期刊文献+

单种及多种盐分在土壤中的运移 被引量:3

Transports of single or multiple solutes in soil
原文传递
导出
摘要 建立了土壤热、湿、气及盐分耦合运移的数学模型,通过数值模拟研究了地下水深度分别为0.5 m,1.0m,1.5 m和2.0 m,地下水矿化度为5.0×10-3,以及土壤盐分初始质量分数为0时,5 a后土壤溶液中NaCl,KCl,CaCl2和MgSO4分别沿土壤剖面的质量分数分布.计算结果表明相同深度处4种盐分的质量分数大小顺序为:KCl>NaCl>CaCl2>MgSO4,可见扩散系数越大的盐分,其质量分数也越高;地下水位较高时这种差别更大.此外,还分别采用单组分和多组分模型对KCl和NaCl在土壤中的运移进行了比较,发现多组分效应对NaCl的影响更大,而对KCl的影响较小,因此采用多组分模型能够提高NaCl的预报精度. A mathematical model to simulate the transports of heat, moisture, gas and solute in soil was established. First, numerical simulations were conducted to investigate the transports of four single solutes, NaCl, KCl, CaCl2 and MgSO4, under the following conditions, ground water levels of 0. 5 m, 1.0 m, 1.5 m and 2.0 m; ground water salinity of 5.0×10^5, and initial concentration of 0. The numerical results of 5 years show that at the same depth, the concentration sequence of the four solutes was: KCl〉NaCl〉CaCl2〉MgSO4, the larger the diffusivity of the solute, the higher of its concentration. Moreover, the concentration differences were more evident in the case of shallow groundwater level. The multiple species effect of simultaneous transport of NaCl and KCl was also studied, after the single species model (SSM) was compared with the multiple species model (MSM), which demonstrated that the multiple species effect was more prominent for NaCl and less for KCl. Therefore, using the multiple species model can improve the prediction accuracy of NaCl.
出处 《华中科技大学学报(自然科学版)》 EI CAS CSCD 北大核心 2010年第9期116-119,共4页 Journal of Huazhong University of Science and Technology(Natural Science Edition)
基金 国家自然科学基金资助项目(50876035)
关键词 盐分运移 土壤 地下水 多组分效应 耦合模型 solute transport soil groundwater multiple species effect coupled modeling
  • 相关文献

参考文献8

二级参考文献21

  • 1卢玉邦.土壤水分预报模型的研究[J].土壤学报,1989,26(1):51-56. 被引量:22
  • 2罗小兵.土壤中热湿气迁移的数值模拟与实验研究:硕士论文[D].华中理工大学,1998.
  • 3张浙.含湿多孔介质的热质传递机理及其应用研究:博士论文[D].华中理工大学,1994.
  • 4曾丹苓.工程热力学[M].高等教育出版社,1986..
  • 5颜启全.种植基础[M].北京:高等教育出版社,1995..
  • 6丘华昌 陈明亮.土壤学[M].北京:中国农业科技出版社,1995..
  • 7丘华昌 陈明亮.土壤学[M].北京:中国农业科技出版社,1995..
  • 8Philip J R, De Vries D A. Moisture Movement in Porous Materials Under Temperature Gradients. Trans. Amer.Geophys. Union, 1957, 38(2): 222-232
  • 9Haridaan M, Jensen R D. Effect of Temperature on Pressure Head-Water Content Relationship and Conductivity of Two Soils. Soil Sci. Soc. Amer. J., 1972, 36(3): 703-708
  • 10Philip J R. The Theory of Infiltration: 4. Sorptivity and Algebraic Infiltration Equations. Soil Science, 1957,84(8): 257-264

共引文献83

同被引文献61

引证文献3

二级引证文献33

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部