Seasonal variability of Crvena river water mineralization

The mineralization of water and its content in Crvena River so far have not been studied. Water sampling was conducted from April 2008 - May 2009. Total mineralization is relatively low, which is consistent with the dominant lithological structure (Permian red sandstone). Dry residue contains Ca2...

Full description

Bibliographic Details
Main Authors: Manojlović Predrag, Nikolić Milena, Mustafić Sanja, Luković Jelena
Format: Article
Language:English
Published: Serbian Geographical Society 2010-01-01
Series:Glasnik Srpskog Geografskog Društva
Subjects:
SIC
Online Access:http://www.doiserbia.nb.rs/img/doi/0350-3593/2010/0350-35931004009M.pdf
Description
Summary:The mineralization of water and its content in Crvena River so far have not been studied. Water sampling was conducted from April 2008 - May 2009. Total mineralization is relatively low, which is consistent with the dominant lithological structure (Permian red sandstone). Dry residue contains Ca2+ ion, with the increased participation of SiO2. During the observational period it is clearly expressed seasonal effect. It is reflected not in the direct but the indirect impact. Based on the ratio of individual ions a model is determined for estimation of water flow at the confluence of the Crvena River in Nisava River. It could be applied to other drainage basins that have not been studied so far.
ISSN:0350-3593