The Respiratory Health Hazards of Volcanic Ash: a Review for Volcanic Risk Mitigation
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Module III – Fire Analysis Fire Fundamentals: Definitions
Module III – Fire Analysis Fire Fundamentals: Definitions Joint EPRI/NRC-RES Fire PRA Workshop August 21-25, 2017 A Collaboration of the Electric Power Research Institute (EPRI) & U.S. NRC Office of Nuclear Regulatory Research (RES) What is a Fire? .Fire: – destructive burning as manifested by any or all of the following: light, flame, heat, smoke (ASTM E176) – the rapid oxidation of a material in the chemical process of combustion, releasing heat, light, and various reaction products. (National Wildfire Coordinating Group) – the phenomenon of combustion manifested in light, flame, and heat (Merriam-Webster) – Combustion is an exothermic, self-sustaining reaction involving a solid, liquid, and/or gas-phase fuel (NFPA FP Handbook) 2 What is a Fire? . Fire Triangle – hasn’t change much… . Fire requires presence of: – Material that can burn (fuel) – Oxygen (generally from air) – Energy (initial ignition source and sustaining thermal feedback) . Ignition source can be a spark, short in an electrical device, welder’s torch, cutting slag, hot pipe, hot manifold, cigarette, … 3 Materials that May Burn .Materials that can burn are generally categorized by: – Ease of ignition (ignition temperature or flash point) . Flammable materials are relatively easy to ignite, lower flash point (e.g., gasoline) . Combustible materials burn but are more difficult to ignite, higher flash point, more energy needed(e.g., wood, diesel fuel) . Non-Combustible materials will not burn under normal conditions (e.g., granite, silica…) – State of the fuel . Solid (wood, electrical cable insulation) . Liquid (diesel fuel) . Gaseous (hydrogen) 4 Combustion Process .Combustion process involves . – An ignition source comes into contact and heats up the material – Material vaporizes and mixes up with the oxygen in the air and ignites – Exothermic reaction generates additional energy that heats the material, that vaporizes more, that reacts with the air, etc. -
Correlating the Electrification of Volcanic Plumes With
Earth and Planetary Science Letters 492 (2018) 47–58 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl Correlating the electrification of volcanic plumes with ashfall textures at Sakurajima Volcano, Japan ∗ Cassandra M. Smith a, , Alexa R. Van Eaton b, Sylvain Charbonnier a, Stephen R. McNutt a, Sonja A. Behnke c, Ronald J. Thomas d, Harald E. Edens d, Glenn Thompson a a University of South Florida, School of Geosciences, Tampa, FL, United States of America b U.S. Geological Survey, Cascades Volcano Observatory, Vancouver, WA, United States of America c Los Alamos National Laboratory, Los Alamos, NM, United States of America d New Mexico Institute of Mining and Technology, Department of Physics, Socorro, NM, United States of America a r t i c l e i n f o a b s t r a c t Article history: Volcanic lightning detection has become a useful resource for monitoring remote, under-instrumented Received 7 September 2017 volcanoes. Previous studies have shown that the behavior of volcanic plume electrification responds to Received in revised form 26 March 2018 changes in the eruptive processes and products. However, there has not yet been a study to quantify the Accepted 27 March 2018 links between ash textures and plume electrification during an actively monitored eruption. In this study, Available online 11 April 2018 we examine a sequence of vulcanian eruptions from Sakurajima Volcano in Japan to compare ash textural Editor: T.A. Mather properties (grain size, shape, componentry, and groundmass crystallinity) to plume electrification using Keywords: a lightning mapping array and other monitoring data. -
Risk Factors for Malignant Mesothelioma
cancer.org | 1.800.227.2345 Malignant Mesothelioma Causes, Risk Factors, and Prevention Risk Factors A risk factor is anything that affects your chance of getting a disease such as cancer. Learn more about the risk factors for malignant mesothelioma. ● Risk Factors for Malignant Mesothelioma ● What Causes Malignant Mesothelioma? Prevention There's no way to completely prevent mesothelioma. But there are things you can do that might lower your risk. Learn more. ● Can Malignant Mesothelioma Be Prevented? Risk Factors for Malignant Mesothelioma A risk factor is anything that increases your chance of getting a disease such as cancer. Different cancers have different risk factors. Some risk factors, like smoking, can be changed. Others, like a person’s age or family history, can’t be changed. But having a 1 ____________________________________________________________________________________American Cancer Society cancer.org | 1.800.227.2345 known risk factor, or even many, does not mean that you will get the disease. And some people who get the disease may have few or no known risk factors. Researchers have found some factors that increase a person’s risk of mesothelioma. Asbestos The main risk factor for pleural mesothelioma is exposure to asbestos. In fact, most cases of pleural mesothelioma have been linked to high levels of asbestos exposure, usually in the workplace. Asbestos is a group of minerals that occur naturally as bundles of tiny fibers. These fibers are found in soil and rocks in many parts of the world. When asbestos fibers in the air are inhaled, they can get into the lungs. Fibers that stay in the lungs can travel to the ends of the small airways and enter the pleural lining of the lung and chest wall. -
Occupational Airborne Particulates
Environmental Burden of Disease Series, No. 7 Occupational airborne particulates Assessing the environmental burden of disease at national and local levels Tim Driscoll Kyle Steenland Deborah Imel Nelson James Leigh Series Editors Annette Prüss-Üstün, Diarmid Campbell-Lendrum, Carlos Corvalán, Alistair Woodward World Health Organization Protection of the Human Environment Geneva 2004 WHO Library Cataloguing-in-Publication Data Occupational airborne particulates : assessing the environmental burden of disease at national and local levels / Tim Driscoll … [et al.]. (Environmental burden of disease series / series editors: Annette Prüss-Ustun ... [et al.] ; no. 7) 1.Dust - adverse effects 2.Occupational exposure 3.Asthma - chemically induced 4.Pulmonary disease, Chronic obstructive - chemically induced 5.Pneumoconiosis - etiology 6.Cost of illness 7.Epidemiologic studies 8.Risk assessment - methods 9.Manuals I.Driscoll, Tim. II.Prüss-Üstün, Annette. III.Series. ISBN 92 4 159186 2 (NLM classification: WA 450) ISSN 1728-1652 Suggested Citation Tim Driscoll, et al. Occupational airborne particulates: assessing the environmental burden of disease at national and local levels. Geneva, World Health Organization, 2004. (Environmental Burden of Disease Series, No. 7). © World Health Organization 2004 All rights reserved. Publications of the World Health Organization can be obtained from Marketing and Dissemination, World Health Organization, 20 Avenue Appia, 1211 Geneva 27, Switzerland (tel: +41 22 791 2476; fax: +41 22 791 4857; email: [email protected]). -
Flood After Fire Fact Sheet: Risks and Protection
FACT SHEET Flood After Fire Fact Sheet Risks and Protection Floods are the most common and costly natural hazard in the nation. Whether caused by heavy rain, BE FLOODSMART – REDUCE YOUR RISK thunderstorms, or the tropical storms, the results of A flood does not have to be a catastrophic event to flooding can be devastating. While some floods develop bring high out-of-pocket costs, and you do not have over time, flash floods—particularly common after to live in a high-risk flood area to suffer flood wildfires—can occur within minutes after the onset of a damage. Around twenty percent of flood insurance rainstorm. Even areas that are not traditionally flood- claims occur in moderate-to-low risk areas. Property prone are at risk, due to changes to the landscape owners should remember: caused by fire. The Time to Prepare is Now. Gather supplies in Residents need to protect their homes and assets with case of a storm, strengthen your home against flood insurance now—before a weather event occurs damage, and review your insurance coverages. and it’s too late. No flood insurance? Remember: it typically takes 30 days for a new flood insurance policy to go WILDFIRES INCREASE THE RISK into effect, so get your policy now. You may be at an even greater risk of flooding due to . Only Flood Insurance Covers Flood Damage. recent wildfires that have burned across the region. Most standard homeowner’s policies do not cover Large-scale wildfires dramatically alter the terrain and flood damage. Flood insurance is affordable. An ground conditions. -
Fire Service Features of Buildings and Fire Protection Systems
Fire Service Features of Buildings and Fire Protection Systems OSHA 3256-09R 2015 Occupational Safety and Health Act of 1970 “To assure safe and healthful working conditions for working men and women; by authorizing enforcement of the standards developed under the Act; by assisting and encouraging the States in their efforts to assure safe and healthful working conditions; by providing for research, information, education, and training in the field of occupational safety and health.” This publication provides a general overview of a particular standards- related topic. This publication does not alter or determine compliance responsibilities which are set forth in OSHA standards and the Occupational Safety and Health Act. Moreover, because interpretations and enforcement policy may change over time, for additional guidance on OSHA compliance requirements the reader should consult current administrative interpretations and decisions by the Occupational Safety and Health Review Commission and the courts. Material contained in this publication is in the public domain and may be reproduced, fully or partially, without permission. Source credit is requested but not required. This information will be made available to sensory-impaired individuals upon request. Voice phone: (202) 693-1999; teletypewriter (TTY) number: 1-877-889-5627. This guidance document is not a standard or regulation, and it creates no new legal obligations. It contains recommendations as well as descriptions of mandatory safety and health standards. The recommendations are advisory in nature, informational in content, and are intended to assist employers in providing a safe and healthful workplace. The Occupational Safety and Health Act requires employers to comply with safety and health standards and regulations promulgated by OSHA or by a state with an OSHA-approved state plan. -
Source to Surface Model of Monogenetic Volcanism: a Critical Review
Downloaded from http://sp.lyellcollection.org/ by guest on September 28, 2021 Source to surface model of monogenetic volcanism: a critical review I. E. M. SMITH1 &K.NE´ METH2* 1School of Environment, University of Auckland, Auckland, New Zealand 2Volcanic Risk Solutions, Massey University, Palmerston North 4442, New Zealand *Correspondence: [email protected] Abstract: Small-scale volcanic systems are the most widespread type of volcanism on Earth and occur in all of the main tectonic settings. Most commonly, these systems erupt basaltic magmas within a wide compositional range from strongly silica undersaturated to saturated and oversatu- rated; less commonly, the spectrum includes more siliceous compositions. Small-scale volcanic systems are commonly monogenetic in the sense that they are represented at the Earth’s surface by fields of small volcanoes, each the product of a temporally restricted eruption of a composition- ally distinct batch of magma, and this is in contrast to polygenetic systems characterized by rela- tively large edifices built by multiple eruptions over longer periods of time involving magmas with diverse origins. Eruption styles of small-scale volcanoes range from pyroclastic to effusive, and are strongly controlled by the relative influence of the characteristics of the magmatic system and the surface environment. Gold Open Access: This article is published under the terms of the CC-BY 3.0 license. Small-scale basaltic magmatic systems characteris- hazards associated with eruptions, and this is tically occur at the Earth’s surface as fields of small particularly true where volcanic fields are in close monogenetic volcanoes. These volcanoes are the proximity to population centres. -
Anatomy of a Volcanic Eruption: Case Study: Mt. St. Helens
Anatomy of a Volcanic Eruption: Case Study: Mt. St. Helens Materials Included in this Box: • Teacher Background Information • 3-D models of Mt. St. Helens (before and after eruption) • Examples of stratovolcano rock products: Tuff (pyroclastic flow), pumice, rhyolite/dacite, ash • Sandbox crater formation exercise • Laminated photos/diagrams Teacher Background There are several shapes and types of volcanoes around the world. Some volcanoes occur on the edges of tectonic plates, such as those along the ‘ring of fire’. But there are also volcanoes that occur in the middle of tectonic plates like the Yellowstone volcano and Kilauea volcano in Hawaii. When asked to draw a volcano most people will draw a steeply sided, conical mountain that has a depression (crater) at the top. This image of a 'typical' volcano is called a stratovolcano (a.k.a. composite volcano). While this is the often visualized image of a volcano, there are actually many different shapes volcanoes can be. A volcano's shape is mostly determined by the type of magma/lava that is created underneath it. Stratovolcanoes get their shape because of the thick, sticky (viscous) magma that forms at subduction zones. This magma/lava is layered between ash, pumice, and rock fragments. These layers of ash and magma will build into high elevation, steeply sided, conical shaped mountains and form a 'typical' volcano shape. Stratovolcanoes are also known for their explosive and destructive eruptions. Eruptions can cause clouds of gas, ash, dust, and rock fragments to eject into the atmosphere. These clouds of ash can become so dense and heavy that they quickly fall down the side of the volcanoes as a pyroclastic flow. -
Impact of Trace Metal Concentrations on Coccolithophore Growth and Morphology: Laboratory Simulations of Cretaceous Stress
Biogeosciences Discuss., doi:10.5194/bg-2017-138, 2017 Manuscript under review for journal Biogeosciences Discussion started: 21 April 2017 c Author(s) 2017. CC-BY 3.0 License. Impact of trace metal concentrations on coccolithophore growth and morphology: laboratory simulations of Cretaceous stress. Giulia Faucher1, Linn Hoffmann2, Lennart T. Bach3, Cinzia Bottini1, Elisabetta Erba1, Ulf Riebesell3 1 Earth Sciences Department “Ardito Desio”, Università degli Studi di Milano, Milan, Italy 5 2 Department of Botany, University of Otago, Dunedin, New Zealand 3 Biological Oceanography, GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany Correspondence to: Giulia Faucher ([email protected]) 10 Abstract. The Cretaceous ocean witnessed intervals of profound perturbations such as volcanic input of large amounts of CO2, anoxia, eutrophication, and introduction of biologically relevant metals. Some of these extreme events were characterized by size reduction and/or morphological changes of a few calcareous nannofossil species. The correspondence between intervals of high trace metal concentrations and coccolith dwarfism suggests a negative effect of these elements on nannoplankton biocalcification process in past oceans. In order to verify this hypothesis, we explored the potential effect of a 15 mixture of trace metals on growth and morphology of four living coccolithophore species, namely Emiliania huxleyi, Gephyrocapsa oceanica, Pleurochrysis carterae and Coccolithus pelagicus. These taxa are phylogenetically linked to the Mesozoic species showing dwarfism under excess metal concentrations. The trace metals tested were chosen to simulate the environmental stress identified in the geological record and upon known trace metal interaction with living coccolithophores algae. 20 Our laboratory experiments demonstrated that elevated trace metal concentrations not only affect coccolithophore algae production but, similarly to the fossil record, coccolith size and/or weight. -
Respiratory Health Effects of Volcanic Ash with Special Reference To
The Clinical Respiratory Journal REVIEW ARTICLE Respiratory health effects of volcanic ash with special reference to Iceland. A reviewcrj_231 2..9 Gunnar Gudmundsson1,2 1 Landspitali University Hospital, Reykjavik, Iceland 2 Faculty of Medicine, University of Iceland, Reykjavik, Iceland Abstract Key words Background and Aims: Volcano eruptions occur around the world and can have an health – respiratory – review – volcanic ash – impact on health in many ways both locally and on a global scale as a result of volcanic gases airborne dispersion of gases and ash or as impact on climate. In this review, a recent Correspondence volcanic eruption in Eyjafjallajökull in Iceland is described and its effects on avia- Gunnar Gudmundsson, MD, PhD, Department tion around the globe and on respiratory health in those exposed to the volcanic of Respiratory Medicine, Allergy and Sleep, ash in Iceland. Also, the effects of a large volcano eruption in Iceland in 1789 are Landspitali-University Hospital, E-7 Fossvogur, described that also had effect on a global scale by causing air pollution. IS-108 Methods and Results: The available studies reviewed here suggest that the acute Reykjavik, Iceland. and chronic health effects of volcanic ash depend on particle size (how much Tel: +354-5436876 Fax: +354-5436568 respirable), mineralogical composition (crystalline silica content) and the physico- email: [email protected] chemical properties of the surfaces of ash particles. These can vary between volca- noes and even between eruptions, making comparison difficult. Acute respiratory Received: 05 October 2010 symptoms suggesting asthma and bronchitis have been well described. Exacerba- Revision requested: 17 October 2010 tions of pre-existing lung and heart disease are common after inhalation of volcanic Accepted: 20 October 2010 ash. -
Systems Analysis of Social Resilience Against Volcanic Risks: Case Studies of Mt
Systems Analysis of Social Resilience against Volcanic Risks: Case Studies of Mt. Merapi, Indonesia and Mt. Sakurajima, Japan by Saut Aritua Hasiholan Sagala A thesis submitted in fulfilment of the requirements of the degree of Doctor of Engineering Supervised by Prof. Norio Okada DEPARTMENT OF URBAN MANAGEMENT GRADUATE SCHOOL OF ENGINEERING Kyoto University August, 2009 Acknowledgements This thesis has benefitted from collaboration with and contribution by many people. Therefore, I want to thank a number of people for their assistance while I was preparing for this thesis and completing my doctoral study in Kyoto University (KU). First of all, I would like to express my gratitude to Prof Norio Okada, my PhD advisor, who has provided a lot of important ideas for the completion of my PhD research. His excellent experiences in research fields and ways of building networks have become my source of inspiration. Finally, Prof Okada has also kindly recommended me to the scholarship provided by Monbukagakusho under Kyoto University - International Doctoral Program which funded my study in Kyoto. The next person I would like to thank is Dr. Muneta Yokomatsu, who are very kind and friendly, but at the same time has been the role model of how a real researcher should be. I have gain many insight during our discussion time. In particular I would like to thank Dr. Yokomatsu for helping me during the field visit to Mt. Sakurajima. Prof Douglas Paton of University of Tasmania has provided an enormous help for my research and has been a great discussion partner in which we have written some research articles which are parts of this thesis. -
Review of Local and Global Impacts of Volcanic Eruptions and Disaster Management Practices: the Indonesian Example
geosciences Review Review of Local and Global Impacts of Volcanic Eruptions and Disaster Management Practices: The Indonesian Example Mukhamad N. Malawani 1,2, Franck Lavigne 1,3,* , Christopher Gomez 2,4 , Bachtiar W. Mutaqin 2 and Danang S. Hadmoko 2 1 Laboratoire de Géographie Physique, Université Paris 1 Panthéon-Sorbonne, UMR 8591, 92195 Meudon, France; [email protected] 2 Disaster and Risk Management Research Group, Faculty of Geography, Universitas Gadjah Mada, Yogyakarta 55281, Indonesia; [email protected] (C.G.); [email protected] (B.W.M.); [email protected] (D.S.H.) 3 Institut Universitaire de France, 75005 Paris, France 4 Laboratory of Sediment Hazards and Disaster Risk, Kobe University, Kobe City 658-0022, Japan * Correspondence: [email protected] Abstract: This paper discusses the relations between the impacts of volcanic eruptions at multiple- scales and the related-issues of disaster-risk reduction (DRR). The review is structured around local and global impacts of volcanic eruptions, which have not been widely discussed in the literature, in terms of DRR issues. We classify the impacts at local scale on four different geographical features: impacts on the drainage system, on the structural morphology, on the water bodies, and the impact Citation: Malawani, M.N.; on societies and the environment. It has been demonstrated that information on local impacts can Lavigne, F.; Gomez, C.; be integrated into four phases of the DRR, i.e., monitoring, mapping, emergency, and recovery. In Mutaqin, B.W.; Hadmoko, D.S. contrast, information on the global impacts (e.g., global disruption on climate and air traffic) only fits Review of Local and Global Impacts the first DRR phase.