• ISSN 1008-505X
  • CN 11-3996/S

石灰性土壤小麦根际pH及磷动态变化的研究

DYNAMIC OF pH AND PHOSPHORUS OF WHEAT RHIZOSPHERE IN CALCAREOUS SOIL

  • 摘要: 本文采用网隔栽培室种植小麦,置于人工气候室内生长,对不同温度条件下土小麦根际及距根不同距离土体中pH,Olsen-P及无机磷组分动态变化进行了研究。主要结果有:(1)根际及0~3mm土体pH较低,而3~8mm和8~50mm土体pH较高;(2)Olsen-P含量为根际<0~3mm土体<3~8mm和8~50mm土体,温度升高,各土层Olsen-P含量呈降低趋势;(3)距小麦根系越近,Ca2-P、AlP、Fe-P和Ca8-P含量越低,O-P和Ca10-P变化不明显;随时间延长和温度升高,Ca10-P含量有所增加,Ca2-P、Al-P、Fe-P和Ca8-P含量有所降低,O-P含量变化不大

     

    Abstract: The net separation culture pots were empoyed to plant winter wheat Those pots were put into E8H artificial climate box The pH, Olsen P and inorganic phosphate form in cumulic cinnamon soil under vary temperature conditions were studied The results showed that: (1) the pH of wheat rhizosphere and 0~3 mm soil layer were higher than that of 3~8mm and 8~50mm soil layers; (2) the furthest from the wheat roots, the content of Olsen P was higher and the content of Olsen P was reduce with the temperature ; (3) In more near from the wheat roots, the content of Ca2-P, Al-P, Fe-P and Ca8-P, was lower, and the content of O-P and Ca10-P had no obvious change With growth time prolonged and temperature raised , the content of Ca10-P was inerease, Ca2-P, Al-P,Fe-P and Ca8-P were decrease, and O-P had no obvious change

     

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