Pore-scale simulation of gas diffusion in unsaturated soil aggregates: Accuracy of the dusty-gas model and the impact of saturation

文献类型: 外文期刊

第一作者: Li, Zhongyang

作者: Li, Zhongyang;Zhang, Xiaoxian;Liu, Yuan;Zhang, Xiaoxian

作者机构:

关键词: Dusty-gas model;Pore-scale modelling;Effective diffusion coefficient;Knudsen diffusion;Soil aggregates

期刊名称:GEODERMA ( 影响因子:6.114; 五年影响因子:6.183 )

ISSN:

年卷期:

页码:

收录情况: SCI

摘要: Gas diffusions in soil control all physical and biogeochemical processes in terrestrial ecosystems and correctly describing them is critical to numerical modelling of these processes. The movement of gases in soil needs to overcome the resistances caused by both gas-gas collision and gas-wall collision, and the relative significance of one resistance over another depends on the size and spatial distribution of the pores. Practical models often use the empirical dusty-gas formula to estimate the effective gas diffusion coefficient, assuming that all resistances are addable even after a volumetric average. Since it is impossible to separately measure the two resistances, the accuracy and reliability of this approach remains unknown. We investigate this using pore-scale modelling and tomography. Soil aggregates are acquired using X-ray computed tomography and the size and spatial distribution of their pores are calculated using a morphological model; each pore is associated with a bulk diffusion coefficient and a Knudsen diffusion coefficient, with the latter calculated based on the pore size. We then develop pore-scale models to simulate gas diffusion, and the diffusive flux and gas concentration simulated at pore scale are volumetrically averaged to calculate i) the effective Knudsen diffusion coefficient assuming the bulk diffusion coefficient is infinite, ii) the effective bulk diffusion coefficient assuming the Knudsen diffusion coefficient is infinite, and iii) the overall effective diffusion coefficient considering both the bulk and the Knudsen diffusions. The dusty-gas model estimates the effective diffusion coefficient using the effective bulk and the Knudsen diffusion coefficients, and its accuracy is tested against the effective diffusion coefficient directly calculated from the pore-scale simulations. The results indicate that the dusty-gas model is accurate when the diffusion is dominated by either bulk diffusion or Knudsen diffusion, whereas in the transition regime it systematically overestimates the effective diffusion coefficient. We also investigate the impact of saturation on the effective diffusion coefficients when the aggregates are either hydrophobic or hydrophilic, elucidating the significance of the Knudsen diffusion as the saturation of the aggregates increases.

分类号: S15

  • 相关文献

[1]The nonlinear adsorptive kinetics of solute transport in soil does not change with pore-water velocity: Demonstration with pore-scale simulations. Zhang, Xiaoxian,Zhang, Xiaoxian,Lv, Mouchao.

[2]Development of Soil Crusts Under Simulated Rainfall and Crust Formation on a Loess Soil as Influenced by Polyacrylamide. Li Shun-Jiang,Hu Xia,Liu Lian-You,Lu Yan-Li,Guo Jin-Rui,Hu Xia,Liu Lian-You,Lu Yan-Li,Guo Jin-Rui,Cai Qiang-Guo. 2012

[3]Effects of Integrated Soil-Crop System Management on Soil Organic Carbon Characteristics in a Primosol in Northeast China. Zhang Jinjing,Cao Zhiyuan,Feng Guozhong,Li Mengyao,Li Cuilan,Gao Qiang,Wang Lichun. 2017

[4]Spatial distribution of rhizodeposit carbon of maize (Zea mays L.) in soil aggregates assessed by multiple pulse C-13 labeling in the field. Qiao, Yunfa,Miao, Shujie,Li, Na,Han, Xiaozeng,Zhang, Bin,Zhang, Bin.

[5]Change in the abundance and community composition of ammonia-oxidizing bacteria and archaea at soil aggregate level as native pasture converted to cropland in a semiarid alpine steppe of central Asia. Chen, Zhu,Guo, Yanbin,Wu, Wenliang,Meng, Fanqiao,Du, Zhangliu. 2016

[6]Dynamics of physically-separated soil organic carbon pools assessed from delta C-13 changes under 25 years of cropping systems. Dou, Xiaolin,Dou, Xiaolin,He, Ping,Zhou, Wei,Wang, Ligang,Cheng, Xiaoli,Zhu, Ping. 2017

[7]Organic carbon fractions affected by long-term fertilization in a subtropical paddy soil. Huang, Shan,Rui, Wenyi,Peng, Xianxian,Huang, Qianru,Zhang, Weijian,Zhang, Weijian.

[8]Crop species affect soil organic carbon turnover in soil profile and among aggregate sizes in a Mollisol as estimated from natural C-13 abundance. Qiao, Yunfa,Miao, Shujie,Qiao, Yunfa,Miao, Shujie,Li, Na,Xu, Yanli,Han, Xiaozeng,Zhang, Bin,Zhang, Bin.

[9]Long-Term Manure Amendments Enhance Soil Aggregation and Carbon Saturation of Stable Pools in North China Plain. Du Zhang-liu,Zhang Qing-zhong,Wu Wen-liang,Guo Yan-bin,Meng Fan-qiao. 2014

[10]Shifts in soil organic carbon and nitrogen dynamics for afforestation in central China. Dou, Xiaolin,Shu, Xiao,Zhang, Quanfa,Cheng, Xiaoli,Dou, Xiaolin,Xu, Xia.

[11]Soil Aggregation and Microbial Responses to Straw Pulping Byproducts. Xiao, C.,Fauci, A.,Bezdicek, D. F.,Pan, W. L.,Xiao, C.,McKean, W. T..

[12]Variation of soil aggregation and intra-aggregate carbon by long-term fertilization with aggregate formation in a grey desert soil. Jiang, Maibo,Wang, Xihe,Liu, Hua,Jiang, Maibo,Liusui, Yunhao,Han, Chao,Jiang, Maibo,Zhao, Chengyi.

[13]Soil aggregation and organic carbon fractions affected by long-term fertilization in a red soil of subtropical China. Huang, Shan,Peng, Xianxian,Huang, Qianru,Zhang, Weijian,Zhang, Weijian.

作者其他论文 更多>>