Nickel and Its Alloys L
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Invar, Established a New Standard in the Way Precise Surveying Measurements Were Made, Both in Reliability and Accuracy
I N VA R The Breakthrough for a Low Expansion Alloy he discovery of the low expansion alloy, Invar, established a new standard in the way precise surveying measurements were made, both in reliability and accuracy. It became the first successful attempt to produce a metal alloy exhibiting a nearly zero coefficient of thermal expansion. In 1889, James Riley of Glasgow, Scotland, brought before the Iron and Steel Institute his investigations into the making of an alloy through a series of tests which combined up to 49 percent nickel with iron. Seven years later, in 1896, Charles Edouard Guillaume, a Swiss-born metallurgist and employee with the International Bureau of Weights and Measures near Paris, began looking specifically for an alloy to be used for surveyors’ wires that would not noticeably change when exposed to temperature variations. While experimenting with nickel contents between 30 and 60 percent, Guillaume discovered the coefficient of expansion at room temperature was lowest when mixing a nickel content of 36 percent with 64 percent iron. Since his new alloy exhibited the least amount of thermal expansion, and because Guillaume considered it invariable, it quickly became known as “Invar”. In 1920, Guillaume was awarded the Nobel Prize in Physics for his discovery of Invar >> By Jerry Penry, PS Displayed with permission • The American Surveyor • Vol. 9 No. 10 • Copyright 2012 Cheves Media • www.Amerisurv.com The Sokkia BIS30 3-meter Invar bar code leveling staff in use during a high precision survey. Image courtesy of Sokkia Corporation. Displayed with permission • The American Surveyor • Vol. 9 No. -
Handbook of Iron Meteorites, Volume 2 (Bitburg
326 Bishop Canyon - Bitburg fibrous and brecciated, and 1-100 p wide veins through it ' l ' j are filled with a glass in which silicate fragments and a little ) ·. / troilite are embedded.lt is surprising to note how the shock . e·· f . has been able to create such heavy local transformation; 10 mm away nothing unusual is observed. The local damage resembles in several respects the structural changes associated with spot welding. Examination under the electron microprobe suggests that the unknown silicate is ~' almost pure Si02 , possibly tridymite. Bishop Canyon is chemically and structurally a typical ~ phosphorus-poor, fine octahedrite of groupiVA, . l .. resembling in particular Gibe on. It is, however, unusual in .0 its silicate inclusions, the shock damage and low hardness. ,, .• ~: :t • ·. • cr ··. @ Specimen in the U.S. National Museum in Washington: .. ~ - ,·r -. f '-' f 226 g slice (no. 770, 9.5 x 4.5 x 0.9 em) II . 0 t' / •. ' ~~ ~~ {) r ...~ · -· · ...· ~· -/~... Figure 352. Bitburg. Detail of Figure 350. The dendritic metal was Bitburg, Rhineland, Germany at high temperature austenite but transformed upon cooling to unequilibrated a • Etched. Scale bar 50 f.l. 49°58'N, 6°32'E 2 A mass said to have weighed 1.5 tons was smelted in a furnace before 1805. It was recognized as a meteorite (Chladni 1819: 353), but virtually nothing was saved of the undamaged material (Hey 1966: 57). The smelted material, e.g., no. 1881, 1534 of 546 gin .. \ . • I : '/ 'I \ ' . ~\.. // .·· Figure 350. Bit burg (Copenhagen no. 1886, 493). A rectangular bar cut from melted material of the Bitburg meteorite. -
Special-Purpose Nickel Alloys
© 2000 ASM International. All Rights Reserved. www.asminternational.org ASM Specialty Handbook: Nickel, Cobalt, and Their Alloys (#06178G) Special-Purpose Nickel Alloys NICKEL-BASE ALLOYS have a number of meet special needs. The grades considered in ganese, and copper, a 0.005% limit on iron, and unique properties, or combinations of proper- this section include the following: a 0.02% limit on carbon. This high purity re- ties, that allow them to be used in a variety of sults in lower coefficient of expansion, electri- specialized applications. For example, the high • Nickel 200 (99.6% Ni, 0.04% C) cal resistivity, Curie temperature, and greater resistivity (resistance to flow of electricity) and • Nickel 201 (99.6% Ni, 0.02% C maximum) ductility than those of other grades of nickel heat resistance of nickel-chromium alloys lead • Nickel 205 (99.6% Ni, 0.04% C, 0.04% Mg) and makes Nickel 270 especially useful for to their use as electric resistance heating ele- • Nickel 233 (see composition in table that fol- some electronics applications such as compo- ments. The soft magnetic properties of lows) nents of hydrogen thyratrons and as a substrate nickel-iron alloys are employed in electronic • Nickel 270 (99.97% Ni) for precious metal cladding. devices and for electromagnetic shielding of computers and communication equipment. Iron- Composition limits and property data on sev- eral of these grades can be found in the article nickel alloys have low expansion characteris- Resistance Heating Alloys tics as a result of a balance between thermal ex- “Wrought Corrosion-Resistant Nickels and pansion and magnetostrictive changes with Nickel Alloys” in this Handbook. -
The Tawallah Valley Meteorite. General Description. the Microstructure.Records of the Australian Museum 21(1): 1–8, Plates I–Ii
AUSTRALIAN MUSEUM SCIENTIFIC PUBLICATIONS Hodge-Smith, T., and A. B. Edwards, 1941. The Tawallah Valley meteorite. General description. The Microstructure.Records of the Australian Museum 21(1): 1–8, plates i–ii. [4 July 1941]. doi:10.3853/j.0067-1975.21.1941.518 ISSN 0067-1975 Published by the Australian Museum, Sydney nature culture discover Australian Museum science is freely accessible online at http://publications.australianmuseum.net.au 6 College Street, Sydney NSW 2010, Australia THE TAW ALLAH VALLEY METEORITE. General Description. By T. HODGE-SMI'l'H, The Australian Museum. The Microstructure. By A. B. EDWARDS, Ph.D., D.I.C.,* Research Officer, Mineragraphy Branch, Council for Scientific and Industrial Research. (Plates i-ii and Figures 1-2.) General Description. Little information is available about the finding of this meteorite. Mr. Heathcock, Constable-in-Charge of the Borroloola Police Station, Northern Territory, informed me in April, 1939, that it had been in the Police Station for eighteen months or more. It was found by Mr. Condon, presumably some time in 1937. The weight of the iron as received was 75·75 kg. (167 lb.). A small piece had been cut off, but its weight probably did not exceed 200 grammes. The main mass weighing 39·35 kg. (86i lb.) is in the collection of the Geological Survey, Department of the Interior, Canberra. A portion weighing 30·16 kg. (66~ lb.) and five pieces together weighing 1·67 kg. are in the collection of the Australian Museum, and a slice weighing 453 grammes is in the Museum of the Geology Department, the University of Melbourne. -
BSTJ 27: 3. July 1948: the Evolution of the Quartz Crystal Clock
The Evolution of the Quartz Crystal Clock* By WARREN A. MARRISON SOME of the earliest documents in human history relate to man's interest in timekeeping. This interest arose partly because of his curiosity about the visible world around him, and partly because the art of time measure- ment became an increasingly important part of living as the need for cooper- ation between the members of expanding groups increased. There are still in existence devices believed to have been made by the Egyptians six thousand years ago for the purpose of telling time from the stars, and there is good reason to believe that they were in quite general use by the better educated people of that period. 1 Since that period there has been a continuous use and improvement of timekeeping methods and devices, following sometimes quite independent lines, but developing through a long series of new ideas and refinements into the very precise means at our disposal today. The art of timekeeping and time measurement is of very great value, both from its direct social use in permitting time tables and schedules to be made, and in its relation to other arts and the sciences in which the measurement of rate and duration assume ever increasing importance. The early history of timekeeping was concerned almost entirely with the first of these and for many centuries the chief purpose of timekeeping devices was to provide means for the approximate subdivision of the day, particularly of the day- light hours. The most obvious events marking the passage of time were the rising and setting of the sun and its continuous apparent motion from east to west through the sky. -
A New Meteoric Iron from Piedade Do Bagre, Minas Geraes, Brazil
271 A new meteoric iron from Piedade do Bagre, Minas Geraes, Brazil. (With Plates XI and XII.) By L. J. SPENCER, M.A., Sc.D., F.R.S. With a chemical analysis by M. It. HEY, B.A., B.Se. Mineral Department, British Museum of Natural History. [Read June 3, 1930.] MASS of iron weighing 130 lb., stated to have been found in A 1922 near the village of Piedade do Bagre in Minas Geraes, Brazil, and believed to be meteoric, was submitted by Mr. N. Medawar in January 1929 to the Mineral Department of the British Museum for examination. The following description of the mass fully confirms the supposition of its meteoric origin. Unfortunately, only scanty details are available of the circumstances of the finding of the mass. All the information that Mr. Medawar was able to supply is given in the following short note written by Mr. R. J. Bohrer, with a rough sketch-map of the locality. Meteorito encontrado no ponto mareado +. Vendido por intermedio do Snr. Padre Jos6 Alves de Curvello a Rodolpho J. Bohrer. Encontrado em 1922 por um situante cujo nome n~o se conhece. Vendido a Snr. Medawar em Margo de 1927. Mr. Medawar's translation of this is : Meteorite found at the point marked +. Sold by the intermediary of Mr. Padre Jos6 Alves of Curvello to Rodolpho J. Bohrer. Found in 1922 by a local native whose name not known. Sold to Mr. Medawar in March of 1927. The spot marked is about 16 km. (10 miles) SW. of the village of Piedade do Bagre in Minas Geraes. -
Early Fracturing and Impact Residue Emplacement: Can Modelling Help to Predict Their Location in Major Craters?
Early fracturing and impact residue emplacement: Can modelling help to predict their location in major craters? Item Type Proceedings; text Authors Kearsley, A.; Graham, G.; McDonnell, T.; Bland, P.; Hough, R.; Helps, P. Citation Kearsley, A., Graham, G., McDonnell, T., Bland, P., Hough, R., & Helps, P. (2004). Early fracturing and impact residue emplacement: Can modelling help to predict their location in major craters?. Meteoritics & Planetary Science, 39(2), 247-265. DOI 10.1111/j.1945-5100.2004.tb00339.x Publisher The Meteoritical Society Journal Meteoritics & Planetary Science Rights Copyright © The Meteoritical Society Download date 23/09/2021 21:19:20 Item License http://rightsstatements.org/vocab/InC/1.0/ Version Final published version Link to Item http://hdl.handle.net/10150/655802 Meteoritics & Planetary Science 39, Nr 2, 247–265 (2004) Abstract available online at http://meteoritics.org Early fracturing and impact residue emplacement: Can modelling help to predict their location in major craters? Anton KEARSLEY,1* Giles GRAHAM,2 Tony McDONNELL,3 Phil BLAND,4 Rob HOUGH,5 and Paul HELPS6 1Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK 2Institute of Geophysics and Planetary Physics, Lawrence Livermore National Laboratory, California, USA 3Planetary and Space Sciences Research Institute, The Open University, Milton Keynes, MK7 6AA, UK 4Department of Earth Science and Engineering, Imperial College London, London SW7 2AZ, UK 5Museum of Western Australia, Francis Street, Perth, Western Australia 6000, Australia 6School of Earth Sciences and Geography, Kingston University, Kingston-upon-Thames, Surrey, KT1 2EE, UK *Corresponding author. E-mail: [email protected] (Received 30 June 2003; revision accepted 15 December 2003) Abstract–Understanding the nature and composition of larger extraterrestrial bodies that may collide with the Earth is important. -
General Index Vols. XLI-L, Third Series
GENERAL INDEX OF VOLUMES XLI-L OF THE THIRD SERIES. WInthe references to volumes xli to I, only the numerals i to ir we given. NOTE.-The names of mineral8 nre inaerted under the head ol' ~~IBERALB:all ohitllary notices are referred to under OBITUARY. Under the heads BO'PANY,CHK~I~TRY, OEOLO~Y, Roo~s,the refereuces to the topics in these department8 are grouped together; in many cases, the same references appear also elsewhere. Alabama, geological survey, see GEOL. REPORTSand SURVEYS. Abbe, C., atmospheric radiation of Industrial and Scientific Society, heat, iii, 364 ; RIechnnics of the i. 267. Earth's Atmosphere, v, 442. Alnska, expedition to, Russell, ii, 171. Aberration, Rayleigh, iii, 432. Albirnpean studies, Uhler, iv, 333. Absorption by alum, Hutchins, iii, Alps, section of, Rothpletz, vii, 482. 526--. Alternating currents. Bedell and Cre- Absorption fipectra, Julius, v, 254. hore, v, 435 ; reronance analysis, ilcadeiny of Sciences, French, ix, 328. Pupin, viii, 379, 473. academy, National, meeting at Al- Altitudes in the United States, dic- bany, vi, 483: Baltimore, iv, ,504 : tionary of, Gannett, iv. 262. New Haven, viii, 513 ; New York, Alum crystals, anomalies in the ii. 523: Washington, i, 521, iii, growth, JIiers, viii, 350. 441, v, 527, vii, 484, ix, 428. Aluminum, Tvave length of ultra-violet on electrical measurements, ix, lines of, Runge, 1, 71. 236, 316. American Association of Chemists, i, Texas, Transactions, v, 78. 927 . Acoustics, rrsearchesin, RIayer, vii, 1. Geological Society, see GEOL. Acton, E. H., Practical physiology of SOCIETYof AMERICA. plants, ix, 77. Nuseu~nof Sat. Hist., bulletin, Adams, F. -
WO 2016/193753 A2 8 December 2016 (08.12.2016) P O P C T
(12) INTERNATIONAL APPLICATION PUBLISHED UNDER THE PATENT COOPERATION TREATY (PCT) (19) World Intellectual Property Organization I International Bureau (10) International Publication Number (43) International Publication Date WO 2016/193753 A2 8 December 2016 (08.12.2016) P O P C T (51) International Patent Classification: (74) Agent: BOULT WADE TENNANT; Verulam Gardens, A61B 90/00 (2016.01) 70 Gray's Inn Road, London WC1X 8BT (GB). (21) International Application Number: (81) Designated States (unless otherwise indicated, for every PCT/GB20 16/05 1649 kind of national protection available): AE, AG, AL, AM, AO, AT, AU, AZ, BA, BB, BG, BH, BN, BR, BW, BY, (22) International Filing Date: BZ, CA, CH, CL, CN, CO, CR, CU, CZ, DE, DK, DM, 3 June 2016 (03.06.2016) DO, DZ, EC, EE, EG, ES, FI, GB, GD, GE, GH, GM, GT, (25) Filing Language: English HN, HR, HU, ID, IL, IN, IR, IS, JP, KE, KG, KN, KP, KR, KZ, LA, LC, LK, LR, LS, LU, LY, MA, MD, ME, MG, (26) Publication Language: English MK, MN, MW, MX, MY, MZ, NA, NG, NI, NO, NZ, OM, (30) Priority Data: PA, PE, PG, PH, PL, PT, QA, RO, RS, RU, RW, SA, SC, 62/170,768 4 June 2015 (04.06.2015) US SD, SE, SG, SK, SL, SM, ST, SV, SY, TH, TJ, TM, TN, TR, TT, TZ, UA, UG, US, UZ, VC, VN, ZA, ZM, ZW. (71) Applicant: ENDOMAGNETICS LTD. [GB/GB]; Jef freys Building, St John's Innovation Park, Cowley Road, (84) Designated States (unless otherwise indicated, for every Cambridge, Cambridgeshire CB4 0WS (GB). -
New Mineral Names
222 TH E AM ERICAN MIN ERALOGIST scattered around the craters are cudously twisted and bent, suggesting that they of a single crystal. Silica-glass, which is of rare occurrence in nature, shows a remarkable develop- ment at Wabar. A snow-white, highly vesicular glass was formed by the fusion of the clean desert sand; and bombs of this material shot out from the craters were coated with a thin skin of black glass free from bubbles and containing iron and nickel in the same ratio as in the meteoric iron. This must have condensed on the surface from the vapours of silica, iron, and nickel, indicating temperatures up to 3r300"C. The silica-glass at Henbury is much less abundant, and being formed from a ferruginous sandstone it is less pure. These bombs of silica-glass present many points of resemblance to tektites. Dn. A. BneuuAr,r. AND Mn. s. BnncBWnrt-: Garnet in the Dartmoor gronite: ils petrogeneLicsignif,cawe. Seventeen occurrences prove to be manganiferous aI- ,nuodirr"s containing 37o to 2270 of MnO. Two or more varieties may occur in a (7%MnO) single hand-specimen of the granite. The more manganiferous varieties are restricted to the tor-horizons; the less manganiferous varieties occur (a) below these horizons, (b) in shale-contaminated facies of the granite, and (c) in xenolithic hornfelsed shale. Basic igneous inclusions are barren of garnet, and grossularite, not almandine, occurs in contact-altered spilites. The mineral is attributed to con- tamination of the granite by country-rock-probably deep-seated shales. Ten j7oMnO) Lake District occurrences show a similar variation (1.3/s-7 ' Mr. -
Charles-É. Guillaume
C HARLES - É . G UILLAUME Invar and elinvar Nobel Lecture, December 11, 1920 The anomaly of nickel steels Discovery of the anomaly - In 1889 the General Conference on Weights and Measures met at Sèvres, the seat of the International Bureau. It performed the first great deed dictated by the motto inscribed in the pediment of the splendid edifice that is the metric system : "A tous les temps, a tous les peuples" (For all times, to all peoples); and this deed consisted in the approval and distribution, among the governments of the states supporting the Metre Con- vention, of prototype standards of hitherto unknown precision intended to propagate the metric unit throughout the whole world. These prototypes were indeed noteworthy. They were made of a plati- num-iridium alloy developed by Henri Sainte-Claire-Deville which com- bined all the qualities of hardness, permanence, and resistance to chemical agents which rendered it suitable for making into standards required to last for centuries. Yet their high price excluded them from the ordinary field of science; at that time a single metre actually cost 7,000 crowns - and how much more today! A less costly answer had to be sought since between these precious proto- types and standards affording only uncertain guarantees there was a gap which nothing could fill. I first examined this problem in 1891 and soon discovered the really ex- cellent properties of pure nickel and still today this is the metal used to make a non-oxidizable standard, unaffected by the passage of time, rigid and of average expansibility. -
NATURE Obituary Notices
No. 3590, AUGUST 20, 1938 NATURE 321 Obituary Notices Dr. A. E. H. Tutton, F.R.S. magnificent crystals with six molecules of water. In LFRED EDWIN HOWARD TUTTON, who all, ninety-one salts were studied, and the results A died on July 14, was born on August 22, communicated in about fifty papers from 1890 until 1864, at Cheadle Moseley, now the Edgeley district 1929. As a result of this painstaking and accurate of the borough of Stockport. He attended science work, it was established that the crystallographic classes at the Stockport Mechanics Institute and properties vary regularly with the atomic weights also the evening courses in chemistry of Prof. of the interchangeable elements. The same result Roscoe at Owens College, Manchester. In 1883 was established for the perchlorates and double he went to the Normal School of Science (later the chroma.tes of the alkalis. This work could be brought Royal College of Science) and Royal School of into relation with the structures as revealed by the Mines, South Kensington, with an exhibition, which X-rays when this new method became available. In he took in preference to a scholarship which he had carrying out his crystallographic investigations gained for Owens College. During his period as a Tutton showed the greatest ingenuity in devising student, Huxley was professor of biology, Frankland and perfecting the measuring instruments, so that his of chemistry, Guthrie of physics, Judd of geology methods became well known as representing the and Lockyer of astronomy, and a fellow-student highest standard of crystallographic research. was H.