| 基于气体分子动理论的土壤孔隙结构特征研究 |
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| 引用本文： | 孙义亨,施少敏,宋学姝,孟平,张劲松,任荣秀,陆森.基于气体分子动理论的土壤孔隙结构特征研究[J].土壤,2021,53(2):398-402. |
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| 作者姓名： | 孙义亨 施少敏 宋学姝 孟平 张劲松 任荣秀 陆森 |
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| 作者单位： | 中国林业科学研究院林业研究所,中国林业科学研究院林业研究所,中国林业科学研究院林业研究所,中国林业科学研究院林业研究所 |
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| 基金项目： | 国家自然科学基金项目（面上项目，重点项目，重大项目） |
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| 摘 要： | 通过测定两种土壤和一种玻璃珠的两相热导率随气压的变化,分析变压条件下气体分子碰撞平均自由程和多孔介质孔隙结构间的关系。研究计算了表征土壤平均孔隙结构的孔隙特征长度(d),同时依据静态几何学方法计算获取了颗粒平均间距(D)。结果表明,基于热传输方法获取的d值是从气体分子碰撞传热的动态观点获取的孔隙结构表征,标识着土壤颗粒间的热分离特征,是表征土壤孔隙结构的有效指标。由于土壤的d和D值相差3个数量级,但在玻璃珠上无量级差异,这说明d值可能只能表征土壤团聚体间的平均孔隙结构,不能反映团聚体内部及黏土颗粒内部的微细孔隙结构。
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| 关 键 词： | 土壤，孔隙结构，热导率，气体分子动理论 |
| 收稿时间： | 2020/2/20 0:00:00 |
| 修稿时间： | 2020/5/11 0:00:00 |
Study on Soil Pore Structure with Kinetic Molecule Theory of Gases |
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| SUN Yiheng,SHI Shaomin,SONG Xueshu,MENG Ping,ZHANG Jinsong,REN Rongxiu,LU Sen.Study on Soil Pore Structure with Kinetic Molecule Theory of Gases[J].Soils,2021,53(2):398-402. |
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| Authors: | SUN Yiheng SHI Shaomin SONG Xueshu MENG Ping ZHANG Jinsong REN Rongxiu LU Sen |
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| Institution: | Research Institute of Forestry,Chinese Academy of Forestry,Research Institute of Forestry,Chinese Academy of Forestry,Research Institute of Forestry,Chinese Academy of Forestry,Research Institute of Forestry,Chinese Academy of Forestry |
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| Abstract: | In this study, the two-phase thermal conductivity of two soils and a glass bead under various pressures was measured. The relationship between the pore structure of porous media and mean free path of air molecular was investigated. The characteristic dimension of the gas space among particles (d) which represents the average pore structure of the soil was calculated. Moreover, the static mean separation of particles (D), i.e., the geometric mean dimension of the gas space among particles was also calculated. The d value obtained based on the heat transfer method reflects the collision process of gas molecules and solid particles in the soil pores. The results showed that d represents the thermal separation characteristics among solid particles, and is an effective index to characterize the soil pore structure. There are three orders of magnitude difference between soil d and D values. However, there is no order of magnitude difference on the glass beads. The d value may only represent the average pore structure of inter-aggregate pores, and cannot reflect the fine pore structure of intra-aggregate pores and clay particles. |
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| Keywords: | soils pore structure thermal conductivity kinetic theory of gases |
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