Subsea Mineral Resources
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Xrd and Tem Studies on Nanophase Manganese
Clays and Clay Minerals, Vol. 64, No. 5, 488–501, 2016. 1 1 2 2 3 XRD AND TEM STUDIES ON NANOPHASE MANGANESE OXIDES IN 3 4 FRESHWATER FERROMANGANESE NODULES FROM GREEN BAY, 4 5 5 6 LAKE MICHIGAN 6 7 7 8 8 S EUNGYEOL L EE AND H UIFANG X U* 9 9 NASA Astrobiology Institute, Department of Geoscience, University of Wisconsin Madison, Madison, 10 À 10 1215 West Dayton Street, A352 Weeks Hall, Wisconsin 53706 11 11 12 12 13 Abstract—Freshwater ferromanganese nodules (FFN) from Green Bay, Lake Michigan have been 13 14 investigated by X-ray powder diffraction (XRD), micro X-ray fluorescence (XRF), scanning electron 14 microscopy (SEM), high-resolution transmission electron microscopy (HRTEM), and scanning 15 transmission electron microscopy (STEM). The samples can be divided into three types: Mn-rich 15 16 nodules, Fe-Mn nodules, and Fe-rich nodules. The manganese-bearing phases are todorokite, birnessite, 16 17 and buserite. The iron-bearing phases are feroxyhyte, goethite, 2-line ferrihydrite, and proto-goethite 17 18 (intermediate phase between feroxyhyte and goethite). The XRD patterns from a nodule cross section 18 19 suggest the transformation of birnessite to todorokite. The TEM-EDS spectra show that todorokite is 19 associated with Ba, Co, Ni, and Zn; birnessite is associated with Ca and Na; and buserite is associated with 20 2+ +2 3+ 20 Ca. The todorokite has an average chemical formula of Ba0.28(Zn0.14Co0.05 21 2+ 4+ 3+ 3+ 3+ 2+ 21 Ni0.02)(Mn4.99Mn0.82Fe0.12Co0.05Ni0.02)O12·nH2O. -
Redalyc.Mineralogical Study of the La Hueca Cretaceous Iron-Manganese
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Corona Esquivel, Rodolfo; Ortega Gutiérrez, Fernando; Reyes Salas, Margarita; Lozano Santacruz, Rufino; Miranda Gasca, Miguel Angel Mineralogical study of the La Hueca Cretaceous Iron-Manganese deposit, Michoacán, south-western Mexico Revista Mexicana de Ciencias Geológicas, vol. 17, núm. 2, 2000, pp. 142-151 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57217206 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de Ciencias Geológicas, volumen 17, número 2, 143 2000, p. 143- 153 Universidad Nacional Autónoma de México, Instituto de Geología, México, D.F MINERALOGICAL STUDY OF THE LA HUECA CRETACEOUS IRON- MANGANESE DEPOSIT, MICHOACÁN, SOUTHWESTERN MEXICO Rodolfo Corona-Esquivel1, Fernando Ortega-Gutiérrez1, Margarita Reyes-Salas1, Rufino Lozano-Santacruz1, and Miguel Angel Miranda-Gasca2 ABSTRACT In this work we describe for the first time the mineralogy and very briefly the possible origin of a banded Fe-Mn deposit associated with a Cretaceous volcanosedimentary sequence of the southern Guerrero terrane, near the sulfide massive volcanogenic deposit of La Minita. The deposit is confined within a felsic tuff unit; about 10 meters thick where sampled for chemical analysis. Using XRF, EDS and XRD techniques, we found besides todorokite, cryptomelane, quartz, romanechite (psilomelane), birnessite, illite-muscovite, cristobalite, chlorite, barite, halloysite, woodruffite, nacrite or kaolinite, and possibly hollandite-ferrian, as well as an amorphous material and two unknown manganese phases. -
Alexander Von Humboldt: Dilletante of Natural History Or Oracle of Modern Science?
Geophysical Research Abstracts Vol. 21, EGU2019-3798, 2019 EGU General Assembly 2019 © Author(s) 2019. CC Attribution 4.0 license. Alexander von Humboldt: Dilletante of Natural History or Oracle of Modern Science? A.M. Celâl ¸Sengör ITU Eurasia Institute of Earth Sciences, Turkey ([email protected]) When the German satirist and journalist Alexander Moskowski interviewed Einstein in 1920 and implied that in Einstein’s Valhalla of scientific geniuses Alexander von Humboldt surely had a place, he was taken aback with the surprising denial: ‘At least Alexander von Humboldt I do not count among the geniuses. One has to realise that when we today look back upon the great discoverers, Humboldt hardly comes to mind.’ Writing to his friend Joseph Dalton Hooker, Darwin was more appreciative, but essentially made the same point: ‘I believe that you are fully right in calling Humboldt the greatest scientific traveller who ever lived. His Geology is funny stuff; but that merely means that he was not in advance of his age. I should say he was wonderful, more for his near approach to omniscience than for originality. Whether or not his position as a scientific man is as eminent as we think, you might truly call him the parent of a grand progeny of scientific travellers, who, taken together, have done much for science.’ Was Humboldt, the greatest geographer ever, only a wandering dilletante who amassed a vast amount of knowledge or did Darwin and Einstein miss something in him that made him a true oracle of modern science, a genius who saw farther than others in his time? Darwin did not live long enough to be able to read Suess’ Face of the Earth and Einstein probably never perused it as it was too far afield for him. -
Washington State Minerals Checklist
Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite -
Mineral Processing
Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19 -
Benchmark 3: Evaluation of Alternatives with Respect to Existing Conditions August 2015
Salton Sea Funding and Feasibility Action Plan Benchmark 3: Evaluation of Alternatives With Respect to Existing Conditions August 2015 Prepared by: Prepared for: This document is prepared as a living document for public review and comment. Comments may be provided to: Salton Sea Authority 82995 Hwy 111, Suite 200 Indio, CA 92201 Email: [email protected] Comments will be reviewed and incorporated as appropriate. If substantive comments are received, a revised document may be produced and distributed. Preferred citation: Salton Sea Authority (2015). Salton Sea Funding and Feasibility Action Plan Benchmark 3 Report: Evaluation of Alternatives With Respect to Existing Conditions, August Report. Revision Record Revisions to this document will be reviewed and approved through the same level of authority as the original document. All changes to the Benchmark 3 Report must be authorized by the Principal in Charge. Date Version Changes January Working Posted on Salton Sea Authority website. 2015 Draft Included changes from draft review by Salton Sea TCT. June 2015 First Updated hydrology section and inflow Complete projections including Figures 48-52, along with Document editorial revisions. August Revision 1 Added this Revision Record. Corrected title of 2015 California Department of Fish and Wildlife and other minor editorial revisions. Updated discussion of historical flows from 2003-present. Tetra Tech, Inc. i August 2015 Executive Summary This report presents a review of Salton Sea restoration alternatives and their components and determine how well they would perform under current and future inflows. Alternatives are considered with respect to existing hydrologic conditions at the Sea, as of 2014, and projected future hydrology. -
From: John Mcphee Basin and Range EXCERPT on AN
From green meadow beside it, and dry russet uplands rising behind. I said I thought that was lovely. He said yes, it was Basin and Range lovely indeed, it was one of the loveliest angular by John McPhee unconformities I was ever likely to see. © 1980, 1981 The Noonday Press, New York The river turned in our direction after bending by a wall of its canyon, and the wall had eroded so unevenly [Excerpt on an “Angular Unconformity” that a prominent remnant now stood on its own as a steep and some history of the founding six-hundred-foot hill. It made a mammary silhouette of the Science of Geology] against the sky. My mind worked its way through that image, but still I was not seeing what Deffeyes was seeing. Finally, I took it in. More junipers and rubble and minor Interstate 80, in its complete traverse of the North creases of erosion had helped withhold the story from my American continent, goes through much open space and eye. The hill, structurally, consisted of two distinct rock three tunnels. As it happens, one tunnel passes through formations, awry to each other, awry to the gyroscope of young rock, another through middle-aged rock, and the the earth—just stuck together there like two artistic third through rock that is fairly old, at least with respect to impulses in a pointedly haphazard collage. Both the rock now on earth which has not long since been formations were of stratified rock, sedimentary rock, put recycled. At Green River, Wyoming, the road goes under a down originally in and beside the sea, where they had lain, remnant of the bed of a good-sized Cenozoic lake. -
Consequences of Drying Lake Systems Around the World
Consequences of Drying Lake Systems around the World Prepared for: State of Utah Great Salt Lake Advisory Council Prepared by: AECOM February 15, 2019 Consequences of Drying Lake Systems around the World Table of Contents EXECUTIVE SUMMARY ..................................................................... 5 I. INTRODUCTION ...................................................................... 13 II. CONTEXT ................................................................................. 13 III. APPROACH ............................................................................. 16 IV. CASE STUDIES OF DRYING LAKE SYSTEMS ...................... 17 1. LAKE URMIA ..................................................................................................... 17 a) Overview of Lake Characteristics .................................................................... 18 b) Economic Consequences ............................................................................... 19 c) Social Consequences ..................................................................................... 20 d) Environmental Consequences ........................................................................ 21 e) Relevance to Great Salt Lake ......................................................................... 21 2. ARAL SEA ........................................................................................................ 22 a) Overview of Lake Characteristics .................................................................... 22 b) Economic -
Lled Basins of the Red
Deep-Sea Research I 46 (1999) 1779}1792 Hydrographic changes during 20 years in the brine-"lled basins of the Red Sea Pierre Anschutz! *,GeH rard Blanc!, Fabienne Chatin", Magali Geiller", Marie-Claire Pierret" !De& partement de Ge& ologie et Oce&anographie (D.G.O.), Universite& Bordeaux 1, CNRS UMR 5805, 33405 Talence Cedex, France "Centre de Ge& ochimie de la Surface, Institut de Ge&ologie, Universite& Louis Pasteur, CNRS UMR 7517, 67084, Strasbourg, France Received 16 June 1998; accepted 8 February 1999 Abstract Many of the deep basins "lled by hot brines in the Red Sea have not been investigated since their discovery in the early 1970s. Twenty years later, in September 1992, six of these deeps were revisited. The temperature and salinity of the Suakin, Port Sudan, Chain B, and Nereus deeps ranged from 23.25 to 44.603C and from 144 to 270&. These values were approximately the same in 1972, indicating that the budget of heat and salt was quite balanced. We measured strong gradients of properties in the transition zone between brines and overlying seawater. The contribution of salinity to the density gradient was more than one order of magnitude higher than the opposite contribution of temperature across the seawater}brine interface. Therefore the interface was extemely stable, and the transfer of properties across it was considered to be controlled mostly by molecular di!usion. We calculate that the di!usional transport of salt from the brines to seawater cannot a!ect signi"cantly the salinity of the brines over a 20 year period, which agrees with the observations. -
Ocean Drilling Program Scientific Results Volume
9. GEOCHEMICAL EXPRESSION OF EARLY DIAGENESIS IN MIDDLE EOCENE-LOWER OLIGOCENE PELAGIC SEDIMENTS IN THE SOUTHERN LABRADOR SEA, SITE 647, ODP LEG 1051 M. A. Arthur,2 W. E. Dean,3 J. C. Zachos,2 M. Kaminski,4 S. Hagerty Rieg,2 and K. Elmstrom2 ABSTRACT Geochemical analyses of the middle Eocene through lower Oligocene lithologic Unit IIIC (260-518 meters below seafloor [mbsf]) indicate a relatively constant geochemical composition of the detrital fraction throughout this deposi tional interval at Ocean Drilling Program (ODP) Site 647 in the southern Labrador Sea. The main variability occurs in redox-sensitive elements (e.g., iron, manganese, and phosphorus), which may be related to early diagenetic mobility in anaerobic pore waters during bacterial decomposition of organic matter. Initial preservation of organic matter was me diated by high sedimentation rates (36 m/m.y.). High iron (Fe) and manganese (Mn) contents are associated with car bonate concretions of siderite, manganosiderite, and rhodochrosite. These concretions probably formed in response to elevated pore-water alkalinity and total dissolved carbon dioxide (C02) concentrations resulting from bacterial sulfate reduction, as indicated by nodule stable-isotope compositions and pore-water geochemistry. These nodules differ from those found in upper Cenozoic hemipelagic sequences in that they are not associated with methanogenesis. Phosphate minerals (carbonate-fluorapatite) precipitated in some intervals, probably as the result of desorption of phosphorus from iron and manganese during reduction. The bulk chemical composition of the sediments differs little from that of North Atlantic Quaternary abyssal red clays, but may contain a minor hydrothermal component. The silicon/ aluminum (Si/Al) ratio, however, is high and variable and probably reflects original variations in biogenic opal, much of which is now altered to smectite and/or opal CT. -
Meteoric Be and Be As Process Tracers in the Environment
Chapter 5 Meteoric 7Be and 10Be as Process Tracers in the Environment James M. Kaste and Mark Baskaran 7 10 Abstract Be (T1/2 ¼ 53 days) and Be (T1/2 ¼ occurring Be isotopes of use to Earth scientists are the 7 1.4 Ma) form via natural cosmogenic reactions in the short-lived Be (T1/2 ¼ 53.1 days) and the longer- 10 atmosphere and are delivered to Earth’s surface by wet lived Be (T1/2 ¼ 1.4 Ma; Nishiizumi et al. 2007). and dry deposition. The distinct source term and near- Because cosmic rays that cause the initial cascade of constant fallout of these radionuclides onto soils, vege- neutrons and protons in the upper atmosphere respon- tation, waters, ice, and sediments makes them valuable sible for the spallation reactions are attenuated by tracers of a wide range of environmental processes the mass of the atmosphere itself, production rates of operating over timescales from weeks to millions of comsogenic Be are three orders of magnitude higher in years. Beryllium tends to form strong bonds with oxygen the stratosphere than they are at sea-level (Masarik and atoms, so 7Be and 10Be adsorb rapidly to organic and Beer 1999, 2009). Most of the production of cosmo- inorganic solid phases in the terrestrial and marine envi- genic Be therefore occurs in the upper atmosphere ronment. Thus, cosmogenic isotopes of beryllium can be (5–30 km), although there is trace, but measurable used to quantify surface age, sediment source, mixing production as oxygen atoms in minerals at the Earth’s rates, and particle residence and transit times in soils, surface are spallated (in situ produced; see Lal 2011, streams, lakes, and the oceans. -
Tin, Tungsten, and Tantalum Deposits of South Dakota
TIN, TUNGSTEN, AND TANTALUM DEPOSITS OF SOUTH DAKOTA. By FRANK L. HESS. INTRODUCTION. Many articles have been written 011 the tin deposits of the Black Hills, and an excellent paper by J. D. Irving a on the tungsten deposits at Lead was published in 1901. Nothing is known to have been pub lished on the tungsten deposits of the southern Black Hills, but several articles have been written on the deposits of tantalum. Nearly all the papers on these different deposits, however, are a num ber of years old, and later developments have given several of the deposits an aspect somewhat different from their appearance at the time they were described. It therefore seems well to give a brief account of observations made by the writer during a short reconnais sance trip in September, 1908, together with such reviews of the his tory and the literature of the region as may seem advisable. All the known deposits of tin, tungsten, and tantalum in South Dakota occur in the Black Hills, in Lawrence and Pennington coun ties, in the southwestern part of the State. Although designated as "hills," these elevations reach a height of 7,216 feet in Harney Peak, 500 feet above the highest of the Appalachians (Mount Mitchell, 6,711 feet) and almost a thousand feet above the highest of the White Mountains (Mount Washington, 6,279 feet). They are about 60 to 75 miles long by 50 miles wide, the longer axis lying nearly north and south. There is a considerable diversity of topography in the different parts of the area to be considered.