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天然粘土样品分析的伊利石/蒙皂石间层矿物的间层比计算方法

陈洪起 赵杏媛 张有瑜

陈洪起, 赵杏媛, 张有瑜. 天然粘土样品分析的伊利石/蒙皂石间层矿物的间层比计算方法[J]. 石油实验地质, 1991, 13(4): 408-418. doi: 10.11781/sysydz199104408
引用本文: 陈洪起, 赵杏媛, 张有瑜. 天然粘土样品分析的伊利石/蒙皂石间层矿物的间层比计算方法[J]. 石油实验地质, 1991, 13(4): 408-418. doi: 10.11781/sysydz199104408
Chen Hongqi, Zhao Xingyuan, Zhang youyu. A PRECISE PROCEDURE OF THE PROPORTION OF SMECTITE LAYER CALCULATION SUITABLE FOR INTERSTRATIFIED ILLITE/SMECTITES ANALYSIS OF NATURAL CLAY SAMPLES[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1991, 13(4): 408-418. doi: 10.11781/sysydz199104408
Citation: Chen Hongqi, Zhao Xingyuan, Zhang youyu. A PRECISE PROCEDURE OF THE PROPORTION OF SMECTITE LAYER CALCULATION SUITABLE FOR INTERSTRATIFIED ILLITE/SMECTITES ANALYSIS OF NATURAL CLAY SAMPLES[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1991, 13(4): 408-418. doi: 10.11781/sysydz199104408

天然粘土样品分析的伊利石/蒙皂石间层矿物的间层比计算方法

doi: 10.11781/sysydz199104408

A PRECISE PROCEDURE OF THE PROPORTION OF SMECTITE LAYER CALCULATION SUITABLE FOR INTERSTRATIFIED ILLITE/SMECTITES ANALYSIS OF NATURAL CLAY SAMPLES

  • 摘要: 乙二醇(EG)处理定向样品的X射线衍射谱图上有无17Å衍射峰,是区分伊利石/蒙皂石无序间层和伊利石/蒙皂石有序间层的重要标志.实验证明,对于纯样品,伊利石/蒙皂石无序间层矿物的17A衍射峰强度变化主要决定于间层比(S%)的大小;对于天然样品,尤其是含有分散伊利石的天然样品,伊利石/蒙皂石无序间层矿物的17Å衍射峰强度除了受间层比的影响以外,还受样品中该间层矿物相对含量的影响,即受其它伴生矿物,尤其是分散伊利石相对含量的影响.本文根据具不同间层比的纯伊利石/蒙皂石无序间层矿物与分散伊利石以不同比例的混合样品的X射线衍射分析结果,提出一种适用于天然粘土样品分析的伊利石/蒙皂石无序间层矿物的间层比计算方法,同时还介绍天然粘土样品分析的伊利石/蒙皂石有序间层矿物的间层比计算方法.

     

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出版历程
  • 收稿日期:  1989-03-20
  • 刊出日期:  1991-10-25

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