...
首页> 外文期刊>PHYSICAL REVIEW E >Effect of hydrogel particle additives on water-accessible pore structure of sandy soils: A custom pressure plate apparatus and capillary bundle model
【24h】

Effect of hydrogel particle additives on water-accessible pore structure of sandy soils: A custom pressure plate apparatus and capillary bundle model

机译:水凝胶颗粒添加剂对沙质土壤水可渗透孔隙结构的影响:定制压板装置和毛细管束模型

获取原文
获取原文并翻译 | 示例
           

摘要

To probe the effects of hydrogel particle additives on the water-accessible pore structure of sandy soils, wenintroduce a custom pressure plate method in which the volume of water expelled from a wet granular packing isnmeasured as a function of applied pressure. Using a capillary bundle model, we show that the differential changenin retained water per pressure increment is directly related to the cumulative cross-sectional area distribution f (r)nof the water-accessible pores with radii less than r. This is validated by measurements of water expelled fromna model sandy soil composed of 2-mm-diameter glass beads. In particular, it is found that the expelled waternis dramatically dependent on sample height and that analysis using the capillary bundle model gives the samenpore size distribution for all samples. The distribution is found to be approximately log normal, and the totalncross-sectional area fraction of the accessible pore space is found to be f0 = 0.34.We then report on how the porendistribution and total water-accessible area fraction are affected by superabsorbent hydrogel particle additives,nuniformly mixed into a fixed-height sample at varying concentrations. Under both fixed volume and free swellingnconditions, the total area fraction of water-accessible pore space in a packing decreases exponentially as thengel concentration increases. The size distribution of the pores is significantly modified by the swollen hydrogelnparticles, such that large pores are clogged while small pores are formed.
机译:为了探究水凝胶颗粒添加剂对沙质土壤水可渗透孔隙结构的影响,温特罗斯特采用了一种惯用的压板方法,其中测量了从湿颗粒填料排出的水量与施加压力的关系。使用毛细管束模型,我们表明每单位压力增量的滞留变化水量与半径小于r的可进入水的孔的累积横截面面积分布f(r)n直接相关。通过测量从直径为2毫米的玻璃珠组成的模型沙质中排出的水可以验证这一点。特别是,发现被排出的水很大程度上取决于样品高度,并且使用毛细管束模型进行的分析给出了所有样品的相同孔径分布。发现该分布近似为对数正态分布,可及孔隙空间的总横截面积分数为f0 = 0.34,然后我们报告了超吸收性水凝胶颗粒如何影响孔隙分布和总可及水区域分数添加剂,以不同的浓度均匀混合到固定高度的样品中。在固定体积和自由溶胀条件下,填料中水可及的孔隙空间的总面积分数随凝胶浓度的增加而呈指数下降。溶胀的水凝胶颗粒显着改变了孔的尺寸分布,使得大孔被堵塞而小孔形成。

著录项

  • 来源
    《PHYSICAL REVIEW E》 |2013年第5期|1-10|共10页
  • 作者

    Y. Wei; D. J. Durian;

  • 作者单位

    Department of Physics and Astronomy University of Pennsylvania Philadelphia Pennsylvania 19104-6396 USAComplex Assemblies of Soft Matter CNRS-Rhodia-UPenn UMI 3254 Bristol Pennsylvania 19007-3624 USA;

    Department of Physics and Astronomy University of Pennsylvania Philadelphia Pennsylvania 19104-6396 USA;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号