Helium: Exploration Methodology for a Strategic Resource
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Guidance for Using Continuous Monitors in Pm Monitoring
United States Office of Air Quality EPA-454/R-98-012 Environmental Protection Planning and Standards May 1998 Agency Research Triangle Park, NC 27711 Air GUIDANCE FOR USING CONTINUOUS MONITORS IN PM2.5 MONITORING NETWORKS GUIDANCE FOR USING CONTINUOUS MONITORS IN PM2.5 MONITORING NETWORKS May 29, 1998 PREPARED BY John G. Watson1 Judith C. Chow1 Hans Moosmüller1 Mark Green1 Neil Frank2 Marc Pitchford3 PREPARED FOR Office of Air Quality Planning and Standards U.S. Environmental Protection Agency Research Triangle Park, NC 27711 1Desert Research Institute, University and Community College System of Nevada, PO Box 60220, Reno, NV 89506 2U.S. EPA/OAQPS, Research Triangle Park, NC, 27711 3National Oceanic and Atmospheric Administration, 755 E. Flamingo, Las Vegas, NV 89119 DISCLAIMER The development of this document has been funded by the U.S. Environmental Protection Agency, under cooperative agreement CX824291-01-1, and by the Desert Research Institute of the University and Community College System of Nevada. Mention of trade names or commercial products does not constitute endorsement or recommendation for use. This draft has not been subject to the Agency’s peer and administrative review, and does not necessarily represent Agency policy or guidance. ii ABSTRACT This guidance provides a survey of alternatives for continuous in-situ measurements of suspended particles, their chemical components, and their gaseous precursors. Recent and anticipated advances in measurement technology provide reliable and practical instruments for particle quantification over averaging times ranging from minutes to hours. These devices provide instantaneous, telemetered results and can use limited manpower more efficiently than manual, filter-based methods. -
Late Quaternary Tectonic Activity and Lake Level Change in the Rukwa Rift Basin
Journal of African Earth Sciences, Vol. 26. No.3. pp. 397-421, 1998 c 1998 Elsevier Science Ltd Pergamon All rights reserved. Printed in Great Britain PII:S0899-5362(98)00023-2 0899-5362/98 $19.00 + 000 Late Quaternary tectonic activity and lake level change in the Rukwa Rift Basin D. DELVAUX,1 F. KERVYN,l E. VITTORI,2 R. S. A. KAJARN and E. KILEMBE4 1Royal Museum for Central Africa, B-3080 Tervuren, Belgium 2ANPA, Via Vitaliano Brancati, 48, 00144 Roma, Italy 3MADINI, Box 903 Dodoma, Tanzania 4TPDC, Exploration-Production, Box 2774 Dar-es-Salaam, Tanzania Abstract-Interpretation of remotely sensed images and air photographs, compilation of geological and topographical maps, morphostructural and fault kinematic observations and 14C dating reveal that, besides obvious climatic influences, the lake water extent and sedimentation in the closed hydrological system of Lake Rukwa is strongly influenced by tectonic processes. A series of sandy ridges, palaeolacustrine terraces and palaeounderwater delta fans are related to an Early Holocene high lake level and subsequent progressive lowering. The maximum lake level was controlled by the altitude of the watershed between the Rukwa and Tanganyika hydrological systems. Taking as reference the present elevation of the palaeolacustrine terraces around Lake Rukwa, two orders of vertical tectonic movement are evidenced: i) a general uplift centred on the Rungwe Volcanic Province between the Rukwa and Malawi Rift Basins; and ii) a tectonic northeastward tilting of the entire Rukwa Rift Basin, including the depression and rift shoulders. This is supported by the observed hydromorphological evolution. Local uplift is also induced by the development of an active fault zone in the central part of the depression, in a prolongation of the Mbeya Range-Galula Fault system. -
Select Bibliography
Select Bibliography by the late F. Seymour-Smith Reference books and other standard sources of literary information; with a selection of national historical and critical surveys, excluding monographs on individual authors (other than series) and anthologies. Imprint: the place of publication other than London is stated, followed by the date of the last edition traced up to 1984. OUP- Oxford University Press, and includes depart mental Oxford imprints such as Clarendon Press and the London OUP. But Oxford books originating outside Britain, e.g. Australia, New York, are so indicated. CUP - Cambridge University Press. General and European (An enlarged and updated edition of Lexicon tkr WeltliU!-atur im 20 ]ahrhuntkrt. Infra.), rev. 1981. Baker, Ernest A: A Guilk to the B6st Fiction. Ford, Ford Madox: The March of LiU!-ature. Routledge, 1932, rev. 1940. Allen and Unwin, 1939. Beer, Johannes: Dn Romanfohrn. 14 vols. Frauwallner, E. and others (eds): Die Welt Stuttgart, Anton Hiersemann, 1950-69. LiU!-alur. 3 vols. Vienna, 1951-4. Supplement Benet, William Rose: The R6athr's Encyc/opludia. (A· F), 1968. Harrap, 1955. Freedman, Ralph: The Lyrical Novel: studies in Bompiani, Valentino: Di.cionario letU!-ario Hnmann Hesse, Andrl Gilk and Virginia Woolf Bompiani dille opn-e 6 tUi personaggi di tutti i Princeton; OUP, 1963. tnnpi 6 di tutu le let16ratur6. 9 vols (including Grigson, Geoffrey (ed.): The Concise Encyclopadia index vol.). Milan, Bompiani, 1947-50. Ap of Motkm World LiU!-ature. Hutchinson, 1970. pendic6. 2 vols. 1964-6. Hargreaves-Mawdsley, W .N .: Everyman's Dic Chambn's Biographical Dictionary. Chambers, tionary of European WriU!-s. -
Cenozoic Paleostress and Kinematic Evolution of the Rukwa - North Malawi Rift Valley (East African Rift System)
CENOZOIC PALEOSTRESS AND KINEMATIC EVOLUTION OF THE RUKWA - NORTH MALAWI RIFT VALLEY (EAST AFRICAN RIFT SYSTEM) Damien DELVAUX, Kirill LEVI, Rugaibuhamu KAJARA and Julius SAROTA DELVAUX, D" LEVI, K" KAJARA, R, & SAROTA, J (1992), - Cenozoic paleostress and kinematic evolution of the Rukwa - North Malawi rift valley (East African Rift System), - Bull Centres Recti. Explor-Prod. Elf Aquitaine, 16, 2, 383-406, 13 fig" 2 tab.: Boussens, December 24, 1992, - ISSN ; 0396-2687 CODEN' BCREDP. l.'evolution cinematique du secteur Tanganyika - Rukwa - Malawi de la branche occidentale du rift est-africain est encore relativement mal connue. Le r61e respectif des mouvements verticaux ou horizontaux Ie long des failles liees au developpement des bassins du rift est toujours I'objet de discussions contradictoires, ainsi que l'estimation de la direction d'extension principale. Afin d'eclaircir ces problernes, 976 failles mineures provenant de 29 sites difte rents ont ete mesurees dans I'ouest de la Tanzanie, Ie long de la partie nord de la depression du lac Malawi et de sa jonction triple avec Ie rift de Rukwa et la depression transversale d'Usanqu. Ces mesures ont ete ettectuees Ie long des failles majeures ainsi que dans les sediments et volcanites du rift. Les donnees de faille avec stries de glissement ont ete analysees en termes de palsctenseurs de contraintes. D'apres les donnees de terrain et ainsi qu'il a ete montre par d'autres, il est clair que la direction NW-SE majeure des failles du rift Rukwa - Nord Malawi a etc fortement influencee par les directions structurales precarnbriennnes. D'autre part, elles sont egalement largement heritees de la phase de rifting Karoo (perrno-triassique). -
Workshop on the Early Solar System Impact Bombardment II
Program and Abstract Volume LPI Contribution No. 1649 Workshop on the Early Solar System Impact Bombardment II February 1–3, 2012 • Houston, Texas Sponsors National Aeronautics and Space Administration Universities Space Research Association Lunar and Planetary Institute NASA Lunar Science Institute Conveners David A. Kring Center for Lunar Science and Exploration Lunar and Planetary Institute William F. Bottke Center for Lunar Origin and Evolution Southwest Research institute Scientific Organizing Committee Robin Canup Southwest Research Institute Gareth Collins Imperial College London James Head Brown University Alessandro Morbidelli Observatoire de la Cote d’Azur (France) Marc Norman Australian National University Richard Walker University of Maryland Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPI Contribution No. 1649 Compiled in 2012 by Meeting and Publication Services Lunar and Planetary Institute USRA Houston 3600 Bay Area Boulevard, Houston TX 77058-1113 The Lunar and Planetary Institute is operated by the Universities Space Research Association under a cooperative agreement with the Science Mission Directorate of the National Aeronautics and Space Administration. Any opinions, findings, and conclusions or recommendations expressed in this volume are those of the author(s) and do not necessarily reflect the views of the National Aeronautics and Space Administration. Material in this volume may be copied without restraint for library, abstract service, education, or personal research purposes; however, republication of any paper or portion thereof requires the written permission of the authors as well as the appropriate acknowledgment of this publication. Abstracts in this volume may be cited as Author A. B. (2012) Title of abstract. In Workshop on the Early Solar System Bombardment II, p. -
[PDF] Sedimentology and Depositional Environments of the Red
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Journal of African Earth Sciences 57 (2010) 179–212 Contents lists available at ScienceDirect Journal of African Earth Sciences journal homepage: www.elsevier.com/locate/jafrearsci Geological Society of Africa Presidential Review No. 15 Sedimentology and depositional environments of the Red Sandstone Group, Rukwa Rift Basin, southwestern Tanzania: New insight into Cretaceous and Paleogene terrestrial ecosystems and tectonics in sub-equatorial Africa Eric M. Roberts a,*, Patrick M. O’Connor b, Nancy J. Stevens b, Michael D. Gottfried c, Zubair A. Jinnah d, Sifael Ngasala c, Adeline M. Choh d, Richard A. Armstrong e a Department of Physical Sciences, Southern Utah University, Cedar City, UT 84720, USA b Department of Biomedical Sciences, 228 Irvine Hall, College of Osteopathic Medicine, Ohio University, Athens, OH, 45701, -
Hearst Corporation Los Angeles Examiner Photographs, Negatives and Clippings--Portrait Files (A-F) 7000.1A
http://oac.cdlib.org/findaid/ark:/13030/c84j0chj No online items Hearst Corporation Los Angeles Examiner photographs, negatives and clippings--portrait files (A-F) 7000.1a Finding aid prepared by Rebecca Hirsch. Data entry done by Nick Hazelton, Rachel Jordan, Siria Meza, Megan Sallabedra, and Vivian Yan The processing of this collection and the creation of this finding aid was funded by the generous support of the Council on Library and Information Resources. USC Libraries Special Collections Doheny Memorial Library 206 3550 Trousdale Parkway Los Angeles, California, 90089-0189 213-740-5900 [email protected] 2012 April 7000.1a 1 Title: Hearst Corporation Los Angeles Examiner photographs, negatives and clippings--portrait files (A-F) Collection number: 7000.1a Contributing Institution: USC Libraries Special Collections Language of Material: English Physical Description: 833.75 linear ft.1997 boxes Date (bulk): Bulk, 1930-1959 Date (inclusive): 1903-1961 Abstract: This finding aid is for letters A-F of portrait files of the Los Angeles Examiner photograph morgue. The finding aid for letters G-M is available at http://www.usc.edu/libraries/finding_aids/records/finding_aid.php?fa=7000.1b . The finding aid for letters N-Z is available at http://www.usc.edu/libraries/finding_aids/records/finding_aid.php?fa=7000.1c . creator: Hearst Corporation. Arrangement The photographic morgue of the Hearst newspaper the Los Angeles Examiner consists of the photographic print and negative files maintained by the newspaper from its inception in 1903 until its closing in 1962. It contains approximately 1.4 million prints and negatives. The collection is divided into multiple parts: 7000.1--Portrait files; 7000.2--Subject files; 7000.3--Oversize prints; 7000.4--Negatives. -
Lunar Cold Spots and Crater Production on the Moon 10.1029/2018JE005652 J.-P
Journal of Geophysical Research: Planets RESEARCH ARTICLE Lunar Cold Spots and Crater Production on the Moon 10.1029/2018JE005652 J.-P. Williams1 , J. L. Bandfield2 , D. A. Paige1, T. M. Powell1, B. T. Greenhagen3, S. Taylor1, 4 5 6 7,8 Key Points: P. O. Hayne , E. J. Speyerer , R. R. Ghent , and E. S. Costello • We measure diameters of craters 1 2 associated with cold spots. Their Earth, Planetary, and Space Sciences, University of California, Los Angeles, CA, USA, Space Science Institute, Boulder, CO, USA, size-frequency distribution indicates 3Applied Physics Laboratory, Johns Hopkins University, Laurel, MD, USA, 4Department of Astrophysical & Planetary Sciences, cold spots survive a few hundred kyr University of Colorado, Boulder, Boulder, CO, USA, 5School of Earth and Space Exploration, Arizona State University, Tempe, AZ, • fl The distribution of cold spots re ects USA, 6Earth Sciences, University of Toronto, Toronto, ON, Canada, 7Department of Geology and Geophysics, University of ’ the Moon s synchronous rotation ’ ā 8 with cold spots focused on the apex Hawai iatM noa, Honolulu, HI, USA, Hawaii Institute of Geophysics and Planetology, Honolulu, HI, USA of motion • The largest cold spots with source craters larger than 800 m are Abstract Mapping of lunar nighttime surface temperatures has revealed anomalously low nighttime concentrated on the trailing side of temperatures around recently formed impact craters on the Moon. The thermophysically distinct “cold the moon spots” provide a way of identifying the most recently formed impact craters. Over 2,000 cold spot source craters were measured with diameters ranging from 43 m to 2.3 km. -
Climate Change and Freshwater Fisheries
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/282814011 Climate change and freshwater fisheries Chapter · September 2015 DOI: 10.1002/9781118394380.ch50 CITATIONS READS 15 1,011 1 author: Chris Harrod University of Antofagasta 203 PUBLICATIONS 2,695 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: "Characterizing the Ecological Niche of Native Cockroaches in a Chilean biodiversity hotspot: diet and plant-insect associations" National Geographic Research and Exploration GRANT #WW-061R-17 View project Effects of seasonal and monthly hypoxic oscillations on seabed biota: evaluating relationships between taxonomical and functional diversity and changes on trophic structure of macrobenthic assemblages View project All content following this page was uploaded by Chris Harrod on 28 February 2018. The user has requested enhancement of the downloaded file. Chapter 7.3 Climate change and freshwater fisheries Chris Harrod Instituto de Ciencias Naturales Alexander Von Humboldt, Universidad de Antofagasta, Antofagasta, Chile Abstract: Climate change is among the most serious environmental challenge facing humanity and the ecosystems that provide the goods and services on which it relies. Climate change has had a major historical influence on global biodiversity and will continue to impact the structure and function of natural ecosystems, including the provision of natural services such as fisheries. Freshwater fishery professionals (e.g. fishery managers, fish biologists, fishery scientists and fishers) need to be informed regarding the likely impacts of climate change. Written for such an audience, this chapter reviews the drivers of climatic change and the means by which its impacts are predicted. -
The Impact of Selling the Federal Helium Reserve O E
o e h i ue t r use t are t ease l P breaks ed. age The Impact of Selling the Federal P iles. ally insert f Helium Reserve ng i t peset y http://www.nap.edu/catalog/9860.html The ImpactofSellingtheFederalHeliumReserve been accident have y a he original t t Committee on the Impact of Selling the Federal Helium Reserve m om r Board on Physics and Astronomy f not Commission on Physical Sciences, Mathematics, and Applications National Materials Advisory Board pographic errors Commission on Engineering and Technical Systems y t e National Research Council riginal paper book, and som , he o t ined a om r ed f be ret Copyright © National Academy ofSciences. Allrights reserved. iles creat cannot f L M X om however, r ng, i t at posed f rm o f ic recom ng-specif i t has been ion. peset ibut y r t r at her t o f original work e h and ot t version yles, ion of ive st at at horit heading aut e represent l h a as t breaks, ion word is new digit h hs, T is publicat ile: h t NATIONAL ACADEMY PRESS f F of line lengt D Washington D.C. is P h t version original; bout he print t A The Impact of Selling the Federal Helium Reserve http://www.nap.edu/catalog/9860.html ii NOTICE: The project that is the subject of this report was approved by the Governing Board of the National Research Council, whose members are drawn from the councils of the National Academy of Sciences, the National Academy of Engineering, and the Institute of Medicine. -
Hydrogeologic Information on the Glorieta Sandstone and the Ogallala Formation in the Oklahoma Panhandle and Adioining Areas As Related to Underground Waste Disposal
Hydrogeologic Information on the Glorieta Sandstone and the Ogallala Formation in the Oklahoma Panhandle and Adioining Areas as Related to Underground Waste Disposal GEOLOGICAL SURVEY CIRCULAR 630 Hydrogeologic Information on the Glorieta Sandstone and the Ogallala Formation in the Oklahoma Panhandle and Adioining Areas as Related to Underground Waste Disposal By James H. Irwin and Robert B. Morton GEOLOGICAL SURVEY CIRCULAR 630 Washington 1969 United States Department of the Interior CECIL D. ANDRUS, Secretary Geological Survey H. William Menard, Director First printing 1969 Second printing 1978 Free on application to Branch ol Distribution, U.S. Geological Survey 1200 South Eads Street, Arlington, Va. 22202 CONTENTS Page Page J\bstract -------------------------------------- 1 Character of the strata between the Glorieta Introduction ____________ ---------------------- 1 Sandstone and the Ogallala Formation ----- 9 Regional geologic setting ----------------------- 3 Hydrology ------------------------------------ 9 Structure -------------------------------- 3 Ogallala Formation and younger rocks _______ 9 Subsurface rocks ------------------------- 3 . Other aquifers ---------------------------- 10 Rocks of Permian age ----------------- 6 Quality of water------------------------------- 11 Rocks of Triassic age ----------------- 6 Ogallala Formation ------------------------ 11 Rocks of Jurassic age ----------------- 7 Other aquifers ---------------------------- 11 Rocks of Cretaceous age --------------- 7 Rocks of Permian age ------.---------------- -
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Paleoecology of the Freshwater Ampullariidae from the Late Oligocene Nsungwe Formation of Tanzania A thesis presented to the faculty of the College of Arts and Sciences of Ohio University In partial fulfillment of the requirements for the degree Master of Science Yuwan Ranjeev Epa April 2017 © 2017 Yuwan Ranjeev Epa. All Rights Reserved. 2 This thesis titled Paleoecology of the Freshwater Ampullariidae from the Late Oligocene Nsungwe Formation of Tanzania by YUWAN RANJEEV EPA has been approved for the Department of Geological Sciences and the College of Arts and Sciences by Alycia L. Stigall Professor of Geological Sciences Robert Frank Dean, College of Arts and Sciences 3 ABSTRACT EPA, YUWAN RANJEEV, M.S., April 2017, Geological Sciences Paleoecology of the Freshwater Ampullariidae from the Late Oligocene Nsungwe Formation of Tanzania Director of Thesis: Alycia L. Stigall This study examines morphological diversification of the late Oligocene ampullariid species from the Rukwa Rift Basin of Tanzania. Six new species of ampullariids are described, including five species of Lanistes and one species of Carnevalea. The high-spired Lanistes species described record the earliest appearance of this morphotype in the fossil record. Carnevalea santiapillai records the first appearance of this genus outside the Eocene of Oman. Paleoecological interpretations suggest a paludal to lacustrine ecology for C. santiapillai and a lacustrine ecology for L. nsungwensis. Lanistes songwensis and L. songweellipticus were interpreted as fluviate species whereas