SPATIAL VARIATIONS OF DISSOLVED SILICA CONCENTRATIONS AND GROUNDWATERSATURATION INDEX FOR QUARTZ (BYELARUS, AS AN EXAMPLE)

Citation
Na. Makhnach et Lf. Gulis, SPATIAL VARIATIONS OF DISSOLVED SILICA CONCENTRATIONS AND GROUNDWATERSATURATION INDEX FOR QUARTZ (BYELARUS, AS AN EXAMPLE), Doklady Akademii nauk BSSR, 41(3), 1997, pp. 102-106
Citations number
13
Categorie Soggetti
Multidisciplinary Sciences
Journal title
ISSN journal
0002354X
Volume
41
Issue
3
Year of publication
1997
Pages
102 - 106
Database
ISI
SICI code
0002-354X(1997)41:3<102:SVODSC>2.0.ZU;2-8
Abstract
Schematic map of the groundwater saturation index (I-s) for quartz is composed and described. H4SiO4 concentrations in solutions as well as I-s values were revealed to increase in terrain elements sequence: wat ershed top-gentle slope-river terrace-flood plain-bog. I-s values were maximal within the areas of dominating hydromorphic and semihydromorp hic soils and minimal in the fields of the autonomic soils prevalence.