岩土力学
巖土力學
암토역학
ROCK AND SOIL MECHANICS
2014年
9期
2507-2514
,共8页
姜景山%程展林%左永振%丁红顺
薑景山%程展林%左永振%丁紅順
강경산%정전림%좌영진%정홍순
粗粒土%CT试验%三轴试验%流变%颗粒运动%变形机制%应力-应变关系%细观组构
粗粒土%CT試驗%三軸試驗%流變%顆粒運動%變形機製%應力-應變關繫%細觀組構
조립토%CT시험%삼축시험%류변%과립운동%변형궤제%응력-응변관계%세관조구
coarse-grained soil%CT test%triaxial test%rheology%particle movement%deformation mechanism%stress-strain relationship%mesoscopic fabric
一些土石坝在建成后后期变形明显,这与粗粒土的流变密切相关。目前,粗粒土流变研究主要集中在力学性质试验和本构模型研究等方面,较少对粗粒土流变中的颗粒运动规律进行研究。通过单级配矾石CT三轴流变试验,研究了粗粒土流变过程中颗粒运动规律。试验结果表明,粗粒土的流变过程就是粗粒土颗粒位置相互调整的过程,即颗粒从不稳定结构状态向稳定结构状态调整变化的过程,直到所有颗粒的能量都达到最小状态,此时颗粒不再发生错动、转动和破碎,粗粒土达到流变稳定状态。对粗粒土三轴流变过程中颗粒运动规律的认识,有助于加深对粗粒土流变性质的了解,为工程应用提供参考。
一些土石壩在建成後後期變形明顯,這與粗粒土的流變密切相關。目前,粗粒土流變研究主要集中在力學性質試驗和本構模型研究等方麵,較少對粗粒土流變中的顆粒運動規律進行研究。通過單級配礬石CT三軸流變試驗,研究瞭粗粒土流變過程中顆粒運動規律。試驗結果錶明,粗粒土的流變過程就是粗粒土顆粒位置相互調整的過程,即顆粒從不穩定結構狀態嚮穩定結構狀態調整變化的過程,直到所有顆粒的能量都達到最小狀態,此時顆粒不再髮生錯動、轉動和破碎,粗粒土達到流變穩定狀態。對粗粒土三軸流變過程中顆粒運動規律的認識,有助于加深對粗粒土流變性質的瞭解,為工程應用提供參攷。
일사토석패재건성후후기변형명현,저여조립토적류변밀절상관。목전,조립토류변연구주요집중재역학성질시험화본구모형연구등방면,교소대조립토류변중적과립운동규률진행연구。통과단급배반석CT삼축류변시험,연구료조립토류변과정중과립운동규률。시험결과표명,조립토적류변과정취시조립토과립위치상호조정적과정,즉과립종불은정결구상태향은정결구상태조정변화적과정,직도소유과립적능량도체도최소상태,차시과립불재발생착동、전동화파쇄,조립토체도류변은정상태。대조립토삼축류변과정중과립운동규률적인식,유조우가심대조립토류변성질적료해,위공정응용제공삼고。
Some earth and rockfill dams have significant later stage deformations after constructions, which are closely related to the rheology of coarse-grained soils. The study of rheology for coarse-grained soils mainly focuses on mechanical tests and constitutive models. However, particle movement of coarse-grained soils in rheological test is not well evaluated. The CT triaxial rheological test of a single grading aluminite is conducted to investigate the particle movement of coarse-grained soils. The test results show that the rheological process is an adjustment process of particle position from unstable structure state to stable structure state for particles in coarse-grained soils. The rheological process will not stop until all particles reach the minimum energy state. No particles move, rotate, and break under the rheological steady state. The investigation of particle movement for coarse-grained soils contributes to the understanding of rheological behavior of coarse-grained soils, and also helps to provide reference to engineering application.