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中国沙漠 ›› 2001, Vol. 21 ›› Issue (3): 286-290.

• 实验研究 • 上一篇    下一篇

土壤水盐运动模式研究及其在干旱区农田的应用

姚德良1,2, 朱进生1, 谢正桐1, 李新荣2, 张景光2, 刘立超2   

  1. 1. 中国科学院力学研究所, 北京 100080;
    2. 中国科学院寒区旱区环境与工程研究所沙坡头沙漠试验研究站, 甘肃兰州 730000
  • 收稿日期:2000-12-15 修回日期:2001-02-13 出版日期:2001-09-20 发布日期:2001-09-20
  • 作者简介:姚德良(1943-),男(汉族),浙江慈溪人,研究员,主要从事陆面过程模式研究。
  • 基金资助:
    中国科学院沙坡头沙漠试验研究站基金(200007);国家自然科学基金(1983206040071007)

Model on Water-Salt Movement and Application in Field of Arid Land

YAO De-liang1,2, ZHU Jing-sheng1, XIE Zheng-tong1, LI Xin-rong2, ZHANG Jing-guang2, LIU Li-chao2   

  1. 1. Institute of Mechanics, Chinese Academy of Sciences, Beijing 100080, China;
    2. Shapotou Desert Research & Experiment Station, Cold and Ar id Regions Environmental and Engineering Research Institute, CAS, Lanzhou 730000, China
  • Received:2000-12-15 Revised:2001-02-13 Online:2001-09-20 Published:2001-09-20

摘要: 采用预估校正法求解土壤水分运动的h型Richards方程,此方法可以控制一定的迭代步数,但同样可达到二阶精度。同时采用具有二阶高精度的差分法求解土壤盐分运移的对流扩散方程,此格式可避免采用一般差分格式时出现的数值弥散问题。并将上述数学模式对干旱区绿洲棉田,在蒸散条件下土壤水分运动和土壤盐分向上运动积累过程进行数值模拟,模拟结果与测量值吻合较好,可为预报土壤盐碱化提供科学依据。

关键词: 绿洲棉田, 水盐运动, 预估校正法, 迎风二次型插值, 数值模拟

Abstract: The Prediction-Correction method is applied to solve the h type of Richards equation for water movement in soil. Satisfactory precision is gotten while the iteration steps are constrained by this method. Furthermore, the quadratic upstream interpolation difference method is adopted to solve the convection-diffusion equation for soil salt movement. It can avoid the problem of numerical dispersion and presents steeper apex of soil salt profile. Finally, this mathematical model is also utilized to simulate water-salt movement and the process of upwards accumulation of soil salt in cotton field of arid land under the condition of evaporation. The numerical results turn out in good agreement with the experimental data, thus the mathematical model may provide seientific basis for predicting salinization of soil. The water-salt movement in cropland with canopy and evaporation influence may be calculated by the present model, and the variation with depth of salt can also be obtained.

Key words: oasis cropland, water-salt movement, Prediction-Correction method, quadratic upstream interpolation, numerical simulation

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