灌溉入渗条件下农田土壤水盐动态简化模型及应用
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* 国家重点基础研究发展规划项目G1999011803支持


THE SIMPLIFIED MODEL OF SALT-WATER REGIME IN CROPLAND SOIL UNDER INFILTRATION CONDITION AND ITS APPLICATION
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    摘要:

    率先采用线性简化式,并引入优先流系数来表示计算土层下边界渗漏水流通量;然后导出了计算土层入渗前后土壤储水量变化公式,在此基础上又引入淋洗系数,导出了入渗前后土壤储盐量变化公式。通过对公式的讨论,提出了灌溉水矿化度临界方程,讨论了淋洗系数和优先流系数的物理意义和影响因素。本文所建模型简单适用,而且与田间实测灌溉水矿化度临界方程极其吻合,可为农田灌溉水矿化度的选择提供参考。

    Abstract:

    In this paper,the lower boundary flow of considered upper soil stratum was expressed into linear relation with infiltration ratio and saturated degree by introducing preferential flow coefficient.So according to principle of salt-water balance,the water deposit formula and salt deposit formula was conducted out by introducing leaching coefficient.Through discussing above formulas,the critical mineralization degree equation of irrigation water was presented.The physical significance and af ected factors of the preferential flow coefficient and leaching coefficient were discussed.The salt-water regime model is simple and suitable for farmland irrigation management,the critical mineralization degree equation of irrigation water maybe provide reference for option of mineralization degree of irrigation water.

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张妙仙,杨劲松.灌溉入渗条件下农田土壤水盐动态简化模型及应用[J].土壤学报,2002,39(1):81-88. DOI:10.11766/trxb200004260112 Zhang Miao-xian, Yang Jing-song. THE SIMPLIFIED MODEL OF SALT-WATER REGIME IN CROPLAND SOIL UNDER INFILTRATION CONDITION AND ITS APPLICATION[J]. Acta Pedologica Sinica,2002,39(1):81-88.

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  • 收稿日期:2000-04-26
  • 最后修改日期:2001-02-05
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  • 在线发布日期: 2013-02-25
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