn, Qingdao 266100, Peoples R China
[3] Pilot Natl Lab Marine Sci & Technol Qingdao, Lab Marine Geol, Qingdao 266237, Peoples R China
[4] Shandong Univ, Inst Marine Sci & Technol, Qingdao 266237, Peoples R China
[5] Ocean Univ China, Coll Marine Geosci, Qingdao 266100, Peoples R China
基金
中国国家自然科学基金;
关键词
micro characteristics; CT scanning; gas content; number and volume of bubbles; gas reservoir pressure; seabed sediments; BEHAVIOR;
D O I
10.1007/s13131-021-1834-y
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Gas-bearing sediments are widely distributed in five continents all over the world. Most of the gases exist in the soil skeleton in the form of discrete large bubbles. The existence of gas-phase may increase or decrease the strength of the soil skeleton. So far, bubbles' structural morphology and evolution characteristics in soil skeleton lack research, and the influence of different gas reservoir pressures on bubbles are still unclear. The micro characteristics of bubbles in the same sediment sample were studied using an industrial CT scanning test system to solve these problems. Using the image processing software, the micro variation characteristics of gas-bearing sediments in gas reservoir pressure change are obtained. The results show that the number and volume of bubbles in different equivalent radius ranges will change regularly under different gas reservoir pressure. With the increase of gas reservoir pressure, the number and volume of tiny bubbles decrease. In contrast, the number and volume of large bubbles increase, and the gas content in different positions increases and occupies a dominant position, driving the reduction of pore water and soil skeleton movement.
引用
收藏
页码:144 / 151
页数:8
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