天津城建大学学报
天津城建大學學報
천진성건대학학보
Journal of Tianjin CHENGJIAN University
2015年
2期
84-88
,共5页
非饱和土%土-水特征曲线%渗透系数%模型预测
非飽和土%土-水特徵麯線%滲透繫數%模型預測
비포화토%토-수특정곡선%삼투계수%모형예측
unsaturated soil%soil-water characteristic curve%permeability coefficient%prediction model
在分析土-水特征曲线及预测非饱和土渗透系数方法的基础上,以甘肃兰州重塑黄土为研究对象,采用非饱和土固结仪,测定初始饱和度相同、干密度不同的土样的土-水特征曲线,基于拟合效果较好的Fredlund&Xing三参数方程对试验数据进行拟合。以实测的土-水特征曲线为基础,采用 Childs & Collis-Geroge 预测非饱和渗透系数的模型,计算得到非饱和黄土渗透系数与基质吸力的关系,结果表明:渗透系数随吸力的增大呈非线性减小,两者的关系可用幂函数表示,这为黄土地区土体工程性质的研究和预测,如降雨入渗的边坡稳定性评价、非饱和地基湿陷变形计算等提供了理论支持。
在分析土-水特徵麯線及預測非飽和土滲透繫數方法的基礎上,以甘肅蘭州重塑黃土為研究對象,採用非飽和土固結儀,測定初始飽和度相同、榦密度不同的土樣的土-水特徵麯線,基于擬閤效果較好的Fredlund&Xing三參數方程對試驗數據進行擬閤。以實測的土-水特徵麯線為基礎,採用 Childs & Collis-Geroge 預測非飽和滲透繫數的模型,計算得到非飽和黃土滲透繫數與基質吸力的關繫,結果錶明:滲透繫數隨吸力的增大呈非線性減小,兩者的關繫可用冪函數錶示,這為黃土地區土體工程性質的研究和預測,如降雨入滲的邊坡穩定性評價、非飽和地基濕陷變形計算等提供瞭理論支持。
재분석토-수특정곡선급예측비포화토삼투계수방법적기출상,이감숙란주중소황토위연구대상,채용비포화토고결의,측정초시포화도상동、간밀도불동적토양적토-수특정곡선,기우의합효과교호적Fredlund&Xing삼삼수방정대시험수거진행의합。이실측적토-수특정곡선위기출,채용 Childs & Collis-Geroge 예측비포화삼투계수적모형,계산득도비포화황토삼투계수여기질흡력적관계,결과표명:삼투계수수흡력적증대정비선성감소,량자적관계가용멱함수표시,저위황토지구토체공정성질적연구화예측,여강우입삼적변파은정성평개、비포화지기습함변형계산등제공료이론지지。
Based on the analysis of soil water characteristic curve and prediction method of permeability coefficient, this paper takes remolded loess in Lanzhou of Gansu province as research objects. Soil water characteristic curve is obtained from the unsaturated soil consolidation apparatus, and the experimental data are then fitted with Fredlund&Xing Equation which has a better fitting effect. With the use of permeability prediction on Childs&Collis-Geroge Model, the relationship between permeability coefficient and matrix suction is built on the strength of the measurement of soil-water characteristic curve. The results show that the permeability coefficient decreases along with the nonlinear increase of the matrix suction, and they can be expressed in power function. It provides theoretical support to the research and prediction of engineering properties in loess area, such as slope stability evaluation under rainfall infiltration and the calculation of collapsibility deformation for unsaturated foundation.