摘要
采用黄河及长江中的沙样在不同Ca2+浓度下分别进行电位滴定试验和干容重试验,得到以下结论:①随Ca2+浓度的增加,泥沙颗粒表面负电荷先不断减少然后趋于不变。②Ca2+对泥沙淤积干容重的影响可分为三个阶段:第一阶段干容重减小;第二阶段增加并达到最大值;第三阶段减小最后趋于不变。③在Ca2+浓度相同条件下,泥沙浓度对淤积干容重的影响根据所加Ca2+浓度不同也呈现不同的变化。④Ca2+浓度、泥沙浓度相同时,中值粒径越大干容重越大,且中值粒径大的泥沙干容重达到最大值所需Ca2+少。⑤在不同Ca2+浓度下泥沙颗粒由于表面电荷不同造成静电斥力不同,同时表面水膜作用力也不同,二者共同作用使得干容重体现不同的变化。
The potentiometric titration and dry-bulk density experiment was done using the sediment of different Ca^2+ concentration in the Yellow River and the Yangtze River and some conclusions are given as following: (1)The surface negative charge of sediment firstly unceasingly reduces and then tends stable with the increasing of the Ca^2+ concentration; (2)The influence of theCa^2+ concentration on the dry-bulk density can be divided into three phases with the increasing of Ca^2+ concentration: the first phase is that the dry-bulk density reduces, the second one is that the dry-bulk density increases and gets the maximal value, and the third one is that the dry-bulk density reduces and finally doesn't change; (3)When the Ca^2+ concentration is equal, the influence of sediment concentration on the dry-bulk density has different change with the increasing of the Ca^2+ concentration; (4)As the Ca^2+ concentration and the sediment concentration are the same, the dry-bulk density will get bigger when the sediment median size increases, and the sand whose median size is big needs litter Ca^2+ when its dry-bulk density gets the maximal value; And (5)the sediment electrostatic repulsion is different because of the different surface negative charges in the different Ca^2+concentration, and the water film force is different, too. Both of two reasons show that the dry-bulk density reflects the above-mentioned changes.
出处
《水科学进展》
EI
CAS
CSCD
北大核心
2007年第6期807-811,共5页
Advances in Water Science
基金
国家自然科学基金资助项目(50479036)
国家重点基础研究发展计划(973)资助项目(2003CB415205)~~
关键词
泥沙颗粒
电位滴定
表面电荷
CA^2+浓度
干容重
试验研究
sediment particles
potentiometric titration
surface charge
Ca^2+ concentration
dry bulk density
experimental study