Experimental Study on Membrane Performance of Cohesive Undisturbed Soil Salty Area of Eastern China

ZUO Wen-zhe; XU Ye-jing; WANG Ying; LI Ming-yan

doi:10.13961/j.cnki.stbctb.2014.02.015

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Experimental Study on Membrane Performance of Cohesive Undisturbed Soil Salty Area of Eastern China

- Experimental Study on Membrane Performance of Cohesive Undisturbed Soil Salty Area of Eastern China
- Bulletin of Soiland Water Conservation Vol. 33, Issue 2, Pages: 69-72(2014)
- 作者机构：
  
  1. 河北联合大学矿业工程学院,河北,唐山,063009
  2. 河北钢铁集团矿业有限公司,河北,唐山,063000
- 作者简介：
- 基金信息：
- DOI：10.13961/j.cnki.stbctb.2014.02.015
  CLC：
- Published：2014
- 稿件说明：
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ZUO Wen-zhe, XU Ye-jing, WANG Ying, et al. Experimental Study on Membrane Performance of Cohesive Undisturbed Soil Salty Area of Eastern China[J]. Bulletin of Soiland Water Conservation, 2014, 33(2): 69-72.
DOI：

ZUO Wen-zhe, XU Ye-jing, WANG Ying, et al. Experimental Study on Membrane Performance of Cohesive Undisturbed Soil Salty Area of Eastern China[J]. Bulletin of Soiland Water Conservation, 2014, 33(2): 69-72. DOI： 10.13961/j.cnki.stbctb.2014.02.015.

摘要

为验证黏性土的膜性能

进行了原状土的固结渗透试验。原状土样采自唐山市滨海有咸区地下65 m处。对原状土样的粒度组成、孔隙特征及黏土矿物含量进行了测试

并将原状土样压入环刀

饱和固结后

用10 g/L的盐水进行稳压渗透

定期监测出水流量及出水溶液的Cl

和Na

浓度。渗透试验结束

测试入流液及原状土表面溶液的浓度。试验结果显示

渗出液中N

和Cl

浓度同步缓慢增长

达到初始入渗溶液的浓度后仍呈增长趋势

试验结束时入渗液的浓度达初始值的1.1倍

原状土表面溶液浓度达初始值的1.5倍。这种浓差极化现象说明原状土具有一定的膜性能

但试验条件下原状土不能起到对盐分的截留作用。

Abstract

An experiment of consolidation and permeability in undisturbed soil was carried out to test and verify the membrane performance of cohesive soil. Undisturbed soil samples were collected from 65 m underground in Tangshan coastal salty area and then size composition

pore characteristics and clay mineral content were tested. The undisturbed soil sample was pressured into ring knife for saturation and consolidation

permeation under stable osmotic pressure was tested with 10 g/L saline

and water flow and Cl- and Na+ concentration of the aqueous solution were regularly monitored. When the permeability experiment came to end

inflow fluid concentration and ion concentration on the surface of the undisturbed soil were tested separately. Results show that Na+ and Cl- concentration almost synchronously increased

and were still rising after reaching the initial infiltration solution concentration. At the end of the experiment

inflow liquid concentration was 1.1 times the initial value of the inflow liquid

and the solution concentration on the surface of the undisturbed soil was 1.5 times the initial value of the infiltration solution. The phenomenon of concentration polarization testifies that the undisturbed soil has certain membrane performance

but cannot play a role in intercepting salt under the experimental conditions.

关键词

Keywords

references

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