首页|海底沉积物中气囊产生过程超孔隙水压力变化特征分析

海底沉积物中气囊产生过程超孔隙水压力变化特征分析

扫码查看
在外部因素的作用下,海底沉积物中向上运移的深源气体在浅层粗-细沉积物界面处形成气囊,气囊中的气体逸出将带来一定危害.对气囊进行实时监测,能有效判定其发展规律并预测后续相关灾害发生.本研究利用多点孔隙水压力监测技术,通过数学模拟实验和物理模拟实验两种方式模拟饱和细粒沉积物中气囊的发生和消散过程,重点讨论裂缝产生、气囊形成、气体释放的典型超孔隙水压力变化特征和变化机制.在理论分析的基础上,根据数学模拟和物理模拟实验的结果,将气囊的形成-生长-消散过程分为横向裂缝产生、气囊纵向膨胀、斜/竖向裂缝产生三个阶段,对应的超孔隙水压力时间序列呈"凹"字形.气囊形成始于粗-细沉积物界面处横向裂缝产生,此时超孔隙水压力值迅速衰减;之后气囊纵向腔膨胀发育,超孔隙水压力保持相对稳定;气囊演化末期出现斜/竖向裂缝,超孔隙水压力再次累积与消散.气体释放阶段的超孔隙水压力变化曲线呈锯齿状波动,可根据压力锯齿状波动的差异性区分气体是间歇性释放还是连续性释放.土层经历气体释放过程后,再次注气时超孔隙水压力能够累积的极值降低,这意味着较小的压力就能产生裂缝再次打开气体通道,破坏沉积物使气体逸出.
Analysis of characteristics of excess pore water pressure changes in the process of gasbag formation in marine sediments
Under the action of external factors,the deep gas in seafloor sediments moves upward,which is easy to accumulate at the interface of shallow coarse-fine sediments and form gasbags.When the gas in the gasbag escapes,it will induce a variety of submarine geological disasters and bring harm to hu-man engineering construction.Therefore,real-time monitoring of the formation-growth-dissipation process of gasbags is of great significance for effectively judging its development law and predicting the occurrence of follow-up potential disasters.In this study,the multi-point pore water pressure monito-ring technique was used to simulate and monitor the forming and dissipation of gasbags in saturated fine-grained sediments by mathematical simulation and physical simulation experiments.The variation characteristics and mechanism of typical excess pore water pressure of fracture formation,gasbag for-mation and gas release were discussed in detail.According to the results of mathematical simulation and physical simulation experiments,combined with theoretical analysis,the formation-growth-dissipa-tion process of gasbag was divided into three stages:transverse crack generation,gasbag longitudinal expansion and oblique or vertical crack generation,and its corresponding excess pore water pressure was concave.The formation of gasbag began with the transverse cracks at the interface of coarse and fine sediments,and excess pore water pressure attenuated rapidly.The gasbag showed the expansion of longitudinal cavity,and excess pore water pressure remained almost unchanged;oblique or vertical cracks appeared at the end of the evolution of gasbag,and excess pore water pressure accumulated and dissipated again.The variation curve of excess pore water pressure in gas release stage had obvious saw-tooth fluctuation characteristics,and it could be used to distinguish whether the gas was released intermittently or continuously.The accumulated extreme value of excess pore water pressure could be reduced during gas reinjection,which meant that a lower pressure could create cracks and reopen the gas channel,destroying the sediment and causing the gas to escape.

pore water pressure monitoring technologyexcess pore water pressuregasbagcracksgas migration

雷诗芸、刘慧芳、郭秀军、孙浩、邢程

展开 >

中国海洋大学环境科学与工程学院,山东青岛 266100

山东省海洋环境地质工程重点实验室,山东青岛 266100

孔隙水压力监测 超孔隙水压力 气囊 裂缝 气体运移

国家自然科学基金国家重点研发计划

419772342017YFC037701

2024

海洋湖沼通报
山东海洋湖沼学会

海洋湖沼通报

CSTPCD北大核心
影响因子:0.464
ISSN:1003-6482
年,卷(期):2024.46(2)
  • 29