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外生菌根真菌Laccaria bicolor S238N增强花旗松生长及其对磷钾吸收的能力
引用本文:HUANG Jian-Guo,F. LAPEYRIE. 外生菌根真菌Laccaria bicolor S238N增强花旗松生长及其对磷钾吸收的能力[J]. 土壤圈, 1994, 4(3): 217-224
作者姓名:HUANG Jian-Guo  F. LAPEYRIE
作者单位:[1]InstituteofSoilScience,AcademiaSinica,P.O.Box821,Nanjing210008,China [2]InstituteofSoilScience,AcademiaS
基金项目:*1Project financially supported by Microbiologie, INRA, Center de Nancy, Champenoux 54280, France.
摘    要:Two variable charge soils were submerged after the addition of 30g/kg of organic matter to examine the differences in behavior between iron and manganese with respect to reduction and the distribution of different froms of the reduced elements.The reduction of manganese proceeded almost synchronously with the fall in redox potential,while the reduction of iron showed a remarkable lag behind the Eh change.Once formed,the distribution of water-soluble,exchangeable and precipitatied forms of ferrous iron was controlled by pH,CEC of the soil and total concentration of the element.For manganous ions,the proportions of water-soluble and exchangeable forms in total Mn^2 were larger than those for ferrous ions.The reduction of the two elements led to a mobilization of them,and such effect persisted even after drying of the soil,i.e.,the content of amorphous Fe became higher than that of the original soil.

关 键 词:土壤电荷 淹水 淹没 铁 镁 转化

Ability of ectomycorrhizal fungns Laccaria bicolor S238N to increase the growth of Donglas Fir seedlings and their phosphorns and potassinm uptake
HUANG Jian-Guo and F. LAPEYRIE. Ability of ectomycorrhizal fungns Laccaria bicolor S238N to increase the growth of Donglas Fir seedlings and their phosphorns and potassinm uptake[J]. Pedosphere, 1994, 4(3): 217-224
Authors:HUANG Jian-Guo and F. LAPEYRIE
Affiliation:[1]InstituteofSoilScience,AcademiaSinica,P.O.Box821,Nanjing210008,China [2]InstituteofSoilScience,AcademiaS
Abstract:Two variable charge soils were submerged after the addition of 30g/kg of organic matter to examine the differences in behavior between iron and manganese with respect to reduction and the distribution of different froms of the reduced elements.The reduction of manganese proceeded almost synchronously with the fall in redox potential,while the reduction of iron showed a remarkable lag behind the Eh change.Once formed,the distribution of water-soluble,exchangeable and precipitatied forms of ferrous iron was controlled by pH,CEC of the soil and total concentration of the element.For manganous ions,the proportions of water-soluble and exchangeable forms in total Mn^2 were larger than those for ferrous ions.The reduction of the two elements led to a mobilization of them,and such effect persisted even after drying of the soil,i.e.,the content of amorphous Fe became higher than that of the original soil.
Keywords:Douglas Fir   ectomycorrhizal fungi   K   P
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