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首页> 外文期刊>Acta Geotechnica: An International journal for Geoengineering >Stability and tightness evaluation of bedded rock salt formations for underground gas/oil storage
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Stability and tightness evaluation of bedded rock salt formations for underground gas/oil storage

机译:地下储气/储油层状岩盐岩层的稳定性和气密性评估

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The presence of interfaces has a critical influence on the stability and tightness of underground gas/oil storages. In China, these energy storages are constructed mainly in bedded salt formations and are widely distributed. Therefore, it is necessary to study the sedimentary rhythm and mechanical characteristics of the interfaces between beds. The petrologic study of core samples from exploratory wells in Yunying Salt Mine, Hubei Provence, China, reveals a sedimentary rhythm and multiple interfaces of bedded salt formations: (1) Mudstone-anhydrite- glauberite-Glauber's salt-salt rock-mudstone are periodically deposited in sequences. Chemical deposition, the predominant formation mechanism, and mechanical deposition appear alternately and result in the formation of sedimentary multicycles; (2) depending on whether a certain component of the rhythm is lacking or not, interfaces are divided into sequential depositional interfaces and intermittent depositional interfaces. Depending on the deposition frequency, interfaces can also be classified into dominant interfaces and secondary interfaces. Depending on whether the mineral composition changes gradually or abruptly, interfaces can be divided into gradual transition interfaces and discrete discontinuous interfaces. Based on the classification of the interfaces together with scanning electron microscope analyses, the cementation state and strength of the interfaces are discussed. Both field investigations and laboratory tests show that the strengths of the chemical deposition interfaces are higher than those of the mechanical deposition interfaces. Specifically, interfaces of mudstone and rock salt are mostly weak. Taking into account the presence of weak interfaces, the strength of interbedded salt formations around caverns can be represented by a U-shaped lower-bound strength envelope curve, which means that shear failure may occur more easily at the haunches of the cavern. Therefore, when setting the range of the internal operating pressures, more attention should be paid to the shear strength of the weak interlayers and weak interfaces, in particular those at the haunches of the cavern, to ensure the stability and tightness of underground gas/oil stores.
机译:界面的存在对地下储气库/储油库的稳定性和密闭性具有至关重要的影响。在中国,这些储能库主要以层状盐岩构造,分布广泛。因此,有必要研究层间界面的沉积节奏和力学特征。对来自中国湖北普罗旺斯云英盐矿勘探井的岩心样品的岩石学研究表明,沉积节奏和层状盐形成的多个界面:(1)定期沉积泥岩-硬石膏-钙芒硝-Glauber盐-盐岩-泥岩按顺序。化学沉积,主要的形成机理和机械沉积交替出现,并导致形成沉积多环。 (2)根据是否缺少节律的某种成分,将界面分为连续的沉积界面和间歇的沉积界面。根据沉积频率,界面也可以分为主要界面和次要界面。根据矿物成分是逐渐变化还是突然变化,界面可以分为渐进过渡界面和离散不连续界面。在对界面的分类和扫描电镜分析的基础上,讨论了界面的胶结状态和强度。现场调查和实验室测试均表明,化学沉积界面的强度高于机械沉积界面的强度。具体而言,泥岩和岩盐的界面大多较弱。考虑到存在弱的界面,洞穴周围的层状盐形成的强度可以用U形下界强度包络线表示,这意味着剪切破坏可能更容易发生在洞穴的直角处。因此,在设定内部工作压力范围时,应特别注意薄弱夹层和薄弱界面的剪切强度,特别是在岩洞斜角处的剪切强度,以确保地下气/油的稳定性和气密性。商店。

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