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Trace elements in soils from the Mediterranean agricultural karst catchment of the Vrana Lake (Croatia) (CROSBI ID 585180)

Prilog sa skupa u zborniku | sažetak izlaganja sa skupa | međunarodna recenzija

Romić, Marija ; Bakić, Helena ; Romić, Davor Trace elements in soils from the Mediterranean agricultural karst catchment of the Vrana Lake (Croatia) // Abstracts, 28th IAS Meeting of Sedimentology 2011 / Bádenas, Beatriz ; Aurell, Marcos ; Alonso-Zarza, Ana M. (ur.). Zaragoza, 2011. str. 554-554

Podaci o odgovornosti

Romić, Marija ; Bakić, Helena ; Romić, Davor

engleski

Trace elements in soils from the Mediterranean agricultural karst catchment of the Vrana Lake (Croatia)

The Vrana Basin, located in the central part of the Croatian Adriatic Sea coast, is a typical cryptodepression formed by tectonic activities, with 6830 ha of agricultural land and Lake Vrana situated in the very basin. The area is highly sensitive ecologically and is characterised by intensive vegetable production in a karst environment where, due to geological and climatic conditions as well as anthropogenic influence, it is easy for harmful substances to enter the food chain or penetrate ground water or open watercourses. This threatens the largest Croatian lake, Lake Vrana, as well, which is a large potential source of water for agriculture, possibly also drinking water, as well as for tourism and leisure activities. Because it is one of the rare natural habitats of waterbirds and because of its fresh water springs and biodiversity, the Vrana Lake and its surroundings have been declared a nature park. To evaluate the impact of agricultural practices on trace metals accumulation and behaviour in soils a multi-element geochemical survey was carried out. The objectives of this study were: (i) to determine contents of trace metals in soils and (ii) to assess their natural or anthropogenic source using multivariate statistical analysis. Topsoil (0-30 cm) and sub-soil (30-60 cm) samples were taken from 74 locations following regular square sampling grid with 1x1 km distances. Element contents (Ca, Cd, Co, Cr, Cu, Fe, Mg, Mn, Ni, P, Pb, Zn) were determined by ICP-OES after aqua regia extraction, while Hg was determined using the CV AAS technique. A GIS geospatial database was compiled. Furthermore, after statistical and geostatistical analyses, trace metal distribution maps were produced. The trace metal contents do not exceed the threshold value established by the Croatian government regulation, with exception of copper. The practice of using Cu-sulphates and other copper containing fungicides to protect grapevines mostly, resulted in significant Cu accumulations in soils worldwide. A high chromium and nickel concentration in spots seems to be of geogenic origin. By applying factor analysis (FA), complex linear correlations between metal concentrations in soils were determined which enabled the interpretation of correlations of elements in the studied area. Considering the influence they exerted on the determined distribution of elements, the said multi-element factors were divided into three groups: (1)factors caused by predominantly natural geogenic and pedogenic processes, (2) factors caused by specific long-term agricultural practices, mainly fertilization and (3) soil organic matter and nitrogen content variations. The identification of factors is based on the dominant influence. The distribution of individual associations of elements in topsoils was determined by principal components method. Based on eigenvalues, three main factors explained 72.6% of the total variance.

karst environment; nature park; trace metals in soils; geostatistical analyses; factor analysis; trace metal distribution maps

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Podaci o prilogu

554-554.

2011.

objavljeno

Podaci o matičnoj publikaciji

Abstracts, 28th IAS Meeting of Sedimentology 2011

Bádenas, Beatriz ; Aurell, Marcos ; Alonso-Zarza, Ana M.

Zaragoza:

Podaci o skupu

28th IAS Meeting of Sedimentology

predavanje

05.07.2011-08.07.2011

Zaragoza, Španjolska

Povezanost rada

Geologija