水利学报
水利學報
수리학보
2015年
5期
612-618
,共7页
陈勇%韦双%Dave Chana
陳勇%韋雙%Dave Chana
진용%위쌍%Dave Chana
循环加卸载%非等向受压%孔隙水压力%应力路径%有效应力比
循環加卸載%非等嚮受壓%孔隙水壓力%應力路徑%有效應力比
순배가사재%비등향수압%공극수압력%응력로경%유효응력비
Cyclic loading and unloading%Anisotropic compression%Pore water pressure%Stress path triaxi-al test%Effective stress ratio
水库运行期水位每年周期性涨落,岸坡土体在库水循环加卸载作用下会发生不同程度的阶梯状变形。为探求循环加卸载对岸坡深部变形的诱发机理,本文以水库防洪限制水位以下岸坡土体为研究对象,在饱和土应力路径三轴试验过程中,控制非等向受压试样的孔隙水压力周期变化,模拟岸坡土体的水力-力学状态,实时测定土体的周期性变形特性及破坏特征。研究结果表明:等偏应力孔压循环加卸载过程中,试样剪应变为台阶式上升趋势,而体应变是循环的弹性变化;孔压持续增大造成试样破坏呈现脆变和剪胀的特征。最后,结合等偏应力孔压增大条件下粉质黏土的破坏特征与常规三轴剪切试验成果,对比两种应力路径下试样的有效应力比和剪应变的发展过程,分析了其强度差异的内在原因。
水庫運行期水位每年週期性漲落,岸坡土體在庫水循環加卸載作用下會髮生不同程度的階梯狀變形。為探求循環加卸載對岸坡深部變形的誘髮機理,本文以水庫防洪限製水位以下岸坡土體為研究對象,在飽和土應力路徑三軸試驗過程中,控製非等嚮受壓試樣的孔隙水壓力週期變化,模擬岸坡土體的水力-力學狀態,實時測定土體的週期性變形特性及破壞特徵。研究結果錶明:等偏應力孔壓循環加卸載過程中,試樣剪應變為檯階式上升趨勢,而體應變是循環的彈性變化;孔壓持續增大造成試樣破壞呈現脆變和剪脹的特徵。最後,結閤等偏應力孔壓增大條件下粉質黏土的破壞特徵與常規三軸剪切試驗成果,對比兩種應力路徑下試樣的有效應力比和剪應變的髮展過程,分析瞭其彊度差異的內在原因。
수고운행기수위매년주기성창락,안파토체재고수순배가사재작용하회발생불동정도적계제상변형。위탐구순배가사재대안파심부변형적유발궤리,본문이수고방홍한제수위이하안파토체위연구대상,재포화토응력로경삼축시험과정중,공제비등향수압시양적공극수압력주기변화,모의안파토체적수력-역학상태,실시측정토체적주기성변형특성급파배특정。연구결과표명:등편응력공압순배가사재과정중,시양전응변위태계식상승추세,이체응변시순배적탄성변화;공압지속증대조성시양파배정현취변화전창적특정。최후,결합등편응력공압증대조건하분질점토적파배특정여상규삼축전절시험성과,대비량충응력로경하시양적유효응력비화전응변적발전과정,분석료기강도차이적내재원인。
The reservoir water level periodicly fluctuates every year, and different degree of ladder shape deformation will occur on the soil of the bank slope under the cyclic loading and unloading action of reser?voir water. To explore the induced mechanism of deep soil deformation, in this paper, the deep silty clay of bank slope is selected as the main research object, it’s hydraulic and mechanical state are simulated in the stress-path triaxial test by controlling the cyclic loading and unloading of pore water pressure in the condition of anisotropic compression, and it’s deformation and damage characteristics are real-time mea?sured and analyzed. The result shows that the sample shear strain tends to terraced rising and the volumet?ric strain presents elastic change during the cyclic loading and unloading of pore water pressure under a constant deviatoric stress, and the samples are destroyed by continuous increasing pore water pressure with the characteristics of embrittlement and dilatancy. Finalily, the evolution processes of effective stress ratio and shear strain are contrasted between two different stress paths in combination with the result of conven?tional triaxial test,and the internal mechanism of their shear strength differences is analyzed.