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石灰性土壤小麦根际pH及磷动态变化的研究 被引量:35

DYNAMIC OF pH AND PHOSPHORUS OF WHEAT RHIZOSPHERE IN CALCAREOUS SOIL
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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。 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 Ca 2 P, Al P, Fe P and Ca 8 P, was lower, and the content of O P and Ca 10 P had no obvious change With growth time prolonged and temperature raised , the content of Ca 10 P was inerease, Ca 2 P, Al P,Fe P and Ca 8 P were decrease, and O P had no obvious change
出处 《植物营养与肥料学报》 CAS CSCD 1999年第1期32-39,共8页 Journal of Plant Nutrition and Fertilizers
关键词 石灰性土壤 小麦根际 PH 动态变化 磷肥 Calcareous soil Olsen P pH Wheat rhizosphere Dynamic
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