LIN Yun-zhao, JIAN Wen-bin, LAI Zeng-rong, et al. Mechanical properties of root-soil composite in tree-covered
landslide area based on field prototype test[J]. 2024, 45(11): 3423-3434.
DOI:
LIN Yun-zhao, JIAN Wen-bin, LAI Zeng-rong, et al. Mechanical properties of root-soil composite in tree-covered
landslide area based on field prototype test[J]. 2024, 45(11): 3423-3434.DOI: 10.16285/j.rsm.2023.1955.
Mechanical properties of root-soil composite in tree-covered
landslide area based on field prototype test
为揭示乔木根系力学特性及其对斜坡的力学效应,选取福建武平高植被覆盖区滑坡为研究点,对研究区典型乔木根系按径级分类后进行根系抗拉力学特性测试,并在滑坡现场进行不同根系横截面积比(root cross-sectional area ratio,简称RAR)、含水率下的根-土复合体原位直剪试验以及剖面根系分布特征调查,对根系在浅层滑坡的力学效应展开探究。研究结果表明:(1)1~7径级下马尾松、杉木抗拉力范围为12.45~673.09 N,抗拉力与根径呈幂函数正相关;抗拉强度范围为7.16~60.95 MPa,抗拉强度与根径呈幂函数负相关。杉木根系平均抗拉力与抗拉强度均大于马尾松。(2)乔木根系显著提高了土体抗剪强度,根系对土体提供的附加黏聚力与剪切面RAR显著正相关。杉木根系构型更接近R型,马尾松为VH型,相近RAR下杉木对土体的加固作用优于马尾松。(3)随着含水率增加,马尾松、杉木根-土复合体抗剪强度显著下降,水分入渗使根系对土体提供的附加黏聚力受到削减。(4)基于Wu模型,考虑水分对土体黏聚力与根系附加黏聚力的影响,建立了考虑含水率的根-土复合体抗剪强度值估算模型,经检验,精度高于Wu模型,结果较为合理。(5)根系对浅层滑坡虽然具有加固作用,但受到根系分布深度、密度以及降雨等因素限制,强降雨作用下根系对浅层滑坡稳定性贡献具有局限性。
Abstract
In order to understand the mechanical characteristics of tree roots and their mechanical effects on slopes
the landslide in Wuping high vegetation coverage area of Fujian province was selected as the research site
and the root tensile mechanical properties of typical tree roots in the study area were tested after classification by diameter class. Furthermore
in-situ direct shear tests of root-soil composites under different root cross-sectional area ratios (RAR) and moisture content were conducted at the landslide site
and investigations were made into the distribution characteristics of roots in the profile to explore the mechanical effects of roots on shallow landslides. The results showed as follows: (1) The tensile force of Pinus massoniana and Cunninghamia lanceolata ranged from 12.45−673.09 N in 1−7 diameter class
and the tensile force was positively correlated with the root diameter by power function; The tensile strength ranges from 7.16 MPa to 60.95 MPa
and the tensile strength is negatively correlated with the root diameter as a power function. The average tensile force and tensile strength of Cunninghamia lanceolata root were higher than those of Pinus massoniana. (2) Tree roots significantly improved the shear strength of soil
and the additional cohesion provided by roots to soil was significantly positively correlated with the shear plane RAR. The root structure of Cunninghamia lanceolata is closer to R type
and that of Pinus massoniana is VH type. Under similar RAR
Cunninghamia lanceolata roots has a better reinforcing effect on the soil than Pinus massoniana. (3) With the increase in moisture content
the shear strength of the root-soil composites of Pinus massoniana and Cunninghamia lanceolata significantly decreases
as water infiltration diminishes the additional cohesion provided by the root systems to the soil. (4) Based on the Wu model
considering the influence of moisture content on soil cohesion and additional root cohesion
an estimation model for the shear strength value of root-soil composites considering moisture content was established. Upon verification
the accuracy of this model proved to be higher than that of the Wu model
and the results were reasonable. (5) Although the root system has a reinforcement effect on shallow landslides
its contribution to the stability of shallow landslides under heavy rainfall is limited due to the influence of root distribution depth
Effect of root decay on mechanical properties of root-soil composite
Research on calculation model for stability evaluation of rainfall-induced shallow landslides
Parametric analyses of intensity-duration curve for predicting rainfall-induced landslides in residual soil slope in Southeastern coastal areas of China
Application of deterministic model to analyzing stability of hillslope of loess gully area
Discussion on stability of shallow landslide under rainfall
Related Author
WU Yi-long
JIAN Wen-bin
LIN Yun-zhao
ZHU Zu-teng
ZHENG Guo-ming
QIN Ya-zhou
XU Jian-cong
LI Ning
Related Institution
Fujian Institute of Geological Survey
Key Laboratory of Geohazard Prevention of Hilly Mountains, Ministry of Natural Resources, Geological Engineering Survey in Fujian Province
Institute of Geotechnical and Geological Engineering, Fuzhou University
Department of Geotechnical Engineering, Tongji University
Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education, Tongji University