防灾减灾工程学报
防災減災工程學報
방재감재공정학보
JOURNAL OF DISASTER PREVENTION AND MITIGATION ENGINEERING
2009年
6期
604-609
,共6页
张振东%栾茂田%金丹%许成顺
張振東%欒茂田%金丹%許成順
장진동%란무전%금단%허성순
单调剪切%总主应力方向%孔隙水压力%各向异性%水平沉积面
單調剪切%總主應力方嚮%孔隙水壓力%各嚮異性%水平沉積麵
단조전절%총주응력방향%공극수압력%각향이성%수평침적면
monotonic shear%orientation of major principal stress%pore water pressure%anisotropy%horizontal sedimentary plane
利用土工静力一动力液压三轴一扭转多功能剪切仪,针对相对密度D_r=30%的福建标准砂,进行了不排水条件下的单调剪切试验.在剪切过程中,控制平均固结应力和中主应力系数保持不变,而总主应力方向不固定.与剪切过程中总主应力方向固定不变条件下的单调剪切试验进行了对比分析.试验研究表明,当饱和砂土试样具有水平沉积面时,初始固结主应力方向与剪切方向的不同组合,导致单调剪切过程中总的主应力方向的不断变化,从而显著地影响着饱和砂土不排水单调剪切特性.总的主应力方向是影响饱和砂土不排水单调剪切特性的最根本原因.
利用土工靜力一動力液壓三軸一扭轉多功能剪切儀,針對相對密度D_r=30%的福建標準砂,進行瞭不排水條件下的單調剪切試驗.在剪切過程中,控製平均固結應力和中主應力繫數保持不變,而總主應力方嚮不固定.與剪切過程中總主應力方嚮固定不變條件下的單調剪切試驗進行瞭對比分析.試驗研究錶明,噹飽和砂土試樣具有水平沉積麵時,初始固結主應力方嚮與剪切方嚮的不同組閤,導緻單調剪切過程中總的主應力方嚮的不斷變化,從而顯著地影響著飽和砂土不排水單調剪切特性.總的主應力方嚮是影響飽和砂土不排水單調剪切特性的最根本原因.
이용토공정력일동력액압삼축일뉴전다공능전절의,침대상대밀도D_r=30%적복건표준사,진행료불배수조건하적단조전절시험.재전절과정중,공제평균고결응력화중주응력계수보지불변,이총주응력방향불고정.여전절과정중총주응력방향고정불변조건하적단조전절시험진행료대비분석.시험연구표명,당포화사토시양구유수평침적면시,초시고결주응력방향여전절방향적불동조합,도치단조전절과정중총적주응력방향적불단변화,종이현저지영향착포화사토불배수단조전절특성.총적주응력방향시영향포화사토불배수단조전절특성적최근본원인.
Using the soil static and dynamic universal triaxial and torsional shear apparatus,a series of undrained monotonic shear tests are performed for saturated Fujian standard sands with a relative density of 30%.The mean consolidation stress and the coefficients of the intermediate principal stress are invariable while the orientation of principal stress is variable in the proceeding of tests.By contrasting with the monotonic shear test results under the condition that the orientation of principal stress is invariable,it is concluded that when the saturated sand sample has horizontal sedimentary plane,the different combinations of initial orientation of major principal stress and direction of monotonic shearing make the actual orientation of major principal stress different during the shearing,which affecting the undrained monotonic shearing behavior of sand remarkably.The actual orientation of major principal stress is the most essential factor which affects the undrained monotonic shearing behavior of the saturated sand.