TRITIUM ANALYSIS of SEAWATER. TRESIS Submitted for the Degree,Of

Total Page:16

File Type:pdf, Size:1020Kb

TRITIUM ANALYSIS of SEAWATER. TRESIS Submitted for the Degree,Of TRITIUM ANALYSIS OF SEAWATER. TRESIS submitted for the degree,of DOCTOR OF PHILOSOPHY of the UNIVERSITY OF GLASGOW by H. MARK BLAUER Chemistry Department May, 1977 ProQuest Number: 13804114 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a com plete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest ProQuest 13804114 Published by ProQuest LLC(2018). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States C ode Microform Edition © ProQuest LLC. ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106- 1346 ACKNOWLEDGEMENTS'. The author is indebted to the Natural Environmental Research Council for financial support throughout this research project and to the University of Glasgow for laboratory and support facilities. Thanks are extended to A. Anderson and his staff for design and construction of the Constant Current Density Unit and maintenance of all electronic equipment; to A. Hislop and his staff for construction of the reaction vessels and other equipment; and to J. Connelly and his staff for glassblowing. Appreciation is extended to the crew of the U.S.N.S. Bartlett, Drs. W.S. Moore, M.S. Baxter and A.E. Fallick for collection of eastern tropical Pacific Ocean samples and supplementary hydrographic data. The same is extended to the crew of the U.S.N.S. Eltanin (Cruise 47) and Dr. J.M. Edmond for the Antarctic samples. The Inter­ national Atomic Energy Agency and Dr. C.B. Taylor supplied tritium standards and intercalibration facilities. The expertise of A. Ritchie for mass-spectrometric measurements of D/H ratios and the extended collection of tritium results by K. McKay are acknowledged. Thanks are also due to. Drs. A.E. Fallick and A.B. Mackenzie and Messrs. D. Swan and J. Campbell for providing the opportunity for many frank and illuminating discussions in the best of Scottish tradition. Appreciation for final preparation of this manuscri is extended to Messrs. C. Stuart, C, Cook s.nd M. Gray, and most especially to Miss.T. Collins. The author is especially grateful to Dr. M.S. Baxte for his diligent supervision, guidance and constructive criticism throughout the period of research. Without hi assistance this thesis would never have been possible. TABLE OF CONTENTS. Page. CHAPTER. I. INTRODUCTION . 1.1 Prolegomena ........... 1 1.2 Properties of tritium and tritium oxide .......................... 3 1.3^ Sources of tritium ............ 3 1.4 Tritium in the ocean .......... 10 1.5 Aims of research ..... 23 CHAPTER II. SAMPLING AND ANALYTICAL PROCEDURE II.1 Introduction .................. 25 .11.2 Methods of measurement of tritium 25 II. 3 Sampling ....................... 31 11.4 Distillation ................... 35 11.5 Electrolytic enrichment ....... 35 11.6 Methane synthesis ............. 47 11.7 Gas storage and counter filling sections ....................... 68 II. 8 Tritium counting system ....... 70 II.9 Counter characteristics ..... 76 CHAPTER III. CALIBRATION AND STANDARDISATION III.l Contamination and hlank values.. 88 III. 2 Storage ..... 106 III. 3 Enrichment factors .. 107 CHAPTER IV. DISCUSSION OF EASTERN TROPICAL PACIFIC OCEAN DATA IV. 1 Introduction ................... 123 IV.2 General oceanography ......... 125 IV. 3 Hydrographic features ..... 134 IV.4 Tritium features .............. 161 % IV.5 Summary ............... 181 TABLE OF CONTENTS (continued). Page. CHAPTER V. MEASUREMENTS FROM ANTARTIC. WATERS V.l Introduction ........ 184 V.2 General oceanography .......... 185 V.3 Hydrographic features ...... 194 ♦ .V.4 Tritium features ..... 206 APPENDIX 1 212 APPENDIX 2 ...... 213 APPENDIX 3 ... ... 214 REFERENCES 221 LIST OF FIONRES. Page. Cumulative tritium inventory . 8 11*1 Flow diagram for tritium assay 32 II-2 Atmospheric moisture condenser 33 II. 3. Distillation apparatus ..... 36 II-4 . Electrolysis cell and electrodes 37 II-5 Reservoir and feeding system ... 40 II.6 Probe placement versus current density in main electrodes ..... 43 II. 7 Perspex holding cage ........... 44 II;8 Current density, amperage and volume reduction versus electrolysis time ..... ;.................... 46 11.9 Distillation ampoule .......... 48 11.10 Final distillation apparatus ... 49 11.11 Flow system for methane synthesis 54 11.12 Vacuum line for routine methane purification ................... 56 11.13 Cross-section of reaction Vessel 37 11.14 Counter filling section ....... 65 11.15 ; Histogram of methane synthesis yields versus frequency ....... 66 11.16 Block diagram of counting electronics 72 11.17 Cross section of detector ...... 73 II.18A Background count rate versus external Cs-137 ratios .................. 79 II.18B Figure of merit versus external Cs- 137 ratios ..................... 80 II.18C Counting efficiency versus external Cs-137 ratios .......... 81 11.19 Plateaux of detector and guard .. 83 11.20 Distribution of counting rates in net a and net 6 channels 85 11.21 Pressure versus background count rates ............ '............... LIST OF FIGURES (continued.) Page. .111.1 Inert atmosphere dry box. ...... 91 111.2 Blank count rates during concurrent syntheses ....................... .95 111.3 Outgassing rate versus time .... 98 III. 4 Electrolytic enrichment curve .. 115 111.5 Electrolytic calibration curve . 117 111.6 Theoretical tritium recovery curve 119 IV.1 Station locations in eastern tropical Pacific Ocean ......... 124 IV.2 Surface currents of the Pacific ' _ Ocean ........................... 129 IV.3 Salinity versus depth at eastern tropical Pacific stations ..... 148 IV.4 Dissolved oxygen versus depth at eastern tropical Pacific Stations ........................ 149 IV.5 Temperature versus depth at eastern tropical Pacific Stations ..... 150 IV.6 Subsurface salinity profile ... at eastern tropical Pacific I . Stations ......................... 152 IV.7 , Subsurface temperature profile at eastern tropical Pacific Stations 153 IV.8 Subsurface dissolved oxygen profile for eastern tropical Pacific Stations 154 IV.9 Entire plot 0 -S for eastern tropical Pacific Stations ............... 156 IV.10 Q -S plot for eastern tropical Pacific deep water ............. 157 IV.11 0 -S for Bartlett Stations deep water .............. 160 IV.12 Potential temperature versus dissolved oxygen for Bartlett Stations deep water ............ 162 IV.13 South Tow tritium profiles .... 164 LIST ( FIGURES (continued,) Page. IV.14 . Tritium concentration versus depth for Bartlett Stations "3 and 12 ................. 166 IV.15 Tritium concentration along a surface of 25 168 IV.16 Tritium concentration along a surface of 26 ;.. 169 IV.17 Tritium concentration along a surface of 27 170 IV.18 Surface tritium concentrations in eastern tropical Pacific Ocean 172 IV.19 Average tritium distribution in surface seawater of the Pacific Ocean ....................... 173 IV.20 Temperature gradient versus tem­ perature for Bartlett Stations 3,5,7 and 9 174 IV.21 Approximate exponential subrange for Bartlett Stations 3,5,7 and 9 175 V.l Southern Ocean - surface circu­ lation and mean positions of the Antarctic and Subtropical Convergences 188 V.2 Schematic of vertical components of the circulation in the Southern Ocean and prominent hydrographic features 190 V.3 Temperature versus depth at Cruise 47 stations .................... 197 V.4 Salinity versus depth at Cruise 47 stations ......... 198 V.5 Dissolved oxygen distribution at Cruise 47 stations ............. 199 V.6 0 -S plot for complete water column 203 V.7 Subsurface ®-S plot of Cruise 47 stations ............ 204 V.8 0-S plot for Deep and Bottom Water 205 V.9 Surface tritium concentrations in T , U .......................... 209 V.10 Depth-tritium profiles at four Southern Latitudes ............ 210 LIST OF TABLES. Page. 1.1 Natural distribution of tritium 5 1.2 Thermonuclear energy yields of atmospheric tests in megatons .. 6 11.1 Ampoule vapour.losses-final distillation ; . 50 11.2 Comparison of volume reduction factors ................. 50 11.3 Gasket material - associated blank count rate .................... 59 11.4 Methane purification test - per­ centage recovery .............. 64 * II.5 Memory effect - reaction-vessels • 67 11.6 Determination c-f the presence of short-lived radionuclides ..... 69 11.7 Determination of the figure of merit .......................... 78 111.1 Background levels of tritium ... 89 111.2 Initial period blank determinations ~concurrent syntheses ........... 93 111.3 Final period blank determinations 94 111.4 Bakeout times for 2mm thick sheet steel .......................... 101 111.5 Outgassing rates for various metals 103 111.6 Measurement of the blank counting rate contamination throughout analytical procedure . .......... 105 111.7 Mass-spectrometry calibration for D/H measurement ........ Ill 111.8 Calibration of tritium enrichment and determination of the apparent fractionation factors ........ 114 111.9 Reproducibility - tritium recovery between cells ................. 120 III. 10 Tritium recovery between method:' 121 IV.1 Location of eastern tropical 'Pacific oceanographic stations . 136 LIST OF TABLES (continued.) Page. IV.2 Hydrographic properties at Bartlett Station 3 .... 137 IV. 3 Hydrographic properties at Bartlett Station 5 .... 138 IV.4 Hydrographic properties at • Bartlett Station 7 ...,. 139
Recommended publications
  • THE CONTINENTAL DRIFT CONTROVERSY Volume IV: Evolution Into Plate Tectonics
    Comp. by: Kkavitha Stage: Proof Chapter No.: FrontMatter Title Name: FRANKEL_Vol-4 Page Number: 0 Date:20/1/12 Time:17:17:28 THE CONTINENTAL DRIFT CONTROVERSY Volume IV: Evolution into Plate Tectonics Resolution of the sixty-year debate over continental drift, culminating in the triumph of plate tectonics, changed the very fabric of Earth Science. Plate tectonics can be considered alongside the theories of evolution in the life sciences and of quantum mechanics in physics in terms of its fundamental importance to our scientific under- standing of the world. This four-volume treatise on The Continental Drift Controversy is the first complete history of the origin, debate and gradual acceptance of this revolutionary explanation of the structure and motion of the Earth’s outer surface. Based on extensive interviews, archival papers, and original works, Frankel weaves together the lives and work of the scientists involved, producing an accessible narrative for scientists and non-scientists alike. Explanations of the curious magnetic anomalies on the seafloor and discovery and explanation of transform faults in the ocean crust in the mid-sixties led to the rapid acceptance of seafloor spreading. The birth of plate tectonics followed soon after with the geometrification of geology. Finally it was understood that the Earth’s surface is divided into a small number of nearly rigid plates, most of which contain continental and oceanic parts, and whose relative motions are describable in terms of Euler’s fixed point theorem. Although plate tectonics did not explain the cause or dynamic mechanism of drifting continents, it provided a convincing kinematic explanation that continues to inspire geodynamic research to the present day.
    [Show full text]
  • United States National Museum Bulletin 291
    SYSTEMATICS AND ZOOGEOGRAPHY OF THE WORLDWIDE BATHYPELAGIC SQUID BATHYTEUTHIS (CEPHALOPODA: OEGOPSIDA) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1.50 (paper covers) UNITED STATES NATIONAL MUSEUM BULLETIN 291 Systematics and Zoogeography of the Worldwide Bathypelagic Squid Bathyteuthis (Cephalopoda: Oegopsida) CLYDE F. E. ROPER Division of Mollusks Smithsonian Institution SMITHSONIAN INSTITUTION PRESS CITY OF WASHINGTON • 1969 Publications of the United States National Museum The scientific publications of the United States National Museum include two series, Proceedings of the United States Nationcd Museum and United States National Museum Bulletin. In these series are published original articles and monographs deal- ing with the collections and work of the Museum and setting forth newly acquired facts in the field of anthropology, biology, geology, history, and technology. Copies of each publication are distributed to libraries and scientific organizations and to specialists and others in- terested in the various subjects. The Prooeedings^f begun in 1878, are intended for the publication, in separate form, of shorter papers. These are gathered in volumes, oc- tavo in size, with the publication date of each paper recorded in the table of contents of the volume. In the Bulletin series, the first of which was issued in 1875, appear longer, separate publications consisting of monographs (occasionally in several parts) and volumes in w^iich are collected works on related subjects. Bulletins are either octavo or quarto in size, depending on the needs of the presentation. Since 1902, papers relating to the bo- tanical collections of the Museum have been published in the Bulletin series under the heading Contributions from the.
    [Show full text]
  • Prenos PDF Datoteke
    Podatki o projektu: Izvedba strokovnooperativnih del za Komisijo za standrdizacijo zemljepisnih imen Vsebinski sklop: Imenik tujih imen v slovenskem jeziku Naročnik projekta: Geodetska uprava Republike Slovenije, Zemljemerska ulica 12, Ljubljana Odgovorna oseba: Aleš Seliškar Zastopniki projekta: Jurij Mlinar, Ema Pogorelčnik Izvajalec projekta: Znanstvenoraziskovalni center Slovenske akademije znanosti in umetnosti, Geografski inštitut Antona Melika, Gosposka ulica 13, Ljubljana Odgovorna oseba: dr. Drago Perko Avtor vsebinskega sklopa: mag. Drago Kladnik, Inštitut za geografijo, Trg francoske revolucije 7, Ljubljana © Geodetska uprava Republike Slovenije, januar 2001 UVOD Zemljepisna imena - pokrajinska, vodna, reliefna, ledinska, upravna in krajevna, iz katerih izhajajo imena prebivalcev - so svojevrsten duhovni, kulturni, socialni, zgodovinski, jezikovni in politični pokazatelj. Iz njih je mogoče razbrati marsikatero potezo naravne, družbene in značajske preteklosti ter sedanjosti posameznega naseljenega in nenaseljenega območja na našem planetu. Ena njegovih bistvenih značilnosti je jezikovna raznolikost, ki se pogosto ne omejuje le na raznoliko sporočilnost, ampak je tudi zapisana z različnimi pisavami. Tako se tiha in nema pokrajina v marsičem bolje odpira tistemu, ki zna brati ne le govorico naravnih značilnosti, temveč tudi prodreti v globino izvirnega imenoslovja. Problematika tujih zemljepisnih imen kaže tudi na odnos določenega naroda do svetovnih dogajanj in na jezikovne razvojne vidike. Uporaba tujih zemljepisnih imen v
    [Show full text]
  • Geological Exploration of South Atlantic Islands and Its Contributions to the Continental Drift Debate of the Early 20Th Century
    Published in Proceedings of the Geologists’ Association, 2015, Volume 126, 266-281. Note that this version of the text does not include the Journal’s editorial and proof corrections Geological exploration of South Atlantic islands and its contributions to the continental drift debate of the early 20th century Philip Stone British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, Scotland, UK. E-mail: [email protected] Key Words: South Atlantic Ocean, Scotia Arc, Falkland Islands, South Georgia, Gondwana, continental drift. Abstract The geological character of the South Atlantic islands was only slowly established during the first half of the 20th century. That same period was marked by a generally dismissive view of continental drift but, as the continental nature of the islands became apparent, their ‘oceanic’ setting was utilised by both sides of the ‘drift’ debate to support their respective positions. So islands such as the Falklands archipelago and South Georgia were cited either as fragments detached from larger continental bodies during drift, or as the last surviving vestiges of a huge continental landmass that had subsided beneath the water of the South Atlantic. The appreciation of the Scotia Arc as a dynamic geological construct arising from lateral tectonics, and the Falkland Islands as representative of an itinerant continental fragment, were features of some early accounts of the region, but such ideas were generally discounted by the geological establishment of the day. This paper reviews the early, pioneering contributions to the geological understanding of the Falkland Islands, South Georgia and the Scotia Arc region, assessing their contemporary reception and tracing their influence on the developing continental drift controversy.
    [Show full text]
  • The Earth and the Ocean Basins
    CHAPTERII The Earth and the Ocean Basins Figure and Size of the Earth As a first approximation the earth maybe considered as a sphere, but, according to accurate observations, its figure is more closely represented by an ellipseof rotation—that is, an oblate spheroid,the shorter axisbeing the axis of rotation. The figure of the earth hm been defined by various empirical equations, the constants of which are based on observations and are subject to modification m the number of observations increases and their accuracy is improved. The geometrical figures defined by these equations cannot exactly representthe shape of the earth because of the asymmetrical distribution of the water and land masses. To define the position of a point on the earth’s surface, a system’of coordinates is needed, and as such the terms latitude, longitude, and ekwa- kionor depth are used. The first two are expressed by angular coordi- nates and the third is expressedby the vertical distance, stated in suitable linear units, above or below a reference level that is generally closely related to mean sea level. The Ja$itzdeof any point is the angle between the local plumb line and the equatorial plane. Because the earth can be considered as having the form of a spheroid, and as the plumb line, for all practical purposes, is perpendicular to the surface of the spheroid, any plane parallel to the Equator cuts the surface of the spheroid in a circle, and all points on this circle have the same latitude. These circles are called parallelsoj latitude. The latitude is measuredin degrees, minutes, and seconds north and south of the Equator.
    [Show full text]
  • Marine Protected Areas for Whales, Dolphins, and Porpoises : a World Handbook for Cetacean Habitat Conservation / by Erich Hoyt
    MARINE PROTECTED AREAS FOR WHALES, DOLPHINS AND PORPOISES This book is dedicated to those who work on behalf of cetaceans and marine ecosystems, and to those who cannot speak, write and argue for their place in the sea: the whales, dolphins and porpoises and other marine species ‘There is a tide in the affairs of men, which taken at the flood leads on to fortune… The flood is occurring regarding the high seas’ Graeme Kelleher (paraphrasing William Shakespeare in Julius Caesar) saying that now is the time to create and fight for high-seas marine protected areas MARINE PROTECTED AREAS FOR WHALES, DOLPHINS AND PORPOISES A World Handbook for Cetacean Habitat Conservation Erich Hoyt London • Sterling, VA First published by Earthscan in the UK and USA in 2005 Copyright © Erich Hoyt, 2005 All rights reserved ISBN: 1-84407-064-6 paperback 1-84407-063-8 hardback Typesetting by MapSet Ltd, Gateshead, UK Printed and bound in the UK by Cromwell Press Ltd, Trowbridge, Wiltshire Cover design by Anthony Waters Cover photo: Sperm whale off Kamchatka, Russia, © Hal Sato, Far East Russia Orca Project (WDCS) Maps: Lesley Frampton Illustrations: © Pieter Arend Folkens/A Higher Porpoise Design Group For a full list of publications please contact: Earthscan 8–12 Camden High Street London, NW1 0JH, UK Tel: +44 (0)20 7387 8558 Fax: +44 (0)20 7387 8998 Email: [email protected] Web: www.earthscan.co.uk 22883 Quicksilver Drive, Sterling, VA 20166-2012, USA Earthscan publishes in association with WWF-UK and the International Institute for Environment and Development The royalties from sales of this book will go toward the MPA work of WDCS, the Whale and Dolphin Conservation Society.
    [Show full text]
  • “Comment About Tsunamis Occurrence in Northern Caribbean”
    1 SOME GLIMPSES OF THE TSUNAMIGENIC POTENTIAL OF THE CARIBBEAN REGION 2 Mario Octavio COTILLA RODRÍGUEZ and Diego CÓRDOBA BARBA Departamento de Física de la Tierra y Astrofísica Facultad de Ciencias Físicas Universidad Complutense de Madrid Ciudad Universitaria, S/N. 28040 Madrid [email protected]; [email protected] 3 “Science is the instrument that human society has to explain natural phenomena.” 4 Index Prólogo Foreword-Prefacio Introduction 1- Review of tsunami studies 2- Tsunami activity in the Pacific region 3- Tsunamis data of the Atlantic Ocean 4- Some information about tectonic activity in the Caribbean region 5- Seismicity and focal mechanisms in the Caribbean plate 6- Tsunamigenic activity of the Caribbean region 7- Final comments Main conclusions Acknowledgements References 5 Prólogo El peligro olvidado, que resucitó y posteriormente ha sido magnificado por Hollywood, así podríamos definir a los tsunamis. Son diferentes los procesos que dan origen a los tsunamis: terremotos que provocan un movimiento con componente vertical del fondo marino; explosiones de islas volcánicas; grandes movimientos de masas en pendientes continentales y/o a la orilla de las costas; caída de meteoritos; los más comunes son los dos primeros. Hay informes sobre grandes tsunamis históricos que han causado mucha destrucción, algunos muy famosos donde quizá el más antiguo conocido sea el de la Isla Santorini en 1650 AC, pasando por los de Lisboa en 1755 y Krakatoa en 1883 hasta los de 1964 en Alaska, de 2004 en Indonesia y 2011 en Tohoku. De estos seis, posiblemente los de más impacto en su momento, dos son de origen volcánico (Santorini y Krakatoa).
    [Show full text]
  • Ancient Xenocrystic Zircon in Young Volcanic Rocks of the Southern Lesser Antilles Island Arc
    ÔØ ÅÒÙ×Ö ÔØ Ancient xenocrystic zircon in young volcanic rocks of the southern Lesser Antilles island arc Yamirka Rojas-Agramonte, Ian Williams, Richard Arculus, Alfred Kr¨oner, Antonio Garc´ıa-Casco, Concepci´on L´azaro, Stephan Buhre, Jean Wong, Helen Geng, Carlos Morales Echeverr´ıa, Teresa Jeffries, Hangqian Xie, Regina Mertz-Kraus PII: S0024-4937(17)30272-4 DOI: doi:10.1016/j.lithos.2017.08.002 Reference: LITHOS 4385 To appear in: LITHOS Received date: 10 March 2017 Accepted date: 7 August 2017 Please cite this article as: Rojas-Agramonte, Yamirka, Williams, Ian, Arculus, Richard, Kr¨oner, Alfred, Garc´ıa-Casco, Antonio, L´azaro, Concepci´on, Buhre, Stephan, Wong, Jean, Geng, Helen, Echeverr´ıa, Carlos Morales, Jeffries, Teresa, Xie, Hangqian, Mertz- Kraus, Regina, Ancient xenocrystic zircon in young volcanic rocks of the southern Lesser Antilles island arc, LITHOS (2017), doi:10.1016/j.lithos.2017.08.002 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Ancient xenocrystic zircon in young volcanic rocks of the southern Lesser Antilles island arc Yamirka Rojas-Agramonte1,2,3, Ian Williams4; Richard Arculus4,
    [Show full text]
  • Título Documento (Heading 1)
    Project Document An assessment of the economic and social impacts of climate change on the water sector in the Caribbean Economic Commission for Latin America and the Caribbean (ECLAC) The views expressed in this document, which has been reproduced without formal editing, are those of the author and do not necessarily reflect those of the Organization. Acknowledgements The present study was prepared by Juan Llanes-Regueiro. Notes and explanations of symbols: A full stop (.) is used to indicate decimals The use of a hyphen (-) between years, for example, 2010-2019, signifies an annual average for the calendar years involved, including the beginning and ending years, unless otherwise specified. The word “dollar” refers to United States dollars, unless otherwise specified. The term “billion” refers to a thousand million. The boundaries and place names shown and the designations used on maps do not imply official endorsement or acceptance by the United Nations. LC/CAR/L399 Copyright © United Nations. March 2013. All rights reserved Printed at United Nations, Port of Spain, Trinidad and Tobago ECLAC – Project Documents collection An assessment of the economic and social impacts of climate change... Contents Executive summary ..................................................................................................................................... viii I. Introduction ................................................................................................................................................. 1 A. Literature review
    [Show full text]
  • The Water Masses and Currents of the Oceans Within Anygiven Region, the Character of the Water Massesdepends Mainly Upon Three F
    . CHAPTERXV The Water Masses and Currents of the Oceans `.m. mm.. ms .......m .......m* ....m..*.. m.....* ....................mm... *. .. ........ .......m..m. ..... ........ Within anygiven region, the character of the water masses depends mainly upon three fac$ors—the latitude of the region, the degree of isolation, and the types of currents-the relative importance of which will be brought out in the course of the discussion. It is rational to deal first with the simpler conditions and gradually to enter upon the more complicated. This can be done by first dis- cussing the Antarctic Ocean, where the latitude effect is easily explained, where the waters are in free communication with those of the major oceans, and where the system of prevailing currents is unusually clear- cut. After a description of conditions within the Antarctic Ocean we shall consider the Atlantic, Indian, and Pacific Oceans, the adjacent seas of these oceans, and in conclusion we shall discuss the deep-water circulation between the large ocean basins. The Antarctic Circumpolar Ocean BOUNDARIESANDGENERALCHARACTERISTICSOF WATER MASSES. It is difficult to assign a northern boundary to the Antarctic Ocean because it is in open communication with the three major oceans: the Atlantic, the Indian, and the Pacific Oceans. In some instances the antarctic waters are dealt with as parts of the adjacent oceans and are designated the Atlantic Antarctic Ocean, or the Indian or Pacific Ant- arctic Ocean, whereas in other instances the antarctic waters must be considered an integral part of all oceans. The latter case, for instance, applies when dealing with the deep-water circulation, which is of such a nature that the intercommunication between dif?erent regions must be taken into account.
    [Show full text]
  • A News Bulletin New Zealand Antarctic Society
    A N E W S B U L L E T I N p u b l i s h e d q u a r t e r l y b y t h e NEW ZEALAND ANTARCTIC SOCIETY THE NEW ENDEAVOUR Flying the New Zealand flag, H.M.N.Z.S. Endeavour off Hawaii during her voyage to New Zealand to begin Antarctic supply work this summer. Official U.S. Navy Photograph. Vol. 3, No. 4 DECEMBER, 1962 AUSTRALIA Winter and Summer bases Scott / W/ ' S u t n m e r b a s e o n l y t S k y - H i Jointly operated base H.illett NEW ZEALAND (Hi N2) Transferred base Wilkes Ui fcAust TASMANIA Temporarilyiion-operation.il *Syowa , Campbell |, (HI) t Micauanc I, lAuit) ^>' \" ^allefr(i/.i..#. Wilkes— (7 x\\ \ \ a ■■. >VUiHIoRixlfoi ' \ / h m * l/.S.ft»(u5f.\ \\ i>. 1 x**r 77° ""•> A>\ ,*"l.-Hur.W'/ * ^Amundsen-Scott (U5J . ;i_ 4*-i A N T A R DaviOwA <* M*w*tfn\ \ . { ( U . K . ) / x V i x - *''<? Maud A > < « f V, < < V W -*j8^ * T" ■ Marlon I. U.AJ DRAWN BY DEPARTMENT OF LANDS 1 SURVEY WELLINGTON. NEW ZEALAND, SEP I9fcl (Successor to "Antarctic News Bulletin") Vol. 3, No. 4 DECEMBER, 1962 Editor: L. B. Quartennain, M.A., 1 Ariki Road, Wellington, E.2, New Zealand. Business Communications, Subscriptions, etc., to: Secretary. New Zealand Antarctic Society, P.O. Box 2110. Wellington. N.Z. R.G.S. AWARD The Cuthbert Peck Grant ol the SUBSCRIPTION TO Royal Geographical Society lor 1962 "ANTARCTIC " has been awarded to Captain P.
    [Show full text]
  • New Finding of the Ancient Primitive Mollusc Neopilina in the Atlantic Part of the Antarctic Effects of Stable Chlorine-Containi
    Nature Vol. 249 June 14 1974 675 mercury compounds deposited in soil are more readily available form of the Neopilina we describe. The taxonomic position of to humans and animals than previously anticipated, the the small mollusc is being investigated. consequent health hazard being magnified by the higher . The bottom _fauna found with our specimen was very rich and methylmercury. toxicity of diverse, contammg more than 20 groups of bottom inverte­ (including w. F . BECKERT bra~e~. There w~re several hundred holothurians A. A . MOGHISSI* Elp1d1a-the leadmg form of bottom fauna here), numerous F. H. F.Au ~ourtalesiida_e (irregula r deep sea urchins) and Ophiuroidea, _of Polychaeta (Aphroditidae, Flabelligeridae E. W. BRETTHAUER nch populat10n and others), vanous Spongia, Actinia, Pogonophora, Amphi­ J.C. McFARLANE poda and Isopoda. Molluscs (apart from Neopilina) were US Environmental Protection Agency, represented by Gastropoda, Prosobranchia and Opistho­ National Environmental Research Center-Las Vegas, branchia and Bivalvia (Cyclopecten and Neila). PO Box 15027, Las Vegas, Nevada 89114 It therefore seems that the food and conditions are quite adequate for recent Neopi/ina and other detritus-feeding bottom Received January 28; revised April 1, 1974. invertebrates in the South Atlantic eutrophic regions. The hard , manganese *Present address : Office of Interdisciplinary Programs, Georgia substratum to which N eopilina adheres (stones Institute of Technology, Atlanta, Georgia 30332. nodules or pebbles) is dispersed in good quantity in the Ant­ arctic region by the action of floating ice. The mucus bacterial 1 Wood, J. M. , Kennedy, F. Scott, and Rosen, C. G., Nature, 220, l 73 (l 968). film or organic detritus in various forms usually existing on the 2 West66, G., Acta Chem.
    [Show full text]