摘要
土水特征曲线(SWCC)的影响因素有很多,为了探究其主要影响因素,采用压力板仪测定了初始干密度为1.78 g/cm^3的土样A和初始干密度为1.65 g/cm^3、经固结试验后干密度为1.78 g/cm^3的土样B它们的初始脱湿线,发现二者基本重合。这说明在其他条件相同的情况下,是干密度而非固结压力决定了SWCC形态。测定了土样B的主吸湿线和主脱湿线,并采用毛细滞回简化模型计算了土样的主脱湿线,计算所得主脱湿线和试验得到的主脱湿线基本重合,验证了该模型的有效性。
There are many factors affecting the soil-water characteristic curve( SWCC). Soil sample A with initial dry density of 1. 78 g/cm3 and soil sample B with initial dry density of 1. 65 g/cm3 and dry density of 1. 78 g/cm3 after consolidation were tested by pressure plate apparatus and their initial drying curves were determined. It was found that the two curves are basically coincident,showing that dry density rather than the consolidation pressure is the determining factor in SWCC morphology. The main drying and wetting curves of soil sample B were measured and the main drying curve was simulated by using the simplified capillary hysteresis model. The calculated main drying curve was basically the same with the measured one,showing that the presented model is correct.
作者
李幻
谭晔
梁文鹏
吴家琦
张蒙飞
黄志全
LI Huan;TAN Ye;LIANG Wenpeng;WU Jiaqi;ZHANG Mengfei;HUANG Zhiquan(School of Resources and Environment,North China University of Water Conservancy and Electric Power,Zhengzhou 450011,China;Xinjiang Institute of Engineering,Urumqi 830091,China)
出处
《人民长江》
北大核心
2018年第14期110-114,共5页
Yangtze River
基金
国家自然科学基金项目(41202246)
河南省科技创新人才计划项目(154100510006)
河南省重点科技攻关项目(152102210111
132102210113)
新疆自治区高层次人才引进工程
新疆维吾尔自治区科技援疆项目(201491105)
华北水利水电大学研究生教育创新计划基金(YK2016-03)
关键词
非饱和土
土水特征曲线
固结试验
毛细滞回简化模型
unsaturated soil
soil water characteristic curve
consolidation test
simplified capillary hysteresis model