西南地區(qū)某機(jī)場(chǎng)高填方邊坡變形破壞特征及穩(wěn)定性分析
[Abstract]:The airport is a high-fill airport. After the backfilling of the airport, crack deformation occurs in the soil surface area and channel area of the fill slope of the airport's No. 4 / 5 section. According to the monitoring data provided by the monitoring unit, the deformation in this area has not been stabilized. The convergent trend of the slope is not obvious. The deformation of the slope at present may affect the stability of the upper filling area and the upper runway area of the slope, thus threatening the overall stability of the slope, further affecting the safety of the channel and threatening the take-off and landing of the aircraft. The purpose of this project is to find out the causes and characteristics of the deformation of the slope, and to provide the basis for dealing with the deformation in the region. The deformation range of the fill is furthest bounded by the cracks on the ground of the runway, and the front edge is mainly on the upper part of the backpressure platform of the slope according to the monitoring data of the previous deformation, and the deformation on both sides is not obvious. There is no obvious lateral shear fracture, and the slope is generally similar to the ring chair (ice bucket) distribution on the plane. The main deformation ranges are about 200m in length, 400m in width and 25m in average thickness. The slope shape of slope is steep and gentle from high to low, and the profile is zigzag. The slope began to be filled on April 14, 2012. When the slope was filled to 1952m in December 2012 (the design elevation was 1964m), a large displacement occurred on the inner slope of the backpressure platform, and more damage was caused to the inner drainage ditch of the platform. The soil layer with a width of 25m and a thickness of 30m is added outside the backpressure platform, and the soil layer with a thickness of 20m is added in the upper part of the backpressure platform, and then the top of the slope is filled in the middle of April 2013. The height is about 12m at the end of May 2013 and the height of the soil layer is about 12m at the end of May 2013. After backpressure treatment, the slope deformation converges obviously, the deformation area is smooth, and the addition of backpressure platform plays a better role in pressing foot. Based on the data of emergency survey, deep displacement monitoring and ground displacement monitoring of the deformation slope, the paper puts forward some measures to control the slope with the high filling deformation, and puts forward some measures to control the slope with anti-slide pile and the anti-slide pile soil layer by the anti-slide pile soil anti-pressure treatment. The slope deformation is restrained and is in a stable state. In this paper, the development characteristics, influencing conditions and mechanism of the high fill deformation slope are analyzed, and the stability of the deformation slope is calculated quantitatively.
【學(xué)位授予單位】:西南交通大學(xué)
【學(xué)位級(jí)別】:碩士
【學(xué)位授予年份】:2017
【分類號(hào)】:V351.1;TU43
【參考文獻(xiàn)】
相關(guān)期刊論文 前10條
1 陳建君;趙昌貴;;鋼管樁在滑坡應(yīng)急搶險(xiǎn)中的應(yīng)用[J];山西建筑;2014年30期
2 錢(qián)日高;宋文平;;地質(zhì)模型與物理模擬在建立滑坡預(yù)報(bào)模型和預(yù)報(bào)判據(jù)中的綜合應(yīng)用[J];科技致富向?qū)?2012年12期
3 張開(kāi);;滑坡國(guó)內(nèi)外研究概況的綜述[J];科技創(chuàng)新導(dǎo)報(bào);2012年04期
4 李亮;褚雪松;;An Improved Particle Swarm Optimization Algorithm with Harmony Strategy for the Location of Critical Slip Surface of Slopes[J];China Ocean Engineering;2011年02期
5 張金山;沈興菊;魏軍林;;泥石流堆積扇發(fā)育演化特征觀測(cè)研究[J];長(zhǎng)江流域資源與環(huán)境;2010年12期
6 王運(yùn)生;徐鴻彪;羅永紅;吳俊峰;;地震高位滑坡形成條件及拋射運(yùn)動(dòng)程式研究[J];巖石力學(xué)與工程學(xué)報(bào);2009年11期
7 馮文凱;石豫川;何川;鮑立新;;恩子坪2~#滑坡特征及穩(wěn)定性三維數(shù)值模擬分析[J];水文地質(zhì)工程地質(zhì);2008年05期
8 陳祿俊;邢愛(ài)國(guó);陳龍珠;殷躍平;童立強(qiáng);;高速遠(yuǎn)程滑坡飛行數(shù)值分析[J];水文地質(zhì)工程地質(zhì);2008年05期
9 何冬曉;謝世友;孫在斌;鄧曉軍;;中國(guó)地質(zhì)災(zāi)害發(fā)育特點(diǎn)及防治對(duì)策綜述[J];四川地質(zhì)學(xué)報(bào);2007年01期
10 劉傳正;張明霞;孟暉;;論地質(zhì)災(zāi)害群測(cè)群防體系[J];防災(zāi)減災(zāi)工程學(xué)報(bào);2006年02期
相關(guān)碩士學(xué)位論文 前3條
1 黃河清;地震誘發(fā)滑坡(碎屑流)成因機(jī)理及運(yùn)動(dòng)學(xué)特性初步研究[D];成都理工大學(xué);2010年
2 陳江;貴州省六盤(pán)水機(jī)場(chǎng)道中高填方邊坡穩(wěn)定性研究[D];成都理工大學(xué);2008年
3 張寧;荔波機(jī)場(chǎng)高填方邊坡穩(wěn)定性研究[D];四川大學(xué);2003年
,本文編號(hào):2209885
本文鏈接:http://sikaile.net/kejilunwen/diqiudizhi/2209885.html