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山区公路顺层边坡首次失稳长度影响因素及确定方法

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西部山区公路建设中常遭遇顺层边坡,其首次失稳长度Lc 是失稳机制及加固设计的关键参数,现有Lc 确定方法存在一定局限性.依托31 个四川盆周山区公路顺层边坡失稳案例,系统调查坡体结构特征(岩层倾角α、边坡走向与岩层走向的夹角θ和坡长L)及外在灾变诱因(切层厚度D和降雨量Q)对首次失稳长度的特征,并结合数值分析,探讨顺层边坡首次失稳长度的主要影响因子及确定方法,建立更加完善的多因素首次失稳长度的拟合关系式.结果表明:顺层边坡破坏主要发生在θ≤30°范围,坡体双面临空甚至三面临空时,θ>30°的顺层边坡也发生失稳;Lc 随L的增大而增大,且Lc/L等于 0.3~1.0;Lc/D介于 3~24 之间,不含软弱夹层时Lc/D等于 3~10;α在 12°~35°时,顺层边坡稳定性最差,且Lc/D随α的增大而减小;降雨对顺层边坡的失稳诱发源于软弱夹层的饱水软化,汛期开挖是含软弱夹层顺层边坡失稳的灾变诱因.边坡首次失稳长度影响因子敏感度从大到小排序为:①含软弱夹层边坡:岩层倾角、坡长、切层厚度、内摩擦角、黏聚力、弹性模量、开挖高度;②无软弱夹层边坡:岩层倾角、内摩擦角、切层厚度、黏聚力、坡长.提出的走向夹角折减系数和多因素首次失稳长度计算公式对边坡破坏范围的确定有指导意义.
Influencing factors and determination method of the initial instability length of bedding slope along mountainous highways
Bedding slope is often encountered in highway construction in western mountainous areas.The initial instability length Lc is the key parameter of instability mechanism and reinforcement design.At present,there are some limitations in the determination method of the first instability length.Based on 31 cases of highway bedding slope instability in mountainous areas around Sichuan Basin,the influencing factors of slope structure characteristics(rock dip angle α,angle θ between slope strike and rock strike and slope length L)and external disaster inducement(cutting thickness D and rainfall Q)on Lc was systematically investigated.Combined with finite element analysis,the main influencing factors and determination method of Lc were emphatically discussed.The results show that Lc/D ranges from 3~24,with a value of 3 to 10 excluding argillaceous interlayer.For α ranging between 12° and 35°,bedding slope stability is the weakest,and Lc/D decreases with α increments.Failure in bedding slopes primarily occurs within θ≤30°,extending to unstable conditions for θ>30° with double or even three free faces in the slope.Lc increases with the increase of L,and Lc/L is in the range of 0.3~1.0.Bedding slopes within an H range of 5 m to 30 m tend to lose stability easily.The instability of bedding slope induced by rainfall is due to the saturation softening of muddy interlayer,and the excavation in flood season is the catastrophic cause of bedding slope instability with argillaceous interlayer.The sensitivity in descending order of the influencing factors of initial instability length is as follows:①Slope with weak interlayer:rock dip angle,slope length,cutting thickness,internal friction angle,cohesion,elastic modulus,excavation height;②Slope without weak interlayer:rock dip angle,internal friction angle,cutting layer thickness,cohesion,slope length.The proposed calculation formula of strike angle reduction coefficient and multi-factor Lc has guiding significance for the determination of slope failure range.

bedding slopehighway along Sichuan Basininitial instability lengthinfluencing factorfitting relationship

向波、罗晗玲、邬凯、冯君、张乐、顾涛、张俊云

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四川省公路规划勘察设计研究院有限公司,四川 成都 610041

西南交通大学 土木工程学院,四川 成都 610031

顺层边坡 四川盆周公路 首次失稳长度 影响因素 拟合关系式

四川省交通运输科技项目四川省交通运输科技项目

2021-A-022021-A-04

2024

自然灾害学报
中国地震局工程力学所 中国灾害防御协会

自然灾害学报

CSTPCD北大核心
影响因子:0.862
ISSN:1004-4574
年,卷(期):2024.33(5)
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