Pregled bibliografske jedinice broj: 665272
Chemical and textural composition of the Krka river tufa deposits from the Dinaric karst region of Croatia
Chemical and textural composition of the Krka river tufa deposits from the Dinaric karst region of Croatia // Protected karst territories - monitoring and management ; Proceedings / Stefanov, Petar ; Yordanova, Marina ; Stefanova, Dilyana ; Mikhova, Dimitrina (ur.).
Sofija: Bugarska akademija znanosti, 2013. str. 128-137 (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 665272 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Chemical and textural composition of the Krka
river tufa deposits from the Dinaric karst region
of Croatia
Autori
Medunić, Gordana ; Juranović Cindrić, Iva ; Pivčević, Nina ; Kampić, Štefica ; Prohić, Esad ; Goreta, Gordana ; Čobić, Andrea
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Protected karst territories - monitoring and management ; Proceedings
/ Stefanov, Petar ; Yordanova, Marina ; Stefanova, Dilyana ; Mikhova, Dimitrina - Sofija : Bugarska akademija znanosti, 2013, 128-137
ISBN
978-954-9531-18-3
Skup
Protected karst territories - monitoring and management
Mjesto i datum
Shumen, Bugarska, 16.09.2012. - 24.09.2012
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
tufa ; sequential extraction ; mossy encrustation ; trace metal correlation ; re-crystallisation ; Krka river
Sažetak
Tufa deposits, carbonates precipitated by freshwater organic and inorganic processes, occur abundantly in the Krka National Park situated inside the Dinaric Karst region of Croatia, at past and present sites of waterfalls. Chemical, petrographic and statistical analyses were carried out on six tufa samples to relate their textural constituents and trace element composition to the geochemical processes operating within this diverse environment. Trace metal concentrations in carbonate phase were analysed by ICP-AES method, after a single extraction with 1M Na-acetate. The insoluble residue (I.R.) could resulted from the karstic weathering processes, ranging from 2.20 to 21.10% (median 3.70%), influencing the chemical composition of tufa samples. Generally, increased Fe, Mn, and I.R. levels are accompanied by decreased Sr and Mg levels, and vice versa.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Kemija, Biologija
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Andrea Čobić
(autor)
Gordana Goreta
(autor)
Štefica Kampić
(autor)
Esad Prohić
(autor)
Iva Juranović Cindrić
(autor)
Gordana Medunić
(autor)