JpGU-AGU Joint Meeting 2017

Presentation information

[EE] Poster

A (Atmospheric and Hydrospheric Sciences) » A-GE Geological & Soil Environment

[A-GE40] [EE] Energy-Environment-Water Nexus and Sustainable Development

Mon. May 22, 2017 10:45 AM - 12:15 PM Poster Hall (International Exhibition Hall HALL7)

convener:Ming Zhang(Institute for Geo-Resources and Environment, Geological Survey of Japan, AIST), Xue Qiang(Institute of Rock and Soil Mechanics, The Chinese Academy of Science), Wen Jet-Chau(National Yunlin University of Science & Technology), Ken Kawamoto(Graduate School of Science and Engineering, Saitama University)

[AGE40-P09] Analysis of pore structure for different textured soils by Micro-focus X-ray CT system

*Daiki Morino1, Ken Kawamoto1, Takeshi Saito1 (1.Graduate School of Science and Engineering, Saitama University)

Keywords:Micro focus X-ray CT system, pore structure, mass transport confficients

Understanding mass transport properties in soils is important to develop techniques. The mass transport properties can be controlled by soil pore structure. The many analyses by visualization techniques for soil pore structure including a micro-focus X-ray CT system were carried out. However, few reports are available on the examinations of correlations between pore structure parameters and mass transport parameters. In this study, we visualized pore network for different textured soils by using Micro Focus X-ray CT system (inspeXio SMX-90CT, Shimadzu Corporation, Japan) and analyzed pore structure parameters (mean effective pore radius(reff,), pore coordination number(N), and pore tortuosity(Tzz)). Moreover, we measured gas diffusivity(Dp/D0) and air permeability(ka) as mass transport parameters. Different textured soils including sand, loam, and silty clay loam were used. The sand samples with different particle shape were packed at different densities. Similar to sand samples, the loam samples were packed. Undisturbed silty clay loam soils were collected from two different positions of an apple orchard, and two conditions (field water content and air dried after freeze drying) was used.
As a result, gas diffusivity increased with decreasing effective pore radius for the all dry samples. Correlations between effective pore radius and mean particle size have been reported. Thus, this results suggest that gas diffusivity is controlled by mean particle size. On the other hand, the gas diffusivity values of moist silty clay loam taken from alley area in apple orchard are lower than these of dry samples. Blocking by water in soil occurs the degradation of gas diffusion ability.