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昌马扇缘镁质碱化盐土风化—成土过程的主组元分析 被引量:1

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摘要 昌马冲积扇缘潜水溢出带,潜水埋深多在1~2米之间,部分地段浅于1米。水化学类型多属HCO^-_3—Mg^(2+)型。土壤盐化过程强烈,并伴随有草甸化和碱化成土过程,
作者 元柄成
出处 《甘肃农业科技》 北大核心 1991年第7期26-27,共2页 Gansu Agricultural Science and Technology
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  • 2PESSARAKLI M, SZABOLICS I. Soil salinity and sodicity as particular plant/crop stress factors. In: Pessarakli M. (Ed.), Handbook of Plant And Crop Stress, second ed. MarcelDekker, NewYork, NY, 1999:1 - 16.
  • 3KEREN R. Salinity. In:Sumner, M.E.(Ed.), Handbook of Soil Science. CRC Press, Boca Raton, 2000:G3 - G25.
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  • 7RIETZ D N, HAYNES R J. Effects of irrigation induced salinity and sodicity on soil microbial activity [J]. Soil Biol Biochem, 2003, 35: 845 - 854.
  • 8HINRICH L, BOHN B L, MCNEAL, et al. Soil chemistry [M]. John Wiley & Sons, inc, 2001:35 - 40.
  • 9陈月清.试论河西走廊盐渍土分类[A].中国土壤学会盐渍土专业委员会.中国盐渍土分类分级文集[c].南京,江苏科学技术出版社.1989.
  • 10GUPTA R N. Development and morphology of Vindhyan soils. II Nature of exchangeable bases in the soil sequence of the upper Vindhyan plateau in Uttar Pradesh [J]. India J Agric Sci, 1958, 28:491 - 498.

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