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作物生长条件下层状土壤水分运动数值模拟
引用本文:马英杰,陈大春,虎胆·吐马尔白. 作物生长条件下层状土壤水分运动数值模拟[J]. 新疆农业大学学报, 2006, 29(4): 70-72
作者姓名:马英杰  陈大春  虎胆·吐马尔白
作者单位:新疆农业大学,水利与土木工程学院,乌鲁木齐,830052
基金项目:新疆农业大学校科研和教改项目;新疆维吾尔自治区高校创新群体基金
摘    要:本文根据野外实测资料,分析了作物根系的生长规律。确定了作物腾发量,并用多元回归分析方法,拟合了作物根系吸水的数学模型,通过对一维土壤水分运动方程采用数值模拟的方法,分析了作物生长条件下层状土壤水分运动过程,与实测值比较认为拟合结果较好。表明所建立的根系吸水模型是合适的。

关 键 词:根系吸水率  回归分析  层状土壤
文章编号:1007-8614(2006)04-0070-03
修稿时间:2006-06-16

A Numerical Model of Layered Soils Moisture Equation under the Condition of Plant Consumption
MA Ying-jie,CHEN Da-chun,Hudan·Tumaerbai. A Numerical Model of Layered Soils Moisture Equation under the Condition of Plant Consumption[J]. Journal of Xinjiang Agricultural University, 2006, 29(4): 70-72
Authors:MA Ying-jie  CHEN Da-chun  Hudan·Tumaerbai
Abstract:The numerical model of the crop root uptake is developed with the help of multiple regression on the basis of the data measured in field.This paper also analyses the wheat root's rule of growth and evaporation.The one-diameter layered soils moisture equation under the condition of plant consumption is simulated,the simulating results are better by comparing simulated results with the data measured in field.It is shown that the numerical model of the crop root uptake is right.
Keywords:rate of crop root uptake  regression analysis  layered soils
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