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Mineralogical analyses and in vitro screening tests for the rapid evaluation of the health hazard of volcanic ash at Rabaul volcano, Papua New Guinea
Authors:Jennifer S Le Blond  Claire J Horwell  Peter J Baxter  Sabina A K Michnowicz  Maura Tomatis  Bice Fubini  Pierre Delmelle  Christina Dunster  Herman Patia
Institution:1. Department of Geography, University of Cambridge, Downing Place, Cambridge, CB2 3EN, UK
2. Department of Mineralogy, Natural History Museum, Cromwell Road, London, SW7 5BD, UK
3. Institute of Hazard, Risk and Resilience, Department of Earth Sciences, Durham University, Science Labs, South Road, Durham, DH1 3LE, UK
4. Institute of Public Health, University of Cambridge, Cambridge, CB2 2SR, UK
5. Dipartimento di Chimica I.F.M., Interdepartmental Center “G. Scansetti” for Studies on Asbestos and other Toxic Particulates, Università degli studi di Torino, Via P. Giuria 7, 10125, Torino, Italy
6. Environment Department, University of York, Heslington, York, YO10 5DD, UK
7. Lung Biology Group, Pharmaceutical Science Division, King’s College London, London, SE1 9NH, UK
8. Rabaul Volcano Observatory, P O Box?386, Rabaul, East New Britain Province, Papua New Guinea
Abstract:The continuous ash and gas emissions from the Tavurvur cone in Rabaul caldera, Papua New Guinea, during 2007–08, raised concerns regarding how exposure would affect the respiratory health of nearby populations and impact on the environment. As part of a formal evaluation of the effects of volcanic emissions on public health, we investigated the potential health hazard of the ash using a suite of selected mineralogical analyses and in vitro toxicity screening tests. The trachy-andesitic ash comprised 2.1–6.7 vol.% respirable (sub-4 μm diameter) particles. The crystalline silica content was 1.9–5.0 wt.% cristobalite (in the bulk sample) with trace amounts of quartz and/or tridymite. Scanning electron microscopy showed that the ash particles were angular with sparse, fibre-like particles (∼3–60 μm max. diameter) observed in some samples, which we confirmed to be CaSO4 (gypsum, at <6 wt.% in the bulk samples) and not asbestiform fibres. The ash specific surface area was low (0.1–2.7 m2 g−1). The leached solution from one of the ash samples was slightly acidic (pH 5.6), but did not contain high levels of toxic metals (such as F, Cu, Zn, Mn, As, Ni and Cd) when compared to previously tested volcanic ash leachates. Ash samples generated potentially-harmful hydroxyl radicals through an iron-mediated catalytic reaction, in the range of 0.15–2.47 μmol m−2 (after 30 min of reaction). However, measurement of particle oxidative capacity (potential oxidative stress reaction using ascorbic acid) and silica-like injury to red blood cells (erythrolysis assay, i.e. measurement of cell death) nevertheless revealed low biological reactivity. The findings suggest that acute exposure to the ash would have a limited potential to exacerbate pre-existing conditions such as asthma or chronic bronchitis, and the potential for chronic exposure leading to silicosis was low.
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