Properties and classification of soils developed from bog iron ore

The soils developed from bog iron ore and distributed locally on Vistula valley near Warsaw, among of muck, bog and gley soils. These soils have under the surface layer strongly cemented bog iron B10x horizon containing to 60 percent of Fe203. The contents of Fe203 in the surface Ah, M and ApBox hor...

Full description

Saved in:
Bibliographic Details
Published inRoczniki gleboznawcze Vol. 47
Main Authors Czerwinski, Z, Kaczorek, D. (Warsaw Agricultural University (Poland). Dept. of Soil Science)
Format Journal Article
LanguagePolish
Published 1996
Subjects
CADMIO
CADMIUM
CARACT MICROMORFOLOGICAS DEL SUELO
CLASIFICACION DE SUELOS
CLASSIFICATION DES SOLS
COBALT
COBALTO
FER
GENESIS DEL SUELO
HIERRO
MANGANESE
MANGANESO
METAL LOURD
METALES PESADOS
NICKEL
NIQUEL
PEDOGENESE
PLOMB
PLOMO
POLOGNE
POLONIA
PROPIEDADES FISICO-QUIMICAS SUELO
PROPRIETE PHYSICOCHIMIQUE DU SOL
SOL HYDROMORPHE
SUELO HIDROMORFICO
TIPOS DE SUELOS
TRAIT MICROMORPHOLOGIQUE DU SOL
TYPE DE SOL
Online AccessGet more information

Cover

More Information
Summary:The soils developed from bog iron ore and distributed locally on Vistula valley near Warsaw, among of muck, bog and gley soils. These soils have under the surface layer strongly cemented bog iron B10x horizon containing to 60 percent of Fe203. The contents of Fe203 in the surface Ah, M and ApBox horizons range from 4.75 to 48 percent but in underlying IICgg horizons only from 0.08 to 0.18 percent. Apart from iron these soils are also enriched with the compounds of Mn, Co, Ni, Cd and Pb. With regard to the feature of these soils it is suggested to classification them as a new type of ferritic soil developed from the bog iron ore with the sub-types of the ferritic-humus, siliceous-ferritic-humus and ferritic-muck soils
Bibliography:9701009
P32
ISSN:0080-3642