Estimates of volcanic mercury emissions from Redoubt Volcano, Augustine Volcano, and Mount Spurr eruption ash

Ash is a potential sink of volcanically sourced atmospheric mercury (Hg), and the concentration of particle-bound Hg may provide constraints on Hg emissions during eruptions. We analyze Hg concentrations in 227 bulk ash samples from the Mount Spurr (1992), Redoubt Volcano (2009), and Augustine Volcano (2006) volcanic eruptions to investigate large-scale spatial, temporal, and volcanic-source trends. We find no significant difference in Hg concentrations in bulk ash by distance or discrete eruptive events at each volcano, suggesting that in-plume reactions converting gaseous Hg0 to adsorbed Hg2+ are happening on shorter timescales than considered in this study (minutes) and any additional in-plume controls are not discernable within intra-volcanic sample variability. However, we do find a significant difference in Hg concentration of ash among volcanic sources, which indicates that volcanoes may emit comparatively high or low quantities of Hg. We combine our Hg findings with total mass estimates of ashfall deposits to calculate minimum, first-order Hg emissions of 8.23 t Hg for Mount Spurr (1992), 1.25 t Hg for Redoubt Volcano (2009), and 0.16 t Hg for Augustine Volcano (2006). In particular, we find that Mount Spurr is a high Hg emitting volcano, and that its 1992 particulate Hg emissions likely contributed substantially to the global eruptive volcanic Hg budget for that year. Based on our findings, previous approaches that use long-term Hg/SO2 mass ratios to estimate eruptive total Hg under-account for Hg emitted in explosive events, and global volcanogenic Total Hg estimates need revisiting

Self-limiting atmospheric lifetime of environmentally reactive elements in volcanic plumes

The 2018 eruption of Kīlauea, Hawai’i, produced exceptionally high discharge of metal pollutant elements, and an unprecedented opportunity to track them from vent to exposed communities over 200 km downwind. We discovered that magmatic volatility is an important control on the atmospheric behavior of elements, with [volatile elements] decreasing up to 100 times faster after emission than [refractory elements]. The differential deposition disproportionately impacts populated areas closest to the active vents, as the rapidlydeposited volatile elements generally have the highest environmental lability and potential toxicity

Rapid metal pollutant deposition from the volcanic plume of Kīlauea, Hawai’i

AbstractLong-lived basaltic volcanic eruptions are a globally important source of environmentally reactive, volatile metal pollutant elements such as selenium, cadmium and lead. The 2018 eruption of Kīlauea, Hawai’i produced exceptionally high discharge of metal pollutants, and was an unprecedented opportunity to track them from vent to deposition. Here we show, through geochemical sampling of the plume that volatile metal pollutants were depleted in the plume up to 100 times faster than refractory species, such as magnesium and iron. We propose that this rapid wet deposition of complexes containing reactive and potentially toxic volatile metal pollutants may disproportionately impact localised areas close to the vent. We infer that the relationship between volatility and solubility is an important control on the atmospheric behaviour of elements. We suggest that assessment of hazards from volcanic emissions should account for heterogeneous plume depletion of metal pollutants.</jats:p

The effect of aluminium and sodium impurities on the in vitro toxicity and pro-inflammatory potential of cristobalite

Background: Exposure to crystalline silica (SiO2), in the form of quartz, tridymite or cristobalite, can cause respiratory diseases, such as silicosis. However, the observed toxicity and pathogenicity of crystalline silica is highly variable. This has been attributed to a number of inherent and external factors, including the presence of impurities. In cristobalite-rich dusts, substitutions of aluminium (Al) for silicon (Si) in the cristobalite structure, and impurities occluding the silica surface, have been hypothesised to decrease its toxicity. This hypothesis is tested here through the characterisation and in vitro toxicological study of synthesised cristobalite with incremental amounts of Al and sodium (Na) dopants. Methods: Samples of synthetic cristobalite with incremental amounts of Al and Na impurities, and tridymite, were produced through heating of a silica sol-gel. Samples were characterised for mineralogy, cristobalite purity and abundance, particle size, surface area and surface charge. In vitro assays assessed the ability of the samples to induce cytotoxicity and TNF-α production in J774 macrophages, and haemolysis of red blood cells. Results: Al-only doped or Al+Na co-doped cristobalite contained between 1 and 4 oxide wt% Al and Na within its structure. Co-doped samples also contained Al- and Na-rich phases, such as albite. Doping reduced cytotoxicity to J774 macrophages and haemolytic capacity compared to non-doped samples. Al-only doping was more effective at decreasing cristobalite reactivity than Al+Na co-doping. The reduction in the reactivity of cristobalite is attributed to both structural impurities and a lower abundance of crystalline silica in doped samples. Neither non-doped nor doped crystalline silica induced production of the pro-inflammatory cytokine TNF-α in J774 macrophages. Conclusions: Impurities can reduce the toxic potential of cristobalite and may help explain the low reactivity of some cristobalite-rich dusts. Whilst further work is required to determine if these effects translate to altered pathogenesis, the results have potential implications for the regulation of crystalline silica exposures

Progressive failure cycles and distributions of earthquake-triggered landslides

Advances in the collection and analysis of landslide inventory data have allowed for greater understanding of spatial distributions of landslides triggered by earthquakes. However, current approaches to analysing and modelling these phenomena do not account for the response of the individual potential landslide masses and their temporally evolving stability. This stems, in part, from the lack of a conceptual model describing the effect of seismic waves on the strength and stability of hillslopes, which can be applied at the regional scale and over long (multiple earthquake) time scales. Here we present such a conceptual model linking weakening via progressive failure, inertial displacements driven by seismic ground accelerations, and the repeating failure of sections of hillslopes through time. We explore the implications of the model for how various characteristics of earthquake-triggered landslide distributions are interpreted and understood. These include the apparently stochastic nature of spatial landslide occurrence, spatial patterns of landsliding, landslide magnitude-frequency distributions, global variability in numbers of landslides triggered by earthquakes, and in particular why in any earthquake smaller areas of hillslope fail than do not, even in regions of apparently high landslide susceptibility. Finally, we also propose means of testing the validity of this model relative to alternative hypotheses