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湖北省红壤与黄棕壤的粘粒矿物组成与磷,钾的固定
引用本文:徐凤琳,李学垣.湖北省红壤与黄棕壤的粘粒矿物组成与磷,钾的固定[J].华中农业大学学报,1990,9(2):163-170.
作者姓名:徐凤琳  李学垣
作者单位:华中农业大学土化系 武汉430070 (徐凤琳,李学垣),华中农业大学土化系 武汉430070(董元华)
摘    要:

关 键 词:红壤  黄棕壤  磷钾的固定  粘粒矿物

THE CLAY MINERAL COMPOSITION OF RED EARTH AND YELLOW-BROWN EARTH IN HUBEI PROVINCE AND ITS RELATION TO THE FIXATION OF P AND K
Xu Fenglin,Li Xueyuan,Dong Yuanhu.THE CLAY MINERAL COMPOSITION OF RED EARTH AND YELLOW-BROWN EARTH IN HUBEI PROVINCE AND ITS RELATION TO THE FIXATION OF P AND K[J].Journal of Huazhong Agricultural University,1990,9(2):163-170.
Authors:Xu Fenglin  Li Xueyuan  Dong Yuanhu
Abstract:The clay minerals of red earth mainly consist of kaolinite and hydromicas, whilethose of the yellow-brown earth mainly consist of hydromicas, kaolinite and vermicu-lite. And all of the soils have few amount of 14(?) intergradient minerals. According to the experiment, the free iron oxides and hydroxyl aluminium of thesoils are the main carriersin fixing P, while the fixing power of kaolinites is smaller. As for the fixation of P in red earth, the fixing power of hydroxyl aluminium ishigher than that of free iron oxide. But in yellow-brown earth, the result turns outcontrary to the above-mentioned conclusion. To the fixation of k, the fixing powerof yellow-brown earth is higher than that of the red earth. The hydroxyl aluminium is favourable for the fixation of P, but is unfavourable forfixation of K. This effect is proportional so the content of 14(?) intergradient mille-rals as well as the heat-stable ability in soil clay fraction.
Keywords:yellow brown earth  red earth  fixation of P and K  free iron oxide  hydroxyl aluminium  14(?) intergradient minerals
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