Geomechanical responses of sand-clay interbedded gas hydrate-bearing deposits under depressurization-driven gas production at site UBGH2-6 in Ulleung Basin, offshore Korea

被引:2
作者
Sohn, Yongjune [1 ]
Park, Taehyung [2 ]
Kwon, Tae-Hyuk [3 ]
机构
[1] SK E&C, Seoul, South Korea
[2] Korea Atom Energy Res Inst, Disposal Performance Demonstrat Res Div, Daejeon, South Korea
[3] Korea Adv Inst Sci & Technol KAIST, Dept Civil & Environm Engn, Daejeon, South Korea
来源
GAS SCIENCE AND ENGINEERING | 2024年 / 126卷
基金
新加坡国家研究基金会;
关键词
Natural gas hydrate; Hydrate-bearing sediment; Layered reservoir; Interbedded layer; Depressurization; T -H -M model; PRODUCTION-MODEL; METHANE; FLOW; PERMEABILITY; SIMULATION; SEDIMENTS; CONDUCTIVITY; DISSOCIATION; COMPRESSION; PREDICTION;
D O I
10.1016/j.jgsce.2024.205337
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
This study explores geomechanical responses of sand-clay interbedded hydrate reservoirs subjected to depressurization. A thermo-hydro-mechanically (T-H-M) coupled simulation code was created to simulate T-H-M interactions in layered hydrate reservoirs, utilizing an explicit two-way coupling scheme. The code was then used to model a hydrate reservoir analogous to a hydrate deposit system in Ulleung Basin, Offshore Korea (Site UBGH2-6). Hydrate reservoirs comprising thin and interbedded sand-clay layers exhibit unique geomechanical responses due to the localized gas hydrate dissociation along sand-clay layer interfaces. The localized dissociation pattern leads to accelerated sediment consolidations along the layer interfaces. The simulation results also reveal development of shear deformation along the sand-clay interfaces, which implies the layer interfaces may act as the main sources of sand productions and fines migration within a depressurized hydrate reservoir. Additional simulations are conducted to further investigate the effects of depressurization rate and formation wettability on gas productivity. Although faster depressurization speeds up initial gas production, ultimately, the production rate is governed by the final bottom hole pressure, regardless of the depressurization rate. Nonetheless, slower depressurization appears more favorable, given its capacity to mitigate initial geomechanical responses, such as reservoir compaction and sand production, thus preserving the long-term production potential of a hydrate reservoir. On the other hand, a cyclic depressurization scheme also proves to be able to mitigate the level of initial geomechanical responses, but only at the cost of reduced gas productivity. A comparative analysis with varying wettability indicates that water-wet reservoirs may be more favorable target for gas hydrate exploitation than gas-wet reservoirs. The presented results enhance understanding of complex hydrate reservoir dynamics and contribute to advancement of sustainable and efficient hydrate production techniques.
引用
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页数:23
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