文章摘要
杨建林, 王来贵, 李喜林, 戴长毅.水作用下泥岩崩解过程与微观机理研究Journal of Water Resources and Water Engineering[J].,2014,25(1):67-70
水作用下泥岩崩解过程与微观机理研究
Research on disintegration process and micro mechanism of mudstone under water action
  
DOI:10.11705/j.issn.1672-643X.2014.01.014
中文关键词: 泥岩  次生孔隙  饱水  微观机理  崩解
英文关键词: mudstone  secondary porosity  saturation  micro mechanism  disintegration
基金项目:国家自然科学基金项目(51274110,51304106); 辽宁工程技术大学博士科研启动金资助项目(11 417)
Author NameAffiliation
YANG Jianlina,b, WANG Laiguia, LI Xilinc, DAI Changyib (辽宁工程技术大学 a.力学与工程学院 b.材料科学与工程学院c.建筑工程学院 辽宁 阜新 123000) 
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中文摘要:
      为研究水作用下泥岩崩解的微观机理,利用X射线衍射仪、激光共聚焦显微镜对泥岩的成分、饱水后试样表面三维形貌变化进行测试,揭示了水作用下泥岩形貌的变化规律,分析了泥岩崩解的微观机理。研究表明:试样表面的裂纹数目、宽度随饱水时间的增加而增加;泥岩的崩解主要受饱水过程中产生的次生孔隙和裂纹/孔隙表面受到的楔裂压力影响,总次生孔隙主要由水化学作用产生的次生孔隙和水的冲刷、运移物理作用产生的次生孔隙构成,孔隙在楔裂压力的作用下相互扩展形成裂纹,裂纹相互贯穿使试样崩解。
英文摘要:
      In order to study the disintegration process and micro mechanism of mudstone under water action,the paper used X ray diffraction and laser scanning confocal microscopy to measure the composition of mudstone and the change of three-dimensional topography after water saturated,announced the change law of mudstone topography and analyzed the micro mechanism of mudstone disintegration.The results show that the quantity and width of crack increase with the increase of saturation time. The disintegration of mudstone is caused by the second porosity and wedging pressure in saturation process. The whole second porosity is caused by the second porosity results from chemical effect of water and the action of water flushing and transport. Crack is formed by wedging pressure of porosity surface in the process of saturation. The sample is disintegrated because of crack penetration each other.
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