长江科学院院报 ›› 2020, Vol. 37 ›› Issue (9): 115-121.DOI: 10.11988/ckyyb.20190569

• 岩土工程 • 上一篇    下一篇

黄土垂直和构造节理的几何差异性及拓扑学研究

康尘云, 王少凯, 潘登丽, 贺鸣   

  1. 长安大学 地质工程与测绘学院,西安 710054
  • 收稿日期:2019-05-16 修回日期:2020-05-15 出版日期:2020-09-01 发布日期:2020-09-25
  • 作者简介:康尘云(1995- ),男,陕西乾县人,硕士研究生,主要从事黄土工程地质和灾害防治方面的工作。E-mail: kangchenyun@outlook.com
  • 基金资助:
    国家自然科学基金项目(41790441, 41807234)

Geometric Differences and Topology of Tectonic and Vertical Joints of Loess

KANG Chen-yun, WANG Shao-kai, PAN Deng-li, HE Ming   

  1. School of Geology Engineering and Surveying, Chang'an University, Xi'an 710054, China
  • Received:2019-05-16 Revised:2020-05-15 Online:2020-09-01 Published:2020-09-25

摘要: 黄土节理是地下水的赋存场所和运移通道,它们使土体破碎进而影响稳定性和强度,是各类地质灾害的构造基础,准确分析其发育特点和展布规律,是理解黄土频发灾害的关键步骤。通过现场调查、数理统计和拓扑分析,对陇西地区黄土进行系统研究。结果表明:①陇西地区主要发育优势走向为NNW、NWW和NE向的构造节理,这是受区域内走滑断裂带和逆倾滑断裂带影响的结果;②构造节理优势组的产状服从高斯正态分布,倾角多为60°~80°,垂直节理的产状随机分布、离散型较强;③2种节理的平均间距均较宽,张开度属“开裂”范围,延续性中等,但垂直节理的间距分布范围更集中,构造节理的张开度相比更小;④拓扑分析显示I型节点占主导,节理延伸过程易被中断,分支比处于3以下的低水平,该方法能更简单、直观地描述连通性。研究结果可以为新构造应力场恢复、掌握黄土节理发育基本规律、节理网络数值建模等提供基础数据。

关键词: 黄土, 节理, 几何特征, 拓扑分析, 连通性

Abstract: Loess joints are the places where groundwater exists and migrates. They break the soil, and affect the stability and strength of loess, causing enormous losses on both economy and human lives. Joints are the structural basis of all kinds of loess disasters. Accurate analysis of its development characteristics and distribution rules is crucial to understanding the frequent occurrence of loess disasters. Through systematic field investigation, mathematical statistics and topological analysis of loess in Longxi, we found that: (1) The dominant strikes of loess tectonic joints in Longxi are NNW,NWW and NE, which is influenced by strike-slip fault and reverse tilting fault.(2) The occurrence of dominant tectonic joints group obeys the Gaussian normal distribution, with the dip angle mostly within 60-80°. The occurrence of vertical joints are more randomly distributed and highly discrete. (3) The average spacing of both tectonic and vertical joints is wide, the opening of joints belongs to “crack” in standard, and the continuity medium, except that the spacing of vertical joints is more concentrated, while the opening of tectonic joints is smaller by comparison. (4) Topological analysis shows that I-node is the majority. Joints extension process is easily interrupted. Branch ratio is at a low level below 3. Topological analysis is more simple and intuitive to describe connectivity, especially under the help of powerful toolbox in software, and has been discussed for decades in the world, yet is rarely used in relative research in China. The research results provide basic data for the recovery of Neotectonics stress fields, for understanding the basic laws of joints development and the numerical modeling of joints network.

Key words: loess, joints, geometrical features, topological analysis, connectivity

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