水化时间对含人工环隙GMZ膨润土压实水力学行为的影响

H. Luo, W. Ye, Qiong Wang, Li-Bo Xu
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摘要

根据高放废物(HLW)处置库的概念设计,缓冲屏障将由压实的膨润土块建造,这将不可避免地在处置库中产生技术空白(空洞)。在后续的长期运行过程中,随着围岩地下水的渗入,膨润土块体的水化作用将逐渐填补工艺空白。这种水化过程将伴随着缓冲体系的流体力学行为的变化。因此,有必要研究考虑工艺间隙影响的膨润土块体水力学行为的变化过程。本文对具有初始环隙的GMZ膨润土压实试样进行了一系列水化试验。在水化过程中,测量了膨胀压力和水导率的变化。每次试验结束后,测定试样干密度和含水量的分布,并对不同位置的微观结构进行研究。结果表明:在水化过程中,试样的膨胀压力先快速增大后略有减小,而水力导率则随时间不断减小;此外,技术间隙的关闭导致膨润土块体的非均质性,其特征是随着离中心距离的增加,干密度降低,含水量增加。随着水化时间的延长,膨润土块体沿半径可分为压缩区和膨胀区。在压缩区,试样的干密度逐渐增大,总孔隙空隙比和宏观孔隙空隙比减小。在膨胀区,干密度随总孔隙率和不可探测孔隙率的增大而减小。
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Effect of Hydration Time on the Hydro-Mechanical Behavior of Compacted GMZ Bentonite With an Artificial Annular Gap
According to the conceptual design of high-level radioactive waste (HLW) disposal repositories, the buffer barrier will be constructed by compacted bentonite blocks, which will inevitably produce technological gaps (voids) in the repository. During the consequent long-term operation of the repository, the technological gaps will be gradually filled up on hydration of the bentonite blocks with infiltration of underground water from the host rock. This hydration process will be accompanied by variations of the hydro-mechanical behavior of the buffer system. Therefore, it is necessary to study the changing process of the hydro-mechanical behavior of bentonite blocks with consideration of influences of the technological gaps. In the present work, a series of hydration tests were carried out on compacted GMZ bentonite specimens with initial annular gaps. During the hydration, variations of swelling pressure and hydraulic conductivity were measured. After each test, distributions of dry density and water content in the specimen were determined and the microstructure at different positions was investigated. Results show that, the swelling pressure of the specimen increased rapidly first and then decreased slightly during the hydration process, while the hydraulic conductivity kept decreasing with time. Moreover, closure of the technological gaps induced heterogeneity of the bentonite blocks, which was characterized by the decrease of dry density and the increase of water content with increasing distance to the center of the specimen. With the hydration time elapsed, the bentonite blocks could be divided into compression zone and swelling zone along the radius. In the compression zone, the dry density of the specimen gradually increased, with a decrease in the total pore void ratio and the macro-pores void ratio. In the swelling zone, the dry density decreased with an increase of the total pore void ratio and the undetectable pore void ratio.
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