GEOCHEMICAL CHARACTERIZATION OF RIVER DANUBE FROM CERNAVODA AREA Print

GEOCHEMICAL CHARACTERIZATION OF RIVER DANUBE FROM CERNAVODA AREA

 

 

Claudia Sandru*, Elena David

 

National Research and Development Institute for Cryogenics and Isotopic Technologies - ICIT Rm. Valcea, code 240050 - Rm. Valcea,

Uzinei 4, CP7 Raureni, Valcea, Romania

 

 

ABSTRACT

 

               The Danube played a vital role in the settlement and political evolution of central and southeastern Europe, which is an important water source for irrigation and drinking in Romania. Twelve representative samples were collected from the river Danube from Cernavoda Area . These samples were chemically analyzed for major cations and anions in order to understand the different geochemical processes affecting the surfacewater quality. Piper plot of the collected samples indicates that Na and K exceed Ca and Mg in most samples, whereas Cl and SO4 are the dominant anions. CO32- is the predominant anion in samples, indicating the effect of dissolution of carbonate minerals in the soil and silicates in the aquifer matrix.

 

KEYWORDS: surfacewater quality, geochemical characterization, Piper plot



*Corresponding author: Claudia Sandru, phone: 0040 250  732744, fax: 0040 250 732746, e-mail: This e-mail address is being protected from spambots. You need JavaScript enabled to view it