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水-力耦合条件下膨润土-砂混合物的体变特性研究
  • ISSN号:1000-7598
  • 期刊名称:《岩土力学》
  • 时间:0
  • 分类:TU433[建筑科学—岩土工程;建筑科学—土工工程]
  • 作者机构:[1]南京大学地球科学与工程学院,江苏南京210023, [2]同济大学岩土及地下工程教育部工程重点实验室,上海200092
  • 相关基金:基金项目优秀青年科学基金(No.41322019);国家自然学科基金(No.41572246);岩土及地下工程教育部重点实验室(同济大学)开放基金项目mo.KLE-TJGE-B1105):国家自然科学基金重点项目(No.41230636);江苏省“青蓝工程”(2014);中央高校基本科研业务费专项资金(2015).
中文摘要:

在高放核废物处置库中,膨润土-砂混合物是一种可选的缓冲回填材料,掌握其在水-力耦合条件下的体变特征对正确评价处置库的长期安全性有重要意义。按照不同的石英砂掺量(0%-50%)配制了6组膨润土/砂混合物,依次进行了单轴侧限压缩、有荷膨胀(轴向应力为0.2 MPa)和饱和再压缩试验,获得了混合物在不同水-力路径下的变形特征,并着重分析了砂掺量的影响。结果表明:(1)膨润土-砂混合物的压缩性与掺砂量、饱和状态和密实度有关。在非饱和及密实度较低(ρd〈1.7 g/cm3)的条件下,混合物的压缩指数随砂掺量的增加近似线性减小;当混合物压缩到较高的密实度(ρd〉1.7 g/cm3)并且饱和后,压缩指数受掺砂量的影响不明显,但其值远小于非饱和及低密实度状态。(2)混合物的最终膨胀率随着掺砂量的增加呈指数减小,随膨润土有效干密度的增加而呈指数增加。掺砂量达到40%时,膨胀过程伴随有体积回落现象,且体积回落率随砂掺量的增加而加剧。(3)混合物在不同水-力路径中及不同砂掺量条件下呈现的体变差异性与膨润土和砂在试样中的分布状态及二者对土体骨架的主导作用有关,总体上,掺砂量越高或试样密实度越大,砂对体变的主导作用越强。(4)混合物的膨胀力随掺砂量的增加而减小,通过引入膨润土有效干密度参数,建立了混合物膨胀力与该参数间的指数定量关系,可对膨胀力进行预测,并从蒙脱石的体积变化率与质量分布率的角度进一步分析了混合物膨胀力的作用机制。

英文摘要:

The bentonite/sand mixture is an optional buffer/backfill material in the geological disposal of high level nuclear waste. Understanding the volume change characteristics of this mixture under coupled hydro-mechanical condition is highly significant for evaluating the long-term safety of the repository. In this investigation, six groups of bentonite/sand mixtures were prepared with different contents of quartz sand, i.e. 0%, 10%, 20%, 30%, 40% and 50%. Then a series of experiments including uniaxial confined compression (to a final dry density of 1.7 Mg/m3), saturation (under 0.2 MPa vertical pressure) and reloading tests was carried out in sequence. The volume change behavior of bentonite/sand mixtures was understood, in addition, the effect of sand content was also analyzed emphatically. It is found that: (1) The compression behaviour of mixture significantly depends on sand content, saturation state and density. As the mixture is unsaturated and at relative low dry density (Pd 〈1.7 g/cm3), the compression index decreases linearly with increasing sand content. However, as the mixture is saturated and at relative high dry density (po 〈1.7 g/cm3), the compression index of mixture is independent of sand content, and the corresponding value is much less than that at unsaturated and loose state. (2) The final swelling strain of the mixture decreases exponentially with increasing sand content, while increases exponentially with effective bentonite dry density. As the sand content in the mixture is higher than 40%, volume collapse can occur during saturation, and collapse extent is enhanced by increasing sand content. (3) The observed volume change characteristics of themixture under different hydro-mechanical conditions or at different sand contents are mainly related to the distribution of bentonite and sand in the mixture, and their dominant effect on soil skeleton. Generally, the higher sand content and higher density, the volume change behavior the mixture is more conditioned by

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期刊信息
  • 《岩土力学》
  • 中国科技核心期刊
  • 主管单位:中国科学院
  • 主办单位:中国科学院武汉岩土力学研究所
  • 主编:孔令伟
  • 地址:武汉市武昌小洪山中国科学院武汉岩土力学研究所
  • 邮编:430071
  • 邮箱:ytlx@whrsm.ac.cn
  • 电话:027-87198484 87199252
  • 国际标准刊号:ISSN:1000-7598
  • 国内统一刊号:ISSN:42-1199/O3
  • 邮发代号:38-383
  • 获奖情况:
  • 全国中文核心期刊,美国《工程索引》EI收录期刊
  • 国内外数据库收录:
  • 美国化学文摘(网络版),荷兰文摘与引文数据库,美国工程索引,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:56873