GIBBSITE-KAOLINITE EQUILIBRIA

被引：12

作者：

KITTRICK, JA

机构：

来源：

SOIL SCIENCE SOCIETY OF AMERICA PROCEEDINGS | 1967年 / 31卷 / 03期

关键词：

D O I：

10.2136/sssaj1967.03615995003100030010x

中图分类号：

S15 [土壤学];

学科分类号：

0903 ; 090301 ;

摘要：

In order to help determine if the equilibria reached by soil mineral mixtures is that predicted on the basis of single minerals, 2 kaolinite samples were equilibrated individually and also with gibbsite of known stability. One set of samples was equilibrated from undersaturation, the other from super-saturation. Samples were analyzed periodically and equilibrium values obtained by extrapolation to infinite time. The solution ion compositions found were those predicted on the basis of the solubilities of the individual minerals.

引用

页码：314 / +

页数：1

共 12 条

[1]

GARRELS RM, 1957, AM MINERAL, V42, P780

[2]

GARRELS RM, 1965, SOLUTIONS MINERALS E, pCH10

[3]

GRUNER JW, 1950, AM MINERAL, V35, P137

[4]

HSU PA HO, 1963, SOIL SCI, V96, P230, DOI 10.1097/00010694-196310000-00002

[5]

KELLER WD, 1954, AM MINERAL, V29, P783

[6]

KITTRICK JA, 1966, AM MINERAL, V51, P1457

[7] FREE ENERGY OF FORMATION OF GIBBSITE AND AL(OH)4-FROM SOLUBILITY MEASUREMENTS [J].

KITTRICK, JA .

SOIL SCIENCE SOCIETY OF AMERICA PROCEEDINGS, 1966, 30 (05) :595-+

[8]

KLOTZ IM, 1950, CHEM THERMODYN, P329

[9]

SIEVER R, 1957, AM MINERAL, V42, P821

[10]

VANLIER JA, 1960, J PHYS CHEM-US, V64, P1675

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