摘要
以甘肃省兰州市青白石乡的黄土为研究对象,通过对3组相同含水率,不同干密度(1.5,1.6,1.7)下的重塑试样进行毛细吸水试验,研究了干密度对毛细吸水的影响。研究发现:干密度越大,毛细吸水速率越慢,水分到达顶端需要的时间越长;试样底部的含水率最高,在26%~30%之间,含水率沿着试样向上逐渐降低,在试样中部4 cm处出现明显变化,0~4 cm含水率变化幅度大,4~8 cm含水率变化幅度小,说明毛细作用主要集中在试样的中下部分;在相同初始含水率条件下,干密度越小,毛细作用越明显。
In order to investigate the influence of capillary water absorption by different dry density,we conduct free capillary water absorption test by using 3 different dry density(1. 5,1. 6,1. 7) remodeled loess which from Qingbaishi village,Lanzhou,Gansu province. Research shows that:(1) The greater the dry density,the slower the capillary water absorption rate,and the longer it takes for the moisture to reach the top;(2) The moisture content of the sample at the bottom of the sample is the highest,between 26 % - 30 %,the moisture content along the sample gradually decreased,at the middle of the sample 4 cm significant changes,0 - 4 cm water content changes is large,the rate of change is small at 4 - 8 cm. Indicating that the capillary effect is mainly concentrated in the middle and lower part of the sample;(3) Under the same initial moisture content,the smaller the dry density,the more obvious the capillary effect.
作者
张文辉
杨烜宇
ZHANG Wen - hui;YANG Xuan - yu(School of Civil Engineering and Mechanics , Lanzhou University , Lanzhou 730000, Chin)
出处
《地下水》
2018年第2期133-134,200,共3页
Ground water
关键词
黄土
毛细作用
含水率
吸水高度
Experimental Study on Effects of Different Dry Density on Capillary Water Absorption of Loess in Lanzhou Gansu Province