In view of the insufficient recognition of the failure mechanism of submarine clayey slope induced by gas hydrate dissociation, the effect of gas on submarine slope after gas hydrate dissociation was simulated by means of venting. Furthermore, multiple of experiments were carried out under different combinations of soil strength, embedment depth of gas hydrate, flow rate and dissociation zone. Combining with the image processing, the deformation and the evolutionary process of slope surface and slope body were deeply investigated. The deformation and failure characteristics of submarine clayey slope induced by hydrate dissociation were initially revealed. On this basis, a limit equilibrium method was used to establish the critical pressure analytic expression of submarine slope failure, which is theoretically explained the critical pressure value in the failure process of slope deformation. The results show that the deformation and failure processes of the submarine slope are divided into four stages: the accumulation of air pressure, the elastic compression of soil, the upheaval failure of slope, and the deformation stability of slope. Although, there is a deviation between the calculated and experimental results of gas critical pressure, it can reflect the true level of the critical pressure to some extent. The research results can provide some references for the further understanding of the deformation and failure mechanism of submarine clayey slope induced by gas hydrate dissociation, and the developments of the stability analysis theory and evaluation method.
[1]SLOAN E D. Physical/chemical properties of gas hydrates and application to world margin stability and climatic change[J]. Geological Society, London, Special Publications, 1998, 137(1): 31-50.
[2]KVENVOLDEN K A. Gas hydrates: Geological perspective and global change[J]. Reviews of Geophy-sics, 1993, 31(2): 173-187.
[3]HOVLAND M, GUDMESTAD O T. Potential influence of gas hydrates on seabed installations[M]//PAULL C K, DILLON W P. Natural gas hydrates: Occurrence, distribution, and detection. Washington, USA: American Geophysical Union, 2001: 307-315.
[4]LI A, DAVIES R J, YANG J X. Gas trapped below hydrate as a primer for submarine slope failures[J]. Marine Geology, 2016, 380: 264-271.
[5]ELGER J, BERNDT C, RPKE L, et al. Submarine slope failures due to pipe structure formation[J]. Nature Communications, 2018, 9: 715.
[6]LU X B, CHEN X D, LU L, et al. Numerical simulation on the marine landslide due to gas hydrate dissociation[J]. Environmental Earth Sciences, 2017, 76(4): 172.
[7]HANDWERGER A L, REMPEL A W, SKARBEK R M. Submarine landslides triggered by destabilization of high-saturation hydrate anomalies[J]. Geochemistry, Geophysics, Geosystems, 2017, 18(7): 2429-2445.
[8]LI C L, WU S G, ZHU Z Y, et al. The assessment of submarine slope instability in Baiyun Sag using gray clustering method[J]. Natural Hazards, 2014, 74(2): 1179-1190.
[9]AKAKI T, KIMOTO S, OKA F. Dynamic analysis of hydrate-bearing seabed sediments considering methane gas production induced by depressurization[J]. Japanese Geotechnical Society Special Publication, 2016, 2(18): 676-680.
[10]MORIDIS G J, COLLETT T S, BOSWELL R, et al. Gas hydrates as a potential energy source: State of knowledge and challenges[M]//LEE J W. Advanced Biofuels and Bioproducts. New York, USA: Springer, 2013: 977-1033.
[11]KLAR A, SOGA K, NG M Y A. Coupled deformation-flow analysis for methane hydrate extraction[J]. Géotechnique, 2010, 60(10): 765-776.
[12]ZHANG X H, LU X B, SHI Y H, et al. Centrifuge experimental study on instability of seabed stratum caused by gas hydrate dissociation[J]. Ocean Engineering, 2015, 105: 1-9.
[13]ZHANG X H, LU X B. Initiation and expansion of layered fracture in sediments due to thermal-induced hydrate dissociation[J]. Journal of Petroleum Science and Engineering, 2015, 133: 881-888.
[14]ZHANG X H, LU X B, CHEN X D, et al. Mechanism of soil stratum instability induced by hydrate dissociation[J]. Ocean Engineering, 2016, 122: 74-83.
[15]YANG S L, CHOI J C, VANNESTE M, et al. Effects of gas hydrates dissociation on clays and submarine slope stability[J]. Bulletin of Engineering Geology and the Environment, 2018, 77(3): 941-952.
[16]KWON T H, OH T M, CHOO Y W, et al. Geo-mechanical and thermal responses of hydrate-bearing sediments subjected to thermal stimulation: Physical modeling using a geotechnical centrifuge[J]. Energy & Fuels, 2013, 27(8): 4507-4522.
[17]ZHANG J H, LIN H L, WANG K Z. Centrifuge modeling and analysis of submarine landslides triggered by elevated pore pressure[J]. Ocean Engineering, 2015, 109: 419-429.
[18]BARRY M A, BOUDREAU B P, JOHNSON B D. Gas domes in soft cohesive sediments[J]. Geology, 2012, 40(4): 379-382.
[19]魏伟, 陈旭东, 鲁晓兵, 等. 水合物分解气体泄漏引起的海床破坏实验研究[J]. 力学与实践, 2013, 35(5): 30-34.
WEI Wei, CHEN Xudong, LU Xiaobing, et al. Experimental study of the sea floor damage due to gas escape in hydrate dissociation[J]. Mechanics in Engineering, 2013, 35(5): 30-34.
[20]栾锡武, 孙钿奇, 彭学超. 南海北部陆架南北卫浅滩的成因及油气地质意义[J]. 地质学报, 2012, 86(4): 626-640.
LUAN Xiwu, SUN Dianqi, PENG Xuechao. Genesis of the Nanbeiwei shoal on the shelf of the northern South China Sea and its petroliferous significance[J]. Acta Geologica Sinica, 2012, 86(4): 626-640.
[21]HYMAN D, BURSIK M. Deformation of volcanic materials by pore pressurization: Analog experiments with simplified geometry[J]. Bulletin of Volcanology, 2018, 80(3): 19.
[22]ZHENG R Y, LI S X, LI Q P, et al. Using similarity theory to design natural gas hydrate experimental model[J]. Journal of Natural Gas Science and Engineering, 2015, 22: 421-427.
[23]GALLAND O, GISLER G R, HAUG T. Morphology and dynamics of explosive vents through cohesive rock formations[J]. Journal of Geophysical Research: Solid Earth, 2014, 119(6): 4708-4728.
[24]WEIJERMARS R, SCHMELING H. Scaling of Newtonian and non-Newtonian fluid dynamics without inertia for quantitative modelling of rock flow due to gravity (including the concept of rheological similarity) [J]. Physics of the Earthand Planetary Interiors, 1986, 43(4): 316-330.
[25]YUAN Q, SUN C Y, WANG X H, et al. Experimental study of gas production from hydrate dissociation with continuous injection mode using a three-dimensional quiescent reactor[J]. Fuel, 2013, 106: 417-424.
[26]万义钊, 吴能友, 胡高伟, 等. 南海神狐海域天然气水合物降压开采过程中储层的稳定性[J]. 天然气工业, 2018, 38(4): 117-128.
WAN Yizhao, WU Nengyou, HU Gaowei, et al. Reservoir stability in the process of natural gas hydrate production by depressurization in the Shenhu area of the South China Sea[J]. Natural Gas Industry, 2018, 38(4): 117-128.
[27]朱超祁, 贾永刚, 张民生, 等. 南海北部陆坡表层沉积物强度特征研究[J]. 工程地质学报, 2016, 24(5): 863-870.
ZHU Chaoqi, JIA Yonggang, ZHANG Minsheng, et al. Surface sediment strength in bed-slope of northern South China Sea[J]. Journal of Engineering Geo-logy, 2016, 24(5): 863-870.
[28]HE Y, ZHONG G F, WANG L L, et al. Characteristics and occurrence of submarine canyon-associated landslides in the middle of the northern continental slope, South China Sea[J]. Marine and Petroleum Geology, 2014, 57: 546-560.