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
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.