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Издание:Springer, 2010 г., 311 стр., ISBN: 978-90-481-2998-0
Язык(и)Английский
Radiogenic isotopes in geologic processes / Радиогенные изотопы в геологических процессах

Do we actually understand geologic processes? New technology brings new information and perceptions, which sometimes overturn imaginations based on simple observation and estimation, in conjunction with common sense inference. In 1902– 1904, Pierre Curie and Ernest Rutherford first formulated the idea of using radioactive transformation of nuclides as a geologic chronometer. After a century of working with such tools, geology has advanced from a descriptive science to an analytic science that formulates conclusions based on exact values. The technology of radiogenic isotope geology has created a branch of science that considers the Earth as a planet generated within a Solar system and studies the subsequent evolution of geologic processes that has resulted in the present formation of our planet’s continents and oceans.<...>

Редактор(ы):Rull F., Caumon M.-C., Dubessy I.
Издание:The Mieralogical Society of Great Britain and Ireland, London, 2012 г., 504 стр., ISBN: 978-0-903056-31-1
Язык(и)Английский
Raman Spectroscopy applied to the Eath Sciences and Cultural Heritage

In Earth Sciences and Cultural Heritage Science we can only understand the formation of the 'objects' if they are well characterized. Optical observation, including optical microscopy, is still the primary tool and is essential in obtaining a preliminary, qualitative determination of an object, to determine the relations between it and other objects, and to place it in a general context. Most of the time, however, optical observations are insufficient. Spectroscopic methods are the second "set of eyes" used to gain greater insight into these objects and to use physical chemistry, if applicable, to derive the mechanisms of formation. Spectroscopic methods are numerous and have been described in a previous volume (6) in the EMU Notes in Mineralogy series, edited by A. Beran & E. Libowitzky (2004).

Источник:Geo.web.ru
Автор(ы):Grauch R.I., Orris G.J.
Издание:2002 г., 173 стр.
Язык(и)Английский
Rare earth element mines, deposits, and occurrences / Рудники, месторождения и рудопроявления редкоземельных элементов

Data on rare earth (including yttrium) mines, deposits, and occurrences were compiled as part of an effort by the USGS and the University of Arizona Center for Mineral Resources to summarize current knowledge on the supply and demand outlook and related topics for this group of elements. Economic competition and environmental concerns are increasingly constraining the mining and processing of rare earths from the Mountain Pass mine in California. For many years, the deposit at Mountain Pass was the world's dominant source of rare earth elements and the United States was essentially self-sufficient. Starting approximately 10 years ago, the U.S. has become increasingly dependent (> 90 percent of separated rare earths) upon imports from China, now the dominant source of rare earths. Knowledge of the known economic and noneconomic sources of rare earths is basic to evaluating the outlook  for rare earth upply and associated issues. <...>

Автор(ы):Леснов Ф.П.
Издание:CRC Press, 2010 г., 586 стр., ISBN: 978-0-415-57890-5
Язык(и)Английский (перевод с русского)
Rare earth elements in ultramafic and mafic rocks and their minerals. Main types of rocks. Rock-forming minerals / Редкоземельные элементы в ультраосновных и основных породах и их минералах. Главные породы. Породообразующие минералы

This monograph is the generalization of up-to-date data and theoretical ideas on the problems of the geochemistry of rare earth elements (REE) in ultramafic and mafic rocks as well as in their minerals. As is the convention in the Russian, URSS literature, by the term “rare earth elements’’ or REE, we mean, after Henderson (Rare Earth Element Geochemistry, 1984), the chemical elements of Group IIIA of the Periodic Table of Elements from lanthanum to lutetium with atomic numbers from 57 to 71: La, Ce, Pr, Nd, Pm, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, and Lu. For brevity, this group of elements is sometimes referred to as “lanthanides’’ (Solodov et al., 1998).

Издание:Elsevier, 2015 г., 10 стр.
Язык(и)Английский
Rare earth elements: industrial applications and economic dependency of Europe / Редкоземельные элементы: промышленное применение и экономическая зависимость Европы

Rare Earth Oxides are used in mature markets (such as catalysts, glassmaking and metallurgy), which account for 59% of the total worldwide consumption of rare earth elements, and in newer, high-growth markets (such as battery alloys, ceramics, and permanent magnets), which account for 41% of the total worldwide consumption of rare earth elements.

Автор(ы):Humphries M.
Издание:CRC Report for congress, 2012 г., 30 стр.
Язык(и)Английский
Rare earth elements: The global supply chain / Редкоземельные элементы: Глобальная цепочка поставок

The concentration of production of rare earth elements (REEs) outside the United States raises the important issue of supply vulnerability. REEs are used for new energy technologies and national security applications. Is the United States vulnerable to supply disruptions of REEs? Are these elements essential to U.S. national security and economic well-being?
There are 17 rare earth elements (REEs), 15 within the chemical group called lanthanides, plus yttrium and scandium. The lanthanides consist of the following: lanthanum, cerium, praseodymium, neodymium, promethium, samarium, europium, gadolinium, terbium, dysprosium, holmium, erbium, thulium, ytterbium, and lutetium. Rare earths are moderately abundant in the earth’s crust, some even more abundant than copper, lead, gold, and platinum.

Издание:Journal of Geochemical Exploration, 1998 г., 17 стр.
Язык(и)Английский
Readsorption of gold during selective extraction — observations and potential solutions

This paper describes a soil extraction method developed to investigate the different chemistries of Au in various soils in the Yilgarn Craton. The extraction solution is 1 M sodium bicarbonater0.1 M potassium iodide, saturated with CO2 and adjusted to pH 7.4 with hydrochloric acid. A soil : solution ratio of 1 : 2 Žg : ml. is used. Two different methods were used: Ž1. net iodide-extractable Au, with solutions analysed directly for Au; Ž2. gross iodide-soluble Au, where activated carbon is added to the mixture and the carbon analysed at the end of the extraction, thus providing a measure of all Au dissolved during the extraction Žincluding that readsorbed during the net extraction.. Depending on the extraction conditions, there may be appreciable readsorption of Au, particularly for organic-rich ŽG50%. and Fe-rich lateritic soils Ž)80%.. This readsorption is enhanced by pulverizing to -75 mm. Consequently, for simple extractions longer than 1 day, pulverized soils give lower apparent Au solubility than do unpulverized soils. Unpulverized carbonate-rich soils show high Au solubilities and little Žoften -20%. readsorption, and consequently show high net iodide-solubilities. These readsorption phenomena could affect other methods used in exploration and should be thoroughly investigated before incorrect conclusions are drawn. The readsorption problems are removed by adding activated carbon to the extraction mixtures; the carbon adsorbs Au as it is dissolved from the sample and is subsequently analysed. However, different soil types still show distinctly different Au solubilities, which should be recognized for interpretation of extraction results. Again, this effect should be tested for other extraction techniques. A more intractable problem may be that biological cycling of the Au through plants and other organisms appears to cause high Au solubilities in many soils. This effect may obscure any potential ‘mineralization signature’ that is being tested by selective extractions, and could cause problems for any extraction method, no matter how well designed

Редактор(ы):LeVier M., Malhotra D., Spiller E., Taylor P.R.
Издание:Society for Mining Metallurgy and Exploration Inc., 2009 г., 586 стр., ISBN: 978-0-87335-318-2
Язык(и)Английский
Recent advances in mineral processing plant design / Последние достижения в проектировании установок по переработке полезных ископаемых

In 1963 the Chairman of Metallurgical Engineering at Queen’s University of Kingston, Ontario, Canada encouraged me to apply for a position in his department. This led to an appointment as an Assistant Professor of Metallurgical Engineering with a mandate to teach undergraduate and graduate courses in Mineral Process Engineering. Graduating metallurgists take positions available to them in the mining industry and mill “metallurgists” were in strong demand. Discussions with industry-oriented colleagues at the Department of Energy, Mines and Resources (Mines Branch) and with senior operators and plant design personnel at conferences such as the Conference of Metallurgists provided details of jobs available Canada-wide. This helped to fortify course content.

Автор(ы):Rey J.
Издание:Laboratoire de Geologie de L'Universite Paul Sabatier, Toulouse, 1972 г., 573 стр.
Язык(и)Французский
Recherches géologiques sur le Crétacé inférieur de L'Estramadura (Portugal) / Геологические исследования нижнего мела Эстрамадура (Португалия)

Le Crétacé inférieur de l’Estramadura, au Portugal, m’apparaissait, lorsque j’en entrepris l'étude, comme un thème de recherches à la fois séduisant et redoutable. Séduisant, car tout examen systématique avait été abandonné depuis plus de soixante ans, en dépit de la présence de classiques ensembles stratigraphiques, de la richesse des faunes et de la variété des faciès. Redoutable, car il m’amenait à suivre les traces de cet illustre géologue que fut Choffat. Il était bien évident que je ne pouvais mener cette tâche à son terme que grâce à de nombreux et bienveillants appuis. J’en ai largement bénéficié, sinon même abusé. Il m’est donc particulièrement agréable de remercier aujourd’hui tous ceux qui, durant les longues années de travail, m’ont aidé, conseillé et encouragé. <...>

Автор(ы):Casteras M.
Издание:Laboratoire de Geologie de L'Universite Paul Sabatier, Toulouse, 1972 г., 575 стр.
Язык(и)Португальский
Recherches geologiques sur le cretace inferieur de LEstramadura (Portugal)

Le Crétacé inférieur de LEstramadura, au Portugal, m'apparaissait, lors-que j'en entrepris Vêtude, comme un thème de recherches à la fois séduisant et redoutable. Séduisant, car tout examen systématique avait été abandonné depuis plus de soixante ans, en dépit de la présence de classiques ensembles stratigraphiques, de la richesse des faunes et de la variété des fácies. Redoutable, car il m'amenait à suivre les traces de cet illustre géologue que fut Choffat. II était bien évident que je ne pouvais mener cette tache à son terme que grâce à de nombreux et bienveillants appuis. I'en ai large-ment beneficie, sinon même abuse. II m'est donc particulièrement agréable de remercier aujourd'hui tous ceux qui, durant les longues années de travail, m'ont aidé, conseillé et encouragé

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