The Influence of Impurities and Fabrics on Mechanical Properties of Rock Salt for Underground Storage in Salt Caverns – a Review

IF 1.2 4区 工程技术 Q3 MINING & MINERAL PROCESSING
K. Cyran
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引用次数: 10

Abstract

Salt caverns are used for the storage of natural gas, LPG, oil, hydrogen, and compressed air due to rock salt advantageous mechanical and physical properties, large storage capacity, flexible operations scenario with high withdrawal and injection rates. the shortand long-term mechanical behaviour and properties of rock salt are influenced by mineral content and composition, structural and textural features (fabrics). Mineral composition and fabrics of rock salt result from the sedimentary environment and post sedimentary processes. the impurities in rock salt occur in form of interlayers, laminae and aggregates. the aggregates can be dispersed within the halite grains or at the boundary of halite grains. Mineral content, mineral composition of impurities and their occurrence form as well as halite grain size contribute to the high variability of rock salt mechanical properties. the rock or mineral impurities like claystone, mudstone, anhydrite, carnallite and sylvite are discussed. Moreover, the influence of micro fabrics (in micro-scale) like fluid inclusions or crystals of other minerals on rock salt mechanical performance is described. In this paper the mechanical properties and behaviour of rock salt and their relation to mineral composition and fabrics are summarised and discussed. the empirical determination of impurities and fabrics impact on deformation mechanism of rock salt, qualitative description and formulation of constative models will improve the evaluation and prediction of cavern stability by numerical modelling methods. Moreover, studying these relations may be useful in risk assessment and prediction of cavern storage capacity.
杂质和织物对地下储盐岩盐力学性能的影响
由于岩盐具有优越的机械物理特性,储存量大,作业场景灵活,抽注速率高,可用于天然气、液化石油气、石油、氢气和压缩空气的储存。岩盐的短期和长期力学行为和性质受到矿物含量和组成、结构和质地特征(织物)的影响。岩盐的矿物组成和组构是沉积环境和沉积后作用的结果。岩盐中的杂质以夹层、层状和集合体的形式存在。团聚体可分散在岩盐颗粒内或岩盐颗粒的边界处。矿物含量、杂质的矿物组成及其赋存形式以及岩盐颗粒大小是造成岩盐力学性质高度变异性的原因。讨论了泥岩、泥岩、硬石膏、光卤石、钾盐等岩石或矿物杂质。此外,还描述了流体包裹体或其他矿物晶体等微结构(在微观尺度上)对岩盐力学性能的影响。本文综述和讨论了岩盐的力学性能和行为及其与矿物组成和组构的关系。经验确定杂质和组构对岩盐变形机理的影响,定性描述和本构模型的建立,将改进数值模拟方法对洞室稳定性的评价和预测。研究这些关系对洞室库容的风险评价和预测具有一定的指导意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Archives of Mining Sciences
Archives of Mining Sciences 工程技术-矿业与矿物加工
CiteScore
2.40
自引率
16.70%
发文量
0
审稿时长
20 months
期刊介绍: Archives of Mining Sciences (AMS) is concerned with original research, new developments and case studies in mining sciences and energy, civil engineering and environmental engineering. The journal provides an international forum for the publication of high quality research results in: mining technologies, mineral processing, stability of mine workings, mining machine science, ventilation systems, rock mechanics, termodynamics, underground storage of oil and gas, mining and engineering geology, geotechnical engineering, tunnelling, design and construction of tunnels, design and construction on mining areas, mining geodesy, environmental protection in mining, revitalisation of postindustrial areas. Papers are welcomed on all relevant topics and especially on theoretical developments, analytical methods, numerical methods, rock testing, site investigation, and case studies.
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