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紫鹊界梯田失稳机制

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为厘清降雨入渗作用对花岗岩区梯田边坡稳定性的影响,本文以湖南省紫鹊界梯田为例,在分析紫鹊界梯田地质条件的基础上,基于有限元数值模拟软件Geostudio多模块的耦合,分析了不同边坡坡度和不同土层厚度在暴雨条件下的渗流场和稳定性.研究结果表明:在降雨强度为90 mm/d、降雨历时为5 d的工况下,坡度为35°和40°的边坡处于失稳状态,稳定性系数与边坡坡度负相关;全风化土层越厚的边坡稳定性系数越低;在降雨历时5 d后,不同土层工况下的稳定性系数相差不大,但无降雨时,全风化土层越薄的边坡明显更加稳定.
Destabilization Mechanism of Ziquejie Terrace
In order to discuss the influence of rainfall infiltration on the stability of granite terrace slope,this paper takes the Ziquejie terrace in Hunan Province as an example.Based on the analysis of the geological conditions of Ziquejie terrace,the seepage field and stability of different slope gradients and different soil layer thicknesses under rainstorm conditions were analyzed based on the coupling of multiple modules of the finite element numerical simulation software Geostudio.The results show that under the working condition of 90 mm/d rainfall intensity and 5 days rainfall duration,the slopes with 35° and 40° gradients are in a state of destabilization,and the stability coefficient is negatively correlated with the increase of slope gradient;The thicker the fully weathered soil layer is,the lower the safety factor of the slope is.After 5 days of rainfall,the stability coefficients of different soil layers under different working conditions are similar.However,when there is no rainfall,the thinner the fully weathered soil layer is,the more stable the slope is.

Ziquejie terracegraniterainfall infiltrationslope stabilitygradientsoil layer thikness

欧阳琦、陈欣、危润初、伍诗梦、朱志远

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长沙理工大学水利与环境工程学院,长沙 410004

长沙理工大学水沙科学与水灾害防治湖南省重点实验室,长沙 410004

长沙理工大学洞庭湖水环境治理与生态修复湖南省重点实验室,长沙 410004

湖南衡阳水文水资源勘测中心,湖南 衡阳 421001

湖南娄底水文水资源勘测中心,湖南 娄底 417000

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紫鹊界梯田 花岗岩 降雨入渗 边坡稳定性 坡度 土层厚度

湖南省教育厅优秀青年项目国家自然科学基金湖南省自然科学基金湖南省自然科学基金长沙理工大学"双一流"科学研究国际合作拓展项目

21B0314416022642020JJ55722023JJ400212019IC08

2024

吉林大学学报(地球科学版)
吉林大学

吉林大学学报(地球科学版)

CSTPCD北大核心
影响因子:1.062
ISSN:1671-5888
年,卷(期):2024.54(2)
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