摘要
在滑坡地质灾害中遇到的滑带土大多数是非饱和土,研究吸力对非饱和滑带土c、φ值的影响,对于滑坡防治具有十分重要的意义。通过不同基质吸力和剪切速率的条件下的四联直剪试验,探讨了基质吸力与非饱和粘性滑带土抗剪强度的关系。试验结果表明,在同一基质吸力条件下,抗剪强度随轴向荷载的增大而增大,且保持平稳线性增长的趋势;随着吸力值的增大,其总粘聚力与内摩擦角均呈现增大趋势。对于总粘聚力来说,当基质吸力≤100 kPa时,随着吸力的增大,总粘聚力增长曲线斜率较大,增长速率较快;当基质吸力>100 kPa时,随着吸力值的增大,总粘聚力增长曲线斜率放缓,增长速率减慢;但总体处于平稳增长的态势。对于内摩擦角来说,当基质吸力≤50 kPa时,随着吸力的增大,内摩擦角增长曲线斜率较大,增长速率较快;当基质吸力>50 kPa时,随着吸力值的增大,内摩擦角增长曲线斜率放缓,增长速率减慢。
It is very important to study the influence of suction on unsaturated slip soil and shear strength in landslide geological disaster.The relationship between matrix suction and the shear strength of unsaturated viscous slippage is discussed through the quadruplet direct shear tests under the condition of different substrate suction and shear rate.The experimental results show that the shear strength increases with the increase of axial load in the same matrix,and the trend of stable linear growth is maintained.With the increase of suction value,the total cohesion and internal friction angle show an increasing trend.When the matrix suction is less than or equal to 100 kPa,with the increase of suction force,the growth curve of the total cohesive force growth curve is larger and the growth rate is faster.When the matrix suction is great than 100 kPa,the slope of the total cohesion growth curve slows down and the growth rate slows down with the suction value increasing.But the overall situation is on the steady rise.When matrix suction is less than or equal to 50 kPa,with the increase of suction force,the growth curve of internal friction angle is larger and the growth rate is faster.When the matrix suction is greater than50 kPa,with the increase of suction value,the slope of the growth curve of internal friction angle decreases,and the growth rate slows down.
作者
甘建军
GAN Jianjun(National-Local Joint Engineering Laboratory of Water Engineering Safety and Efficient Utilization of Resources in Poyang Lake Watershed,Nanchang Institute of Technology,Nanchang 330099,China)
出处
《南昌工程学院学报》
CAS
2018年第4期1-5,共5页
Journal of Nanchang Institute of Technology
基金
江西省教育厅科学技术研究项目(GJJ151124)
国家自然科学基金应急管理资助项目(41641023)
江西省科技厅科技计划项目(20161BBG70051)
江西省交通厅重点科技项目(2016H0022)
江西省科技重点研发计划项目(20077BBG70046)