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水土化学作用对崩岗土体抗剪特性的影响

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[目的]探究水土化学作用对花岗岩崩岗区崩壁土体抗剪特性的影响,为阐明花岗岩崩岗侵蚀的成因机理提供理论依据。[方法]以福建省长汀县典型崩岗区崩壁土体(红土层、砂土层和碎屑层)为研究对象,分析了经不同离子浓度(0。005、0。01和0。1 molL-1)和离子类型(Na+和K+)的盐溶液交换处理后崩岗3个土层的土体抗剪特性(偏应力、黏聚力和内摩擦角)。[结果]红土层的偏应力、黏聚力和内摩擦角均显著高于砂土层和碎屑层。随着溶液浓度的增加,K+体系下崩岗3个土层的黏聚力显著增加,其中红土层增幅最大,增加了 17。39%,Na+体系则表现出相反趋势;2种离子体系下土体的内摩擦角总体差异不显著。K+体系下崩岗3个土层的偏应力和黏聚力均显著大于Na+体系,其中,K+处理的红土层、砂土层和碎屑层的黏聚力比Na+处理的分别高9。99%、3。37%和9。65%,但2种离子对内摩擦角的影响总体并不显著。水土化学作用对黏聚力的影响显著大于内摩擦角。[结论]不同浓度的Na+和K+对黏聚力的影响显著大于内摩擦角,K+可通过增加黏聚力而增加土体的抗剪强度,K+浓度越高,抗剪强度越大。
Influence of Water-soil Chemical Interaction on Shear Characteristics of Benggang
[Objective]The study aimed to explore the effects of water-soil chemical interaction on the shear characteristics of Benggang,and to provide a theoretical basis to understand the causes and mechanism of Benggang.[Method]The soil samples from 3 soil layers in a soil profile(red soil layer,sandy soil layer and detritus layer)of a typical Benggang located in Changting County,Fujian Province,were collected and then exchanged with two kinds of electrolyte solutions(Na+and K+)at four different concentrations(0.005,0.01 and 0.1 mol L-1)to analyze their shear characteristics(deviatoric stress,cohesion and internal friction angle).[Result]① The red soil layer had the highest in deviatoric stress,cohesion and internal friction angle,followed by the sandy soil layer and the detritus layer.② The cohesion of the three soil layers exchanged with K+significantly increased as the electrolyte concentration increased,while exchanged with Na+showed the opposite trend.The cohesion of the red soil layer exchanged with K+(0.10 mol L-1)was 17.39%higher than that of the pure water treatment,whereas the internal friction angle of the soil did not differ significantly as the electrolyte concentration increased.③ The deviatoric stress and cohesion of the three soil layers exchanged with K+were significantly greater than those exchanged with Na+,and the cohesion rates of the red soil layer,sandy soil layer and detritus layer exchanged with K+were 9.99%,3.37%and 9.65%higher than that exchanged with Na+,respectively.However,the internal friction angle of the soil did not differ significantly.The effect of the water-soil chemical interaction on cohesion was significantly greater than that of the internal friction angle.[Conclusion]The influence of the concentration of Na+and K+on cohesion is significantly greater than that of internal friction angle.K+can increase the soil shear strength by increasing the soil cohesion and then improve the erosion resistance of the collapsed soil,and the soil shear strength increase with the K+electrolyte solutions.

BenggangCationDeviatoric stressCohesionInternal friction angle

黄碧妃、杨茂进、李灿娥、张越、蒋芳市、江凌、林金石、黄炎和

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福建警察学院刑事科学技术系,福建福州 350007

福建农林大学金山水土保持科教园,福建福州 350002

崩岗 离子 偏应力 黏聚力 内摩擦角

国家自然科学基金福建省水利科技项目

41907043KJg21009A

2024

土壤通报
中国土壤学会

土壤通报

CSTPCD北大核心
影响因子:0.818
ISSN:0564-3945
年,卷(期):2024.55(1)
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