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红土中游离氧化铁的作用及其机理探讨
引用本文:冯金良,赵泽三.红土中游离氧化铁的作用及其机理探讨[J].河北省科学院学报,1994,11(1):35-43.
作者姓名:冯金良  赵泽三
作者单位:河北省科学院地理所,成都地质学院,南京建筑工程学院
摘    要:红土是在亚热带、热带湿热气候条件下风化形成的一类区域性残积土。天然状态下的红土具有含水量、液限、塑限值较高,孔隙比大,容重低等一些物理性质。同时红土又表现出较高的力学强度及较低的压缩性。这一异常现象的出现与红土中富积的游离氧化物,尤其是游离氧化铁有着密切的关系。本文着重由三个方面就红土中游离氧化铁的作用及其机理进行了初步研究。

关 键 词:红土,游离氧化铁,作用及机理

AN EXPLORATION FOR ACTION AND ACTION MECHANISIM OF FREE FERRIC OXIDE IN LATERITE
Feng Jinliang, Zhao Zesan, Gao Guorui.AN EXPLORATION FOR ACTION AND ACTION MECHANISIM OF FREE FERRIC OXIDE IN LATERITE[J].Journal of The Hebei Academy of Sciences,1994,11(1):35-43.
Authors:Feng Jinliang  Zhao Zesan  Gao Guorui
Affiliation:Feng Jinliang; Zhao Zesan; Gao Guorui
Abstract:Laterine is a weathering and leaching residual soil under sub-tropical and tropical climate. It is one kind of special and regional soil.Laterite has properties with higher natural moisture content,highet planicity and Pore ratio, but in the engineering geological properties laterite showed higher strength and mid-compressibility. As general thinking,this abnomal phenomena emergeing is oweing to free ferric oxide which accumulated richly in laterite.In this Paper,from three aspects author have discussed action of free ferric oxide in laterite,besides have probed into action mechanisim of free ferric oxide.
Keywords:Iaterite  Free ferric oxide  Action and  mechanisim
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