THE EFFECT OF CO2 AND OXIDATION RATE ON THE FORMATION OF GOETHITE VERSUS LEPIDOCROCITE FROM AN FE(II) SYSTEM AT PH-6 AND PH-7

被引：82

作者：

CARLSON, L ^{[1
]}

SCHWERTMANN, U ^{[1
]}

机构：

[1] TECH UNIV MUNICH,LEHRSTUHL BODENKUNDE,W-8050 FREISING,GERMANY

来源：

CLAY MINERALS | 1990年 / 25卷 / 01期

关键词：

D O I：

10.1180/claymin.1990.025.1.07

中图分类号：

O64 [物理化学（理论化学）、化学物理学];

学科分类号：

070304 ; 081704 ;

摘要：

Carbonate anions direct the polymerization of the double bands of FeO3(OH)3 octahedra common to both minerals toward a corner sharing arrangement, and thereby to goethite, whereas chloride permits edge-sharing as in lepidocrocite. -from Authors

引用

页码：65 / 71

页数：7

共 10 条

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