岩石力学与工程学报
巖石力學與工程學報
암석역학여공정학보
CHINESE JOURNAL OF ROCK MECHANICS AND ENGINEERING
2014年
1期
125-133
,共9页
刘汉香%许强%王龙%侯红娟
劉漢香%許彊%王龍%侯紅娟
류한향%허강%왕룡%후홍연
边坡工程%岩质斜坡%振动台模型试验%地震波频率%加速度响应
邊坡工程%巖質斜坡%振動檯模型試驗%地震波頻率%加速度響應
변파공정%암질사파%진동태모형시험%지진파빈솔%가속도향응
slope engineering%rock slope%shaking table test%frequency of seismic wave%acceleration response
斜坡在地震作用下的动力响应是地震波各频率组分与斜坡体共同作用的结果,不同的地震波频率将产生不同的斜坡响应。依托于振动台模型试验,针对均质和层状结构模型斜坡,首先分析试验不同阶段白噪声激振下的动力特性,得出两模型斜坡的共振频率呈现降低趋势,模型内部结构趋于松散,且水平向加速度的第1阶共振频率要低于竖直向加速度的第1阶共振频率。着重分析斜坡加速度动力响应规律及其与地震波频率变化的相关性,结果表明:(1)两模型的水平向加速度响应在相对坡底高程(h/H>1/2)时具有明显的高程放大效应,竖直向加速度响应的高程放大效应出现在h/H<3/4的部位,且这一特征与激振频率的大小无关;(2)在同等激振强度下,随着激振频率增大,越靠近模型斜坡的共振频率,两模型斜坡水平向加速度的响应程度也越高,而竖直向加速度响应强度与激振频率的相关性因模型斜坡结构不同而异;(3)激振强度增加时伴随的模型结构恶化(即共振频率降低)并不一定导致加速度响应强度的减弱,相反,高频激振波由于更加接近模型的共振频率,使得响应减弱的可能性变小;(4)层状结构模型斜坡的加速度响应强度大于均质结构模型斜坡,当激振强度较大时,这种层状结构效应与激振频率的相关性增强,表现为随着激振频率增大,该效应对水平向加速度而言逐渐明显,对竖直向加速度而言则相对减弱。
斜坡在地震作用下的動力響應是地震波各頻率組分與斜坡體共同作用的結果,不同的地震波頻率將產生不同的斜坡響應。依託于振動檯模型試驗,針對均質和層狀結構模型斜坡,首先分析試驗不同階段白譟聲激振下的動力特性,得齣兩模型斜坡的共振頻率呈現降低趨勢,模型內部結構趨于鬆散,且水平嚮加速度的第1階共振頻率要低于豎直嚮加速度的第1階共振頻率。著重分析斜坡加速度動力響應規律及其與地震波頻率變化的相關性,結果錶明:(1)兩模型的水平嚮加速度響應在相對坡底高程(h/H>1/2)時具有明顯的高程放大效應,豎直嚮加速度響應的高程放大效應齣現在h/H<3/4的部位,且這一特徵與激振頻率的大小無關;(2)在同等激振彊度下,隨著激振頻率增大,越靠近模型斜坡的共振頻率,兩模型斜坡水平嚮加速度的響應程度也越高,而豎直嚮加速度響應彊度與激振頻率的相關性因模型斜坡結構不同而異;(3)激振彊度增加時伴隨的模型結構噁化(即共振頻率降低)併不一定導緻加速度響應彊度的減弱,相反,高頻激振波由于更加接近模型的共振頻率,使得響應減弱的可能性變小;(4)層狀結構模型斜坡的加速度響應彊度大于均質結構模型斜坡,噹激振彊度較大時,這種層狀結構效應與激振頻率的相關性增彊,錶現為隨著激振頻率增大,該效應對水平嚮加速度而言逐漸明顯,對豎直嚮加速度而言則相對減弱。
사파재지진작용하적동력향응시지진파각빈솔조분여사파체공동작용적결과,불동적지진파빈솔장산생불동적사파향응。의탁우진동태모형시험,침대균질화층상결구모형사파,수선분석시험불동계단백조성격진하적동력특성,득출량모형사파적공진빈솔정현강저추세,모형내부결구추우송산,차수평향가속도적제1계공진빈솔요저우수직향가속도적제1계공진빈솔。착중분석사파가속도동력향응규률급기여지진파빈솔변화적상관성,결과표명:(1)량모형적수평향가속도향응재상대파저고정(h/H>1/2)시구유명현적고정방대효응,수직향가속도향응적고정방대효응출현재h/H<3/4적부위,차저일특정여격진빈솔적대소무관;(2)재동등격진강도하,수착격진빈솔증대,월고근모형사파적공진빈솔,량모형사파수평향가속도적향응정도야월고,이수직향가속도향응강도여격진빈솔적상관성인모형사파결구불동이이;(3)격진강도증가시반수적모형결구악화(즉공진빈솔강저)병불일정도치가속도향응강도적감약,상반,고빈격진파유우경가접근모형적공진빈솔,사득향응감약적가능성변소;(4)층상결구모형사파적가속도향응강도대우균질결구모형사파,당격진강도교대시,저충층상결구효응여격진빈솔적상관성증강,표현위수착격진빈솔증대,해효응대수평향가속도이언축점명현,대수직향가속도이언칙상대감약。
Slope dynamic response to an earthquake is a product of interaction between seismic waves of complex frequencies and slope body;different frequency components induce different slope responses. Through shaking table tests,effect of wave frequency on two model slopes is analyzed. The two model slopes are composed of the same materials of high strength,but different structures,isotropic and layered. Firstly,dynamic characteristics of model slopes calculated through excitations of white noises show that,resonance frequency of each model decreases and the internal structure becomes loose as the test is going on;and the first resonance frequency of horizontal component acceleration is larger than that of vertical component acceleration. Then,emphasis is put on the slope acceleration responses and their correlations with changing frequencies. Results show that:(1) Obvious topographic amplification occurs in relative elevation h/H>1/2 for horizontal component acceleration;while topographic amplification occurs in relative elevation h/H<3/4 for vertical component acceleration;and the phenomena are independent of the excitation frequency. (2) Under the same excitation intensity,the horizontal component motion produces stronger response as the excitation frequency is increasing,more close to the resonance frequency. The correlation between vertical component response and frequency depends on the structure of model slope. (3) When the excitation intensity increases,the decay of slope structure (i.e. decease of resonance frequency) does not always cause attenuation of response,instead,high frequency excitation still can produce strong response due to the narrowing gap between excitation frequency and resonance frequency. (4) The layered model slope responses more severely than the isotropic model slope. Under strong motion,the structure effect is intensified for horizontal component and weakened for vertical component as excitation frequency increases.