南水北调与水利科技
南水北調與水利科技
남수북조여수리과기
SOUTH-TO-NORTH WATER
2014年
2期
54-58
,共5页
粉土%含水率%压实度%屈服应力%极限状态线
粉土%含水率%壓實度%屈服應力%極限狀態線
분토%함수솔%압실도%굴복응력%겁한상태선
silt%water content%degree of compaction%yield stress%line of limit state
以潍坊中南部地区可作为高层基础持力层的粉土作为研究对象,通过室内试验,获得粉土颗粒级配曲线、粉土试样的基本物理力学特性指标,以及不同含水率和压实度条件下粉土试样的轴向变形与偏应力。对试验结果分析发现,粉土试样颗粒级配较好,能够达到较高的压实度;根据小于最优含水率时不同含水率条件下的屈服应力,确定了粉土层应变硬化与软化的临界点位置,认为含水率、压实度及围压是影响抗剪强度的主要因素;最终获得了小于最优含水率时区域性粉土剪切极限状态线拟合方程,并发现极限状态线的斜率 M(s)及其在偏应力轴上的截距μ(s)均为与含水率无关的常数。
以濰坊中南部地區可作為高層基礎持力層的粉土作為研究對象,通過室內試驗,穫得粉土顆粒級配麯線、粉土試樣的基本物理力學特性指標,以及不同含水率和壓實度條件下粉土試樣的軸嚮變形與偏應力。對試驗結果分析髮現,粉土試樣顆粒級配較好,能夠達到較高的壓實度;根據小于最優含水率時不同含水率條件下的屈服應力,確定瞭粉土層應變硬化與軟化的臨界點位置,認為含水率、壓實度及圍壓是影響抗剪彊度的主要因素;最終穫得瞭小于最優含水率時區域性粉土剪切極限狀態線擬閤方程,併髮現極限狀態線的斜率 M(s)及其在偏應力軸上的截距μ(s)均為與含水率無關的常數。
이유방중남부지구가작위고층기출지력층적분토작위연구대상,통과실내시험,획득분토과립급배곡선、분토시양적기본물리역학특성지표,이급불동함수솔화압실도조건하분토시양적축향변형여편응력。대시험결과분석발현,분토시양과립급배교호,능구체도교고적압실도;근거소우최우함수솔시불동함수솔조건하적굴복응력,학정료분토층응변경화여연화적림계점위치,인위함수솔、압실도급위압시영향항전강도적주요인소;최종획득료소우최우함수솔시구역성분토전절겁한상태선의합방정,병발현겁한상태선적사솔 M(s)급기재편응력축상적절거μ(s)균위여함수솔무관적상수。
The silt in the plain area of south-central Weifang can be used as the bearing stratum of the foundation for high-rise buildings .Laboratory experiments were conducted to obtain the grading curve of silt ,physical properties of silt ,and the axial de-formation and deviatoric stress of silt under different moisture contents and degrees of compaction .The test results showed that the silt has a good grading to reach a relatively high degree of compaction .According to the yield stress under different water contents which were less than the optimal water content ,the critical point of strain hardening and softening was determined . Water content ,degree of compaction ,and confining pressure were the main influence factors of the shear strength .The fitting e-quation of shear limit state for the regional silt was obtained when the water content was less than the optimal water content , and M(s)(slope) and μ(s)(intercept) were all constants which were independent of water content .