滇中红层软岩微观结构及水理特性试验研究
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  • 英文篇名:Experimental Study on Microscopic Structure and Hydraulic Features of Red-Bed Soft Rock in Central Yunnan Province
  • 作者:王飞 ; 曹晨飞 ; 陈吉文
  • 英文作者:WANG Fei;CAO Chen-fei;CHEN Ji-wen;Shaanxi Railway Institute;Zhangjiakou Vocational and Technical College;College of Geoscience and Surveing Engineering,China University of Mining and Technology;
  • 关键词:公路工程 ; 红层软岩 ; 微观结构 ; 水理特性 ; 试验研究
  • 英文关键词:highway engineering;;red-bed soft rock;;microscopic structure;;hydraulic features;;experimental study
  • 中文刊名:DZKT
  • 英文刊名:Geology and Exploration
  • 机构:陕西铁路工程职业技术学院;张家口职业技术学院;中国矿业大学(北京)地球科学与测绘工程学院;
  • 出版日期:2016-11-15
  • 出版单位:地质与勘探
  • 年:2016
  • 期:v.52;No.468
  • 基金:国家自然科学基金项目(编号:10872207)资助
  • 语种:中文;
  • 页:DZKT201606016
  • 页数:7
  • CN:06
  • ISSN:11-2043/P
  • 分类号:156-162
摘要
滇中红层软岩具有成岩作用差、易产生较大变形、遇水易软化、易崩解等特征,本文采用环境扫描电镜试验和水理特性试验,对红层软岩的微观结构特征,崩解、膨胀、软化等水理特性进行了研究。试验结果表明,红层软岩矿物粒间空隙大多被粘土矿物填充,粘土矿物以伊利石和蒙脱石为主,为混层结构,结晶程度相对较差,多数有蚀变的痕迹。具有微小裂隙的红层软岩在1~2次充分饱水烘干后,崩解性开始显现;随着干湿循环次数增加,岩样的质量变化呈减小趋势;干湿循环次数继续增加,崩解性指数趋于平缓。红层软岩由于风化作用影响程度和自然含水率的差异,岩体内部崩解张力具有明显不均匀性。经过自由浸水48h后,红层软岩的单轴抗压强度降低29.83%~58.47%,各地层软化系数在0.4~0.7之间,遇水后呈现显著软化效应。这些结果为红层软岩地区公路工程建设的工程地质研究提供了一定参考。
        The red-bed weak rock in central Yunnan is characterized by poor diagenesis,easy to produce large deformation,and easy to soften and disintegrate in water. This paper presents comprehensive research results of experimental study on microscopic structure and hydraulic features of this rock. The experiments show that the inter-granular space of minerals of this rock is mostly filled with clay minerals,mainly illite and montmorillonite.These clay minerals have dominant mixed layer structure,with relatively poor crystallization degree,most of which have alteration traces. The red-bed weak rock with tiny cracks begins to show disintegrating after 1 ~ 2 times fully water-saturation drying. With increasing times of dry-wet circulation,the quality of the rock change has a trend to become smaller. As this increase continues,its disintegration index tends to be gentle. Because of the differences of weathering degrees and natural moisture content,the internal tension of rock disintegration is obviously inhomogenous. After 48 h of free-water soaking,the uniaxial compressive strength of the red-bed soft rock is decreased by 29. 83% to 58. 47%,and the softening coefficients are between 0. 4 ~0. 7,indicative of a significant softening effect by water. These results can provide some reference for the research of engineering geology in highway engineering construction in areas with red-bed soft rock.
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