Astrobiology and the Possibility of Life on Earth and Elsewhere…
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The History Group's Silver Jubilee
History of Meteorology and Physical Oceanography Special Interest Group Newsletter 1, 2010 ANNUAL REPORT CONTENTS We asked in the last two newsletters if you Annual Report ........................................... 1 thought the History Group should hold an Committee members ................................ 2 Annual General Meeting. There is nothing in Mrs Jean Ludlam ...................................... 2 the By-Law s or Standing Orders of the Royal Meteorological Society that requires the The 2010 Summer Meeting ..................... 3 Group to hold one, nor does Charity Law Report of meeting on 18 November .......... 4 require one. Which papers have been cited? .............. 10 Don’t try this at home! ............................. 10 Only one person responded, and that was in More Richard Gregory reminiscences ..... 11 passing during a telephone conversation about something else. He was in favour of Storm warnings for seafarers: Part 2 ....... 13 holding an AGM but only slightly so. He Swedish storm warnings ......................... 17 expressed the view that an AGM provides an Rikitea meteorological station ................. 19 opportunity to put forward ideas for the More on the D-Day forecast .................... 20 Group’s committee to consider. Recent publications ................................ 21 As there has been so little response, the Did you know? ........................................ 22 Group’s committee has decided that there will Date for your diary .................................. 23 not be an AGM this year. Historic picture ........................................ 23 2009 members of the Group ................... 24 CHAIRMAN’S REVIEW OF 2009 by Malcolm Walker year. Sadly, however, two people who have supported the Group for many years died during I begin as I did last year. Without an enthusiastic 2009. David Limbert passed away on 3 M a y, and conscientious committee, there would be no and Jean Ludlam died in October (see page 2). -
Department of Biology Course Outline SC/BIOL 3300 3.00 Origins And
Department of Biology Course Outline SC/BIOL 3300 3.00 Origins and Development of Biological Theories Fall 2020 Course Description An analysis of the origins and development of biological theories, which may include those in evolutionary biology, ecology, biodiversity, and molecular phylogenetics. Prerequisites Note: Open only to students in the third or final year of a biology program, or with permission of the instructor. Only open to students who have completed a minimum of 12 credits at the 2000 level in Biology courses. Course Credit Exclusion: SC/BIOL 4300 3.00 Course Instructors and Contact Information Professor Jan Sapp Email [email protected] Office: Farquharson 306. Schedule Class time: Thursdays 14:30-17:30 Location: delivered remotely on zoom for live stream lectures. Students will require a computer and internet service. Lectures will also be recorded. • For outside class time questions, I will provide “office hours” after class. You may also contact me at [email protected]. 1 Evaluation Midterm test: 25% October 22- based on lectures and required readings. Jan Sapp, Co- existence: The Ecology and Evolution of Tropical Biodiversity (OUP 2016). Chapters supplied on course e-class. The mid term test may be conducted with the aid of an online proctoring service. All students must write the test on October 13. Research Proposal: 15%, due date October 1. Assessment will be based on formulation of the questions of your essay highlighting the significance of the research you will write about, and how you will investigate the origins and development of that research. ~250 words, plus a bibliography indicating the literature you intend to study. -
A 1 Case-PR/ }*Rciofft.;Is Report
.A 1 case-PR/ }*rciofft.;is Report (a) This eruption site on Mauna Loa Volcano was the main source of the voluminous lavas that flowed two- thirds of the distance to the town of Hilo (20 km). In the interior of the lava fountains, the white-orange color indicates maximum temperatures of about 1120°C; deeper orange in both the fountains and flows reflects decreasing temperatures (<1100°C) at edges and the surface. (b) High winds swept the exposed ridges, and the filter cannister was changed in the shelter of a p^hoehoc (lava) ridge to protect the sample from gas contamination. (c) Because of the high temperatures and acid gases, special clothing and equipment was necessary to protect the eyes. nose, lungs, and skin. Safety features included military flight suits of nonflammable fabric, fuil-face respirators that are equipped with dual acidic gas filters (purple attachments), hard hats, heavy, thick-soled boots, and protective gloves. We used portable radios to keep in touch with the Hawaii Volcano Observatory, where the area's seismic activity was monitored continuously. (d) Spatter activity in the Pu'u O Vent during the January 1984 eruption of Kilauea Volcano. Magma visible in the circular conduit oscillated in a piston-like fashion; spatter was ejected to heights of 1 to 10 m. During this activity, we sampled gases continuously for 5 hours at the west edge. Cover photo: This aerial view of Kilauea Volcano was taken in April 1984 during overflights to collect gas samples from the plume. The bluish portion of the gas plume contained a far higher density of fine-grained scoria (ash). -
Development of DLC-Coated Solid Sialon/Tin Ceramic End Mills for Nickel Alloy Machining: Problems and Prospects
coatings Article Development of DLC-Coated Solid SiAlON/TiN Ceramic End Mills for Nickel Alloy Machining: Problems and Prospects Sergey N. Grigoriev , Marina A. Volosova *, Sergey V. Fedorov, Anna A. Okunkova , Petr M. Pivkin , Pavel Y. Peretyagin and Artem Ershov Department of High-Efficiency Processing Technologies, Moscow State University of Technology “STANKIN”, Vadkovskiy per. 3A, 127055 Moscow, Russia; [email protected] (S.N.G.); [email protected] (S.V.F.); [email protected] (A.A.O.); [email protected] (P.M.P.); [email protected] (P.Y.P.); [email protected] (A.E.) * Correspondence: [email protected]; Tel.: +7-916-308-49-00 Abstract: The study is devoted to the development and testing of technological principles for the manufacture of solid end mills from ceramics based on a powder composition of α-SiAlON, β-SiAlON, and TiN additives, including spark plasma sintering powder composition, diamond sharpening of sintered ceramic blanks for shaping the cutting part of mills and deposition of anti- friction Si-containing diamond-like carbon (DLC) coatings in the final stage. A rational relationship between the components of the powder composition at spark plasma sintering was established. The influence of optimum temperature, which is the most critical sintering parameter, on ceramic samples’ basic physical and mechanical properties was investigated. DLC coatings’ role in changing the surface properties of ceramics based on SiAlON, such as microrelief, friction coefficient, et cetera, was studied. A comparative analysis of the efficiency of two tool options, such as developed samples of experimental mills made of SiAlON/TiN and commercial samples ceramic mills based on SiAlON, Citation: Grigoriev, S.N.; Volosova, doped with stabilizing additives containing Yb when processing nickel alloys (NiCr20TiAl alloy was M.A.; Fedorov, S.V.; Okunkova, A.A.; used as an example). -
Apollo Over the Moon: a View from Orbit (Nasa Sp-362)
chl APOLLO OVER THE MOON: A VIEW FROM ORBIT (NASA SP-362) Chapter 1 - Introduction Harold Masursky, Farouk El-Baz, Frederick J. Doyle, and Leon J. Kosofsky [For a high resolution picture- click here] Objectives [1] Photography of the lunar surface was considered an important goal of the Apollo program by the National Aeronautics and Space Administration. The important objectives of Apollo photography were (1) to gather data pertaining to the topography and specific landmarks along the approach paths to the early Apollo landing sites; (2) to obtain high-resolution photographs of the landing sites and surrounding areas to plan lunar surface exploration, and to provide a basis for extrapolating the concentrated observations at the landing sites to nearby areas; and (3) to obtain photographs suitable for regional studies of the lunar geologic environment and the processes that act upon it. Through study of the photographs and all other arrays of information gathered by the Apollo and earlier lunar programs, we may develop an understanding of the evolution of the lunar crust. In this introductory chapter we describe how the Apollo photographic systems were selected and used; how the photographic mission plans were formulated and conducted; how part of the great mass of data is being analyzed and published; and, finally, we describe some of the scientific results. Historically most lunar atlases have used photointerpretive techniques to discuss the possible origins of the Moon's crust and its surface features. The ideas presented in this volume also rely on photointerpretation. However, many ideas are substantiated or expanded by information obtained from the huge arrays of supporting data gathered by Earth-based and orbital sensors, from experiments deployed on the lunar surface, and from studies made of the returned samples. -
The Composition of the Lunar Crust: Radiative Transfer Modeling and Analysis of Lunar Visible and Near-Infrared Spectra
THE COMPOSITION OF THE LUNAR CRUST: RADIATIVE TRANSFER MODELING AND ANALYSIS OF LUNAR VISIBLE AND NEAR-INFRARED SPECTRA A DISSERTATION SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAI‘I IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN GEOLOGY AND GEOPHYSICS DECEMBER 2009 By Joshua T.S. Cahill Dissertation Committee: Paul G. Lucey, Chairperson G. Jeffrey Taylor Patricia Fryer Jeffrey J. Gillis-Davis Trevor Sorensen Student: Joshua T.S. Cahill Student ID#: 1565-1460 Field: Geology and Geophysics Graduation date: December 2009 Title: The Composition of the Lunar Crust: Radiative Transfer Modeling and Analysis of Lunar Visible and Near-Infrared Spectra We certify that we have read this dissertation and that, in our opinion, it is satisfactory in scope and quality as a dissertation for the degree of Doctor of Philosophy in Geology and Geophysics. Dissertation Committee: Names Signatures Paul G. Lucey, Chairperson ____________________________ G. Jeffrey Taylor ____________________________ Jeffrey J. Gillis-Davis ____________________________ Patricia Fryer ____________________________ Trevor Sorensen ____________________________ ACKNOWLEDGEMENTS I must first express my love and appreciation to my family. Thank you to my wife Karen for providing love, support, and perspective. And to our little girl Maggie who only recently became part of our family and has already provided priceless memories in the form of beautiful smiles, belly laughs, and little bear hugs. The two of you provided me with the most meaningful reasons to push towards the "finish line". I would also like to thank my immediate and extended family. Many of them do not fully understand much about what I do, but support the endeavor acknowledging that if it is something I’m willing to put this much effort into, it must be worthwhile. -
Handbook of Iron Meteorites, Volume 1
CHAPTER FOUR Meteorite Craters Nobody has ever witnessed the formation of a meteor meteorites, and (iii) rapidly solidified metallic droplets, ite crater. Interpretations must therefore be based upon analogous to the spheroids encountered in the vicinity of measurement and comparison with artificial craters, caused Meteor Crater, Arizona (Goldstein et al. 1972; Anders et al. by known magnitudes and depths of explosives. Excellent 1973); see page 397. studies have been performed by Baldwin (1949; 1963; The bulk of the typical large lunar craters were formed 1970) who was particularly interested in the puzzling when the kinetic energy ~mv 2 of the impacting body was problems associated with the lunar craters but, as a basis for converted into thermal energy within a fraction of a his speculations, thoroughly examined several terrestrial second, resulting in an explosion. There is a very high craters and presented extensive bibliographies. Results from probability that the impacting body was thereby itself nuclear test sites have been presented by Hansen (1968) totally destroyed, melted or vaporized (Hartman & and Short (1968a, b). Krinov (1960b; 1966a, b) has dis Wood 1971; Ahrens & O'Keefe 1972). Fortunately, for the cussed several craters and impact holes associated with science of meteoritics and for the inhabitants of Earth, our meteorites and also devoted a liuge chapter to the Tunguska atmosphere will alleviate the impact of celestial bodies and comet, which did not produce craters at all. See page 9. through a gradual deceleration cause an important propor Stanyukovich &' Fedynski (1947), Nininger (1952a; 1956), tion to survive as meteorites. However, large and dense Shoemaker (1963) and Gault et al. -
Lunar Craters Named in Honor of Apollo 8 5 October 2018
Lunar craters named in honor of Apollo 8 5 October 2018 The Apollo 8 mission took place from 21 to 27 December 1968. After completing 10 orbits around the Moon on Christmas Eve, broadcasting images back to Earth and giving live television transmissions, the crew returned to Earth and landed in the Pacific Ocean. The Working Group for Planetary System Nomenclature (WGPSN) of the International Astronomical Union, who named the craters, is the authority responsible for the naming of planetary features in our Solar System. The two named craters were previously designated by letters. The Earthrise color photograph taken by astronaut William Anders. It depicts the moment that our shiny blue Earth came back into view as the spacecraft emerged out of the dark from behind the grey and barren Moon. This is arguably the most famous picture taken by Apollo 8. It became iconic and has been credited with starting the environmental movement.Two of the crates seen in this photo have just been named by the Working Group for Planetary System Nomenclature (WGPSN) of the International Astronomical Union. Credit: NASA/IAU The newly named craters are visible in the The Working Group for Planetary System Nomenclature foreground of the iconic Earthrise colour of the International Astronomical Union has officially photograph taken by astronaut William Anders. It approved the naming of two craters on the Moon to commemorate the 50th anniversary of the Apollo 8 depicts the moment that our shiny blue Earth came mission. The names are Anders’ Earthrise and 8 back into view as the spacecraft emerged out of Homeward. -
Theoretical and Experimental Evidence for Wet Accretion of Earth
Theoretical and experimental evidence for wet accretion of Earth Krishna Muralidharan1, Abu Asaduzzaman1, Luca Vattuone2, Mario Rocca2 1 Department of Materials Science and Engineering, University of Arizona, Tucson, AZ 85721, USA 2 Dipartimento di Fisica dell’Università di Genova and IMEM-CNR Unità operativa di Genova, Via Dodecaneso 33, 16146 Genova, Italy † In memory of Prof. Michael J. Drake There has been an ongoing debate on the origin of water on Earth and other inner-solar system planets. So far, there is no consensus regarding the water-delivery mechanism(s) to the terrestrial planets. While water delivery via comets and asteroids is widely accepted, an upper limit for water delivery to Earth of about 15% is necessary, to ensure consistency with the measurements of D/H and Ar/H2O ratio in water-bearing comets. On similar lines, although asteroids are considered as a plausible source of water, the Os isotope ratio in Earth’s mantle rules out of asteroids as being the dominant source of Earth’s water. In this context, given that water and solid particulates coexisted in the accretion disk prior to planet formation, it was recently hypothesized that some of Earth’s water could be endogenous, with the delivery occurring via direct adsorption of water onto mineral surfaces. To confirm this hypothesis, we have carried out experimental and computational investigations examining water adsorption on olivine grains. The strong binding energy characterizing the adsorption process as seen by both theory and experiments unequivocally indicate that significant amounts of water can be adsorbed on to grains in the accretion disk prior to planetary accretion. -
Origin of Water Ice in the Solar System 309
Lunine: Origin of Water Ice in the Solar System 309 Origin of Water Ice in the Solar System Jonathan I. Lunine Lunar and Planetary Laboratory The origin and early distribution of water ice and more volatile compounds in the outer solar system is considered. The origin of water ice during planetary formation is at least twofold: It condenses beyond a certain distance from the proto-Sun — no more than 5 AU but perhaps as close as 2 AU — and it falls in from the surrounding molecular cloud. Because some of the infalling water ice is not sublimated in the ambient disk, complete mixing between these two sources was not achieved, and at least two populations of icy planetesimals may have been present in the protoplanetary disk. Added to this is a third reservoir of water ice planetesimals representing material chemically processed and then condensed in satellite-forming disks around giant planets. Water of hydration in silicates inward of the condensation front might be a sepa- rate source, if the hydration occurred directly from the nebular disk and not later in the parent bodies. The differences among these reservoirs of icy planetesimals ought to be reflected in diverse composition and abundance of trapped or condensed species more volatile than the water ice matrix, although radial mixing may have erased most of the differences. Possible sources of water for Earth are diverse, and include Mars-sized hydrated bodies in the asteroid belt, smaller “asteroidal” bodies, water adsorbed into dry silicate grains in the nebula, and comets. These different sources may be distinguished by their deuterium-to-hydrogen ratio, and by pre- dictions on the relative amounts of water (and isotopic compositional differences) between Earth and Mars. -
"THE GENERAL THEORY of META-DYNAMICS SYSTEMICITY" Part Four: Early Earth and Origin of Life’S Metadynamics Systemicity
"THE GENERAL THEORY OF META-DYNAMICS SYSTEMICITY" Part four: Early Earth and origin of Life’s metadynamics systemicity Jean-Jacques BLANC Consulting Engineer Crets de Champel, 9 CH - 1206 – Geneva, Switzerland Tel/fax: +41(22)346 30 48 E-mail: [email protected] Url: www.bioethismscience.org The "Cosmo-planetary and terrestrial meta-dynamics systemicity”, the “Life’s meta-dynamics systemicity”, and "Biological meta-dynamics systemicity" are the core of a general theory resulting from a “Bioethism transdisciplinary approach” of the whole set of dynamics that made and sustains Life as to exist throughout the atomic and molecular universal cycles systemicity. Part four of this theory describes the Universe Cosmo-planetary metadynamics as having participated in the Sun system and its planets to form, particularly the Earth at the right “habitable zone”. The physicochemical environmental conditions of this site became propitious for Life to “hatch” within biochemical thermodynamics1 and evolution development metadynamics. ABSTRACT Ever since 1996, J.-J. Blanc, the author of this theory, made an extensive research on "Systems science" that induced to his developing a new systemic2 paradigm in terms of a transdisciplinary approach to "Living systems" that he named “The Bioethism” (see note 3). The transdisciplinary approach is meant to support the acquisition of a large understanding of living systems' origin, of their natural structure and their adaptive behaviors. Their specific bonds and traits, as well as their evolution trends, while permanently interacting with environmental events for survival4, require actions-reactions from ago-antagonistic signals and stimuli. Endogenous within their body milieu and exogenous, these signals and stimuli are adapting with conditions of ecosystemic and sociosystemic environments. -
Water Cycle2013
11/14/13! OCN 401! The Global Water Cycle! The annual circulation of H2O is the largest movement of a! chemical substance at the Earth’s surface.! The distribution of water at the ! Earth's surface! !!!! !!!!% of total! Oceans! !!!97.25! Ice caps and glaciers ! !2.05! Groundwater ! !!0.68! Lakes ! !!!0.01! Soils ! !!!0.005! Atmosphere (as vapour) !0.001! Rivers ! !!!0.0001! Biosphere ! !!0.00004! Total ! !!!100 %! 1! 11/14/13! Origin of water on Earth! Water was delivered to primitive Earth by planetesimals, meteors and comets (Chap. 2) during its accretionary phase, which was largely complete by 3.8 billion years ago (Ga)! Water was released from Earth’s crust in volcanic eruptions (degassing), but remained in the atmosphere as long as Earth’s surface temperature was >100°C! Once Earth cooled below 100°C, most water condensed to form the oceans! Enough water vapor and CO2 remained in the atmosphere to keep the temperature of Earth’s surface above freezing; without this Greenhouse effect the Earth might have remained frozen, like Mars.! There is good evidence of liquid water on Earth at 3.8 bya, and the volume of water has not changed appreciably since then.! 2! 11/14/13! Global water cycle and reservoirs! Units = km3 and km3/yr! 1 km3 = 1x 1012 L ! The Global Water Cycle: Fluxes and Residence Times • Using estimates of the reservoir size and the magnitude of fluxes between reservoirs, can calculate the residence time (Tr) of water in each reservoir:! !- The Tr(H2O) of the ocean with respect to the atmosphere:! !!1350 km3 / 0.425 km3/y