梁栋, 杨彪, 杨仲田, 李洪辉, 刘宇辰, 刘伟. 高庙子钠基膨润土热老化后矿物成分变化[J]. 中国矿业, 2020, 29(11): 212-219. DOI: 10.12075/j.issn.1004-4051.2020.11.004
    引用本文: 梁栋, 杨彪, 杨仲田, 李洪辉, 刘宇辰, 刘伟. 高庙子钠基膨润土热老化后矿物成分变化[J]. 中国矿业, 2020, 29(11): 212-219. DOI: 10.12075/j.issn.1004-4051.2020.11.004
    LIANG Dong, YANG Biao, YANG Zhongtian, LI Honghui, LIU Yuchen, LIU Wei. The alteration on the mineral composition of GMZ sodium bentonite after thermal aging[J]. CHINA MINING MAGAZINE, 2020, 29(11): 212-219. DOI: 10.12075/j.issn.1004-4051.2020.11.004
    Citation: LIANG Dong, YANG Biao, YANG Zhongtian, LI Honghui, LIU Yuchen, LIU Wei. The alteration on the mineral composition of GMZ sodium bentonite after thermal aging[J]. CHINA MINING MAGAZINE, 2020, 29(11): 212-219. DOI: 10.12075/j.issn.1004-4051.2020.11.004

    高庙子钠基膨润土热老化后矿物成分变化

    The alteration on the mineral composition of GMZ sodium bentonite after thermal aging

    • 摘要: 为了了解单纯热老化对高庙子天然钠基膨润土中矿物组分和微观结构的影响,拓展高放地质处置缓冲材料性能评价范围,以内蒙古高庙子天然钠基膨润土和北山地下水为研究对象,利用红外光谱仪、X射线衍射仪和穆斯堡尔谱仪分析了不同老化温度(90 ℃、150 ℃、170 ℃、190 ℃和210 ℃)和老化时间(2个月、4个月、6个月、8个月、10个月和12个月)热老化后高庙子天然钠基膨润土中官能团、矿物组分和Fe的赋存状态以及含量的变化,并对其Si在北山地下水中的溶解性进行测试。结果表明:随着老化温度和老化时间的增加,膨润土中官能团数量有所变化,蒙脱石含量减少,云母和沸石含量增加,但没有发生种类变化;可溶性偏硅酸根增加,存在Fe(Ⅱ)向Fe(Ⅲ)转变的趋势。总体而言,热老化引起了高庙子天然钠基膨润土矿物组分的显著变化,但尚需深入研究。

       

      Abstract: The aim of this paper is to understand the impacts of thermal aging on the mineral composition and microstructure of Gaomiaozi natural sodium bentonite with Beishan groundwater and to broaden the assessment and scope of buffer materials for geological disposal of high-level radioactive waste(HLW).FTIR, XRD and Mössbauer spectra of GMZ sodium bentonite(contain groundwater from Beishan area) heated at 90℃,150℃,170℃,190℃ and 210℃ respectively continue 2 months, 4 months, 6 months, 8 months, 10 months and 12 months have been studied.In addition, the solubility of silicon in groundwater from Beishan area have been tested.The results indicate that, the content of montmorillonite decreases, the content of mica and zeolite increases significantly with the increment of the thermal temperature and time.The concentration of in groundwater increases obviously as the thermal temperature and time increased.There have the tendency that Fe(Ⅱ) transformed to Fe(Ⅲ) in the bentonite after thermal aged.But, the types of mineral and functional groups remain the same.Overall, the mineral composition of GMZ natural sodium bentonite have been varied after thermal aged, further research is needed to comprehend specific situations.

       

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