Abstract

PurposeDiffuse pollution emanating from metal mining-impacted sediment could serve as a barrier to achieving European Union Water Framework Directive and US Clean Water Act requirements. UK climate projections (UKCP09) predict increases in rainfall and aridity that will influence river stage alternately exposing and submersing contaminated riverbank sediment. Research focuses on the environmental contaminant dissolved Zn and investigates patterns of release, key geochemical mechanisms controlling Zn mobilisation and the environmental risk of sediment subjected to these perturbations.Materials and methodsUsing two laboratory mesocosm experiments, metal mining-contaminated sediment was subjected to alternate wet and dry sequences of different duration and frequency. The first experiment was run to determine the influence of submersion and exposure of contaminated sediment on releases of Zn and to establish environmental risk. The second experiment utilised diffusional equilibration in thin film (DET) to observe the patterns of Zn release, with depth, in the sediment. Pore water chemical analysis at the sediment-water interface enabled elucidation of key geochemical mechanisms of control of Zn mobilisation.Results and discussionPatterns of Zn release were found to be different, depending on the length of wet and dry period. High concentrations of dissolved Zn were released at the start of a flood for runs with longer dry periods. A buildup of soluble Zn sulphate minerals over long dry periods followed by dissolution on first flood wetting was a key geochemical mechanism controlling Zn release. For longer wet runs, increases in dissolved Mn and Zn were observed over the flood period. Key geochemical mechanisms controlling Zn mobilisation for these runs were: (i) reductive dissolution of Mn (hydr)oxides and release of partitioned Zn over prolonged flood periods followed by (ii) oxidation and precipitation of Mn (hydr)oxides and sorption of Zn on exposure to atmospheric conditions.ConclusionsMesocosm experiments were a first step in understanding the effects of UK climate projections on the riverbank environment. Contaminated sediment was found to pose a significant environmental risk in response to hydrological perturbations. The ‘transient’ nature of dissolved Zn release could make identifying the exact sources of pollution a challenge; therefore, further field studies are advised to monitor contaminant releases under a range of hydrological conditions and account for complex hydrology at mining sites.

Highlights

  • Metal-polluted river catchments are a legacy arising from historical metal mining, mineral processing, and dumping of waste along water courses throughout the world (Macklin et al 2006; Zhang et al 2012)

  • Mesocosm experiments were a first step in understanding the effects of UK climate projections on the riverbank environment

  • We investigate the geochemical mechanisms of Zn mobilisation in surface and pore water in response to flooding and drought sequences of different duration and frequency and utilise diffusional equilibration in thin film (DET) analysis to understand the co-distribution of Zn and Mn with depth in the sediment

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Summary

Introduction

Metal-polluted river catchments are a legacy arising from historical metal mining, mineral processing, and dumping of waste along water courses throughout the world (Macklin et al 2006; Zhang et al 2012). Zinc is highly mobile due to its hydrolytic stability in weakly acid solutions (Smith 1999; Lee et al 2002) and the high solubility of many Zn sulphate minerals. As a result, it can be transported downstream over large distances as a solute. More bioavailable, dissolved Zn can be re-introduced where river stage variability and riverbank inundation results in changes in redox potential and drying of sediment (Buckby et al 2003; Du Laing et al 2009; Lynch et al 2014)

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