Application of Isotope Techniques for Assessing Nutrient Dynamics in River Basins
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Nitrogen Isotope Variations in the Solar System Evelyn Füri and Bernard Marty
REVIEW ARTICLE PUBLISHED ONLINE: 15 JUNE 2015 | DOI: 10.1038/NGEO2451 Nitrogen isotope variations in the Solar System Evelyn Füri and Bernard Marty The relative proportion of the two isotopes of nitrogen, 14N and 15N, varies dramatically across the Solar System, despite little variation on Earth. NASA’s Genesis mission directly sampled the solar wind and confirmed that the Sun — and, by inference, the protosolar nebula from which the Solar System formed — is highly depleted in the heavier isotope compared with the reference nitrogen isotopic composition, that of Earth’s atmosphere. In contrast, the inner planets, asteroids, and comets are enriched in 15N by tens to hundreds of per cent; organic matter in primitive meteorites records the highest 15N/14N isotopic ratios. The measurements indicate that the protosolar nebula, inner Solar System, and cometary ices represent three distinct isotopic reservoirs, and that the 15N enrichment generally increases with distance from the Sun. The 15N enrichments were probably not inherited from presolar material, but instead resulted from nitrogen isotope fractionation processes that occurred early in Solar System history. Improvements in analytical techniques and spacecraft observations have made it possible to measure nitrogen isotopic variability in the Solar System at a level of accuracy that offers a window into the processing of early Solar System material, large-scale disk dynamics and planetary formation processes. he Solar System formed when a fraction of a dense molecu- a matter of debate, the D/H isotopic tracer offers the possibility of lar cloud collapsed and a central star, the proto-Sun, started investigating the relationships between the different Solar System Tburning its nuclear fuel1. -
Stationary Source Control Techniques Document for Fine Particulate Matter
Stationary Source Control Techniques Document for Fine Particulate Matter EPA CONTRACT NO. 68-D-98-026 WORK ASSIGNMENT NO. 0-08 Prepared for: Mr. Kenneth Woodard Integrated Policy and Strategies Group (MD-15) Air Quality Strategies and Standards Division U.S. Environmental Protection Agency Research Triangle Park, North Carolina 27711 October 1998 Submitted by: EC/R Incorporated Timberlyne Center 1129 Weaver Dairy Road Chapel Hill, North Carolina 27514 Disclaimer This report has been reviewed by the Office of Air Quality Planning and Standards, U.S. Environmental Protection Agency, and has been approved for publication. Mention of trade names or commercial products is not intended to constitute endorsement or recommendation for use. Copies Copies of this document are available through the Library Services Office (MD-35), U.S. Environmental Protection Agency, Research Triangle Park, NC 27711; or from the National Technical Information Service, 5285 Port Royal Road, Springfield, VA 22161 (for a fee). This document can also be found on the Internet at the U.S. Environmental Protection Agency website (http:\\www.epa.gov/ttn/oarpg). ii CONTENTS TABLES .................................................................... ix FIGURES ................................................................... xi 1 INTRODUCTION .....................................................1-1 1.1 PURPOSE OF THIS DOCUMENT ..................................1-1 1.2 OTHER RESOURCES ............................................1-1 1.3 ORGANIZATION ...............................................1-1 -
Relaxation Sports Proximity Heritage Nature Community Transport Education
welcome relaxation sports Colmar proximity - heritage Berg nature community transport education Welcome to Colmar-Berg! Berg Castle Official residence of HRH the Grand Colmar-Berg is located in the centre Duke of Luxembourg and iconic of the country, near the Nordstad municipalities landmark of Colmar-Berg. of Ettelbruck, Diekirch, and Mersch. A brief history “large”. It is therefore not surprising, that the area are held every six years using a simple majority voting Residents are invited to play an active role in The modern history of Colmar-Berg is inexorably linked was inhabited by the Celts. The name “Berg” was system. Eligible citizens wishing to stand for election Colmar-Berg’s political, social and cultural life to the history of Berg Castle, the first section of which mentioned for the first time in documents dating may do so in an individual capacity without needing by way of consultative committees focusing on was constructed in 1740. The castle was purchased, from 800 AD. to be in a political party. In Luxembourg, the simple topics such as youth, integration, traffic and the restored and extended by William II, Luxembourg’s majority voting system is used in municipalities with environment, equality, and cultural activities. second Grand Duke. The castle was remodelled in In 1991, the official name of the municipality was fewer than 3,000 inhabitants. the early 20th century, and remains today the official changed from “Berg” to “Colmar-Berg”. residence of HRH, the Grand Duke and his family. Normally, the Municipal Council meets every two Local politics months, and the meetings are open to the public. -
Element Builder
Name: ______________________________________ Date: ________________________ Student Exploration: Element Builder Prior Knowledge Questions (Do these BEFORE using the Gizmo.) 1. What are some of the different substances that make up a pizza? _____________________ _________________________________________________________________________ 2. What substances make up water? _____________________________________________ 3. What substances make up an iron pot? _________________________________________ Elements are pure substances that are made up of one kind of atom. Pizza is not an element because it is a mixture of many substances. Water is a pure substance, but it contains two kinds of atom: oxygen and hydrogen. Iron is an element because it is composed of one kind of atom. Gizmo Warm-up Atoms are tiny particles of matter that are made up of three particles: protons, neutrons, and electrons. The Element Builder Gizmo™ shows an atom with a single proton. The proton is located in the center of the atom, called the nucleus. 1. Use the arrow buttons ( ) to add protons, neutrons, and electrons to the atom. Press Play ( ). A. Which particles are located in the nucleus? _________________________________ B. Which particles orbit around the nucleus? __________________________________ 2. Turn on Show element name. What is the element? ________________________ 3. Manipulate the gizmo to figure out what actions cause the element name to change. _____________________________________________________________________ _____________________________________________________________________ Get the Gizmo ready: Activity A: Use the arrows to create an atom with two protons, Subatomic two neutrons, and two electrons. particles Turn on Show element name. Question: What are the properties of protons, neutrons, and electrons? 1. Observe: Turn on Show element symbol and Element notation. Three numbers surround the element symbol: the mass number, electrical charge (no number is displayed if the atom is neutral), and the atomic number. -
Stable Isotope Methods in Biological and Ecological Studies of Arthropods
eea_572.fm Page 3 Tuesday, June 12, 2007 4:17 PM DOI: 10.1111/j.1570-7458.2007.00572.x Blackwell Publishing Ltd MINI REVIEW Stable isotope methods in biological and ecological studies of arthropods CORE Rebecca Hood-Nowotny1* & Bart G. J. Knols1,2 Metadata, citation and similar papers at core.ac.uk Provided by Wageningen University & Research Publications 1International Atomic Energy Agency (IAEA), Agency’s Laboratories Seibersdorf, A-2444 Seibersdorf, Austria, 2Laboratory of Entomology, Wageningen University and Research Centre, P.O. Box 8031, 6700 EH Wageningen, The Netherlands Accepted: 13 February 2007 Key words: marking, labelling, enrichment, natural abundance, resource turnover, 13-carbon, 15-nitrogen, 18-oxygen, deuterium, mass spectrometry Abstract This is an eclectic review and analysis of contemporary and promising stable isotope methodologies to study the biology and ecology of arthropods. It is augmented with literature from other disciplines, indicative of the potential for knowledge transfer. It is demonstrated that stable isotopes can be used to understand fundamental processes in the biology and ecology of arthropods, which range from nutrition and resource allocation to dispersal, food-web structure, predation, etc. It is concluded that falling costs and reduced complexity of isotope analysis, besides the emergence of new analytical methods, are likely to improve access to isotope technology for arthropod studies still further. Stable isotopes pose no environmental threat and do not change the chemistry or biology of the target organism or system. These therefore represent ideal tracers for field and ecophysiological studies, thereby avoiding reductionist experimentation and encouraging more holistic approaches. Con- sidering (i) the ease with which insects and other arthropods can be marked, (ii) minimal impact of the label on their behaviour, physiology, and ecology, and (iii) environmental safety, we advocate more widespread application of stable isotope technology in arthropod studies and present a variety of potential uses. -
Groundwater Quality Data for the Northern Sacramento Valley, 2007: Results from the California GAMA Program
Prepared in cooperation with the California State Water Resources Control Board A product of the California Groundwater Ambient Monitoring and Assessment (GAMA) Program Groundwater Quality Data for the Northern Sacramento Valley, 2007: Results from the California GAMA Program SHASTA CO Redding 5 Red Bluff TEHAMA CO Data Series 452 U.S. Department of the Interior U.S. Geological Survey Cover Photographs: Top: View looking down the fence line, 2008. (Photograph taken by Michael Wright, U.S. Geological Survey.) Bottom: A well/pump in a field, 2008. (Photograph taken by George Bennett, U.S. Geological Survey.) Groundwater Quality Data for the Northern Sacramento Valley, 2007: Results from the California GAMA Program By Peter A. Bennett, George L. Bennett V, and Kenneth Belitz In cooperation with the California State Water Resources Control Board Data Series 452 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2009 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. -
SKIMMER 2014-4.Pdf
SKIMMER 2014-4 ddd3 The Wayfarer United States Wayfarer Association Fall 2014-4 As Few Words As Possible So, thank you all. I accept, reassured in the knowledge From Your Vice Commodore that bad publicity is better than no publicity at all. Chip Cunningham, W1321, Solje What can go wrong? Right off the bat I’ve felt “Are we going to keep sailing together?” Nick asked. comfortable with the Wayfarer community, but I’m “Of course,” I answered without giving it much still on the steep part of the learning curve for thought. Wayfarer boats and sailing. I hope my perspective is an interesting way to promote the U.S. Wayfarer “You know, as helm I decide what you do, right?” Association because sailing these boats is such a good “What are you getting at, Nick?” reason for us to keep getting together. “You are going to take over from me as Vice Commodore.” And so began another day of sailing with Nick. COMMODORE COMMENTS Jim Heffernan, W1066, W2458 An organization such as the USWA is made up of volunteers who take on projects and events and those that serve as officers or committee members. The Wayfarer Class and the USWA have been very fortunate since the mid sixties to have Nick Seraphinoff involved in both areas as a skipper of numerous Wayfarers, organizer of regattas, importer of new Wayfarers, Class promoter and until recently, Vice-Commodore. The Class continues to grow throughout North America due to his efforts over the past seven years. As he hands over the sword of office and the tri-cornered chapeau to Chip Cunningham, we Chip contemplates new duties as Vice Commodore. -
12 Natural Isotopes of Elements Other Than H, C, O
12 NATURAL ISOTOPES OF ELEMENTS OTHER THAN H, C, O In this chapter we are dealing with the less common applications of natural isotopes. Our discussions will be restricted to their origin and isotopic abundances and the main characteristics. Only brief indications are given about possible applications. More details are presented in the other volumes of this series. A few isotopes are mentioned only briefly, as they are of little relevance to water studies. Based on their half-life, the isotopes concerned can be subdivided: 1) stable isotopes of some elements (He, Li, B, N, S, Cl), of which the abundance variations point to certain geochemical and hydrogeological processes, and which can be applied as tracers in the hydrological systems, 2) radioactive isotopes with half-lives exceeding the age of the universe (232Th, 235U, 238U), 3) radioactive isotopes with shorter half-lives, mainly daughter nuclides of the previous catagory of isotopes, 4) radioactive isotopes with shorter half-lives that are of cosmogenic origin, i.e. that are being produced in the atmosphere by interactions of cosmic radiation particles with atmospheric molecules (7Be, 10Be, 26Al, 32Si, 36Cl, 36Ar, 39Ar, 81Kr, 85Kr, 129I) (Lal and Peters, 1967). The isotopes can also be distinguished by their chemical characteristics: 1) the isotopes of noble gases (He, Ar, Kr) play an important role, because of their solubility in water and because of their chemically inert and thus conservative character. Table 12.1 gives the solubility values in water (data from Benson and Krause, 1976); the table also contains the atmospheric concentrations (Andrews, 1992: error in his Eq.4, where Ti/(T1) should read (Ti/T)1); 2) another category consists of the isotopes of elements that are only slightly soluble and have very low concentrations in water under moderate conditions (Be, Al). -
Carte Hydrogéologique De Nobressart - Attert NOBRESSART - ATTERT
NOBRESSART - ATTERT 68/3-4 Notice explicative CARTE HYDROGÉOLOGIQUE DE WALLONIE Echelle : 1/25 000 Photos couverture © SPW-DGARNE(DGO3) Fontaine de l'ours à Andenne Forage exploité Argilière de Celles à Houyet Puits et sonde de mesure de niveau piézométrique Emergence (source) Essai de traçage au Chantoir de Rostenne à Dinant Galerie de Hesbaye Extrait de la carte hydrogéologique de Nobressart - Attert NOBRESSART - ATTERT 68/3-4 Mohamed BOUEZMARNI, Vincent DEBBAUT Université de Liège - Campus d'Arlon Avenue de Longwy, 185 B-6700 Arlon (Belgique) NOTICE EXPLICATIVE 2011 Première édition : Janvier 2005 Actualisation partielle : Mars 2011 Dépôt légal – D/2011/12.796/2 - ISBN : 978-2-8056-0080-7 SERVICE PUBLIC DE WALLONIE DIRECTION GENERALE OPERATIONNELLE DE L'AGRICULTURE, DES RESSOURCES NATURELLES ET DE L'ENVIRONNEMENT (DGARNE-DGO3) AVENUE PRINCE DE LIEGE, 15 B-5100 NAMUR (JAMBES) - BELGIQUE Table des matières I. INTRODUCTION .................................................................................................................................. 9 II. CADRE GEOGRAPHIQUE, GEOMORPHOLOGIQUE ET HYDROGRAPHIQUE ..........................11 II.1. BASSIN DE LA SEMOIS-CHIERS............................................................................................ 11 II.2. BASSIN DE LA MOSELLE........................................................................................................ 11 II.2.1. Bassin de la Sûre ................................................................................................................. 12 -
The Government of the Grand Duchy of Luxembourg 2004
2004 The Government of the Grand Duchy of Luxembourg Biographies and Remits of the Members of Government Updated version July 2006 Impressum Contents 3 Editor The Formation of the New Government 7 Information and Press Service remits 33, bd Roosevelt The Members of Government / Remits 13 L-2450 Luxembourg biographies • Jean-Claude Juncker 15 19 Tel: +352 478-2181 Fax: +352 47 02 85 • Jean Asselborn 15 23 E-mail: [email protected] • Fernand Boden 15 25 www.gouvernement.lu 15 27 www.luxembourg.lu • Marie-Josée Jacobs ISBN : 2-87999-029-7 • Mady Delvaux-Stehres 15 29 Updated version • Luc Frieden 15 31 July 2006 • François Biltgen 15 33 • Jeannot Krecké 15 35 • Mars Di Bartolomeo 15 37 • Lucien Lux 15 39 • Jean-Marie Halsdorf 15 41 • Claude Wiseler 15 43 • Jean-Louis Schiltz 15 45 • Nicolas Schmit 15 47 • Octavie Modert 15 49 Octavie Modert François Biltgen Nicolas Schmit Mady Delvaux-Stehres Claude Wiseler Fernand Boden Lucien Lux Jean-Claude Juncker Jeannot Krecké Mars Di Bartolomeo Jean Asselborn Jean-Marie Halsdorf Marie-Josée Jacobs Jean-Louis Schiltz Luc Frieden 5 The Formation of the New Government The Formation of Having regard for major European events, the and the DP, Lydie Polfer and Henri Grethen, for 9 Head of State asked for the government to preliminary discussions with a view to the for- the New Government remain in offi ce and to deal with current matters mation of a new government. until the formation of the new government. The next day, 22 June, Jean-Claude Juncker again received a delegation from the LSAP for The distribution of seats Jean-Claude Juncker appointed a brief interview. -
Measurement of the Isotopic Composition of Dissolved Iron in the Open Ocean F
Measurement of the isotopic composition of dissolved iron in the open ocean F. Lacan, Amandine Radic, Catherine Jeandel, Franck Poitrasson, Géraldine Sarthou, Catherine Pradoux, Remi Freydier To cite this version: F. Lacan, Amandine Radic, Catherine Jeandel, Franck Poitrasson, Géraldine Sarthou, et al.. Measure- ment of the isotopic composition of dissolved iron in the open ocean. Geophysical Research Letters, American Geophysical Union, 2008, pp.L24610. 10.1029/2008GL035841. hal-00399111 HAL Id: hal-00399111 https://hal.archives-ouvertes.fr/hal-00399111 Submitted on 15 Jul 2009 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Measurement of the Isotopic Composition of dissolved Iron in the Open Ocean 2 3 Lacan1 F., Radic1 A., Jeandel1 C., Poitrasson2 F., Sarthou3 G., Pradoux1 C., Freydier2 R. 4 5 1: CNRS, LEGOS, UMR5566, CNRS-CNES-IRD-UPS, Observatoire Midi-Pyrénées, 18, Av. 6 E. Belin, 31400 Toulouse, France. 7 2: LMTG, CNRS-UPS-IRD, 14-16, avenue Edouard Belin, 31400 Toulouse, France. 8 3: LEMAR, UMR CNRS 6539, IUEM, Technopole Brest Iroise, Place Nicolas Copernic, 9 29280 Plouzané, France. 10 11 Paper published in Geophysical Research Letters (2008) L24610. 12 We acknowledge Geophysical Research Letters and the American Geophysical Union copyright 13 14 This work demonstrates for the first time the feasibility of the measurement of the isotopic 15 composition of dissolved iron in seawater for a typical open ocean Fe concentration range 16 (0.1-1nM). -
Investigation of Nitrogen Cycling Using Stable Nitrogen and Oxygen Isotopes in Narragansett Bay, Ri
University of Rhode Island DigitalCommons@URI Open Access Dissertations 2014 INVESTIGATION OF NITROGEN CYCLING USING STABLE NITROGEN AND OXYGEN ISOTOPES IN NARRAGANSETT BAY, RI Courtney Elizabeth Schmidt University of Rhode Island, [email protected] Follow this and additional works at: https://digitalcommons.uri.edu/oa_diss Recommended Citation Schmidt, Courtney Elizabeth, "INVESTIGATION OF NITROGEN CYCLING USING STABLE NITROGEN AND OXYGEN ISOTOPES IN NARRAGANSETT BAY, RI" (2014). Open Access Dissertations. Paper 209. https://digitalcommons.uri.edu/oa_diss/209 This Dissertation is brought to you for free and open access by DigitalCommons@URI. It has been accepted for inclusion in Open Access Dissertations by an authorized administrator of DigitalCommons@URI. For more information, please contact [email protected]. INVESTIGATION OF NITROGEN CYCLING USING STABLE NITROGEN AND OXYGEN ISOTOPES IN NARRAGANSETT BAY, RI BY COURTNEY ELIZABETH SCHMIDT A DISSERTATION SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN OCEANOGRAPHY UNIVERSITY OF RHODE ISLAND 2014 DOCTOR OF PHILOSOPHY DISSERTATION OF COURTNEY ELIZABETH SCHMIDT APPROVED: Thesis Committee: Major Professor Rebecca Robinson Candace Oviatt Arthur Gold Nassar H. Zawia DEAN OF THE GRADUATE SCHOOL UNIVERSITY OF RHODE ISLAND 2014 ABSTRACT Estuaries regulate nitrogen (N) fluxes transported from land to the open ocean through uptake and denitrification. In Narragansett Bay, anthropogenic N loading has increased over the last century with evidence for eutrophication in some regions of Narragansett Bay. Increased concerns over eutrophication prompted upgrades at wastewater treatment facilities (WWTFs) to decrease the amount of nitrogen discharged. The upgrade to tertiary treatment – where bioavailable nitrogen is reduced and removed through denitrification – has occurred at multiple facilities throughout Narragansett Bay’s watershed.