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浙江嵊州-新昌地区红层软岩崩解能量耗散研究

黄生根 何铭健

黄生根, 何铭健. 浙江嵊州-新昌地区红层软岩崩解能量耗散研究[J]. 地质科技通报, 2024, 43(4): 235-243. doi: 10.19509/j.cnki.dzkq.tb20230174
引用本文: 黄生根, 何铭健. 浙江嵊州-新昌地区红层软岩崩解能量耗散研究[J]. 地质科技通报, 2024, 43(4): 235-243. doi: 10.19509/j.cnki.dzkq.tb20230174
HUANG Shenggen, HE Mingjian. Energy dissipation during disintegration of red-bed soft rock in the Shengzhou-Xinchang area of Zhejiang Province, China[J]. Bulletin of Geological Science and Technology, 2024, 43(4): 235-243. doi: 10.19509/j.cnki.dzkq.tb20230174
Citation: HUANG Shenggen, HE Mingjian. Energy dissipation during disintegration of red-bed soft rock in the Shengzhou-Xinchang area of Zhejiang Province, China[J]. Bulletin of Geological Science and Technology, 2024, 43(4): 235-243. doi: 10.19509/j.cnki.dzkq.tb20230174

浙江嵊州-新昌地区红层软岩崩解能量耗散研究

doi: 10.19509/j.cnki.dzkq.tb20230174
基金项目: 

国家自然科学基金项目 42177166

详细信息
    通讯作者:

    黄生根, E-mail: huangshgr@163.com

  • 中图分类号: P642.21

Energy dissipation during disintegration of red-bed soft rock in the Shengzhou-Xinchang area of Zhejiang Province, China

More Information
  • 摘要:

    以浙江嵊州-新昌地区红层软岩为研究对象, 探究该地区红层软岩崩解表面能特性。基于能量耗散原理, 通过分析该地区3组不同组成成分的红层软岩在干湿循环作用下崩解过程中能量的转化、传递和耗散, 得出红层软岩崩解过程中吸收的能量向表面能转化的规律。结果表明, 该地区红层软岩随着干湿循环次数的不断增多, 表面能累计增长量有3个变化过程: 初期呈平缓增长; 中期表面能急剧增加, 增长速率越来越快; 崩解后期其表面能累计增长量逐渐保持平稳状态。试验还表明黏土矿物含量越高的红层软岩, 产生的表面能越多, 耐崩解性越差。本研究提出的能量耗散模型, 为治理浙江嵊州-新昌地区各种红层软岩问题提供了参考价值。

     

  • 图 1  取样现场概况

    Figure 1.  Overview of the rock sampling site

    图 2  红层软岩崩解形态图

    Figure 2.  Disintegration morphology of red-bed soft rock

    图 3  3组崩解物各粒径质量分数随干湿循环次数的变化曲线

    Figure 3.  Variation curve of the percentage content of each disintegration particle size fraction of the three groups of red-bed soft rock with the number of dry-wet cycles

    图 4  3组试样耐崩解指数随干湿循环次数的变化曲线

    Figure 4.  Variation curve of the disintegration resistance index with the number of dry-wet cycles of the three groups of red-bed soft rock

    图 5  3组红层软岩吸水质量随表面积的关系

    Figure 5.  Relation ships between the water absorption mass and surface area of the three groups of red-bed soft rock

    图 6  3组红层软岩每次干湿循环表面积增长量变化柱状图

    Figure 6.  Histogram of surface area growth per wet-dry cycle of the three groups of red-bed soft rock

    图 7  3组红层软岩表面能累计增长量随干湿循环次数的关系

    Figure 7.  Relationships between the cumulative increase in surface energy of the three groups of red-bed soft rock and the number of dry-wet cycles

    图 8  3组红层软岩表面能累计增长量与耐崩解指数的关系

    Figure 8.  Relationships between the surface energy accumulation and disintegration resistance indices of the three groups of red-bed soft rocks

    图 9  3组红层软岩崩解能量利用率随干湿循环次数的关系

    Figure 9.  Relationship between the energy utilization rate and the number of dry-wet cycles of the three groups of red-bed soft rocks

    表  1  岩样矿物成份

    Table  1.   Mineral composition of the rock samples

    岩样编号 蒙脱石 伊利石 石英 钠长石 方解石 微斜长石 赤铁矿 绿泥石 胶结物
    φB/%
    A组 21.98 22.05 21.73 10.70 14.08 8.50 0.96 泥质为主,少量砂质
    B组 18.52 15.81 22.32 24.31 8.71 10.33 泥质为主,少量砂质
    C组 9.98 14.40 51.28 10.57 11.58 2.2 砂质为主,泥质次之
    下载: 导出CSV

    表  2  3组红层软岩不同粒径试样吸水质量

    Table  2.   Water absorption quality of each particle size of the three groups of red bed soft rocks

    粒径/mm 17.3 24.6 30.6 43.8 56.3 72.7 91.6 104.2 112.6 116.2
    吸水质量/g
    A组 2.7 3.4 4.2 6.3 14.7 25.5 40.9 60.7 68.9 79.5
    B组 1.6 2.5 3.3 5.3 8.1 18.3 33.1 49.9 58.7 65.5
    C组 1.5 2.2 2.7 5.2 7.0 12.8 25.2 30.6 41.1 47.4
    下载: 导出CSV
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  • 收稿日期:  2023-03-31
  • 录用日期:  2023-07-12
  • 修回日期:  2023-05-05

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