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Редактор(ы):Clauer N., Paquet H.
Издание:Springer, 1997 г., 208 стр., ISBN: 978-3-642-64443-6
Язык(и)Английский
Soils and sediments. Mineralogy and geochemistry / Почвы и осадки. Минералогия и геохимия

Since Georges MiHot's initial contribution to clays and his thesis on the relationship between composition and development of sedimentary clayey rocks defended in 1949, half a century has passed by. So much has been discovered on clays during that period that it would almost be impossible either to list the work undertaken or to give a comprehensive account of the present situation in a concise presentation.

Автор(ы):Crouse D.A., Moorberg C.J.
Издание:2017 г., 147 стр.
Язык(и)Английский
Soils laboratory manual / Лабораторное руководство по изучению почв

Several instructors have contributed to the evolution of this laboratory manual over the years. Contributors include, alphabetically, Maurice G. Cook, Emeritus Professor of Soil Science, North Carolina State University; David A. Crouse, Associate Professor of Soil Science, North Carolina State University; Larry D. King, Emeritus Professor of Soil Science, North Carolina State University; H. Joseph Kleiss, Emeritus Professor of Soil Science, North Carolina State University; Colby J. Moorberg, Assistant Professor of Soil Science, Kansas State University; Lloyd Stone, Emeritus Professor of Agronomy, Kansas State University; and James A. Thompson, Professor of Soil Science, West Virginia University. Editorial support was provided by Nora Ransom. Contributions were also made by countless graduate teaching assistants over the development of the manual. Funding was provided by the Kansas State University Open/Alternative Textbook Initiative. This is contribution no. 18-128-B of the Kansas Agricultural Experiment Station <...>

Автор(ы):Anderson S., Schaetzl R.
Издание:Cambridge University Press, Cambridge, 2005 г., 833 стр.
Язык(и)Английский
Soils. Genesis and geomorphology / Почвы. Генезис и геоморфология

Soils: Genesis and Geomorphology is a comprehensive and accessible textbook on all aspects of soils.

The book’s introductory chapters on soil morphology, physics, mineralogy and organisms prepare the reader for the more advanced and thorough treatment that follows. Unlike other books on soils, the authors devote considerable space to discussions of soil parent materials and soil mixing (pedotur-bation), along with dating and paleoenvironmen-tal reconstruction techniques. Theory and processes of soil genesis and geomorphology form the backbone of the book, rather than the emphasis on soil classification that permeates other soils textbooks. This refreshingly readable text takes a truly global perspective, with many examples from around the world sprinkled throughout.

Автор(ы):Kanas N.
Издание:Springer, 2014 г., 352 стр., ISBN: 978-1-4614-0895-6
Язык(и)Английский
Solar system maps: From antiquity to the space age / Карта солнечной системы. От античности до космической эры

In 1543, Nicolaus Copemicus iuvenled the solar system. "Hold on!" you say. Surely the solar system had been there forever, and Copemicus didn't just iuvent it. Yes and no! What Copemicus had revealed and iuvented was the arrangement of the planets-a stunningly new way of mappiug them. He revolutionized the way humankind would conceive of the planets as a system, controlled by the Sun. "Thus iudeed," Copernicus wrote, "the sun, as though sealed on a royal throne, governs the family of planets revolving around it." Nick Kanas has documented this revolutionary shift iu his ingeniously illustrated album of solar system images, all historical even though the modern views, ''postcards from space", are scarcely a few decades old.

Автор(ы):Tarleton E.S., Wakeman R.J.
Издание:Elsevier, 2007 г., 464 стр., ISBN: 978-1-85-617421-3
Язык(и)Английский
Solid/Liquid separation: Equipment selection and process design / Разделение твердых и жидких частиц: выбор оборудования и проектирование технологического процесса

Over the years manufacturers have developed many generic forms of solid/liquid separator. The need to compete in the marketplace and gain a competitive edge, however, has led manufacturers to develop a plethora of variants. Rather than detailing all of these variants, this chapter attempts to give a descriptive overview of the generic equipment types and the main alternatives available to the design engineer (see Figure 1.1).

Автор(ы):Moyers A.
Издание:University of Arkansas, Fayetteville, 2015 г., 86 стр.
Язык(и)Английский
Source constraints of ore metals in Mississippi Valley-type deposits in central and eastern Tennessee using Pb Isotopes / Ограничения по источникам получения рудных металлов на месторождениях типа долины Миссисипи в центральном и восточном Теннесси

The Mississippi Valley-Type (MVT) Central and East Tennessee (TN) Districts contain economically significant lead-zinc deposits that occur in the Early Ordovician carbonates of the Knox Group. Although both districts share similar host rock, have similar temperatures of formation, and typically fill open spaces of collapse breccias or replace their host carbonates, previous studies may suggest that these ores did not form from the same mineralizing fluids and may have different Pb sources.

Выпуск 98
Издание:Economic geology, 2003 г., 12 стр.
Язык(и)Английский
Source of iron for sulfidation and gold deposition, Twin Creeks carlin-type deposit, Nevada

This study was undertaken to determine the source of iron in Comus Formation sedimentary rocks that were sulfidized during deposition of gold in the Megapit area of the Twin Creeks Carlin-type deposit. Sedimentary rocks in and near the Megapit contain ferroan dolomite, largely as overgrowths on iron-poor dolomite. Iron to form these overgrowths appears to have been released from mafic volcanic rocks that are interlayered with the sedimentary rocks. These igneous rocks have undergone two stages of hydrothermal alteration. The first stage involved formation of albite and iron-rich chlorite, possibly caused by interaction with seawater. The second stage involved destruction of the iron-rich chlorite by illite or sericite, which released iron to form ferroan dolomite in the sedimentary rocks. Comparisons show that transfer of iron from the igneous rocks to the sedimentary rocks can account for the present distributions of iron in these rocks. Relative to basalts, Comus Formation igneous rocks are enriched in iron and potassium. These results suggest that ferroan dolomite in sedimentary rocks is not solely a product of diagenetic processes and can form when iron is released from adjacent iron-bearing igneous rocks. Recognition of this additional mechanism for formation of ferroan dolomite expands the range of geologic settings that can be favorable for formation of gold deposits formed by sulfidation.

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