人民黄河
人民黃河
인민황하
Yellow River
2015年
11期
125-128
,共4页
膨胀土%挡土墙%侧向土压力%降雨入渗%模型试验
膨脹土%擋土牆%側嚮土壓力%降雨入滲%模型試驗
팽창토%당토장%측향토압력%강우입삼%모형시험
expansive soil%retaining wall%lateral earth pressure%rain infiltration%model test
膨胀土挡土墙在降雨时受侧向膨胀土压力的作用,容易发生失稳破坏。为深入认识降雨作用下膨胀土挡土墙发生变形破坏的机理,通过室内模拟降雨模型试验,对膨胀土挡土墙侧向土压力的变化规律进行了研究。研究表明:挡土墙后侧向膨胀土压力反应滞后于降雨,且在降雨初期呈顶部大、中间小的曲线分布形式,这容易导致挡土墙顶部产生剪切破坏;表层侧向土压力较深层的小,且较快达到稳定;深层侧向土压力在降雨之后随着雨水的下渗会产生递增,当其达到最大值后突然递减,这与深层土体浸水饱和产生软化有关。
膨脹土擋土牆在降雨時受側嚮膨脹土壓力的作用,容易髮生失穩破壞。為深入認識降雨作用下膨脹土擋土牆髮生變形破壞的機理,通過室內模擬降雨模型試驗,對膨脹土擋土牆側嚮土壓力的變化規律進行瞭研究。研究錶明:擋土牆後側嚮膨脹土壓力反應滯後于降雨,且在降雨初期呈頂部大、中間小的麯線分佈形式,這容易導緻擋土牆頂部產生剪切破壞;錶層側嚮土壓力較深層的小,且較快達到穩定;深層側嚮土壓力在降雨之後隨著雨水的下滲會產生遞增,噹其達到最大值後突然遞減,這與深層土體浸水飽和產生軟化有關。
팽창토당토장재강우시수측향팽창토압력적작용,용역발생실은파배。위심입인식강우작용하팽창토당토장발생변형파배적궤리,통과실내모의강우모형시험,대팽창토당토장측향토압력적변화규률진행료연구。연구표명:당토장후측향팽창토압력반응체후우강우,차재강우초기정정부대、중간소적곡선분포형식,저용역도치당토장정부산생전절파배;표층측향토압력교심층적소,차교쾌체도은정;심층측향토압력재강우지후수착우수적하삼회산생체증,당기체도최대치후돌연체감,저여심층토체침수포화산생연화유관。
Retaining wall working with expansive soil is prone to failure under rainfall infiltration, which is mainly caused by the lateral earth pressure from expansion soil. For further understanding this deformation failure mechanism, the paper studied the variation and distribution rules of lateral earth pressure on expansive soil retaining wall with a series of laboratory model tests under rainfall infiltration. The results show that the lateral earth pressure of expansive soil acting on the back of retaining wall respond lagging to rain, and the distribution curve shows the lateral earth pressure of expansive soil at top is bigger than that in the middle at beginning of rain, which is easy to cause shear failure at the top of retaining wall;the earth pressure at top is smaller and reaches stability sooner than that in deep part;the earth pressure in deep part progressive increases as the rainfall infiltration, and suddenly diminishes until reaching the maximum because deep soil is saturation softened.