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Effect of cement solutions on the swelling pressure of compacted GMZ bentonite at different temperatures

机译:水泥溶液对不同温度下压实GMZ膨润土溶胀压力的影响

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Bentonite has been adopted as a buffer/sealing material in most high-level radioactive waste disposal programs. After emplacement in the repository, bentonite will undergo alkaline chemical effects due to cement degradation, changing its hydro-mechanical behaviour. In this study, the swelling pressure of compacted GMZ bentonite at an initial dry density of 1.7 Mg/m 3 was investigated with two synthetic cement solutions (Young Cement Water -YCW and Evolved Cement Water -ECW) at temperatures of 20 and 60 degrees C. After swelling tests environmental scanning electron microscope (ESEM), mercury intrusion porosimetry (MIP) and X-Ray diffractometry (XRD) tests were also performed to analyse the morphology, microstructure and mineralogy characteristics of the specimens.Results show that the swelling property of bentonite would degrade with time under the in-situ pore water and temperature conditions of repository. With cement solutions injection, a mass of macro-pores in compacted bentonite transforms into micro-pores, especially, in case of YCW with higher temperature. Cation exchanges, smectite dissolution and secondary minerals formation (some zeolites and C-S-H gels) are found to occur in compacted GMZ bentonite. Increasing temperature accelerates the smectite dissolution rate. The dissolution of montmorillonite and the formation of secondary minerals should be the fundamental reasons for the swelling pressure decline, and then microstructure change. (C) 2019 Elsevier Ltd. All rights reserved.
机译:膨润土已被大多数高放废物处置计划用作缓冲/密封材料。放入储存库后,由于水泥降解,膨润土将发生碱性化学作用,从而改变其水力机械性能。在这项研究中,使用两种合成水泥溶液(Young Cement Water -YCW和Evolved Cement Water -ECW)在20和60摄氏度的温度下研究了压实的GMZ膨润土在1.7 Mg / m 3的初始干密度下的溶胀压力。经过溶胀试验,采用环境扫描电子显微镜(ESEM),压汞法(MIP)和X射线衍射仪(XRD)对样品的形貌,微观结构和矿物学特征进行了分析。在原位孔隙水和储层温度条件下,膨润土会随时间降解。通过注入水泥溶液,压实膨润土中的大量大孔会转变为微孔,特别是在高温高压水的情况下。发现在密实的GMZ膨润土中会发生阳离子交换,蒙脱石溶解和二次矿物形成(某些沸石和C-S-H凝胶)。温度升高会加速蒙脱石的溶解速度。蒙脱石的溶解和次生矿物质的形成应该是溶胀压力下降然后微观结构发生变化的根本原因。 (C)2019 Elsevier Ltd.保留所有权利。

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