期刊文献+

盐分胁迫条件下苜蓿根系吸水特性的模拟与分析 被引量:6

Simulation to Water Uptake Rate by the Roots of Alfalfa under Salinity Stress
原文传递
导出
摘要 体文借鉴Homaee有关盐分胁迫的部分试验研究结果及一种新的数值迭代反求方法,对无水分、养分限制条件下,Homaee苜蓿盐分胁迫试验中苜蓿根系的吸水规律进行了数值模拟与分析,提出了一种计算相对根长密度分布函数的简便计算方法,建立了盐分胁迫条件下苜蓿根系的吸水模型.结果表明:盐分的存在会显著降低苜蓿的根系吸水速率,当土壤溶液的电导率达到约5dS/m时,将极大地影响苜蓿的根系吸水;本文提出的计算相对根长密度分布函数的计算方法较为简便、可靠;基于相对根长密度分布函数的吸水模型可以较好地模拟根系的吸水规律. In this paper, the root water uptake rate of alfalfa under salinity stress (without water or nu- trient stress) were simulated and analyzed, and an easier method for calculation of the distribution function of relative root length density was put forward. The experimental data were chosen from Homaee' s alfalfa growth experiment under salinity stress. The results showed that: (1) salt in the soil reduced the root water uptake rate of alfalfa remarkably when the electric conductivity of soil solution was higher than 5 dS/m; (2) the method for calculation of the distribution function of relative root length density could be used reliably to simulate root water uptake characteristics of plants.
出处 《土壤通报》 CAS CSCD 北大核心 2001年第z1期81-84,共4页 Chinese Journal of Soil Science
基金 国家重点基础研究发展项目(项目编号0999011700) "中国-以色列科学与战略研究开发专项资金合作研究项目"
关键词 根系吸水速率 盐分胁迫 相对根密度分布函数 数值模拟 苜蓿 Water uptake rate by roots Salinity stress Distribution function of relative root density Numerical simulation Alfalfa
  • 相关文献

参考文献8

  • 1[1]Feddes R A, P Kowalik H. Zarandy. Water uptake by plant roots[A]. In Simulation of field water use and crop yield[C]. Eds. R. A. Feddes, P. J. Kowalik and H. Zaradny. p.16-30. John Wiley & Sons, Inc., New York, USA,1978,16-30.
  • 2[2]Mass E V and G J.Hoffman. Crop salt tolerance-current assessment[J]. J. Irrig. and Drainge Div., ASCE, 1997,103(IR2):115-134.
  • 3[3]Dirksen C,Augustijn D C.Root water uptake function for nonuniform pressure and osmotic potentials[J]. AGR. Abstracts. 1988.188.
  • 4[4]Dirksen C, J B Kool, P Koorevaar and M. Th. van Genuchten. HYSWASOR-Simulation model of hysteretic water and solute transport in the root zone[A]. In Water flow and solute transport in soils[C]. Eds. D. Russo and G. Dagan.Springer Verlag:USA.1993.99-122.
  • 5[5]van Genuchten, M Th. A numerical model for water and solute movement in and below the root zone[R]. Res. Report, U. S. Salinity Lab. Riverside:CA, USA.1987
  • 6[6]Homaee, M.Root water uptake under non-uniform transient salinity and water stress Wageningen Agricultural University, the Netherlands.1999.41-54,93-97
  • 7[7]Wu,J,R Zhang and S Gui. Modeling soil water movement with water uptake by roots[J]. Plant and Soil, 215:7-17.
  • 8[9]U.S. Salinity Laboratory Staff.Diagnosis and improvement of saline and alkali soils. Handbook[M].U.S.Government printing office. Washington:DC USA,1954.60

同被引文献210

引证文献6

二级引证文献64

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