攀枝花機場12#滑坡形成機理的離心模型試驗研究
[Abstract]:There are many airports under construction or have been built in southwest China. Due to the numerous mountainous areas and complicated terrain and geological conditions, the airport construction is characterized by many excavations, high fill and high seismic intensity. The instability of high-fill slope also brings serious loss to people's life, property and economic construction. Therefore, the study of instability mechanism of high fill slope is of great significance to engineering construction. In this paper, with the aid of 500gt geo-centrifuge of Chengdu University of Technology, taking the No. 12 landslide of Panzhihua Airport as the background, the deformation and failure characteristics of the slope under the condition of rainfall and groundwater are simulated in order to reproduce the failure process. Through high speed camera and a series of test elements, the mechanism of sliding failure is analyzed and discussed. The main research results are as follows: (1) A set of new centrifugal model rainfall test device is designed and developed, including atomization centrifugal spray system and pressure system. Lighting system, the device can be sealed with the model box, effectively solve the previous centrifuge rainfall uneven problem; (2) based on Panzhihua Airport fill body as the prototype according to the model to build a three-dimensional centrifuge model NC400, The distribution of sand-mud and mudstone is considered emphatically, and three rows of anti-slide piles are considered. The simulation device of pavement and groundwater is added to simulate the real situation of airport high fill as far as possible. The rainfall simulation is carried out at the acceleration of 150g in order to restore the deformation and failure process of the high fill slope. More than 60 earth pressure sensors, pore water pressure sensors, strain gauges and displacement sensors are used. (3) according to the experimental results and monitoring elements, the slope is mainly composed of subsidence creep at the initial stage, the maximum settlement is about 4 cm, equivalent to 6 m prototype. At the beginning of deformation, it is assumed that the line formed a fine tensile fracture, and after about 200s of rainfall, the U1 pore water pressure sensor located in the slope shoulder was the first to react. And with the increase of infiltration pore pressure, the maximum is 84.43 KPA. (4) after two torrential rains in the deformation stage, the slope body slides obviously. At this stage, the pressure on the pile has been increased to 66.22 MPa due to the continuous creep earth pressure has been reduced. It can also be seen from the strain data of the pile body that the internal force of the back row pile is much greater than that of the front row, and the internal force of the pile body facing the sliding direction is greater than the back side. (5) the damage of the experimental model starts from the slope top platform, and the deformation of the shoulder of the slope is the greatest. And from the plane, the deformation on the left side is larger than that on the right side. The experimental results are similar to the deformation and failure process of the No. 12 landslide. The landslide sliding mechanism is verified by deepening the understanding of landslide sliding mechanism from the aspects of slope deformation and fracture characteristics, anti-slide pile force, pore pressure and soil pressure, etc.
【學(xué)位授予單位】:成都理工大學(xué)
【學(xué)位級別】:碩士
【學(xué)位授予年份】:2017
【分類號】:P642.22
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