BLACK CARBON RESEAR RESEARC CH and FUTURE STRATEGIES Reducing Emissions, Improving Hhumanuman Health and Taking Action on Climate Changec Hange
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U.S. National Black Carbon and Methane Emissions a Report to the Arctic Council
U.S. NATIONAL BLACK CARBON AND METHANE EMISSIONS A REPORT TO THE ARCTIC COUNCIL AUGUST 2015 U.S. NATIONAL BLACK CARBON AND METHANE EMISSIONS A REPORT TO THE ARCTIC COUNCIL AUGUST 2015 TABLE OF CONTENTS EXECUTIVE SUMMARY. 1 ABOUT THIS REPORT. 1 SUMMARY OF CURRENT BLACK CARBON EMISSIONS AND FUTURE PROJECTIONS . 2 SUMMARY OF CURRENT METHANE EMISSIONS AND FUTURE PROJECTIONS. 4 SUMMARY OF NATIONAL MITIGATION ACTIONS BY POLLUTANT AND SECTOR . 6 BLACK CARBON . .6 METHANE . 11 HIGHLIGHTS OF BEST PRACTICES AND LESSONS LEARNED FOR KEY SECTORS . .16 TRANSPORT/MOBILE . 16 OPEN BIOMASS BURNING (INCLUDING WILDFIRES) . 16 RESIDENTIAL/DOMESTIC . .17 OIL & NATURAL GAS. .17 OTHER . 17 PROJECTS RELEVANT FOR THE ARCTIC. .18 ARCTIC AIR QUALITY IMPACT ASSESSMENT MODELING. 18 BLACK CARBON DEPOSITION ON U.S. SNOW PACK . .18 EMISSIONS AND TRANSPORT FROM AGRICULTURAL BURNING AND FOREST FIRES . .18 MEASUREMENT OF BLACK CARBON AND METHANE IN THE ARCTIC. .18 MEASUREMENT OF MARITIME BLACK CARBON EMISSIONS AND DIESEL FUEL ALTERNATIVES. .18 REDUCTION OF BLACK CARBON IN THE RUSSIAN ARCTIC. .19 VALDAY CLUSTER UPGRADE FOR BLACK CARBON REDUCTION IN THE REPUBLIC OF KARELIA, RUSSIAN FEDERATION. 19 AVIATION CLIMATE CHANGE RESEARCH INITIATIVE. .20 TRACKING SOURCES OF BLACK CARBON IN THE ARCTIC . 20 OTHER INFORMATION. .20 APPENDIX 1: U.S. BLACK CARBON EMISSIONS . .22 APPENDIX 2: U.S. METHANE EMISSIONS (MMT CO2E), 1990–2013 . 24 EXECUTIVE SUMMARY U.S. black carbon emissions are declining and additional reductions are expected, largely through strategies to reduce the emissions from mobile diesel engines that account for roughly 40 percent of the U.S. total. A number of fine particulate matter (PM2.5) control strategies have proven successful in reducing black carbon emissions from mobile sources. -
Climate Effects of Black Carbon Aerosols in China and India Surabi Menon, Et Al
Climate Effects of Black Carbon Aerosols in China and India Surabi Menon, et al. Science 297, 2250 (2002); DOI: 10.1126/science.1075159 The following resources related to this article are available online at www.sciencemag.org (this information is current as of October 3, 2008 ): Updated information and services, including high-resolution figures, can be found in the online version of this article at: http://www.sciencemag.org/cgi/content/full/297/5590/2250 Supporting Online Material can be found at: http://www.sciencemag.org/cgi/content/full/297/5590/2250/DC1 A list of selected additional articles on the Science Web sites related to this article can be found at: http://www.sciencemag.org/cgi/content/full/297/5590/2250#related-content This article cites 23 articles, 3 of which can be accessed for free: http://www.sciencemag.org/cgi/content/full/297/5590/2250#otherarticles on October 3, 2008 This article has been cited by 251 article(s) on the ISI Web of Science. This article has been cited by 8 articles hosted by HighWire Press; see: http://www.sciencemag.org/cgi/content/full/297/5590/2250#otherarticles This article appears in the following subject collections: Atmospheric Science http://www.sciencemag.org/cgi/collection/atmos www.sciencemag.org Information about obtaining reprints of this article or about obtaining permission to reproduce this article in whole or in part can be found at: http://www.sciencemag.org/about/permissions.dtl Downloaded from Science (print ISSN 0036-8075; online ISSN 1095-9203) is published weekly, except the last week in December, by the American Association for the Advancement of Science, 1200 New York Avenue NW, Washington, DC 20005. -
This Ubiquitous Carbon…
Engineering Physics Department Presents Dr. Cristian Contescu Senior Research Staff, Materials Science and Technology Division Oak Ridge National Laboratory This ubiquitous carbon… Abstract: After Stone Age, Bronze Age, and Iron Age, and after the Silicon Age of the informational revolution, the technologies of 21st century are marked by the ubiquitous presence of various forms of carbon allotropes. For a very long time, diamond and graphite were the only known carbon allotropes, but that has changed with the serendipitous discovery of fullerenes, carbon nanotubes, and graphene. Every ten or fifteen years scientists unveil new forms of carbons with new and perplexing properties, while computations suggest that the carbon’s family still has members unknown to us today. At a dramatically accelerated pace, new carbon forms find their place at the leading edge of scientific and technological innovations. At the same time traditional forms of carbon are being used in new and exciting applications that make our life safer, healthier, and more enjoyable. The 21st century may soon be recognized as the Age of Carbon forms. This educational talk will show how carbon, the fourth most abundant element in the Galaxy and the basis of life on Earth, was the engine of most important technological developments throughout the history of civilization. It will emphasize the ability of carbon atoms to generate a variety of mutual combinations and with many other chemical elements. These properties have placed carbon at the core of numerous inventions that define our civilization, while emerging new technologies open a rich path for value-added products in today’s market. -
Properties of Carbon the Atomic Element Carbon Has Very Diverse
Properties of Carbon The atomic element carbon has very diverse physical and chemical properties due to the nature of its bonding and atomic arrangement. fig. 1 Allotropes of Carbon Some allotropes of carbon: (a) diamond, (b) graphite, (c) lonsdaleite, (d–f) fullerenes (C60, C540, C70), (g) amorphous carbon, and (h) carbon nanotube. Carbon has several allotropes, or different forms in which it can exist. These allotropes include graphite and diamond, whose properties span a range of extremes. Despite carbon's ability to make 4 bonds and its presence in many compounds, it is highly unreactive under normal conditions. Carbon exists in 2 main isotopes: 12C and 13C. There are many other known isotopes, but they tend to be short-lived and have extremely short half-lives. Allotropes The different forms of a chemical element. Cabon is the chemical element with the symbol C and atomic number 6. As a member of group 14 on the periodic table, it is nonmetallic and tetravalent—making four electrons available to form covalent chemical bonds. Carbon has 6 protons and 6 Source URL: https://www.boundless.com/chemistry/nonmetallic-elements/carbon/properties-carbon/ Saylor URL: http://www.saylor.org/courses/chem102#6.1 Attributed to: Boundless www.saylor.org Page 1 of 2 neutrons, and has a standard atomic weight of 12.0107 amu. Its electron configuration is denoted as 1s22s22p2. It is a solid, and sublimes at 3,642 °C. It's oxidation state ranges from 4 to -4, and it has an electronegativity rating of 2.55 on the Pauling scale. Carbon has several allotropes, or different forms in which it exists. -
Aerosols, Their Direct and Indirect Effects
5 Aerosols, their Direct and Indirect Effects Co-ordinating Lead Author J.E. Penner Lead Authors M. Andreae, H. Annegarn, L. Barrie, J. Feichter, D. Hegg, A. Jayaraman, R. Leaitch, D. Murphy, J. Nganga, G. Pitari Contributing Authors A. Ackerman, P. Adams, P. Austin, R. Boers, O. Boucher, M. Chin, C. Chuang, B. Collins, W. Cooke, P. DeMott, Y. Feng, H. Fischer, I. Fung, S. Ghan, P. Ginoux, S.-L. Gong, A. Guenther, M. Herzog, A. Higurashi, Y. Kaufman, A. Kettle, J. Kiehl, D. Koch, G. Lammel, C. Land, U. Lohmann, S. Madronich, E. Mancini, M. Mishchenko, T. Nakajima, P. Quinn, P. Rasch, D.L. Roberts, D. Savoie, S. Schwartz, J. Seinfeld, B. Soden, D. Tanré, K. Taylor, I. Tegen, X. Tie, G. Vali, R. Van Dingenen, M. van Weele, Y. Zhang Review Editors B. Nyenzi, J. Prospero Contents Executive Summary 291 5.4.1 Summary of Current Model Capabilities 313 5.4.1.1 Comparison of large-scale sulphate 5.1 Introduction 293 models (COSAM) 313 5.1.1 Advances since the Second Assessment 5.4.1.2 The IPCC model comparison Report 293 workshop: sulphate, organic carbon, 5.1.2 Aerosol Properties Relevant to Radiative black carbon, dust, and sea salt 314 Forcing 293 5.4.1.3 Comparison of modelled and observed aerosol concentrations 314 5.2 Sources and Production Mechanisms of 5.4.1.4 Comparison of modelled and satellite- Atmospheric Aerosols 295 derived aerosol optical depth 318 5.2.1 Introduction 295 5.4.2 Overall Uncertainty in Direct Forcing 5.2.2 Primary and Secondary Sources of Aerosols 296 Estimates 322 5.2.2.1 Soil dust 296 5.4.3 Modelling the Indirect -
Black Carbon-Induced Snow Albedo Reduction Over the Tibetan Plateau
Atmos. Chem. Phys., 18, 11507–11527, 2018 https://doi.org/10.5194/acp-18-11507-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Black carbon-induced snow albedo reduction over the Tibetan Plateau: uncertainties from snow grain shape and aerosol–snow mixing state based on an updated SNICAR model Cenlin He1,2, Mark G. Flanner3, Fei Chen2,4, Michael Barlage2, Kuo-Nan Liou5, Shichang Kang6,7, Jing Ming8, and Yun Qian9 1Advanced Study Program, National Center for Atmospheric Research, Boulder, CO, USA 2Research Applications Laboratory, National Center for Atmospheric Research, Boulder, CO, USA 3Department of Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI, USA 4State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing, China 5Joint Institute for Regional Earth System Science and Engineering, and Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, CA, USA 6State key laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, China 7CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, China 8Multiphase Chemistry Department, Max Planck Institute for Chemistry, Mainz, Germany 9Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, USA Correspondence: Cenlin He ([email protected]) Received: 12 May 2018 – Discussion started: 22 May 2018 Revised: 31 July 2018 – Accepted: 4 August 2018 – Published: 15 August 2018 Abstract. We implement a set of new parameterizations into regional and seasonal variations, with higher values in the the widely used Snow, Ice, and Aerosol Radiative (SNICAR) non-monsoon season and low altitudes. -
Sp Carbon Chain Interaction with Silver Nanoparticles Probed by Surface Enhanced Raman Scattering
sp carbon chain interaction with silver nanoparticles probed by Surface Enhanced Raman Scattering A. Lucotti1, C. S. Casari2, M. Tommasini1, A. Li Bassi2, D. Fazzi1, V. Russo2, M. Del Zoppo1, C. Castiglioni1, F. Cataldo3, C. E. Bottani2, G. Zerbi1 1 Dipartimento di Chimica, Materiali e Ingegneria Chimica ‘G. Natta’ and NEMAS - Center for NanoEngineered MAterials and Surfaces, Politecnico di Milano, Piazza Leonardo da Vinci 32, I-20133 Milano, Italy 2 Dipartimento di Energia and NEMAS - Center for NanoEngineered MAterials and Surfaces, Politecnico di Milano, via Ponzio 34/3, I-20133 Milano, Italy 3 Actinium Chemical Research srl, via Casilina 1626/A, 00133 Roma, Italy and INAF – Osservatorio Astrofisico di Catania, Via S. Sofia 78, 95123 Catania, Italy Abstract Surface Enhanced Raman Spectroscopy (SERS) is exploited here to investigate the interaction of isolated sp carbon chains (polyynes) in a methanol solution with silver nanoparticles. Hydrogen-terminated polyynes show a strong interaction with silver colloids used as the SERS active medium revealing a chemical SERS effect. SERS spectra after mixing polyynes with silver colloids show a noticeable time evolution. Experimental results, supported by density functional theory (DFT) calculations of the Raman modes, allow us to investigate the behaviour and stability of polyynes of different lengths and the overall sp conversion towards sp2 phase. 1 2 1. Introduction Linear carbon chains with sp hybridization represent one of the simplest one dimensional systems and have therefore attracted a great interest for many years [1, 2]. sp chains can display two types of carbon-carbon bonding: polyynes, chains with single-triple alternating bonds (…-C≡C- C≡C-…) and polycumulenes, chains with all double bonds (…=C=C=C=…). -
Agricultural Soil Carbon Credits: Making Sense of Protocols for Carbon Sequestration and Net Greenhouse Gas Removals
Agricultural Soil Carbon Credits: Making sense of protocols for carbon sequestration and net greenhouse gas removals NATURAL CLIMATE SOLUTIONS About this report This synthesis is for federal and state We contacted each carbon registry and policymakers looking to shape public marketplace to ensure that details investments in climate mitigation presented in this report and through agricultural soil carbon credits, accompanying appendix are accurate. protocol developers, project developers This report does not address carbon and aggregators, buyers of credits and accounting outside of published others interested in learning about the protocols meant to generate verified landscape of soil carbon and net carbon credits. greenhouse gas measurement, reporting While not a focus of the report, we and verification protocols. We use the remain concerned that any end-use of term MRV broadly to encompass the carbon credits as an offset, without range of quantification activities, robust local pollution regulations, will structural considerations and perpetuate the historic and ongoing requirements intended to ensure the negative impacts of carbon trading on integrity of quantified credits. disadvantaged communities and Black, This report is based on careful review Indigenous and other communities of and synthesis of publicly available soil color. Carbon markets have enormous organic carbon MRV protocols published potential to incentivize and reward by nonprofit carbon registries and by climate progress, but markets must be private carbon crediting marketplaces. paired with a strong regulatory backing. Acknowledgements This report was supported through a gift Conservation Cropping Protocol; Miguel to Environmental Defense Fund from the Taboada who provided feedback on the High Meadows Foundation for post- FAO GSOC protocol; Radhika Moolgavkar doctoral fellowships and through the at Nori; Robin Rather, Jim Blackburn, Bezos Earth Fund. -
Black Carbon and Methane in the Norwegian Barents Region Black Carbon and Methane in the Norwegian Barents Region | M276
REPORT M-276 | 2014 Black carbon and methane in the Norwegian Barents region Black carbon and methane in the Norwegian Barents region | M276 COLOPHON Executive institution The Norwegian Environment Agency Project manager for the contractor Contact person in the Norwegian Environment Agency Ingrid Lillehagen, The Ministry of Climate and Solrun Figenschau Skjellum Environment, section for polar affairs and the High North M-no Year Pages Contract number M-276 2014 15 Publisher The project is funded by The Norwegian Environment Agency The Norwegian Environment Agency Author(s) Maria Malene Kvalevåg, Vigdis Vestreng and Nina Holmengen Title – Norwegian and English Black carbon and methane in the Norwegian Barents Region Svart karbon og metan i den norske Barentsregionen Summary – sammendrag In 2011, land based emissions of black carbon and methane in the Norwegian Barents region were 400 tons and 23 700 tons, respectively. The largest emissions of black carbon originate from the transport sector and wood combustion in residential heating. For methane, the largest contributors to emissions are the agricultural sector and landfills. Different measures to reduce emissions from black carbon and methane can be implemented. Retrofitting of diesel particulate filters on light and heavy vehicles, tractors and construction machines will reduce black carbon emitted from the transport sector. Measures to reduce black carbon from residential heating are to accelerate the introduction of wood stoves with cleaner burning, improve burning techniques and inspect and maintain the wood stoves that are already in use. In the agricultural sector, methane emissions from food production can be reduced by using manure or food waste as raw material to biogas production. -
Saving the Arctic the Urgent Need to Cut Black Carbon Emissions and Slow Climate Change
AP PHOTO/IAN JOUGHIN PHOTO/IAN AP Saving the Arctic The Urgent Need to Cut Black Carbon Emissions and Slow Climate Change By Rebecca Lefton and Cathleen Kelly August 2014 WWW.AMERICANPROGRESS.ORG Saving the Arctic The Urgent Need to Cut Black Carbon Emissions and Slow Climate Change By Rebecca Lefton and Cathleen Kelly August 2014 Contents 1 Introduction and summary 3 Where does black carbon come from? 6 Future black carbon emissions in the Arctic 9 Why cutting black carbon outside the Arctic matters 13 Recommendations 19 Conclusion 20 Appendix 24 Endnotes Introduction and summary The Arctic is warming at a rate twice as fast as the rest of the world, in part because of the harsh effects of black carbon pollution on the region, which is made up mostly of snow and ice.1 Black carbon—one of the main components of soot—is a deadly and widespread air pollutant and a potent driver of climate change, espe- cially in the near term and on a regional basis. In colder, icier regions such as the Arctic, it peppers the Arctic snow with heat-absorbing black particles, increasing the amount of heat absorbed and rapidly accelerating local warming. This accel- eration exposes darker ground or water, causing snow and ice melt and lowering the amount of heat reflected away from the Earth.2 Combating climate change requires immediate and long-term cuts in heat-trap- ping carbon pollution, or CO2, around the globe. But reducing carbon pollution alone will not be enough to avoid the worst effects of a rapidly warming Arctic— slashing black carbon emissions near the Arctic and globally must also be part of the solution. -
Black Carbon's Properties and Role in the Environment
Sustainability 2010, 2, 294-320; doi:10.3390/su2010294 OPEN ACCESS sustainability ISSN 2071-1050 www.mdpi.com/journal/sustainability Review Black Carbon’s Properties and Role in the Environment: A Comprehensive Review Gyami Shrestha 1,*, Samuel J. Traina 1 and Christopher W. Swanston 2 1 Environmental Systems Program, Sierra Nevada Research Institute, University of California- Merced, 5200 N. Lake Road, Merced, CA 95343, USA; E-Mail: [email protected] 2 Northern Institute of Applied Carbon Science, Climate, Fire, & Carbon Cycle Science Research, Northern Research Station, USDA Forest Service, 410 MacInnes Drive, Houghton, MI 49931, USA; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]. Received: 13 November 2009 / Accepted: 7 January 2010 / Published: 15 January 2010 Abstract: Produced from incomplete combustion of biomass and fossil fuel in the absence of oxygen, black carbon (BC) is the collective term for a range of carbonaceous substances encompassing partly charred plant residues to highly graphitized soot. Depending on its form, condition of origin and storage (from the atmosphere to the geosphere), and surrounding environmental conditions, BC can influence the environment at local, regional and global scales in different ways. In this paper, we review and synthesize recent findings and discussions on the nature of these different forms of BC and their impacts, particularly in relation to pollution and climate change. We start by describing the different types of BCs and their mechanisms of formation. To elucidate their pollutant sorption properties, we present some models involving polycyclic aromatic hydrocarbons and organic carbon. Subsequently, we discuss the stability of BC in the environment, summarizing the results of studies that showed a lack of chemical degradation of BC in soil and those that exposed BC to severe oxidative reactions to degrade it. -
Introduction to Chemistry
Introduction to Chemistry Author: Tracy Poulsen Digital Proofer Supported by CK-12 Foundation CK-12 Foundation is a non-profit organization with a mission to reduce the cost of textbook Introduction to Chem... materials for the K-12 market both in the U.S. and worldwide. Using an open-content, web-based Authored by Tracy Poulsen collaborative model termed the “FlexBook,” CK-12 intends to pioneer the generation and 8.5" x 11.0" (21.59 x 27.94 cm) distribution of high-quality educational content that will serve both as core text as well as provide Black & White on White paper an adaptive environment for learning. 250 pages ISBN-13: 9781478298601 Copyright © 2010, CK-12 Foundation, www.ck12.org ISBN-10: 147829860X Except as otherwise noted, all CK-12 Content (including CK-12 Curriculum Material) is made Please carefully review your Digital Proof download for formatting, available to Users in accordance with the Creative Commons Attribution/Non-Commercial/Share grammar, and design issues that may need to be corrected. Alike 3.0 Unported (CC-by-NC-SA) License (http://creativecommons.org/licenses/by-nc- sa/3.0/), as amended and updated by Creative Commons from time to time (the “CC License”), We recommend that you review your book three times, with each time focusing on a different aspect. which is incorporated herein by this reference. Specific details can be found at http://about.ck12.org/terms. Check the format, including headers, footers, page 1 numbers, spacing, table of contents, and index. 2 Review any images or graphics and captions if applicable.