4 edition of The chemistry of clay minerals found in the catalog.
The chemistry of clay minerals
Weaver, Charles E.
Bibliography: p. -205.
|Statement||by Charles E. Weaver and Lin D. Pollard.|
|Series||Developments in sedimentology,, 15|
|Contributions||Pollard, Lin D. 1937- joint author.|
|LC Classifications||QE389.625 .W4|
|The Physical Object|
|Pagination||viii, 213 p.|
|Number of Pages||213|
|LC Control Number||72083214|
The properties and behavior of Fe oxides, Fe-bearing clay minerals, and other Fe minerals in soils are then described, and the text ends with a summary of the role of Fe in soil-forming processes. A Table of Contents and subject index are provided to assist the reader in finding specific topics within the text. Clay Minerals The layer minerals contain one tetrahedral and one octahedral sheet in their basic structural unit (Fig. 2.) This two-sheet mineral type is represented by the kaolin group, with the general formula Al2Si(0H)4. Kaolinite, the most common mineral in this group, is dioctahedral, exhibiting Al3+ octahedral and Si4.
Online shopping for Mineralogy - Chemistry from a great selection at Books Store. Online shopping for Mineralogy - Chemistry from a great selection at Books Store. Skip to main content. Try Prime Hello, X-Ray Diffraction and the Identification and Analysis of Clay Minerals 10 Apr by Duane M. Moore and Robert C. Reynolds Jr. Spiral-bound.4/5. Mineral Group: Kaolinite-serpentine group. Occurrence: Replaces other aluminosilicate minerals during hydrothermal alteration and weathering. A common constituent of the clay-size fraction of sediments, where it may be formed by direct precipitation. Association: Quartz, feldspar, Size: 75KB.
gite minerals may be much slower than in platy minerals. This would be expected if the ions along the channel must diff'use into the solution phase to reach an equilib rium. lllite Group. The illite group of clay minerals are small particle size, plate-shaped clay minerals distin guished by their ability to fix potassium irreversiblj^ The. This book on Clays and Clay Minerals is related research reports conducted by the Geological Survey of Finland. One can look at the book as dealing with seven chapters: (l) Identification and occurrence of clays, (2) structure and composition of the clay minerals, (3) physical and geochemical properties of clay minerals, (4) methods ofFile Size: 6MB.
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Purchase The Chemistry of Clay Minerals, Volume 15 - 1st Edition. Print Book & E-Book. ISBNBook Edition: 1. The chemistry of clay minerals, Volume 15 (Developments in Sedimentology) by Author Unknown (Editor).
Introduction to Clay Minerals: Chemistry, origins, uses and environmental significance (Routledge Geography and Envirmnt) Softcover reprint of the original 1st ed.
Edition. Why is ISBN important. This bar-code number lets you verify that you're getting exactly the right version or edition of a by: The Hardcover of the Chemistry of Clay Minerals by C.
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Surface and Interface Chemistry of Clay Minerals, Volume 9, delivers a fundamental understanding of the surface and interface chemistry of clay minerals, thus serving as a valuable resource for researchers active in the fields of materials chemistry and sustainable chemistry.
Clay minerals, with surfaces ranging from hydrophilic, to hydrophobic, are widely studied and used as adsorbents. Book Review: The chemistry of clay minerals. C.E. Weaver and L.D.
Pollard. Elsevier, Amsterdam,pp., Dfl. Author: H. Murray. Chemistry of clays and clay minerals. Newman. Wiley, - Science - pages. 0 Reviews. Bringing together information widely distributed throughout scientific and industrial.
Introduction to Clay Minerals is designed to give a detailed, concise and clear introduction to clay mineralogy. Using the information presented here, one should be able to understand clays and their mineralogy, their uses and importance in modern life.
ISBN: OCLC Number: Description: pages: illustrations ; 26 cm. Contents: The chemical constitution of clays / A.C.D. Newman and G. Brown --Non-silicate oxides and hydroxides / R.M. Taylor --Dispersion and flocculation / H. van Olphen --Cation exchange equilibria in clays / H. Laudelout --The interaction of water with clay mineral survaces / A.C.D.
Newman. Surface and Interface Chemistry of Clay Minerals. Edited by R. Schoonheydt, C.T. Johnston, F. Bergaya. Volume 9, Determination of surface areas and textural properties of clay minerals. Book chapter Full text access 2 - Determination of surface areas and textural properties of clay minerals.
Regarding the surface chemistry of oil-sands clay minerals, the relevant length scales of the atomic and mineral constituents plotted on a logarithmic scale of nanometers (10 – 9 m) are shown in Figure the size range of clay minerals and the ions associated with the surfaces (e.g.
Na +, K +, Ca 2+, and Mg 2+). Our approach is from mineral chemistry and hence has greatly benefited from disc- sions with people who know soils and plants. The project of this book was realized and encouraged with the help of Wolfgang Engel who, unfortunately is not with us to see its finalization.
We greatly regret his passing. The clay minerals attapulgite and sepiolite have columnar structural features and are less common than the layered clay minerals. Clay mineral particles can have variable degrees of long-range order (crystallinity); they can be platy or fibrous and, although sub-millimetric in size, vary from nanoparticles to grains observable under a.
CHEMISTRY OF CLAYS. clay substance from the sand or quartz. The aiCtion upO'n im pure quartz of a dilute sO'lution of sodium hydrate 0'1' sodium carbonate, furnishes means fO'r separating the quartz from the amorphous silica.
The action of sulfuric acid and the alkali has given rise to a method O'f analysis, which is knO'wn as rationalCited by: This diversity in properties and the possibility to tune the surface properties of clay minerals to match the properties of adsorbed molecules is the basis for study. This book requires a fundamental understanding of the surface and interface chemistry of clay minerals, and of the interaction between adsorbate and adsorbent.
Clay mineral - Clay mineral - Chemical and physical properties: Depending on deficiency in the positive or negative charge balance (locally or overall) of mineral structures, clay minerals are able to adsorb certain cations and anions and retain them around the outside of the structural unit in an exchangeable state, generally without affecting the basic silicate structure.
Open Library is an open, editable library catalog, building towards a web page for every book ever published. Chemistry of clays and clay minerals by,Longman Scientific & Technical edition, in EnglishPages: Book Overview Bringing together information widely distributed throughout scientific and industrial journals, here is an overview of the chemical consititution and properties of clay minerals and the environmental conditions that lead to their formation.
This book is composed of 42 chapters and begins with descriptions of the mechanical, structural, thermodynamic, physical, and thermal properties of clay minerals.
The succeeding chapters are devoted to certain reactions, theoretical and experimental aspects, occurrence, formation, and sorption properties of these minerals. The chemistry of this type of healing clay reveals many similarities to the smectites, although the two clays are truly strikingly different: (K, H)Al2(Si, Al)4O10(OH)2 - xH2O.
Although Illite is an aluminum silicate, it is a non-swelling clay. Illite has the same range of use as the smectite clays. Clay minerals are hydrous aluminium phyllosilicates, sometimes with variable amounts of iron, magnesium, alkali metals, alkaline earths, and other cations found on or near some planetary surfaces.
Clay minerals form in the presence of water and have been important to life, and many theories of abiogenesis involve them.
They are important constituents of soils, and have been useful to humans.Closer Look at Clay Minerals: What It's Made of: Kaolin, or pure clay, is known by the chemical formula Al2O32SiO22H2O.
Dough Clays Dough Clays are made primarily of the following things: Because this clay needs to be both pliable and sturdy, it needs a good material to bind.Chemistry of clays and clay minerals. New York: Wiley ; London, England: Mineralogical Society, (OCoLC) Document Type: Book: All Authors / Contributors: A C D Newman.