Pregled bibliografske jedinice broj: 41004
The Environmental Geochemistry of the Vrana Lake Sediments and Adjacent Soils on Cres Island Croatia
The Environmental Geochemistry of the Vrana Lake Sediments and Adjacent Soils on Cres Island Croatia // Zbornik radova - Proceedings/2nd Croatian Geological Congress / Vlahović, Igor ; Biondić, Ranko (ur.).
Zagreb: Hrvatski geološki institut, 2000. str. 689-693 (poster, nije recenziran, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 41004 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
The Environmental Geochemistry of the Vrana Lake Sediments and Adjacent Soils on Cres Island Croatia
Autori
Miko, Slobodan ; Mesić, Saša ; Prohić, Esad
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Zbornik radova - Proceedings/2nd Croatian Geological Congress
/ Vlahović, Igor ; Biondić, Ranko - Zagreb : Hrvatski geološki institut, 2000, 689-693
Skup
2nd Croatian Geological Congress
Mjesto i datum
Dubrovnik, Hrvatska; Cavtat, Hrvatska, 17.05.2000. - 20.05.2000
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
Environmental geochemistry; lake sediments; soils; trace elements; Vrana Lake; Cres Island
Sažetak
An evaluation of environmental geochemical aspects of Vrana lake in regard to the lake sediments and the surrounding soils was attempted. The possible environmental changes in the local trace element geochemistry of both soils and sediments could be evaluated due to the positive correlation of most elements analyzed in both soils and sediments, with aluminum, implying a direct relationship with the clay minerals. The mean element contents of soils and sediments differ considerably and are much higher in soils (except Ca). The element to Al ratios indicate classify the elements into three general groups, the group of elements that show no difference in ratios in soils and sediments: Ni, Co, Mn, Th, V, Cr, Mg, Ba, Ti, K, and Hg. The elements that are enriched in the sediments are Ca, Cd, and As and in a smaller extent Na. The elements that can be considered as depleted in the clay fraction of the lake sediments are Cu, Pb, Zn, Fe, P and La.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb,
Hrvatski geološki institut