Evolution characteristics and prediction model on suffusion of silty-sand subjected to seepage
Civil Engineering|更新时间:2023-09-19
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Evolution characteristics and prediction model on suffusion of silty-sand subjected to seepage
Journal of Civil and Environmental EngineeringVol. 45, Issue 5, Pages: 18-25(2023)
作者机构:
三峡大学 三峡库区地质灾害教育部重点实验室,湖北 宜昌 443002
作者简介:
CHEN Yong (1980- ), PhD, professor, doctorial supervisor, main research interests: soil-water coupling mechanism and slope stability evaluation, E-mail: cyonger@126.com.
XIA Zhenyao (corresponding author), PhD, professor, doctorial supervisor, E-mail: xzy_yc@126.com.
基金信息:
Key Project Supported by the Joint Funds of the National Natural Science Foundation of China(U2040207);Project of China Geological Survey(0001212020CC60002)
CHEN Yong, MING Zexin, XIA Zhenyao, et al. Evolution characteristics and prediction model on suffusion of silty-sand subjected to seepage[J]. Journal of Civil and Environmental Engineering, 2023, 45(5): 18-25.
DOI:
CHEN Yong, MING Zexin, XIA Zhenyao, et al. Evolution characteristics and prediction model on suffusion of silty-sand subjected to seepage[J]. Journal of Civil and Environmental Engineering, 2023, 45(5): 18-25. DOI: 10.11835/j.issn.2096-6717.2021.152.
Evolution characteristics and prediction model on suffusion of silty-sand subjected to seepage
Soil suffusion induced by long-term seepage generally lead to deformation or damage of soil structure. The suffusion experiments of silty sand had been accomplished by the independently developed seepage instrument
to study the particle loss process and suffusion evolution characteristics of silty sand with different void ratios induced by seepage of different hydraulic gradients
and the influential mechanism of factors is understood on the sand suffusion
then a model is established to predict the increase of particle loss with seepage duration and hydraulic gradient. Furthermore
the development patterns are revealed of particles size distribution and void ratio during suffusion based on the particle grading test and three phases relationship. The results show that: firstly
fine and sandy particles are both washed away by the long-term seepage and some dominant seepage channels will form subsequently in the samples
and then the internal local collapse and the overall differential settlement will be induced by continuous suffusion
until the water pressure mainly dissipates along the dominant channel to achieve the suffusion stability. Secondly
the initial void ratio or compactness is the main internal factor affecting the degree of the seepage suffusion of the soil
which directly changes the hydraulic gradient threshold
loss rate
cumulative total mass of particle movement and settlement deformation of sandy samples. The increase of the hydraulic gradient will also accelerate the particles loss
channel formation and suffusion stability. Thirdly
the prediction model fits the experiment result well
which can reflect evolution characteristics above and the influence on particles loss process of initial void ratio as well as the hydraulic gradient. Finally
the void ratio of samples will increase and the uniformity of particle size will decrease during sand suffusion.
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references
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