Health Risks Due to Air Pollution from Volcanic Eruptions
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Volcanic Gases and Aerosols Guidelines Introduction
IVHHN Gas Guidelines www.ivhhn.org/gas/guidelines.html Volcanic Gases and Aerosols Guidelines The following pages contain information relating to the health hazards of gases and aerosols typically emitted during volcanic activity. Each section outlines the properties of the emission; its impacts on health; international guidelines for concentrations; and examples of concentrations and effects in volcanic contexts, including casualties. Before looking at the emissions data, we recommend that you read the general introduction to volcanic gases and aerosols first. A glossary to some of the terms used in the explanations and guidelines is also provided at the end of this document. Introduction An introduction to the aims and purpose of the Gas and Aerosol Guidelines is given here, as well as further information on international guideline levels and the units used in the website. A brief review of safety procedures currently implemented by volcanologists and volcano observatories is also provided. General Introduction Gas and aerosol hazards are associated with all volcanic activity, from diffuse soil gas emissions to 2- plinian eruptions. The volcanic emissions of most concern are SO2, HF, sulphate (SO4 ), CO2, HCl and H2S, although, there are other volcanic volatile species that may have human health implications, including mercury and other metals. Since 1900, there have been at least 62 serious volcanic-gas related incidents. Of these, the gas-outburst at Lake Nyos in 1986 was the most disastrous, causing 1746 deaths, >845 injuries and the evacuation of 4430 people. Other volcanic-gas related incidents have been responsible for more than 280 deaths and 1120 injuries, and contributed to the evacuation or ill health of >53,700 people (Witham, in review). -
Itinerary Route: Reykjavik, Iceland to Reykjavik, Iceland
ICELAND AND GREENLAND: WILD COASTS AND ICY SHORES Itinerary route: Reykjavik, Iceland to Reykjavik, Iceland 13 Days Expeditions in: Aug Call us at 1.800.397.3348 or call your Travel Agent. In Australia, call 1300.361.012 • www.expeditions.com DAY 1: Reykjavik, Iceland / Embark padding Special Offers Arrive in Reykjavík, the world’s northernmost capital, which lies only a fraction below the Arctic Circle and receives just four hours of sunlight in FREE BAR TAB AND CREW winter and 22 in summer. Check in to our group TIPS INCLUDED hotel in the morning and take time to rest and We will cover your bar tab and all tips for refresh before lunch. In the afternoon, take a the crew on all National Geographic panoramic drive through the city’s Old Town Resolution, National Geographic before embarking National Explorer, National Geographic Geographic Endurance. (B,L,D) Endurance, and National Geographic Orion voyages. DAY 2: Flatey Island padding Explore Iceland’s western frontier by Zodiac cruise, visiting Flatey Island, a trading post for many centuries. In the afternoon, sail past the wild and scenic coast of Iceland’s Westfjords region. (B,L,D) DAY 3: Arnafjörður and Dynjandi Waterfall padding In the early morning our ship will glide into beautiful Arnafjörður along the northwest coast of Iceland. For a more active experience, disembark early and hike several miles along the base of the fjord to visit spectacular Dynjandi Waterfall. Alternatively, join our expedition staff on the bow of the ship as we venture ever deeper into the fjord and then go ashore by Zodiac to walk up to the base of the waterfall. -
GY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 9: Extrusive Igneous Rocks Instructor: Dr. Douglas W. Haywick Last Time 1) The chemical composition of the crust 2) Crystallization of molten rock 3) Bowen's Reaction Series Web notes 8 Chemical Composition of the Crust Element Wt% % of atoms Oxygen 46.6 60.5 Silicon 27.7 20.5 Aluminum 8.1 6.2 Iron 5.0 1.9 Calcium 3.6 1.9 Sodium 2.8 2.5 Potassium 2.6 1.8 Magnesium 2.1 1.4 All other elements 1.5 3.3 Crystallization of Magma http://myweb.cwpost.liu.edu/vdivener/notes/igneous.htm Bowen’s Reaction Series Source http://www.ltcconline.net/julian Igneous Rock Composition Source: http://hyperphysics.phy-astr.gsu.edu Composition Formation Dominant Silica content Temperature Minerals Ultramafic Very high Olivine, pyroxene Very low (<45%) Mafic High Olivine, pyroxene, low Ca-plagioclase Intermediate Medium Na-Plagioclase, moderate amphibole, biotite Felsic Medium-low Orthoclase, quartz, high (>65%) muscovite, biotite Igneous Rock Texture Extrusive Rocks (Rapid Cooling; non visible* crystals) Intrusive Rocks (slow cooling; 100 % visible crystals) *with a hand lens Igneous Rock Texture Igneous Rock Texture Today’s Agenda 1) Pyro-what? (air fall volcanic rocks) 2) Felsic and Intermediate Extrusive Rocks 3) Mafic Extrusive Rocks Web notes 9 Pyroclastic Igneous Rocks Pyroclastic Igneous Rocks Pyroclastic: Pyro means “fire”. Clastic means particles; both are of Greek origin. Pyroclastic Igneous Rocks Pyroclastic: Pyro means “fire”. Clastic means particles; both are of Greek origin. Pyroclastic rocks are usually erupted from composite volcanoes (e.g., they are produced via explosive eruptions from viscous, “cool” lavas) Pyroclastic Igneous Rocks Pyroclastic: Pyro means “fire”. -
Deep Carbon Emissions from Volcanoes Michael R
Reviews in Mineralogy & Geochemistry Vol. 75 pp. 323-354, 2013 11 Copyright © Mineralogical Society of America Deep Carbon Emissions from Volcanoes Michael R. Burton Istituto Nazionale di Geofisica e Vulcanologia Via della Faggiola, 32 56123 Pisa, Italy [email protected] Georgina M. Sawyer Laboratoire Magmas et Volcans, Université Blaise Pascal 5 rue Kessler, 63038 Clermont Ferrand, France and Istituto Nazionale di Geofisica e Vulcanologia Via della Faggiola, 32 56123 Pisa, Italy Domenico Granieri Istituto Nazionale di Geofisica e Vulcanologia Via della Faggiola, 32 56123 Pisa, Italy INTRODUCTION: VOLCANIC CO2 EMISSIONS IN THE GEOLOGICAL CARBON CYCLE Over long periods of time (~Ma), we may consider the oceans, atmosphere and biosphere as a single exospheric reservoir for CO2. The geological carbon cycle describes the inputs to this exosphere from mantle degassing, metamorphism of subducted carbonates and outputs from weathering of aluminosilicate rocks (Walker et al. 1981). A feedback mechanism relates the weathering rate with the amount of CO2 in the atmosphere via the greenhouse effect (e.g., Wang et al. 1976). An increase in atmospheric CO2 concentrations induces higher temperatures, leading to higher rates of weathering, which draw down atmospheric CO2 concentrations (Ber- ner 1991). Atmospheric CO2 concentrations are therefore stabilized over long timescales by this feedback mechanism (Zeebe and Caldeira 2008). This process may have played a role (Feulner et al. 2012) in stabilizing temperatures on Earth while solar radiation steadily increased due to stellar evolution (Bahcall et al. 2001). In this context the role of CO2 degassing from the Earth is clearly fundamental to the stability of the climate, and therefore to life on Earth. -
Insights Into the Recurrent Energetic Eruptions That Drive Awu Among the Deadliest Volcanoes on Earth
Insights into the recurrent energetic eruptions that drive Awu among the deadliest volcanoes on earth Philipson Bani1, Kristianto2, Syegi Kunrat2, Devy Kamil Syahbana2 5 1- Laboratoire Magmas et Volcans, Université Blaise Pascal - CNRS -IRD, OPGC, Aubière, France. 2- Center for Volcanology and Geological Hazard Mitigation (CVGHM), Jl. Diponegoro No. 57, Bandung, Indonesia Correspondence to: Philipson Bani ([email protected]) 10 Abstract The little known Awu volcano (Sangihe island, Indonesia) is among the deadliest with a cumulative death toll of 11048. In less than 4 centuries, 18 eruptions were recorded, including two VEI-4 and three VEI-3 eruptions with worldwide impacts. The regional geodynamic setting is controlled by a divergent-double-subduction and an arc-arc collision. In that context, the slab stalls in the mantle, undergoes an increase of temperature and becomes prone to 15 melting, a process that sustained the magmatic supply. Awu also has the particularity to host alternatively and simultaneously a lava dome and a crater lake throughout its activity. The lava dome passively erupted through the crater lake and induced strong water evaporation from the crater. A conduit plug associated with this dome emplacement subsequently channeled the gas emission to the crater wall. However, with the lava dome cooling, the high annual rainfall eventually reconstituted the crater lake and created a hazardous situation on Awu. Indeed with a new magma 20 injection, rapid pressure buildup may pulverize the conduit plug and the lava dome, allowing lake water injection and subsequent explosive water-magma interaction. The past vigorous eruptions are likely induced by these phenomena, a possible scenario for the future events. -
Volcano Hazards at Newberry Volcano, Oregon
Volcano Hazards at Newberry Volcano, Oregon By David R. Sherrod1, Larry G. Mastin2, William E. Scott2, and Steven P. Schilling2 1 U.S. Geological Survey, Hawaii National Park, HI 96718 2 U.S. Geological Survey, Vancouver, WA 98661 OPEN-FILE REPORT 97-513 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1997 U.S. Department of the Interior U.S. Geological Survey CONTENTS Introduction 1 Hazardous volcanic phenomena 2 Newberry's volcanic history is a guide to future eruptions 2 Flank eruptions would most likely be basaltic 3 The caldera would be the site of most rhyolitic eruptions—and other types of dangerously explosive eruptions 3 The presence of lakes may add to the danger of eruptions in the caldera 5 The most damaging lahars and floods at Newberry volcano would be limited to the Paulina Creek area 5 Small to moderate-size earthquakes are commonly associated with volcanic activity 6 Volcano hazard zonation 7 Hazard zone for pyroclastic eruptions 7 Regional tephra hazards 8 Hazard zone for lahars or floods on Paulina Creek 8 Hazard zone for volcanic gases 10 Hazard zones for lava flows 10 Large-magnitude explosive eruptions of low probability 11 Monitoring and warnings 12 Suggestions for further reading 12 Endnotes 13 ILLUSTRATIONS Plate 1. Volcano hazards at Newberry volcano, Oregon in pocket Figure 1. Index map showing Newberry volcano and vicinity 1 Figure 2. -
Origins of High-Temperature Fluids in the Goshogake Mud Volcano Field, Tohoku, Northern Japan: Chemical and Isotopic Studies of Gas and Water
49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083) 1210.pdf ORIGINS OF HIGH-TEMPERATURE FLUIDS IN THE GOSHOGAKE MUD VOLCANO FIELD, TOHOKU, NORTHERN JAPAN: CHEMICAL AND ISOTOPIC STUDIES OF GAS AND WATER. R. Ishimaru1, N. Miyake1, G. Komatsu2, K. Kawai3, M. Kobayashi4, H. Sakuma5, T. Matsui1 1Planetary Exploration Research Center (PERC), Chiba Institute of Technology (Chitech) (2-17-1 Tsudanuma, Narashino, Chiba 275-0016, Japan; [email protected]), 2International Research School of Planetary Sciences, Università d'Annunzio (Viale Pindaro 42, 65127 Pescara, Italy), 3Department of Earth and Planetary Science, School of Science, University of Tokyo (Hongo 7-3-1, Bunkyo, Tokyo 113-0033, Japan), 4Department of Earth and Planetary Environmental Sci- ence, School of Science, University of Tokyo (Hongo 7-3-1, Bunkyo, Tokyo 113-0033, Japan), 5Reseach Center for Functional Materials, National Institute for Materials Science (1-1 Namiki, Tsukuba, 305-0044 Japan). Introduction: Mud volcanoes occur everywhere Gas sampling and laboratory analysis. Gases were in various geological settings on the Earth [e.g., 1] and, collected with a custom-made sampling device for possibly, on other planetary bodies, such as Mars [e.g., laboratory measurement of the gas species. The com- 2] and Enceladus ocean floor. Their surface terrains position analysis of the gas samples in the chamber are formed by mud ascending and erupting, together was conducted using Gas Chromatography (GS) in the with water and gas, from depths. Therefore, mud vol- laboratory. The GC analyses are made in two ways: cano is one of the most suitable landforms for explor- qualitative and quantitative analyses. -
1998 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory by Robert G
1998 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory by Robert G. McGimsey, Christina A. Neal, and Olga Girina Open-File Report 03-423 U.S. Department of the Interior U.S. Geological Survey 1998 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory By Robert G. McGimsey1, Christina A. Neal1, and Olga Girina2 1Alaska Volcano Observatory, 4200 University Dr., Anchorage, AK 99508-4664 2Kamchatka Volcanic eruptions Response Team, Institute of Volcanic Geology and Geochemistry, Piip Blvd., 9 Petropavlovsk-Kam- chatsky, 683006, Russia AVO is a cooperative program of the U.S. Geological Survey, University of Alaska Fairbanks Geophysical Institute, and the Alaska Division of Geological and Geophysical Surveys. AVO is funded by the U.S. Geological Survey Volcano Hazards Program and the State of Alaska Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government Open-File Report 03-423 U.S. Department of the Interior U.S. Geological Survey TABLE OF CONTENTS Introduction. 1 Reports of volcanic activity, northeast to southwest along Aleutian arc . 4 Shrub Mud Volcano . 4 Augustine Volcano . 6 Becharof Lake Area . 8 Chiginagak Volcano . 10 Shishaldin Volcano. 12 Akutan Volcano . 12 Korovin Volcano . 13 Reports of Volcanic activity, Kamchatka, Russia, North to South . 15 Sheveluch Volcano . 17 Klyuchevskoy Volcano. 19 Bezymianny Volcano . 21 Karymsky Volcano . 23 References. 24 Acknowledgments . 26 Figures 1 A. Map location of historically active volcanoes in Alaska and place names used in this summary . -
One Hundred Volatile Years of Volcanic Gas Studies at the Hawaiian Volcano Observatory
Characteristics of Hawaiian Volcanoes Editors: Michael P. Poland, Taeko Jane Takahashi, and Claire M. Landowski U.S. Geological Survey Professional Paper 1801, 2014 Chapter 7 One Hundred Volatile Years of Volcanic Gas Studies at the Hawaiian Volcano Observatory By A. Jeff Sutton1 and Tamar Elias1 The smell of sulphur is strong, but not unpleasant to Kīlauea’s summit, together with surface-deformation and a sinner. other data, detected an increase in deep magma supply more than a year before a corresponding surge in effusive activity. —Mark Twain, Letters from Hawaii, 1866 Correspondingly, HVO routinely uses SO2 emissions to study shallow eruptive processes and effusion rates. HVO gas studies and Kīlauea’s long-running East Rift Zone eruption also demonstrate that volatile emissions can be a substantial Abstract volcanic hazard in Hawai‘i. From its humble beginning, trying to determine the chemical composition of volcanic The first volcanic gas studies in Hawai‘i, beginning gases over a century ago, HVO has evolved to routinely use in 1912, established that volatile emissions from Kīlauea real-time gas chemistry to track eruptive processes, as well Volcano contained mostly water vapor, in addition to as hazards. carbon dioxide and sulfur dioxide. This straightforward discovery overturned a popular volatile theory of the day and, in the same action, helped affirm Thomas A. Jaggar, Introduction Jr.’s, vision of the Hawaiian Volcano Observatory (HVO) as a preeminent place to study volcanic processes. Decades later, the environmental movement produced a watershed Volcanic gases are a dominating force in eruptive of quantitative analytical tools that, after being tested activity. -
Volcanic SO2 Emissions and the Abundance and Distribution of Exsolved Gas in Magma Bodies
Journal of Volcanologyand Geothermal Research 108 2001) 85±106 www.elsevier.com/locate/jvolgeores Volcanic SO2 emissions and the abundance and distribution of exsolved gas in magma bodies P.J. Wallace* Ocean Drilling Program, Texas A & M University, College Station, TX 77845, USA Abstract The mass of sulfur dioxide SO2) released bymost explosive volcanic eruptions greatlyexceeds the amount originally dissolved in the erupted volume of silicate melt. Several lines of evidence suggest that this discrepancyis due to the presence of SO2-bearing gas bubbles in the magma before the time of eruption. Comparison of remote sensing data for SO2 emissions with conventional petrologic estimates suggests that the discrepancycan be resolved if andesitic and dacitic magmas contain about 1±6 wt% exsolved gas, equivalent to 5±30 vol%, prior to eruption. Such large mass fractions of exsolved gas in pre-eruptive magma are consistent with previously published physical models in which crystallization-induced gas exsolution gradually increases overpressuring of a magma reservoir, eventuallytriggering an eruption. Simple mass balance models for SO 2 emissions from magma bodies in which there is an upwards increasing gradient in exsolved gas mass fraction i.e. gas-rich at the top) yield SO2 vs. eruptive volume trends that are similar to those observed for eruptions ranging in size from 0.01 to 10 km3 of magma. Despite the manyuncertainties involved, these patterns are consistent with the hypothesisthat subvolcanic magma reservoirs are separated from volcanic vents bycupolas of gas-rich magma that supplymuch of the gas released in explosive eruptions. The volume fraction of exsolved gas inferred from SO2 data for the upper regions of manypre-eruptive magma bodies ,30 vol%) is similar to the percolation threshold at which gas bubbles become suf®cientlyinterconnected to allow permeable gas ¯ow through a bubble network. -
Iceland Volcano Unleashes Third Lava Stream 7 April 2021
Iceland volcano unleashes third lava stream 7 April 2021 about halfway between the two sites of the earlier eruptions, gushing lava in small spurts and belching smoke. The new river of bright orange magma flowed down the slope to join an expanding field of lava at the base, now covering more than 33 hectares (81 acres), according to the last press briefing by the Icelandic Meteorological Office late Tuesday. The volcano is about 40 kilometres (25 miles) from the capital Reykjavik Lava is flowing from a third fissure that opened overnight in Iceland's nearly three-week-old volcanic eruption near the capital Reykjavik, officials said Wednesday. Tens of thousands of people have ventured to the site The spectacular eruption began on March 19 when a first fissure disgorged a steady stream of lava, flowing into the Geldingadalir valley of Mount The site had been closed to the public Monday Fagradalsfjall on Iceland's southwestern tip. because of the new activity, then reopened early Wednesday. The new split comes two days after two fissures opened around 700 metres (yards) from the initial Icelandic experts, who initially thought the eruption eruption, creating a long molten rivulet flowing into would be a short-lived affair, now think it could last a neighbouring valley. several weeks or more. The third lava stream, about a metre deep and 150 © 2021 AFP metres (490 feet) long, is a new draw for tens of thousands of gawkers taking advantage of the site's relatively easy access, just 40 kilometres (25 miles) from Reykjavik. It is about half a kilometre from the craters of the initial eruption. -
Chemical Composition of a Mud Volcano LUSI and the Health Risk
Sains Malaysiana 47(8)(2018): 1665–1674 http://dx.doi.org/10.17576/jsm-2018-4708-05 Chemical Composition of a Mud Volcano LUSI and the Health Risk Involved based on the Air Quality Index that Occurred as a Result of Disastrous Gas Exploration Drilling Activities in Sidoarjo, Indonesia (Komposisi Kimia daripada Gunung berapi LUSI dan Risiko Kesihatan yang Terlibat Berdasarkan Indeks Kualiti Udara Hasil daripada Aktiviti Penggerudian Eksplorasi Gas Bencana di Sidoarjo, Indonesia) DEWI HIDAYATI, ISMAIL B.S., SHUHAIMI-OTHMAN M. & NORELA SULAIMAN* ABSTRACT LUSI (Lumpur“mud”-Sidoarjo) is the mud volcanic which was initiated by the failed gas drilling exploration activities carried out near an urban area. The evaluation of the LUSI mud volcanic emission and its dried mud effects on air pollution and human health was carried out from 2011 to 2012. The concentrations of particulate matter (PM2.5), hazardous gases (H2S, SO2, NO2), volatile organic compounds (VOC): Including total hydrocarbons (THC)), toluene (C6H5CH3) and benzene (C6H6) as well as heavy metals (Pb, Cr and Cd) were measured following standard methods. The results showed 3 that the average concentration of PM2.5 ranged from 24.0-399.9 μg/m , H2S: 1.53-2.92 ppm; SO2: 0.021-1.321 ppm and NO2: 0.007-0.076 ppm. The VOC included total hydrocarbons from 0.57-0.96 ppm, toluene 0.33-0.92 ppm and benzene 0.33-0.40 ppm. Furthermore, heavy metal concentrations were as follows: Pb 2.6-37.34 μg/m3; Cr 0.14-12.8 μg/m3 and 3 Cd 0.78-4.16 μg/m .