Soil contamination compositional index: A new approach to quantify contamination demonstrated by assessing compositional source patterns of potentially toxic elements in the Campania Region (Italy). (September 2018)

• Record Type: Journal Article
• Authors: Petrik, Attila; Thiombane, Matar; Lima, Annamaria; Albanese, Stefano; Buscher, Jamie T.; De Vivo, Benedetto
• Is Part Of: Applied geochemistry. Volume 96(2018)
• Page Start: 264
• Page End: 276
• Publication Date: 2018-09
• Subjects: Campania region (Italy) -- Potentially toxic elements -- Spatial abundance -- Source discrimination -- Soil contamination compositional index; Environmental geochemistry -- Periodicals; Water chemistry -- Periodicals; Geochemistry -- Social aspects -- Periodicals; Geochemistry -- Periodicals; 551.9
• DOI: 10.1016/j.apgeochem.2018.07.014
• Languages: English
• ISSNs: 0883-2927

Abstract

Abstract: Potentially toxic elements (PTEs) are a major worldwide threat to the environment due to the constant global increase in industrial activity and urbanisation. Several studies have provided detailed maps and a better understanding of the spatial distribution patterns of PTEs in different matrices, but the majority of these studies have simply neglected the compositional nature of geochemical data. The aims of this study are to reveal the compositional behaviour and relative structure of 15 PTEs (subcomposition) in Campania, one of the most contaminated regions in Italy, and to quantify the spatial abundance and identify the possible origins of these PTEs. Robust compositional biplots were used to understand the natural grouping and origin of the PTEs. Ratios of specific subcompositions (balances) of PTEs were calculated to map the spatial patterns and identify the spatial variability of the PTEs. This study presents the preliminary steps needed to quantify and analyse the relative difference in the spatial abundance of PTEs by applying a compositional abundance index. In addition, a new soil contamination compositional index (SCCI) was elaborated to quantify topsoil contamination by the 15 PTEs and related subgroups following the compositional structure of the geochemical data. The elevated spatial abundance of the 15 PTEs is related to highly urbanised (Naples and Salerno), highly industrialised (Solofra) and intensely cultivated areas (Sarno River Basin), where the high dominance of elements from the anthropogenic subgroup (Pb, Sb, Sn and Zn) and high SCCI values suggest that contamination is from anthropogenic sources. The high spatial dominance of elements from the volcanic rock subgroup (As, Be, Se, Tl and V) in these same areas is likely related to geogenic sources, including alkalic pyroclastic rocks. Although the high spatial abundance of Group B elements (Cd, Cr, Co and Ni) is related to Terra Rossa soils and shaley facies of siliciclastic rocks of the southern Apennines, these same elements can also reach high abundances and reflect contamination (i.e. high SCCI values) from urbanised and industrialised areas due to e.g., tanneries and alloy production. Other high spatial abundances of the 15 PTEs with little or no contamination (i.e. very low SCCI values) can be related to nearby carbonate massifs, where a mixture of geogenic factors including weathering, advanced pedogenic processes, adsorption and co-precipitation with Fe-/Mn-oxyhydroxides and the presence of pyroclastic material might all be responsible for an increase in abundance. The lowest spatial dominance of the 15 PTEs occurs in the northeastern and southwestern siliciclastic zones of the Campania Region, where there is a low level of urbanisation and industrialisation and therefore contamination from any source can be excluded. Highlights: Compositional source patterns of PTEs (Potentially Toxic Elements) in topsoils. Spatial abundance and characterization of specific PTE subgroups. Soil Contamination Compositional Index to reveal and quantify contaminated areas. High spatial abundance and anthropogenic contamination in most urbanised regions. Low spatial abundance and geogenic sources in the siliciclastic zones.