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<metadata xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/"><dc:title>Molybdenum, lead and zinc mobility potential in agricultural environments</dc:title><dc:creator>Rogan Šmuc,	Nastja	(Avtor)
	</dc:creator><dc:subject>potencialno strupeni elementi</dc:subject><dc:subject>tla</dc:subject><dc:subject>mobilnost</dc:subject><dc:subject>okoljska ocena</dc:subject><dc:subject>Severna Makedonija</dc:subject><dc:description>The research focuses on the assessment of potential toxic elements (PTEs) contamination of the soils of the Kočani field  (North  Macedonia)  due  to  the  surrounding  past  and  current  polymetallic  mining  activities.  The  Zletovska  River  drains the untreated wastewater from the Pb-Zn mine in the Zletovo-Kratovo region and is unfortunately used to irrigate the surrounding rice fields. Elevated levels of molybdenum (Mo) and especially lead (Pb) and zinc (Zn) were found in the soil samples from the rice fields near the Zletovska River (in the western part of the Kočani field), which are well above the limit and critical emission values for PTEs content in soils. In addition, Mo was consistently bound to water soluble, exchangeable and oxidizable fractions in all samples, while reducible and residual fractions were predominated by Pb and Zn. According to the sum of the water-soluble and exchangeable fractions, the mobility and environmental bioavailability potential of the investigated PTEs in the soil-plant system decreased in the following order: Mo &gt; Pb &gt; Zn. It is therefore very  important  to  emphasize  that  when  assessing  the  environmental  impact  of  PTEs  on  the  respective  surroundings,  not only the commonly considered trace and minor PTEs (such as Pb and Zn) that occur in geological materials should be taken into account, but also in lower contents (such as Mo). The translocation of PTEs within the ecosystem does not depend on their total content in the primary geological materials, but on their individual mobility and binding capacity.</dc:description><dc:date>2024</dc:date><dc:date>2025-05-21 09:17:30</dc:date><dc:type>Neznano</dc:type><dc:identifier>22461</dc:identifier><dc:identifier>UDK: 55</dc:identifier><dc:identifier>ISSN pri članku: 0016-7789</dc:identifier><dc:identifier>DOI: 10.5474/geologija.2024.013</dc:identifier><dc:identifier>COBISS_ID: 219611907</dc:identifier><dc:language>sl</dc:language></metadata>
