Abstract

PurposeChromium, a potentially harmful element, occurs commonly within the urban sediment cascade as a result of abundant industrial and transport-related sources. The risks that Cr-bearing particles pose to ecosystems and humans depend on the solid-phase chemical speciation of Cr and its environmental mobility. In this study, we adopt an integrated geochemical approach to investigate and determine the long-term fate of Cr in the urban sediment cascade.Materials and methodsWe use bulk chemical digests, sequential chemical extraction analysis, electron microscopy, electron microprobe and microfocus XANES analysis to describe the solid-phase speciation, geochemical characteristics and potential long-term behaviour of Cr in urban particulate matter from both aquatic sediment and road dust sediment (RDS) in Manchester, UK.Results and discussionCr-bearing grains within RDS and aquatic sediment are predominantly iron oxides and alumino-silicate glass grains. Electron microprobe analysis indicates Cr concentrations up to 3300 and 133,400 μg g−1 in the RDS and aquatic grains, respectively. XANES analysis indicates that Cr(III) is the dominant oxidation state, with only trace amounts of Cr(VI). Importantly, Cr speciation does not appear to have changed between sedimentary environments and the dominance of Cr(III) suggests limited bioavailability or toxicity under predominant environmental (anoxic and neutral pH) conditions in the aquatic sediment sink. Furthermore, geochemical analyses suggest the environmental mobility of Cr in the aquatic sediment sink is low (compared to other toxic metals) due to its association mainly with alumino-silicate glass grains and its inclusion as an integral part of the glass structure.ConclusionsIndustrial glass grains are a major component of urban sediment worldwide. The speciation and geochemical investigations performed in this study suggest most Cr within the urban sediment cascade may be resistant to environmental processes that could mobilise other toxic metals.

Highlights

  • Chromium (Cr) has long been known to be a potentially harmful element within the environment (Nriagu and Nieboer 1988)

  • Experimental x-ray absorption near edge structure (XANES) spectra for the present study show strong similarities with those reported by Huggins et al (2000) and Werner et al (2007) for chromite and Cr– Fe spinel, respectively, in ambient air particulate matter (AAPM)

  • Chromium is mainly associated with Fe oxides and industrial glass grains in urban aquatic sediment

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Summary

Introduction

Chromium (Cr) has long been known to be a potentially harmful element within the environment (Nriagu and Nieboer 1988). Humans and ecosystems can be exposed to Cr through natural and anthropogenic pathways in water and particulate (soil, sediment and aerosol) matter (Werner et al 2007). The risks that Cr-bearing particles pose to ecosystems and humans depend on the solid-phase chemical speciation and environmental mobility of Cr in the particles (Kotas and Stasicka 2000). J Soils Sediments (2017) 17:2666–2676 cationic Cr(III) is typically the dominant form and is relatively stable and non-toxic at circum-neutral pH (6.5–8.5) due to the formation of insoluble hydroxide and oxide compounds and strong complexation with minerals and organic matter (Martello et al 2007). Cr is widely recognized as a potentially harmful element and listed as a contaminant of serious concern in environmental legislation worldwide

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