In the Republic of Macedonia, construction and demolition (C&D) waste is often dumped, underestimating the potential recycling and re-use as raw materials for civil engineering works and/or cement/ceramic industries. SAMCODE (Sustainable Approach to Managing Construction and Demolition Waste) is a know-how exchange program, the focus of which is chemical characterisation in terms of major and trace elements in order to evaluate the possible Macedonian C&D waste recycling. Thirty-nine C&D waste samples were collected from different dumps in Skopje and surroundings. X-ray fluorescence analyses, carried out on powdered samples, show i) highly variable concentrations, indicative of the heterogenous nature of C&D waste, and ii) high concentration in Cr, Ni, and Zn with respect to Italian, Chinese, and Dutch tolerance limits, probably due to the presence of these elements in ophiolitic rocks and sulphide-bearing deposits, used as raw material in building activity. Inductively coupled plasma mass spectrometry analyses of leachates, performed to assess the mobility of heavy metals, show significant concentrations of Cr, and to a lesser extent, Ni. Results suggest that homogenisation processes of the recycled materials should be implemented and preliminary screening of C&D waste should be performed to eliminate heavy metals-bearing components.
<p>Construction and Demolition (C&D) waste is the solid debris resulting from construction and demolition activities. Recycling of this solid waste may result in substantial economic and environmental benefits. Unfortunately, is some Balkan countries such as Macedonia C&D recycling awareness is not developed yet. In this country, C&D are often dumped without control. According to the Macedonian landfill operator "Drisla" the estimated amounts of C&D waste generated per year in the Skopje surroundings approach 150.000 tons, but nothing is known on their composition. On this basis, a know-how exchange programme (KEP) called SAMCODE was financed by the Central European Initiative (CEI) and specifically dedicated to the characterization of C&D waste in Macedonia. GAYA operators sampled C&D landfills in the surroundings of Skopje, verified the absence of radioactivity, and then crushed the C&D down to the grain size of two millimetres. Crushed C&D chips were sent to the Department of Physics and Earth Sciences of the University of Ferrara, where the materials were powdered and analysed by X-ray fluorescence (XRF). Moreover, to characterize elemental mobility leaching tests on the C&D powders were carried out according to the following protocol: 1g of C&D powder has been soaked with 10 ml of deionized water, for 24 h. Subsequently the solutions have been centrifuged, filtered (at 45 mm) and analyzed by inductively coupled plasma mass spectrometry (ICP-MS). XRF analyses showed that &#8211; although variable - silica, calcium and aluminium are always the dominant components (SiO<sub>2 </sub>between 32 and 60 wt%, CaO between 7 and 30 wt%, Al<sub>2</sub>O<sub>3</sub> between 7 and 16%) suggesting possible recycling in the ceramic/cement industrial processes. However, the real re-use of these materials in industrial processes is hampered by the lack of homogeneity, a feature required by the industries. The analysis of trace elements emphasized another critical aspect: Macedonian C&Ds often contain anomalously high concentrations of elements potentially hazardous, especially chromium (Cr), nickel (Ni), lead (Pb) and zinc (Zn). Note that the high concentrations of Cr, Ni, Zn and Pb do not necessarily recall the presence of contaminants, as these elements can be present in natural raw materials used in the country. Noteworthy, in Macedonia there are rocks included in the ophiolite sequences such as peridotites, serpentinites, pyroxenites and chromitites that can contain thousand(s) ppm of chromium and nickel, and also mining areas where there are sulphides of lead (galena) and zinc (sphalerite). If similar rocks are used as raw materials in the building activity, it is not strange to have C&D anomalously enriched in Cr, Ni, Pb, Zn. This hypothesis is confirmed by soil studies retrieved in the literature that highlighted that Macedonian soils can contain anomalous content of these elements. ICP-MS analyses of leachates show negligible concentrations of Ni, Pb and Zn, but significant concentrations of Cr. The results indicate that to foresee effective recycling Macedonian C&D have to be preliminarily screened to eliminate Cr-bearing components, crushed and sorted to obtain a better homogenization.</p>
<p>In the upper mantle, volatiles control its composition, partial melting conditions, as well as the ascent rate of the formed melts. As consequence, volatile composition of the mantle is, in turn, recorded in the melts and, therefore, in the erupted basaltic rocks. Despite their importance, origin, budget, and fluxes of the volatiles in the upper mantle are poorly constrained. It is well known that the main input of mantle volatiles, such as carbon (C) and sulphur (S), represents components released from the subducting slab, <em>e.g.</em>, oceanic rocks and sediments, whose have characteristic isotopic signatures. In this view, studies of isotopic ratios of volatiles of subduction-related magmatic rocks could be used to identify the chemical components released by the subducting slab metasomatizing the upper mantle. To confirm this hypothesis, we investigated the major and trace element composition, as well as the C and S elemental contents and isotopic ratios of subvolcanic and volcanic rocks of the Vardar ophiolites of North Macedonia, which represent remnants of the Mesozoic Tethyan oceanic lithosphere formed in supra-subduction zone tectonic settings.</p><p>The ophiolites were sampled at Lipkovo and Demir Kapija localities, in the northern and southern part of North Macedonia, respectively. Based on whole-rock major and trace element composition, two main groups of rocks can be distinguished: i) Group 1 rocks, which are subalkaline basalts with backarc affinity and ii) Group 2 rocks, which are calc-alkaline basalts with arc affinity. The petrogenetic modelling based on trace and Rare Earth Elements, indicates that Group 1 mantle sources were affected by limited metasomatic processes by slab-released components, in particular aqueous fluids and sediment melts, whereas the Group 2 mantle sources were strongly metasomatized by sediment melts and adakitic melts. Accordingly, the Group 1 rocks exhibit C-enriched and S-depleted isotopic signature, indicating a minor involvement of melts from the subducting sediments. On the other hand, the C-depleted and S-enriched isotopic signatures of the Group 2 rocks suggest a major involvement of melts derived from the subducting sediments rich in organic matter and sulphate phases Therefore, both geochemical and isotopic data of the subvolcanic and volcanic samples of the North Macedonia ophiolites show that the sub-arc mantle sources are more affected by slab-released fluids than those of the backarc basin, which are more distal from the trench. Thus, combining the geochemical and isotopic data of subvolcanic and volcanic samples of complex geological framework can contribute to reconstruct the geodynamic scenarios, such as that of the Vardar ophiolites in the Dinaric-Hellenic belt. In addition, this approach may be useful to better understand the global geodynamic cycles of volatiles reconstructing their origin, budget, and isotopic composition, and understand the impacts on climate and environment from local to global scale.</p>
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.
hi@scite.ai
10624 S. Eastern Ave., Ste. A-614
Henderson, NV 89052, USA
Copyright © 2024 scite LLC. All rights reserved.
Made with 💙 for researchers
Part of the Research Solutions Family.