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人民胜利渠灌区水盐运动规律及评价 被引量:2

Motion Patterns of Water and Salt of Renminshengliqu Irrigated Area and Their Evaluation
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摘要 系统总结了人民胜利渠灌区40年来水盐动态状况及水盐运动规律,并对灌区的水盐动态现状进行分析。结果表明:目前,无论地下水埋深还是地下水水质,都处在灌区开灌以来的最好时期;0~100cm土层土壤含盐量正在逐年减少,土体处在脱盐阶段。今后只要注意灌区水盐状况的调控和管理,就可避免土壤次生盐碱化的发生。 After summing up the behaviour and motion patterns of water and salt of Renminshengliqu Irrigated Area in 40 years and analysing the behaviour of water and salt of the irrigated area of the present condition, the author considers that at present, whether the depth or the quality of ground water have been all in their best period since starting the irrigation of the irrigated area; the salt content of 0~100 cm layer soil has been reducing year after year and the soil mass is in the stage of desalting.In the future, the secondary salinization can be avoided as long as the water and salt status of wasted area can be controlled and managed.
作者 袁宾
出处 《人民黄河》 CAS 北大核心 1992年第10期11-14,共4页 Yellow River
关键词 地下水 盐份 运动 规律 农田 灌溉 farmland irrigation motion patterns of water and salt Yellow River water diversion
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  • 2石元春等.区域水盐运动监测预报[M]河北科学技术出版社,1991.
  • 3孙讷正.地下水污染[M]地质出版社,1989.
  • 4石元春.黄淮海平原的水盐运动和旱涝盐碱的综合治理[M]河北人民出版社,1983.
  • 5(苏)柯夫达(В.А.Ковда)著,席承藩等.盐渍土的发生与演变[M]科学出版社,1957.
  • 6Elisabet Lewan. Effects of a catch crop on leaching of nitrogen from a sandy soil: Simulations and measurements[J] 1994,Plant and Soil(1):137~152
  • 7D. K. Benbi,S. S. Prihar,H. S. Cheema. A model to predict changes in soil moisture, NO3-N content and N uptake by wheat[J] 1991,Fertilizer Research(1):73~84
  • 8J. J. R. Groot,P. Willigen. Simulation of the nitrogen balance in the soil and a winter wheat crop[J] 1991,Fertilizer Research(2-3):261~271
  • 9尚三林,贾树宝,余祥海,王瑞.人民胜利渠灌区盐碱地治理实践[J].人民黄河,2000,22(12):21-22. 被引量:4

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