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
2013年
3期
640-648
,共9页
土力学%黄土高填方地基%细观变形机制%土电阻率%初始饱和度%固结蠕变变形
土力學%黃土高填方地基%細觀變形機製%土電阻率%初始飽和度%固結蠕變變形
토역학%황토고전방지기%세관변형궤제%토전조솔%초시포화도%고결연변변형
soil mechanics%loess high-fill foundation%mesoscopic deformation mechanism%soil electrical resistivity%initial saturation%consolidation and creep deformation
为揭示黄土高填方地基产生变形的细观机制,以吕梁机场试验段为背景,基于土电阻率原理,研发土电阻率–固结联合测定仪,通过原位监测、现场取样和大量室内试验得到不同初始饱和度的Q3黄土在恒定荷载下的电阻率动态变化规律,提出以最优含水率为界限的Q3黄土“电阻率–应变曲线”模型,得到Q3黄土在恒定荷载下的水分迁移规律和结构变化特征.研究结果表明:高填方顶面工后总变形包括两大部分,即地基土及填方表面以下一定深度内填筑体的排水固结变形和深部超固结土的蠕变变形;初步揭示土体产生变形的细观演化规律,同时也为黄土高填方土体的本构模型建立和数值分析中模型的合理选取提供科学依据.
為揭示黃土高填方地基產生變形的細觀機製,以呂樑機場試驗段為揹景,基于土電阻率原理,研髮土電阻率–固結聯閤測定儀,通過原位鑑測、現場取樣和大量室內試驗得到不同初始飽和度的Q3黃土在恆定荷載下的電阻率動態變化規律,提齣以最優含水率為界限的Q3黃土“電阻率–應變麯線”模型,得到Q3黃土在恆定荷載下的水分遷移規律和結構變化特徵.研究結果錶明:高填方頂麵工後總變形包括兩大部分,即地基土及填方錶麵以下一定深度內填築體的排水固結變形和深部超固結土的蠕變變形;初步揭示土體產生變形的細觀縯化規律,同時也為黃土高填方土體的本構模型建立和數值分析中模型的閤理選取提供科學依據.
위게시황토고전방지기산생변형적세관궤제,이려량궤장시험단위배경,기우토전조솔원리,연발토전조솔–고결연합측정의,통과원위감측、현장취양화대량실내시험득도불동초시포화도적Q3황토재항정하재하적전조솔동태변화규률,제출이최우함수솔위계한적Q3황토“전조솔–응변곡선”모형,득도Q3황토재항정하재하적수분천이규률화결구변화특정.연구결과표명:고전방정면공후총변형포괄량대부분,즉지기토급전방표면이하일정심도내전축체적배수고결변형화심부초고결토적연변변형;초보게시토체산생변형적세관연화규률,동시야위황토고전방토체적본구모형건립화수치분석중모형적합리선취제공과학의거.
@@@@In order to reveal the mesoscopic deformation mechanism of loess high-fill foundation of Luliang airport,the soil electrical resistivity-consolidation combination measuring instrument are developed based on the principle of soil electrical resistivity. The dynamic variation law of the electrical resistivity of Q3 loess are obtained through in-situ monitoring,field sampling and laboratory test under different initial saturations and constant load. The electrical resistivity-strain curve model of Q3 loess to the limits of optimum moisture content is proposed;and its moisture migration and structural changing characteristics under constant load are also obtained. The study results show that the post-construction deformation of the loess high-fill foundation top surface is composed of the consolidation deformation of initial foundation and the fill bellow the surface to a certain depth and the long-term creep deformation of deep overconsolidated soil. The mesoscopic deformation mechanism of soil is revealed initially;and the study provides scientific basis for the establishment of loess high-fill soil constitutive model and reasonable selection of the numerical analysis model.