Undrained triaxial compression tests on normally consolidated bentonite considering temperature/confining pressure dependency

IF 6.9 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL
Peng Peng , Xiaohua Bao , Keigo Takagi , Ryuhei Urata , Yonglin Xiong , Feng Zhang
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Abstract

In the geological repository of high-level radioactive wastes (HLRW), one of the most important issues is the stability of artificial barrier basically using bentonite. However, due to the exist gaps between bentonite block and surround rock mass, the bentonite can swell relatively freely, whose constraining condition is quite different from the normal swelling pressure test. As an extreme case, the bentonite may engage completely into the surrounding ground and become a complete normal consolidated state. Therefore, in order to investigate the thermo-mechanical behavior of saturated bentonite at normally consolidated state, a newly proposed static compaction method for preparing specimen of saturated normally consolidated bentonite was proposed first. Then, a series of undrained triaxial compression tests were conducted under different confining pressure and temperature, by which the thermo-mechanical behavior of bentonite, used as an artificial barrier of geological repository of HLRW, is investigated systematically. The tests results reveal that the specimen prepared by the proposed method is confirmed to have sufficient saturation (> 0.92), meanwhile the prepared specimen is at slightly overconsolidated state that roughly equal to a K0-line consolidation. The deformation of the bentonite in undrained triaxial compression tests changes from plastic to brittle as the temperature increases. Simulation based on a sophisticated constitutive model considering water compressibility at high confining pressure was also discussed. The results are useful for assessing the mechanical behavior of bentonite after hundreds years of geological repository of HLRW.
考虑到温度/凝结压力相关性的正常固结膨润土不排水三轴压缩试验
在高放射性废物(HLRW)地质处置库中,最重要的问题之一是基本上使用膨润土的人工屏障的稳定性。然而,由于膨润土块与周围岩体之间存在间隙,膨润土可以相对自由地膨胀,其约束条件与正常膨胀压力试验大不相同。在极端情况下,膨润土可能会完全与周围的地层接合,成为完全正常的固结状态。因此,为了研究饱和膨润土在正常固结状态下的热力学行为,首先提出了一种新的静态压实方法来制备饱和正常固结膨润土试样。然后,在不同的约束压力和温度下进行了一系列不排水三轴压缩试验,系统地研究了作为高放射性废物地质封存库人工屏障的膨润土的热力学行为。试验结果表明,采用拟议方法制备的试样具有足够的饱和度(> 0.92),同时制备的试样处于轻微过固结状态,大致相当于 K0 线固结。随着温度的升高,膨润土在不排水三轴压缩试验中的变形由塑性变为脆性。此外,还讨论了基于复杂构造模型的模拟,该模型考虑了高约束压力下的水可压缩性。这些结果有助于评估高放射性废物地质存放数百年后膨润土的机械行为。
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来源期刊
Engineering Geology
Engineering Geology 地学-地球科学综合
CiteScore
13.70
自引率
12.20%
发文量
327
审稿时长
5.6 months
期刊介绍: Engineering Geology, an international interdisciplinary journal, serves as a bridge between earth sciences and engineering, focusing on geological and geotechnical engineering. It welcomes studies with relevance to engineering, environmental concerns, and safety, catering to engineering geologists with backgrounds in geology or civil/mining engineering. Topics include applied geomorphology, structural geology, geophysics, geochemistry, environmental geology, hydrogeology, land use planning, natural hazards, remote sensing, soil and rock mechanics, and applied geotechnical engineering. The journal provides a platform for research at the intersection of geology and engineering disciplines.
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