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延安晚更新世黄土颗粒微观各向异性特征及其成因分析

洪勃, 李喜安, 王力, 孙建强, 简涛, 孟杰. 2021. 延安晚更新世黄土颗粒微观各向异性特征及其成因分析[J]. 中国地质, 48(3): 900-910. doi: 10.12029/gc20210317
引用本文: 洪勃, 李喜安, 王力, 孙建强, 简涛, 孟杰. 2021. 延安晚更新世黄土颗粒微观各向异性特征及其成因分析[J]. 中国地质, 48(3): 900-910. doi: 10.12029/gc20210317
HONG Bo, LI Xi'an, WANG Li, SUN Jianqiang, JIAN Tao, MENG Jie. 2021. Microscopic anisotropy and genesis of Late Pleistocene loess particles in Yan'an[J]. Geology in China, 48(3): 900-910. doi: 10.12029/gc20210317
Citation: HONG Bo, LI Xi'an, WANG Li, SUN Jianqiang, JIAN Tao, MENG Jie. 2021. Microscopic anisotropy and genesis of Late Pleistocene loess particles in Yan'an[J]. Geology in China, 48(3): 900-910. doi: 10.12029/gc20210317

延安晚更新世黄土颗粒微观各向异性特征及其成因分析

  • 基金项目:
    国家自然科学基金面上项目(41572264,41877225)、中央高校基本科研业务费专项资金—长安大学优秀博士学位论文培育资助项目(300102268717)联合资助
详细信息
    作者简介: 洪勃, 男, 1987年生, 博士, 工程师, 主要从事地质灾害调查及防灾减灾研究; E-mail: hongbo@chd.edu.cn/hongbo@chd.edu.cn
    通讯作者: 李喜安, 男, 1968年生, 博士, 教授, 主要从事黄土工程地质方面的研究和教学; E-mail: dclixa@chd.edu.cn
  • 中图分类号: P642.13+1;P534.63+1

Microscopic anisotropy and genesis of Late Pleistocene loess particles in Yan'an

  • Fund Project: Funded by the National Natural Science Foundation of China (No.41572264, 41877225) and the Fundamental Research Funds for the Central Universities, CHD (No. 300102268717)
More Information
    Author Bio: HONG Bo, male, born in 1987, Ph.D, engaged in geo-hazards investigation and disaster prevention and mitigation research; E-mail: hongbo@chd.edu.cn/382492004@qq.com .
    Corresponding author: LI Xi'an, male, born in 1968, Ph.D, professor, engaged in the research and teaching of loess engineering geology; E-mail: dclixa@chd.edu.cn
  • 土颗粒的形状及其空间方位的择优取向是导致宏观土体各向异性的重要原因之一。以具有明显各向异性的晚更新世马兰黄土为研究对象,借助Quanta FEG型电子显微镜扫描照片所包含的相关信息,揭示其微结构在水平向和垂直向上的差异,并对该微观结构的各向异性成因进行了分析。发现:(1)水平向和垂直向切片中颗粒的圆形度R0具有正态分布特征,无论垂直向还是水平向土壤颗粒均以次圆形、圆形和非常圆颗粒为主。(2)水平方向切片中颗粒的方位角具有一定的WN-ES的优势方向,而垂直向切片中土颗粒的长轴有与地面平行的优势取向,且埋深越深这种趋势越明显。(3)水平切片中土颗粒的各向同性性质更为显著,而垂直向切片中颗粒的各向异性性质更为突出,且随埋深的增加,各向异性增强。(4)水平向和垂直向切片中颗粒总的概率分布基本表现为随机分布,粉粒在数量上占绝对优势是导致这种无序分布的重要原因,相对于粉粒而言细砂则可在一定程度上体现其排列具有方向性。分析表明,颗粒的方位角和各向异性率对黄土微观各向异性具有较好的指示作用。同时,颗粒的方向性对黄土高原的古气候也具有重要研究意义。

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  • 图 1  黄土高原盛行风向及研究区域位置(据Zhang et al., 2010修改)

    Figure 1. 

    图 2  颗分曲线

    Figure 2. 

    图 3  SEM后处理图片

    Figure 3. 

    图 4  不同埋深水平方向、垂直方向颗粒圆形度统计图

    Figure 4. 

    图 5  不同埋深水平方向、垂直方向土颗粒定向角玫瑰花图

    Figure 5. 

    图 6  各向异性率

    Figure 6. 

    图 7  概率熵

    Figure 7. 

    图 8  剖面粒径指标(a),马兰黄土的埋深、绝对年龄以及沉积速率(b)(李虎侯, 1986)

    Figure 8. 

    图 9  土颗粒转动、变形类型概念模型

    Figure 9. 

    表 1  试验土样的基本情况

    Table 1.  Basic properties of the soil samples

    下载: 导出CSV

    表 2  颗粒圆度分类

    Table 2.  Classification chart for particle shapes

    下载: 导出CSV
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出版历程
收稿日期:  2018-09-14
修回日期:  2019-09-01
刊出日期:  2021-06-25

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