Briggs, Joseph Henry (2021)

Total Page:16

File Type:pdf, Size:1020Kb

Briggs, Joseph Henry (2021) Briggs, Joseph Henry (2021) The analysis, experimental characterisation and prototyping of technologies for making quantum noise limited detections of gravitational waves. PhD thesis, University of Glasgow. http://theses.gla.ac.uk/82330/ Copyright and moral rights for this work are retained by the author A copy can be downloaded for personal non-commercial research or study, without prior permission or charge This work cannot be reproduced or quoted extensively from without first obtaining permission in writing from the author The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the author When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given Enlighten: Theses https://theses.gla.ac.uk/ [email protected] The Analysis, Experimental Characterisation and Prototyping of Technologies for Making Quantum Noise Limited Detections of Gravitational Waves Joseph Henry Briggs Wednesday 14th July, 2021 Submitted in fulfillment of the requirements for the Degree of Doctor of Philosophy School of Physics and Astronomy College of Science and Engineering University of Glasgow Abstract The detection of gravitational waves is essential for developing our understanding of the Universe. Systems such as inspiralling binaries of black holes and neutron stars produce gravitational waves, and much of the information carried by a gravitational wave cannot be obtained via any other means. Gravitational waves interact weakly with matter, so kilometre-scale interferometers, such as the LIGO detectors, are the only instruments which have directly measured the strain induced in space-time by gravitational waves. To more accurately determine the parameters of individual sources and to refine statistical models of these systems, it is vital that the sensitivity of these interferometers is increased. To reduce the quantum shot noise of the LIGO detectors, they require a low noise, high power laser. This thesis contains experimental characterisation of the prototype for the laser that will be used during LIGO’s fourth observation run. This laser generated over 100 W of amplitude stabilised light in the HG00 mode making it is an important step towards reaching the design sensitivity of the LIGO detectors. i A current shunt was compared to an acousto-optic modulator (AOM) for use as the actuator in the control loop for stabilising the laser’s amplitude. It was found that the AOM was more reliable and more versatile than the current shunt, and so it was recommended that the AOM was used during LIGO’s fourth observation run. However, the current shunt may allow for ∼ 10 W more power to be delivered to the interferometer, so this should be considered when the maximum laser power that is used by LIGO is limited by the power wasted by the AOM. Balanced homodyne detection is a key part of the upgrade from advanced LIGO to LIGO A+. To lower the quantum noise of the detectors by harnessing the quan- tum nature of light, it is crucial that the balanced homodyne detector has minimal loss. Mode mismatches between the interferometer and the output mode cleaners are a source of loss; therefore, active optics for mode matching between the inter- ferometer and the output mode cleaner will be used. In this thesis, the uncertainty in the radii of curvature of the optics in the signal recycling cavity (SRC) was used to calculate the distribution of modes which may be present at the signal recycling mirror (SRM). For the LIGO Livingston Observatory, LA., USA (LLO), it was found that the uncertainty in the radii of curvature of an optic known as SR3 is the largest source of uncertainty in the beam parameter at the SRM. From a measurement of the SRC’s Gouy phase, the arm mode at the SRM was inferred to have a width of 1.8 mm and a defocus of −0:28 m−1. Visualisations for the amount of these modes which the active optics should be able to correct for were created, and it was found that for LIGO A+, a mode mismatch up to 5% can be entirely corrected with the active optics. ii Third-generation ground-based gravitational wave detectors, such as the Ein- stein Telescope and LIGO Cosmic Explorer, will be far more sensitive and be able to probe deeper into the Universe than the current generation of detectors. The increase in sensitivity may be achieved with cryogenically cooled crystalline silicon test masses, but the wavelength of light used in current gravitational wave detectors, 1µm, will not be compatible with these test masses due to them being opaque to this wavelength. Instead, these test masses may work with 2µm light. High quantum efficiency photodiodes are required if the detector’s quantum noise is to be minimal, so off-the-shelf extended InGaAs photodiodes that are sensitive to 2µm light were characterised in the context of the unique requirements of a gravitational wave detector. Both quantum efficiency and 1=f dark noise rise as the reverse bias of an extended InGaAs photodiode increases. A maximum reverse bias was found for the eight photodiodes that were tested such that their dark noises were below the shot noise of a typical current (∼ 10 mA) generated by the photodiode used to sense the gravitational wave signals in an interferometer. The effect of temperature on the dark noise was also investigated. It was found that current off-the-shelf extended InGaAs photodiodes will not be suitable for third-generation detectors as they do not have sufficient quantum efficiency while they are biased such that their dark noise is below shot noise in the frequency band of interest in ground-based gravitational wave detection. Cooling may help reduce this noise, but this poses a significant engineering challenge and the quantum efficiency requirement is still unlikely to be met. Significant amounts of re- search into the optimal conditions for manufacturing extended InGaAs photodiodes iii would be needed before using them in a third-generation detector is viable. iv Acknowledgements I would like to thank Ken Strain for his supervision and advice during the course of my PhD. He set a great example of how to be a scientific thinker, and he was an invaluable source of experience and knowledge. Ken always made time to answer my questions, explain things to me and give me feedback on the work that I was doing. I am grateful to Bryan Barr for his assistance and insights. Many times through- out my PhD, Bryan offered his time and energy to help me understand how I could solve a problem I was having, and his practical advice was indispensable. I also want to thank Stefan Hild for his guidance, enthusiasm, and encouragement during the first two years of my PhD. Regarding the production of this thesis, I would like to thank Ken Strain, Bryan Barr, Harry Ward, Giles Hammond and Peter Veitch. They highlighted numerous places where I could improve its clarity, spotted typos and suggested structural changes. Of course, any remaining typos are solely my responsibility. v Thanks to my friends for all the walks up mountains, pub trips, the coffee breaks and all the fun conversations. I couldn’t know a better bunch of people to spend my free time with. I would like to thank Dwayne Spiteri for being a great friend and housemate. The writing of this thesis happened during an unusual year, and it was certainly made easier by having him around. I would also like to thank him for his (not always solicited) opinions about what I was thinking about and working on. I would like to thank my family for their never-ending love. Mum, Dad, James and Isabelle have encouraged and supported me at every stage of my life so far. They are always there for me and have helped me at many times to get the best out of life. I cannot be more grateful for my family and I would not be the person I am today without them. To Catriona, thank you for your love, care and support. You bring so much vibrancy, warmth and joy to the lives of all the people you know, and I feel so incredibly lucky to be with you. Your companionship has given me a great sense of happiness and fulfilment, and my life has been made so much more wonderful by sharing it with you. vi Declaration I declare that the work described in this thesis was carried out by me and has not been presented in any previous application for a degree at the University of Glasgow or any other institution. The chapters in this thesis and the contributions of others to them are described below. Chapter 1 This chapter contains introductory information pertaining to ground- based gravitational wave interferometry and the LIGO detectors. Chapter 2 In this chapter, experiments to do with the prototype of the laser that will be used for LIGO’s fourth observation run are described. My contribution to this work was in the setup of the optical table and the taking of measurements. These tasks were completed with help from Nina Bode, Matthew Heintze and Michael Fyffe. Rick Savage and Maik Frede contributed to discussions of how this should be done. The diagnostic breadboard was supplied by the AEI. The design of the prototype was undertaken by others. The outcome of this project was published in [1]. The photographs of the laser were taken by Michael Fyffe. This work was carried out at the LIGO Livingston Observatory as part of the LSC fellows programme and was funded by the STFC long-term attachment scheme.
Recommended publications
  • Regional Structural Setting of Yucca Mountain, Southwestern Nevada
    ) i WM RECORD COPY I: // lt- USGS-OFR-84-854 - USGS-OFR-84-854 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY REGIONAL STRUCTURAL SETTING OF YUCCA MOUNTAIN, SOUTHWESTERN NEVADA, AND LATE CENOZOIC RATES OF TECTONIC ACTIVITY IN PART OF THE SOUTHWESTERN GREAT BASIN, NEVADA AND CALIFORNIA by U. J. Carr 06 : . , CD CD. Open-File Report 84-854 Prepared in cooperation with the Nevada Operations Office U.S. Department of Energy (Interagency Agreement DE-AI08-78ET44802) This report is preliminary and has not been reviewed for-conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Company names are for descriptive purposes only and do not constitute endorsement by the U.S. Geological Survey. Denver, Colorado 1984 ~~- ~ - ~~ ___~~~ Copies of this Open-File Report may be purchased from Open-File Services Secton Branch of Distribution U.S. Geological Survey Box 25425, Federal Center Denver, Colorado 80225 PREPAYMENT IS REQUIRED Price information will be published in the monthly listing 'New Publications of the Geological Survey" FOR ADDITIONAL ORDERING INFORMATION CALL: Commercial: (303) 236-7476 FTS: 776-7476 USGS-OFR-84-854 USGS-OFR-84-854 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Denver, Colorado REGIONAL STRUCTURAL SETTING OF YUCCA MOUNTAIN, SOUTHWESTERN NEVADA, AND LATE CENOZOIC RATES OF TECTONIC ACTIVITY IN PART OF THE SOUTHWESTERN GREAT BASIN, NEVADA AND CALIFORNIA by W. J. Carr CONTENTS Page Abstract................................................................... 1 Introduction.................................................................................................. 4 Structural-physiographic subsections of the southwestern Great Basin ....... 9 Walker Lane belt ........................................ ...... ** 9 Basin-range subsection ..................................................21 Inyo-Mono subsection ............................................................26 Boundary between Inyo-Mono and Walker Lane belt subsections ......
    [Show full text]
  • Petrogenes1.S of Apollo 11 Basalts and Implications
    PETROGENES1.S OF APOLLO 11 BASALTS AND IMPLICATIONS FOR LUNAR ORIGIN A, E. Rinqwood Department of Geophysics and Geochemistry Australian National University Canberra ABSTRACT The origin of Apollo 11 basalts is discussed in terms of two hypotheses: (i) formation by a small degree of partial melting in the lunar interior and (ii) formation by prolonged near-surface crystallization differentiation in a lava lake. The second hypoth- esis is rejected on the following grounds: Most Apollo 11 magmas are far removed from the plagioclase-pyroxene-ilmenite cotectic; fractional crystallization cannot explain the large variations in concentrations of incompatible trace elehents in conjunction with the small variations in major element compositions, particularly, _IMg ratios; experimentally determined partition coefficients show Fe Pack3 that the high abundances of Cr and V in Apollo 11 cannot be reconciled A with the previous separation of large quantities of ore minerals and pyroxenes. On the other hand, the major element and trace element jq contents of Apollo 11 rocks can be explained by partial melting of sovvromaterial which buffers the major element compositions and causes enrichments of incompatible elements according to the degree of partial melting( fiisk hypbthesis) Two alternative sources have been suggested for Apollo 11 basalts formed by partial melting: (i) unfractionated pyroxenite source region at depths of 200-600 km, (ii) fractionated source region with incompatible elements (e-g. Ba, U, rare 'earths) strongly enriched over chondritic abundances and containing plagioclase (approximate eucritic composition). Mass balance calculations'and plagioclase stability conditions show that the second hypothesis requires Apollo 1l.basalts to be generated by partial melting in the outer 150 km of the moon.
    [Show full text]
  • Alpha ELT Listing
    Lienholder Name Lienholder Address City State Zip ELT ID 1ST ADVANTAGE FCU PO BX 2116 NEWPORT NEWS VA 23609 CFW 1ST COMMAND BK PO BX 901041 FORT WORTH TX 76101 FXQ 1ST FNCL BK USA 47 SHERMAN HILL RD WOODBURY CT 06798 GVY 1ST LIBERTY FCU PO BX 5002 GREAT FALLS MT 59403 ESY 1ST NORTHERN CA CU 1111 PINE ST MARTINEZ CA 94553 EUZ 1ST NORTHERN CR U 230 W MONROE ST STE 2850 CHICAGO IL 60606 GVK 1ST RESOURCE CU 47 W OXMOOR RD BIRMINGHAM AL 35209 DYW 1ST SECURITY BK WA PO BX 97000 LYNNWOOD WA 98046 FTK 1ST UNITED SVCS CU 5901 GIBRALTAR DR PLEASANTON CA 94588 W95 1ST VALLEY CU 401 W SECOND ST SN BERNRDNO CA 92401 K31 360 EQUIP FIN LLC 300 BEARDSLEY LN STE D201 AUSTIN TX 78746 DJH 360 FCU PO BX 273 WINDSOR LOCKS CT 06096 DBG 4FRONT CU PO BX 795 TRAVERSE CITY MI 49685 FBU 777 EQUIPMENT FIN LLC 600 BRICKELL AVE FL 19 MIAMI FL 33131 FYD A C AUTOPAY PO BX 40409 DENVER CO 80204 CWX A L FNCL CORP PO BX 11907 SANTA ANA CA 92711 J68 A L FNCL CORP PO BX 51466 ONTARIO CA 91761 J90 A L FNCL CORP PO BX 255128 SACRAMENTO CA 95865 J93 A L FNCL CORP PO BX 28248 FRESNO CA 93729 J95 A PLUS FCU PO BX 14867 AUSTIN TX 78761 AYV A PLUS LOANS 500 3RD ST W SACRAMENTO CA 95605 GCC A/M FNCL PO BX 1474 CLOVIS CA 93613 A94 AAA FCU PO BX 3788 SOUTH BEND IN 46619 CSM AAC CU 177 WILSON AVE NW GRAND RAPIDS MI 49534 GET AAFCU PO BX 619001 MD2100 DFW AIRPORT TX 75261 A90 ABLE INC 503 COLORADO ST AUSTIN TX 78701 CVD ABNB FCU 830 GREENBRIER CIR CHESAPEAKE VA 23320 CXE ABOUND FCU PO BX 900 RADCLIFF KY 40159 GKB ACADEMY BANK NA PO BX 26458 KANSAS CITY MO 64196 ATF ACCENTRA CU 400 4TH
    [Show full text]
  • Board Certified Fellows
    AMERICAN BOARD OF MEDICOLEGAL DEATH INVESTIGATORS Certificant Directory As of September 30, 2021 BOARD CERTIFIED FELLOWS Addison, Krysten Leigh (Inactive) BC2286 Allmon, James L. BC855 Travis County Medical Examiner's Office Sangamon County Coroner's Office 1213 Sabine Street 200 South 9th, Room 203 PO Box 1748 Springfield, IL 62701 Austin, TX 78767 Amini, Navid BC2281 Appleberry, Sherronda BC1721 Olmsted Medical Examiner's Office Adams and Broomfield County Office of the Coroner 200 1st Street Southwest 330 North 19th Avenue Rochester, MN 55905 Brighton, CO 80601 Applegate, MD, David T. BC1829 Archer, Meredith D. BC1036 Union County Coroner's Office Mohave County Medical Examiner 128 South Main Street 1145 Aviation Drive Unit A Marysville, OH 43040 Lake Havasu, AZ 86404 Bailey, Ted E. (Inactive) BC229 Bailey, Sanisha Renee BC1754 Gwinnett County Medical Examiner's Office Virginia Office of the Chief Medical Examiner 320 Hurricane Shoals Road, NE Central District Lawrenceville, GA 30046 400 East Jackson Street Richmond, VA 23219 Balacki, Alexander J BC1513 Banks, Elsie-Kay BC3039 Montgomery County Coroner's Office Maine Office of the Chief Medical Examiner 1430 Dekalb Street 30 Hospital Street PO Box 311 Augusta, ME 04333 Norristown, PA 19404 Bautista, Ian BC2185 Bayer, Lindsey A. BC875 New York City Office of Chief Medical Examiner District 5 and 24 Medical Examiner Office 421 East 26th Street 809 Pine Street New York, NY 10016 Leesburg, FL 34756 Beck, Shari L BC327 Beckham, Phinon Phillips BC2305 Sedgwick Co Reg. Forensic Science Center Virginia Office of the Chief Medical Examiner 1109 N. Minneapolis Northern District Wichita, KS 67214 10850 Pyramid Place, Suite 121 Manassas, VA 20110 Bednar Keefe, Gale M.
    [Show full text]
  • Northwest Plant Names and Symbols for Ecosystem Inventory and Analysis Fourth Edition
    USDA Forest Service General Technical Report PNW-46 1976 NORTHWEST PLANT NAMES AND SYMBOLS FOR ECOSYSTEM INVENTORY AND ANALYSIS FOURTH EDITION PACIFIC NORTHWEST FOREST AND RANGE EXPERIMENT STATION U.S. DEPARTMENT OF AGRICULTURE FOREST SERVICE PORTLAND, OREGON This file was created by scanning the printed publication. Text errors identified by the software have been corrected; however, some errors may remain. CONTENTS Page . INTRODUCTION TO FOURTH EDITION ....... 1 Features and Additions. ......... 1 Inquiries ................ 2 History of Plant Code Development .... 3 MASTER LIST OF SPECIES AND SYMBOLS ..... 5 Grasses.. ............... 7 Grasslike Plants. ............ 29 Forbs.. ................ 43 Shrubs. .................203 Trees. .................225 ABSTRACT LIST OF SYNONYMS ..............233 This paper is basicafly'an alpha code and name 1 isting of forest and rangeland grasses, sedges, LIST OF SOIL SURFACE ITEMS .........261 rushes, forbs, shrubs, and trees of Oregon, Wash- ington, and Idaho. The code expedites recording of vegetation inventory data and is especially useful to those processing their data by contem- porary computer systems. Editorial and secretarial personnel will find the name and authorship lists i ' to be handy desk references. KEYWORDS: Plant nomenclature, vegetation survey, I Oregon, Washington, Idaho. G. A. GARRISON and J. M. SKOVLIN are Assistant Director and Project Leader, respectively, of Paci fic Northwest Forest and Range Experiment Station; C. E. POULTON is Director, Range and Resource Ecology Applications of Earth Sate1 1 ite Corporation; and A. H. WINWARD is Professor of Range Management at Oregon State University . and a fifth letter also appears in those instances where a varietal name is appended to the genus and INTRODUCTION species. (3) Some genera symbols consist of four letters or less, e.g., ACER, AIM, GEUM, IRIS, POA, TO FOURTH EDITION RHUS, ROSA.
    [Show full text]
  • 3Rd Edition A.R
    WEAR – MATERIALS, MECHANISMS AND PRACTICE Editors: M.J. Neale, T.A. Polak and M. Priest Guide to Wear Problems and Testing for Industry M.J. Neale and M. Gee Handbook of Surface Treatment and Coatings M. Neale, T.A. Polak, and M. Priest (Eds) Lubrication and Lubricant Selection – A Practical Guide, 3rd Edition A.R. Lansdown Rolling Contacts T.A. Stolarski and S. Tobe Total Tribology – Towards an integrated approach I. Sherrington, B. Rowe and R. Wood (Eds) Tribology – Lubrication, Friction and Wear I.V. Kragelsky, V.V. Alisin, N.K. Myshkin and M.I. Petrokovets Wear – Materials, Mechanisms and Practice G. Stachowiak (Ed.) WEAR – MATERIALS, MECHANISMS AND PRACTICE Edited by Gwidon W. Stachowiak Copyright © 2005 John Wiley & Sons Ltd, The Atrium, Southern Gate, Chichester, West Sussex PO19 8SQ, England Telephone (+44) 1243 779777 Chapter 1 Copyright © I.M. Hutchings Email (for orders and customer service enquiries): [email protected] Visit our Home Page on www.wiley.com Reprinted with corrections May 2006 All Rights Reserved. No part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, scanning or otherwise, except under the terms of the Copyright, Designs and Patents Act 1988 or under the terms of a licence issued by the Copyright Licensing Agency Ltd, 90 Tottenham Court Road, London W1T 4LP, UK, without the permission in writing of the Publisher. Requests to the Publisher should be addressed to the Permissions Department, John Wiley & Sons Ltd, The Atrium, Southern Gate, Chichester, West Sussex PO19 8SQ, England, or emailed to [email protected], or faxed to (+44) 1243 770620.
    [Show full text]
  • Alaska Peninsula Bibliography of Geological Research Ric Wilson, USGS Anchorage, AK from Open File Report 1986 Updated, but Not Necessarily Complete for 1986-1990
    Alaska Peninsula Bibliography of Geological Research Ric Wilson, USGS Anchorage, AK From Open File Report 1986 Updated, but not necessarily complete for 1986-1990 "Abbot, C.G., and Fowle, F.E., 1913, Volcanoes and climate: Smithsonian Miscellaneous Collections, v. 60, no. 29, 24 p." "Abrahamson, S.R., 1949, Geography of the Naknek region, Alaska: Worcester, Mass., Clark University, Ph.D. dissertation, 148 p." "Addicott, W.O., 1971, Tertiary marine mollusks of Alaska: An annotated bibliography: U.S. Geological Survey Bulletin 1343, 30 p. "Addicott, W.O., 1973, Neogene marine mollusks of the Pacific coast of North America: An annotated bibliography, 1797-1969: U.S. Geological Survey Bulletin 1362, 210 p." "Addicott, W.O., 1977, Significance of pectinids in Tertiary biochronology of the Pacific Northwest states [abs.]: Geological Society of America Abstracts with Programs, v. 9, no. 7, p. 874." "Alaska Construction and Oil, 1984, Petroleum update: Alaska Construction and Oil, v. 25, no. 8, p. 164." "Alaska Construction and Oil, 1984, Unga Island mining data announced: Alaska Construction and Oil, v. 25, no. 3, p. 31." "Alaska Department of Mines, 1949, Report of the Commissioner of Mines for the Biennium ended December 31, 1948: Alaska Department of Mines, 50 p." "Alaska Department of Mines, 1951, Report of the Commissioner of Mines for the Biennium ended December 31, 1950: Alaska Department of Mines, 57 p." "Alaska Department of Mines, 1953, Report of the Commissioner of Mines for the Biennium ended December 31, 1952: Alaska Department
    [Show full text]
  • Southeastern Regional Taxonomic Center South Carolina Department of Natural Resources
    Southeastern Regional Taxonomic Center South Carolina Department of Natural Resources http://www.dnr.sc.gov/marine/sertc/ Southeastern Regional Taxonomic Center Invertebrate Literature Library (updated 9 May 2012, 4056 entries) (1958-1959). Proceedings of the salt marsh conference held at the Marine Institute of the University of Georgia, Apollo Island, Georgia March 25-28, 1958. Salt Marsh Conference, The Marine Institute, University of Georgia, Sapelo Island, Georgia, Marine Institute of the University of Georgia. (1975). Phylum Arthropoda: Crustacea, Amphipoda: Caprellidea. Light's Manual: Intertidal Invertebrates of the Central California Coast. R. I. Smith and J. T. Carlton, University of California Press. (1975). Phylum Arthropoda: Crustacea, Amphipoda: Gammaridea. Light's Manual: Intertidal Invertebrates of the Central California Coast. R. I. Smith and J. T. Carlton, University of California Press. (1981). Stomatopods. FAO species identification sheets for fishery purposes. Eastern Central Atlantic; fishing areas 34,47 (in part).Canada Funds-in Trust. Ottawa, Department of Fisheries and Oceans Canada, by arrangement with the Food and Agriculture Organization of the United Nations, vols. 1-7. W. Fischer, G. Bianchi and W. B. Scott. (1984). Taxonomic guide to the polychaetes of the northern Gulf of Mexico. Volume II. Final report to the Minerals Management Service. J. M. Uebelacker and P. G. Johnson. Mobile, AL, Barry A. Vittor & Associates, Inc. (1984). Taxonomic guide to the polychaetes of the northern Gulf of Mexico. Volume III. Final report to the Minerals Management Service. J. M. Uebelacker and P. G. Johnson. Mobile, AL, Barry A. Vittor & Associates, Inc. (1984). Taxonomic guide to the polychaetes of the northern Gulf of Mexico.
    [Show full text]
  • The Chiemgau Crater Strewn Field: Evidence of a Holocene Large Impact Event in Southeast Bavaria, Germany
    Journal of Siberian Federal University. Engineering & Technologies 1 (2010 3) 72-103 ~ ~ ~ УДК 551.3 The Chiemgau Crater Strewn Field: Evidence of a Holocene Large Impact Event in Southeast Bavaria, Germany Kord Ernstson*a, Werner Mayerb, Andreas Neumairb, Barbara Rappenglückb, Michael A. Rappenglückb, Dirk Sudhausc and Kurt W. Zellerd a University of Würzburg, Am Judengarten 23, 97204 Höchberg, Germany b Institute for Interdisciplinary Studies, Bahnhofstraße 1, 82205 Gilching, Germany c Institute of Geography, University of Augsburg, Universitätsstraße 10, 86135 Augsburg, Germany d Österreichisches Forschungszentrum Dürrnberg, Pflegerplatz 5, 5400 Hallein, Austria 1 Received 30.01.2009, received in revised form 27.02.2010, accepted 9.03.2010 The Chiemgau strewn field in the Alpine Foreland discovered in the early new millennium comprises more than 80 mostly rimmed craters in a roughly elliptically shaped area with axes of about 60 km and 30 km. The crater diameters range between a few meters and a few hundred meters. Geologically, the craters occur in Pleistocene moraine and fluvio-glacial sediments. The craters and surrounding areas so far investigated in more detail are featuring heavy deformations of the Quaternary cobbles and boulders, abundant fused rock material (impact melt rocks and various glasses), shock-metamorphic effects, and geophysical anomalies. The impact is substantiated by the abundant occurrence of metallic, glass and carbon spherules, accretionary lapilli, and of strange matter in the form of iron silicides like gupeiite and xifengite, and various carbides like, e.g., moissanite SiC. The hitherto established largest crater of the strewn field is Lake Tüttensee exhibiting an 8 m-height rim wall, a rim-to-rim diameter of about 600 m, a depth of roughly 30 m and an extensive ejecta blanket.
    [Show full text]
  • AMNH Digital Library
    \\ |l^1 ^ 1 llrtk «1^J% •^'^^ ,! , / TOVQv <*%# If' ""Wp \ c %' V .^^ . .«- JS^-^^ It's an engine for economic J^ I V^ VV \im I This V8 engine is part of a very powerful system. Built by the team at Toyota Motor Manufacturing, Alabama, it will provide the power for one of over 1 00,000 Tundra trucks being manufactured at our plant in Indiana* It's all part of our commitment to investing in the places where we do business. A commitment that has grown to include eight U.S. manufacturing facilities, research and design centers, sales and marketing operations, and a network of local suppliers and dealers. As a result, Toyota is responsible for creating more than 1 90,000 jobs across America, and with two new plants under construction in Texas and Tennessee, we'll continue to create opportunities for economic growth.** Local manufacturing, local investment, local jobs - it's a pretty powerful combination. 'Toyota components and vehicles are made using many U.S. sourced parts. "Direct U.S. employment; 31,040 jobs as of 12/03. ©2004 toyota.com/usa TOYOTA Some Previous Laureates Michel Andre Created a system to prevent collisions between whales and ships. TECHNOLOGY Manteca Onate ^ll^HHBtf ^ JHB^^^^^ Promoted sustainable Wwfr farming techniques in JSi^^'^X Could you take if. ^^^B ENVIRONMENT the next small step ^^^^ Laurent Pordie ^^^^^^^1 Revived traditional ^^ ' ->l^^^^l Amchi medicine and for mankind? K-. 'J^^^l improved healthcare in Ladakh. m^^i)^H SCIENCE Jean-Fran?ois Pernette Explored the sub-polar islands of Patagonia, ^^wftiw;. -i*;:3gjBti, -.-*,., Cristina Bubba Zamora 'r-^..-.
    [Show full text]
  • DOGAMI Bulletin 78, Bibliography of the Geology and Mineral Resources of Oregon: Fifth Supplement, January 1, 1961 to December 3
    BULLETIN 78 BIBLIOGRAPHY OF THE GEOLOGY AND MINERAL RESOURCES OF OREGON I FIFTH SUPPI .EMENTI January l, 1961 to December 1, 1970 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL I,NDUSTRIES 1973 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1069 State Office Building Portland, Oregon 97201 BULLETIN 78 BIBLIOGRAPHY of the GEOLOGY · and MINERAL RESOURCES of OREGON Fifth Suppleme nt January 1, 1961 to December 31 , 1970 Compi led by Miriam S. Roberts, Margaret L. Steere, and Caroline S. Brookhyser Oregon Department of Geology and Minera l Industries 1973 GOVERNING BOARD R. W. deWeese, Portland, Chairman William E. Mil ler, Bend STATE GEOLOGIST R. E. Corcoran CONTENTS Introduction . iii Serials cited iv Bibl iography Subject index • 113 BIBLIOGRAPHY of the GEOLOGY and MINERAL RESOURCES of OREGON Fifth Supplement 1 96 1 - 1 970 compiled by Miriam S. Roberts, Margaret L. Steere, and Caroline S. Brookhyser Introduction Bu lletin 78 is the fifth supplement to the origina l "Bibliography of the Geology and Mineral Resources of Oregon," com pi led by Ray C. Treasher and Edwin T. Hodge and published in 1936 . The fifth supplement lists publications that appeared during the ten years, 1961-1970. Severa l articles published before those dates but not listed in previous bibliographies are included because of their potential value to the researcher . As in previous bibI iographi es, this one includes theses, open-fi le reports, and other unpublished materials which may be available only in certain libraries. The first section of this bulletin contains an alphabetical listing by outhor of all citations, complete with publication data .
    [Show full text]
  • How Astronomical Objects Are Named
    How Astronomical Objects Are Named Jeanne E. Bishop Westlake Schools Planetarium 24525 Hilliard Road Westlake, Ohio 44145 U.S.A. bishop{at}@wlake.org Sept 2004 Introduction “What, I wonder, would the science of astrono- use of the sky by the societies of At the 1988 meeting in Rich- my be like, if we could not properly discrimi- the people that developed them. However, these different systems mond, Virginia, the Inter- nate among the stars themselves. Without the national Planetarium Society are beyond the scope of this arti- (IPS) released a statement ex- use of unique names, all observatories, both cle; the discussion will be limited plaining and opposing the sell- ancient and modern, would be useful to to the system of constellations ing of star names by private nobody, and the books describing these things used currently by astronomers in business groups. In this state- all countries. As we shall see, the ment I reviewed the official would seem to us to be more like enigmas history of the official constella- methods by which stars are rather than descriptions and explanations.” tions includes contributions and named. Later, at the IPS Exec- – Johannes Hevelius, 1611-1687 innovations of people from utive Council Meeting in 2000, many cultures and countries. there was a positive response to The IAU recognizes 88 constel- the suggestion that as continuing Chair of with the name registered in an ‘important’ lations, all originating in ancient times or the Committee for Astronomical Accuracy, I book “… is a scam. Astronomers don’t recog- during the European age of exploration and prepare a reference article that describes not nize those names.
    [Show full text]