White Sands Missile Range and Trinity Site
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WINTER 2013 - Volume 60, Number 4 the Air Force Historical Foundation Founded on May 27, 1953 by Gen Carl A
WINTER 2013 - Volume 60, Number 4 WWW.AFHISTORICALFOUNDATION.ORG The Air Force Historical Foundation Founded on May 27, 1953 by Gen Carl A. “Tooey” Spaatz MEMBERSHIP BENEFITS and other air power pioneers, the Air Force Historical All members receive our exciting and informative Foundation (AFHF) is a nonprofi t tax exempt organization. Air Power History Journal, either electronically or It is dedicated to the preservation, perpetuation and on paper, covering: all aspects of aerospace history appropriate publication of the history and traditions of American aviation, with emphasis on the U.S. Air Force, its • Chronicles the great campaigns and predecessor organizations, and the men and women whose the great leaders lives and dreams were devoted to fl ight. The Foundation • Eyewitness accounts and historical articles serves all components of the United States Air Force— Active, Reserve and Air National Guard. • In depth resources to museums and activities, to keep members connected to the latest and AFHF strives to make available to the public and greatest events. today’s government planners and decision makers information that is relevant and informative about Preserve the legacy, stay connected: all aspects of air and space power. By doing so, the • Membership helps preserve the legacy of current Foundation hopes to assure the nation profi ts from past and future US air force personnel. experiences as it helps keep the U.S. Air Force the most modern and effective military force in the world. • Provides reliable and accurate accounts of historical events. The Foundation’s four primary activities include a quarterly journal Air Power History, a book program, a • Establish connections between generations. -
Doctor Atomic
What to Expect from doctor atomic Opera has alwayS dealt with larger-than-life Emotions and scenarios. But in recent decades, composers have used the power of THE WORK DOCTOR ATOMIC opera to investigate society and ethical responsibility on a grander scale. Music by John Adams With one of the first American operas of the 21st century, composer John Adams took up just such an investigation. His Doctor Atomic explores a Libretto by Peter Sellars, adapted from original sources momentous episode in modern history: the invention and detonation of First performed on October 1, 2005, the first atomic bomb. The opera centers on Dr. J. Robert Oppenheimer, in San Francisco the brilliant physicist who oversaw the Manhattan Project, the govern- ment project to develop atomic weaponry. Scientists and soldiers were New PRODUCTION secretly stationed in Los Alamos, New Mexico, for the duration of World Alan Gilbert, Conductor War II; Doctor Atomic focuses on the days and hours leading up to the first Penny Woolcock, Production test of the bomb on July 16, 1945. In his memoir Hallelujah Junction, the American composer writes, “The Julian Crouch, Set Designer manipulation of the atom, the unleashing of that formerly inaccessible Catherine Zuber, Costume Designer source of densely concentrated energy, was the great mythological tale Brian MacDevitt, Lighting Designer of our time.” As with all mythological tales, this one has a complex and Andrew Dawson, Choreographer fascinating hero at its center. Not just a scientist, Oppenheimer was a Leo Warner and Mark Grimmer for Fifty supremely cultured man of literature, music, and art. He was conflicted Nine Productions, Video Designers about his creation and exquisitely aware of the potential for devastation Mark Grey, Sound Designer he had a hand in designing. -
Building 9731 – Secret City Festival’S Y-12 Public Tour Or: Building 9731 to Be Featured in Secret City Festival's Public Tour (Title Provided by the Oak Ridger)
Building 9731 – Secret City Festival’s Y-12 public tour Or: Building 9731 to be featured in Secret City Festival's public tour (title provided by The Oak Ridger) In March 1943 the very first structure to be completed at the newly emerging Y-12 Electromagnetic Separation Plant was Building 9731. It was only a little over a month earlier that ground had been broken for the first of nine major buildings designed to hold cautrons (CALifornia University Cyclotron). But the real push had been to complete the construction of a smaller building, one with a high bay and especially designed to house four very special units of newly designed equipment using huge magnets. The Alpha Calutron magnets stand well over 20 feet tall and are still standing there today―the only ones in the world! For the first time ever, the public will have a chance to see these huge magnets and will also be able to tour inside historic Building 9731. This historic event is a part of the Secret City Festival this year. On Saturday, June 19, 2010, from 9:00 AM to 4:00 PM, a major part of the Y-12 public tour will include Building 9731. The public will be allowed to see inside the historic structure and view the magnets of both the two Alpha and two Beta calutrons. These calutron magnets have been designated as Manhattan Project Signature Artifacts by the Depart- ment of Energy’s Federal Preservation Officer in the DOE Office of History and Heritage Resources. The building is being submitted for Historical Landmark status on the National Register of Historic Places. -
The Making of an Atomic Bomb
(Image: Courtesy of United States Government, public domain.) INTRODUCTORY ESSAY "DESTROYER OF WORLDS": THE MAKING OF AN ATOMIC BOMB At 5:29 a.m. (MST), the world’s first atomic bomb detonated in the New Mexican desert, releasing a level of destructive power unknown in the existence of humanity. Emitting as much energy as 21,000 tons of TNT and creating a fireball that measured roughly 2,000 feet in diameter, the first successful test of an atomic bomb, known as the Trinity Test, forever changed the history of the world. The road to Trinity may have begun before the start of World War II, but the war brought the creation of atomic weaponry to fruition. The harnessing of atomic energy may have come as a result of World War II, but it also helped bring the conflict to an end. How did humanity come to construct and wield such a devastating weapon? 1 | THE MANHATTAN PROJECT Models of Fat Man and Little Boy on display at the Bradbury Science Museum. (Image: Courtesy of Los Alamos National Laboratory.) WE WAITED UNTIL THE BLAST HAD PASSED, WALKED OUT OF THE SHELTER AND THEN IT WAS ENTIRELY SOLEMN. WE KNEW THE WORLD WOULD NOT BE THE SAME. A FEW PEOPLE LAUGHED, A FEW PEOPLE CRIED. MOST PEOPLE WERE SILENT. J. ROBERT OPPENHEIMER EARLY NUCLEAR RESEARCH GERMAN DISCOVERY OF FISSION Achieving the monumental goal of splitting the nucleus The 1930s saw further development in the field. Hungarian- of an atom, known as nuclear fission, came through the German physicist Leo Szilard conceived the possibility of self- development of scientific discoveries that stretched over several sustaining nuclear fission reactions, or a nuclear chain reaction, centuries. -
Bellucci Et Al. 2016 Trinitite Revised V Final
1 Direct Pb isotopic analysis of a nuclear fallout debris particle from the 2 Trinity nuclear test 3 4 5 Jeremy J. Bellucci1*, Joshua F. Snape1, Martin W. Whitehouse1, Alexander A. Nemchin1,2 6 7 *Corresponding author, email address: [email protected] 8 9 1Department of Geosciences, Swedish Museum of Natural History, SE-104 05 10 Stockholm, Sweden 11 2 Department of Applied Geology, Curtin University, Perth, WA 6845, Australia 12 13 Abstract 14 15 The Pb isotope composition of a nuclear fallout debris particle has been directly 16 measured in post-detonation materials produced during the Trinity nuclear test by a 17 secondary ion mass spectrometry (SIMS) scanning ion image technique (SII). This 18 technique permits the visual assessment of the spatial distribution of Pb and can be used 19 to obtain full Pb isotope compositions in user-defined regions in a 70 µm x 70 µm 20 analytical window. In conjunction with BSE and EDS mapping of the same particle, the 21 Pb measured in this fallout particle cannot be from a major phase in the precursor arkosic 22 sand. Similarly, the Pb isotope composition of the particle is resolvable from the 23 surrounding glass at the 2σ uncertainty level. The Pb isotope composition measured in 24 the particle here is in excellent agreement with that inferred from measurements of green 25 and red trinitite, suggesting that these types of particles are responsible for the Pb isotope 26 compositions measured in both trinitite glasses. 27 28 29 Keywords: 30 31 Trinitite, Trinity Test, Post Detonation Nuclear Forensics, Pb isotopes, SIMS, Scanning 32 Ion Imaging, Fallout Debris, Forensics 33 34 35 Introduction 36 37 In the event of a non-state sanctioned nuclear attack, forensic investigations will 38 be necessary to determine the provenance of the weapon and the materials used in 39 construction of the device. -
A New Effort to Achieve World
Marshall and the Atomic Bomb Marshall and the Atomic Bomb By Frank Settle General George C. Marshall and the Atomic Bomb (Praeger, 2016) provides the first full narrative describing General Marshall’s crucial role in the first decade of nuclear weapons that included the Manhattan Project, the use of the atomic bomb on Japan, and their management during the early years of the Cold War. Marshall is best known today as the architect of the plan for Europe’s recovery in the aftermath of World War II—the Marshall Plan. He also earned acclaim as the master strategist of the Allied victory in World War II. Marshall mobilized and equipped the Army and Air Force under a single command, serving as the primary conduit for information between the Army and the Air Force, as well as the president and secretary of war. As Army Chief of Staff during World War II, he developed a close working relationship with Admiral Earnest King, Chief of Naval Operations; worked with Congress and leaders of industry on funding and producing resources for the war; and developed and implemented the successful strategy the Allies pursued in fighting the war. Last but not least of his responsibilities was the production of the atomic bomb. The Beginnings An early morning phone call to General Marshall and a letter to President Franklin Roosevelt led to Marshall’s little known, nonetheless critical, role in the development and use of the atomic bomb. The call, received at 3:00 a.m. on September 1, 1939, informed Marshall that German dive bombers had attacked Warsaw. -
Leslie Richard Groves, Jr. Years
Name: Leslie Richard Groves, Jr. Years: August 17, 1896 – July 13, 1970 Residence: Albany, New York; Brief Biography: Leslie Richard Groves, Jr. was born to Leslie Richard Groves, Sr. and Gwen Griffith. Groves attended both the University of Washington and the Massachusetts Institute of Technology before he attended the U.S. Military Academy in 1916-1918. After his graduation from U.S. Military Academy, Groves spent an additional year at the Engineer School at the Camp A.A. Humphreys when he was made a second lieutenant of engineers. This was followed by a brief tour with the American Expeditionary Force in France soon after the end of World War I. In 1921 he graduated from the Engineer School. In 1922, Groves married Grace Wilson with whom he had two children with. From 1921-1931 Groves traveled extensively to Hawaii, San Francisco, Texas, Delaware, and ending up in Nicaragua in 1931. The work he conducted in Nicaragua led him to receive, from the Nicaraguan government, the medal of merit. Ambition led Groves to attend and graduate from the Command and General Staff College, in 1936, and the Army War College, in 1939. He then received the ranks of lieutenant colonel, which lead him to the War Department where he became the head of the Operations Branch, Corps of Engineers. During this time Groves became responsible for the design of the new Pentagon Building. During World War II he was picked to lead the Manhattan Engineer District, what would later be referred to as the Manhattan Project. Groves involvement in this project resulted in the a promotion to the rank of brigadier general. -
Trinity Scientific Firsts
TRINITY SCIENTIFIC FIRSTS THE TRINITY TEST was perhaps the greatest scientifi c experiment ever. Seventy-fi ve years ago, Los Alamos scientists and engineers from the U.S., Britain, and Canada changed the world. July 16, 1945 marks the entry into the Atomic Age. PLUTONIUM: THE BETHE-FEYNMAN FORMULA: Scientists confi rmed the newly discovered 239Pu has attractive nuclear Nobel Laureates Hans Bethe and Richard Feynman developed the physics fi ssion properties for an atomic weapon. They were able to discern which equation used to estimate the yield of a fi ssion weapon, building on earlier production path would be most effective based on nuclear chemistry, and work by Otto Frisch and Rudolf Peierls. The equation elegantly encapsulates separated plutonium from Hanford reactor fuel. essential physics involved in the nuclear explosion process. PRECISION HIGH-EXPLOSIVE IMPLOSION FOUNDATIONAL RADIOCHEMICAL TO CREATE A SUPER-CRITICAL ASSEMBLY: YIELD ANALYSIS: Project Y scientists developed simultaneously-exploding bridgewire detonators Wartime radiochemistry techniques developed and used at Trinity with a pioneering high-explosive lens system to create a symmetrically provide the foundation for subsequent analyses of nuclear detonations, convergent detonation wave to compress the core. both foreign and domestic. ADVANCED IMAGING TECHNIQUES: NEW FRONTIERS IN COMPUTING: Complementary diagnostics were developed to optimize the implosion Human computers and IBM punched-card machines together calculated design, including fl ash x-radiography, the RaLa method, -
Annual Report 2013.Pdf
ATOMIC HERITAGE FOUNDATION Preserving & Interpreting Manhattan Project History & Legacy preserving history ANNUAL REPORT 2013 WHY WE SHOULD PRESERVE THE MANHATTAN PROJECT “The factories and bombs that Manhattan Project scientists, engineers, and workers built were physical objects that depended for their operation on physics, chemistry, metallurgy, and other nat- ural sciences, but their social reality - their meaning, if you will - was human, social, political....We preserve what we value of the physical past because it specifically embodies our social past....When we lose parts of our physical past, we lose parts of our common social past as well.” “The new knowledge of nuclear energy has undoubtedly limited national sovereignty and scaled down the destructiveness of war. If that’s not a good enough reason to work for and contribute to the Manhattan Project’s historic preservation, what would be? It’s certainly good enough for me.” ~Richard Rhodes, “Why We Should Preserve the Manhattan Project,” Bulletin of the Atomic Scientists, May/June 2006 Photographs clockwise from top: J. Robert Oppenheimer, General Leslie R. Groves pinning an award on Enrico Fermi, Leona Woods Marshall, the Alpha Racetrack at the Y-12 Plant, and the Bethe House on Bathtub Row. Front cover: A Bruggeman Ranch property. Back cover: Bronze statues by Susanne Vertel of J. Robert Oppenheimer and General Leslie Groves at Los Alamos. Table of Contents BOARD MEMBERS & ADVISORY COMMITTEE........3 Cindy Kelly, Dorothy and Clay Per- Letter from the President..........................................4 -
Experimental Γ Ray Spectroscopy and Investigations of Environmental Radioactivity
Experimental γ Ray Spectroscopy and Investigations of Environmental Radioactivity BY RANDOLPH S. PETERSON 216 α Po 84 10.64h. 212 Pb 1- 415 82 0- 239 β- 01- 0 60.6m 212 1+ 1630 Bi 2+ 1513 83 α β- 2+ 787 304ns 0+ 0 212 α Po 84 Experimental γ Ray Spectroscopy and Investigations of Environmental Radioactivity Randolph S. Peterson Physics Department The University of the South Sewanee, Tennessee Published by Spectrum Techniques All Rights Reserved Copyright 1996 TABLE OF CONTENTS Page Introduction ....................................................................................................................4 Basic Gamma Spectroscopy 1. Energy Calibration ................................................................................................... 7 2. Gamma Spectra from Common Commercial Sources ........................................ 10 3. Detector Energy Resolution .................................................................................. 12 Interaction of Radiation with Matter 4. Compton Scattering............................................................................................... 14 5. Pair Production and Annihilation ........................................................................ 17 6. Absorption of Gammas by Materials ..................................................................... 19 7. X Rays ..................................................................................................................... 21 Radioactive Decay 8. Multichannel Scaling and Half-life ..................................................................... -
Journal of Radioanalytical and Nuclear Chemistry
J Radioanal Nucl Chem (2013) 298:993–1003 DOI 10.1007/s10967-013-2497-8 A multi-method approach for determination of radionuclide distribution in trinitite Christine Wallace • Jeremy J. Bellucci • Antonio Simonetti • Tim Hainley • Elizabeth C. Koeman • Peter C. Burns Received: 21 January 2013 / Published online: 13 April 2013 Ó Akade´miai Kiado´, Budapest, Hungary 2013 Abstract The spatial distribution of radiation within trin- The results from this study indicate that the device-related ititethinsectionshavebeenmappedusingalphatrack radionuclides were preferentially incorporated into the radiography and beta autoradiography in combination with glassy matrix in trinitite. optical microscopy and scanning electron microscopy. Alpha and beta maps have identified areas of higher activity, Keywords Trinitite Á Nuclear forensics Á Radionuclides Á and these are concentrated predominantly within the surfi- Fission and activation products Á Laser ablation inductively cial glassy component of trinitite. Laser ablation-inductively coupled plasma mass spectrometry coupled plasma mass spectrometry (LA-ICP-MS) analyses conducted at high spatial resolution yield weighted average 235U/238Uand240Pu/239Pu ratios of 0.00718 ± 0.00018 (2r) Introduction and 0.0208 ± 0.0012 (2r), respectively, and also reveal the presence of some fission (137Cs) and activation products Nuclear proliferation and terrorism are arguably the gravest (152,154Eu). The LA-ICP-MS results indicate positive cor- of threats to the security of any nation. The ability to relations between Pu ion signal intensities and abundances decipher forensic signatures in post-detonation nuclear of Fe, Ca, U and 137Cs. These trends suggest that Pu in debris is essential, both to provide a deterrence and to trinitite is associated with remnants of certain chemical permit a response to an incident. -
Lightning Strikes As a Major Facilitator of Prebiotic Phosphorus Reduction on Early Earth ✉ Benjamin L
ARTICLE https://doi.org/10.1038/s41467-021-21849-2 OPEN Lightning strikes as a major facilitator of prebiotic phosphorus reduction on early Earth ✉ Benjamin L. Hess 1,2,3 , Sandra Piazolo 2 & Jason Harvey2 When hydrated, phosphides such as the mineral schreibersite, (Fe,Ni)3P, allow for the synthesis of important phosphorus-bearing organic compounds. Such phosphides are com- mon accessory minerals in meteorites; consequently, meteorites are proposed to be a main 1234567890():,; source of prebiotic reactive phosphorus on early Earth. Here, we propose an alternative source for widespread phosphorus reduction, arguing that lightning strikes on early Earth potentially formed 10–1000 kg of phosphide and 100–10,000 kg of phosphite and hypo- phosphite annually. Therefore, lightning could have been a significant source of prebiotic, reactive phosphorus which would have been concentrated on landmasses in tropical regions. Lightning strikes could likewise provide a continual source of prebiotic reactive phosphorus independent of meteorite flux on other Earth-like planets, potentially facilitating the emer- gence of terrestrial life indefinitely. 1 Department of Earth and Planetary Sciences, Yale University, New Haven, CT, USA. 2 School of Earth and Environment, Institute of Geophysics and Tectonics, The University of Leeds, Leeds, UK. 3 Department of Geology and Environmental Science, Wheaton College, Wheaton, IL, USA. ✉ email: [email protected] NATURE COMMUNICATIONS | (2021) 12:1535 | https://doi.org/10.1038/s41467-021-21849-2 | www.nature.com/naturecommunications 1 ARTICLE NATURE COMMUNICATIONS | https://doi.org/10.1038/s41467-021-21849-2 ife on Earth likely originated by 3.5 Ga1 with carbon isotopic Levidence suggesting as early as 3.8–4.1 Ga2,3.