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Books > Science & Mathematics > Chemistry > Mineralogy
Mineral resource estimation has changed considerably in the past 25
years: geostatistical techniques have become commonplace and
continue to evolve; computational horsepower has revolutionized all
facets of numerical modeling; mining and processing operations are
often larger; and uncertainty quantification is becoming standard
practice. Recent books focus on historical methods or details of
geostatistical theory. So there is a growing need to collect and
synthesize the practice of modern mineral resource estimation into
a book for undergraduate students, beginning graduate students, and
young geologists and engineers. It is especially fruitful that this
book is written by authors with years of relevant experience
performing mineral resource estimation and with years of relevant
teaching experience. This comprehensive textbook and reference
fills this need.
Although the great diversity of alkaline rocks, with their tion of
alkaline rocks and carbonatites with rifting has long been
acknowledged. However, many large, diverse relatively exotic
rnineralogies. has always attracted the interest of petrologists,
as have the more recently defined and important provinces are not
widely known, includ carbonatites, it could be argued that little
progress has ing the 20 or so major provinces of the U. S. S. R.
and some of the major concentrations of South America. been made
over the past 50 years towards formulating a comprehensive
petrogenesis of these rocks. It could Although alkaline rocks are
known to be characteristic also be maintained that as the alkaline
varieties have the of stable, intra-plate environments, it is
becoming clear most extreme compositions of all igneous rocks, so
an that they also play an important role in the igneous activity
concentrated at plate margins. In this respect understanding of
their genesis is essential if we are to understand fully the
workings of the solid earth, while also, therefore, it is concluded
that thecollation of all the available regional data can make a
significant contribu a knowledge of the most extreme products of
differentia tion must inevitably cast light on rocks of less
extreme tion to understanding these rocks. compositions. The
importance of academic research on Sorensen (1974) in the Preface
to 'The Alkaline Rocks' these rocks is thus clear."
This book is intended to provide the reader with information
regarding diamond prospecting. It also points out areas to
prospect. I have prospected in this area of Virginia and West
Virginia in the past, but my ill health prevents me doing it
anymore. It's all yours now. Finding diamonds will not be that
difficult, but remember, they should be two carats or larger and
free of flaws to be worth much. You may want to save everything
smaller, too. Some third world company may purchase them from you.
Minerals and Human Health is written in response to the demand for
additional knowledge about global climate change, the industrial
contamination of water reservoirs, and epidemiological intoxication
from industrial hazards related to the use of mineral resources.
The book addresses issues associated with the physical and
geological processes of the Earth, the sustainability and fragility
of the Earth's resources, and the interplay between health,
industrial activities, and environments. It combines mineralogy,
medicine, and the environmental, life, and political sciences to
develop solutions to ease human suffering from geological toxicity.
Minerals and Human Health helps students to understand the Earth's
activities and the unique resources that sustain life and
facilitate industrial progress. The text teaches readers how the
dispersal of geological materials effects the human population.
In-book quizzes allow students to assess their own progress.
Questions for discussion and review encourage critical thinking and
debate and support retention. Minerals and Human Health can be used
in courses on earth and environmental sciences, geopollution, and
geochemistry.
Das bewahrte Lehrbuch der Mineralogie Gregor Markls Buch ist eine
verstandliche Einfuhrung in die Grundlagen der Mineralogie,
Petrologie und Geochemie und richtet sich vor allem an Studierende
geowissenschaftlicher Facher. Am Anfang steht eine reich bebilderte
Beschreibung der wichtigsten Minerale und Gesteine. Dann stellt der
Autor Konzepte und Analysemethoden der Mineralogie vor und erklart
die Bildung und Veranderungen von metamorphen, magmatischen und
sedimentaren Gesteinen. Das Kapitel zur Geochemie beleuchtet die
Chemie des Kosmos, die Entstehung der Elemente, Meteorite sowie die
Zusammensetzung der wichtigsten globalen Reservoire (Erdkern,
-mantel, -kruste, Ozeane, Atmosphare). Eine wichtige Anwendung der
Geochemie ist die Messung von Gehalten an Spurenelementen oder
stabilen und radiogenen Isotopen in Gesteinen zur Rekonstruktion
geologischer Prozesse. Das Lehrbuch besticht durch moderne
Stoffauswahl und -darstellung, ubersichtlich strukturierte und
verstandliche Texte, die gelungene Verbindung von Mineralogie,
Petrologie und Geochemie sowie die grosse Zahl farbiger Fotos und
instruktiver zweifarbiger Grafiken. Studierenden der
Geowissenschaften wird dieses Buch vom Grundstudium bis zum
Bachelorabschluss begleiten. Zugleich bietet es allen, die sich fur
die Erde interessieren, spannende Einblicke in die Wissenschaft von
den Mineralen und Gesteinen.
Here is a state-of-the-art survey of artificial intelligence in
modern exploration programs. Focussing on standard exploration
procedures, the contributions examine the advantages and pitfalls
of using these new techniques, and, in the process, provide new,
more accurate and consistent methods for solving old problems. They
show how expert systems can provide the integration of information
that is essential in the petroleum industry when solving the
complicated questions facing the modern petroleum geoscientist.
By definition, biosphere is the Earth's geological shell populated
by living organisms. Therefore, the biosphere's origin and
evolution are primarily a geological problem. At present geological
problems are solved using methods of physics, chemistry, biology,
and mathematics. The multidisciplinary approach is a basis of this
book. Life origin problems occupy the main part of this book. What
is life, and can we understand its origin and evolution on the
basis of laws of physics and chemistry? A number of works are
dedicated to experimental study of the synthesis of organic
compounds of the prebiotic significance, including ATP and
photoactive systems. The characteristic feature of our scientific
approach is to consider the problem of life origin in the context
of the origin and evolution of the solar system, beginning with the
protoplanetary stage and including the events of the Earth's early
history. The last chapter comprises papers that concern modern
problems and approaches to the study of various aspects of
biological evolution. The present edition is a collection of
articles by scientists representing more than 20 institutes of the
Russian Academy of Sciences and other organisations, joined by the
science program "Problems of Biosphere Origin and Evolution". This
book will be interesting for a wide range of researchers:
physicists, chemists, biologists, mathematicians. The book
represents the stance of the Russian scientific school on the
problem of life origin, which does not always coincide with
opinions of other scientific schools.
Hydroxyapatite is the most widely accepted biomaterial for the
repair and reconstruction of bone tissue defects. It has all the
characteristic features of biomaterials, such as, biocompatible,
bioactive, osteoconductive, non-toxic, non-inflammatory and
non-immunogenic properties. In this book, the authors present
current research in the study of the synthesis, properties and
applications of hydroxyapatites. Topics discussed include
nanodimensional and nanocrystalline hydroxyapatite and other
calcium orthophosphates; application of biomimetic nanocrystalline
apatites in drug delivery and tissue engineering; polymer matrix
mediated synthesis of nano hydroxyapatite crystals;
osteointegration of titanium porous implants with carbon
nanocoating and hydroxyapatite particles into the pores;
hydroxyapatite thin film prepared by sputtering technique for
medical applications; and hydroxyapatite application in dentistry
and maxillofacial surgery.
"The Birth of Opal" is the only book in the English speaking world
that is devoted entirely to the topic of opal formation. It is a
detailed investigative and enlightening account of the formation of
opal both in nature and in the Lab. The investigation includes; the
opal environment, Geography, Geology, Geochemistry, the decay
cycle, soil reactions, the effect of salts and chemical reactions
that result in "The Birth of Opal." Outside of Russia, "The Birth
of Opal" is the most complete book about opal genesis in the world.
It is a world first in its class. It dispels the myths and mystery
that has surrounded the formation of opal for centuries. All those
who love gemstones, or geology and are fascinated by opal in
particular or are curious about its true origins will finally find
the answers in this book. It is a must have for Schools, Colleges,
Universities, and Libraries everywhere. Get your copy now
A method of treating a kaolin particulate material to improve its
properties by removal of impurity particles thereform, to improve
the brightness, and whiteness and other properties. Method of
treating raw kaolin clay for preparing nanoparticles of kaolin clay
to replace titanium dioxide in water based coatings, and for use as
an adsorbent for the removal of toxic heavy metal ions such as
lead, zinc, cadmium, cobalt, copper, and chromium ions from aqueous
solutions. A method includes: (a) removing colored impurities by
treating pulverized kaolin clay with diluted hydrochloric acid, (b)
Producing a dispersed aqueous suspension of a kaolin particulate
material containing at least 0.1 % by weight based on the dry
weight of the kaolin deflocculated by sodium polyphosphate (c)
Dispersed aqueous suspension may have a solids content kaolin
particles of 20-30 % by weight and this suspension is subjected to
evaporation to have a solids content of 70-75%, and (d) producing
nanoparticles of kaolin clay by dispersing in water-ethanol
mixture.
In this edition, most of the commonly occurring minerals of
igneous, metamorphic and sedimentary rocks are discussed in terms
of structure, chemistry, optical and other physical properties,
distinguishing features and paragenesis. Important correlations
between these aspects of mineralogy are emphasized wherever
possible. The content of each section has been updated where needed
in the light of published research over the 21 years between
editions. Tables of over 200 chemical analyses and formulae are
included and a number of older entries have been replaced by more
recent examples. Major new features: Entirely new views of crystal
structures in perspective using CrystalMaker colour images; Over 60
colour photographs of minerals in thin sections of rocks under the
petrological microscope; Considerably expanded treatment of
feldspar and zeolite minerals; Mineral identification table based
on birefringence and listing other properties; Colour strip with
appropriate interference colours and birefringences for the main
rock-forming minerals. This book will be useful to undergraduate
students of mineralogy, petrology and geochemistry, especially
those at third or fourth year, engaged in more advanced courses or
specialized projects, and also as a reference work for students for
'Masters' degrees by taught courses or research. For doctorate
students, and research workers in the Earth Sciences as well as
those in Materials Science and other related disciplines, this work
can be useful as a condensed version of the very extensive
treatment presented in the volumes of the DHZ Series 'Rock-Forming
Minerals', second edition. Buyers through online retailers should
contact the Mineralogical Society in order to receive the free CD
which goes with the book ([email protected]).
This work presents mathematical models for pressure and saturation
distributions of oil and water flow through semi-infinite porous
media. The mathematical models were developed from the popular
Darcy's equation and the continuity equation. The mathematical
model, which contains simultaneously saturation and pressure
gradients, was decoupled to have a pure pressure and saturation
differential equations. The Crank-Nicolson Finite Difference Method
was used to provide solution to the partial differential equations.
System of linear equations resulted from the discretized partial
differential equations were solved for saturation and pressure
distributions using the Modified Gaussian Elimination Method
algorithm, which was implemented in Microsoft Excel Visual Basic
for Application. The solution was tested using hypothetical
oil/water well production data. The solution scheme and computer
language adopted in this work are easy to apply and use as opposed
to the sophisticated and expensive computer software used by most
researchers in the area.
Elliot L. Richardson The United States is finally awakening to the
fact that it has a major stake in the future of the Arctic.
Recognition of the national importance of the Arctic has been slow
in coming despite the resource wealth that Arctic Alaska has thus
far yielded. Although the United States has had strategic interests
in the Arctic since World War II and active oil and gas interests
there since the discovery of oil at Prudhoe Bay in 1968, its
interest in the Arctic has been low in comparison with that of its
Arctic neighbors, Canada and the Soviet Union. What has been
described by some as an attitude of neglect toward the Arctic is
now changing. The notion of change has become central in most
current discussions about the future of the Arctic. It is apparent
that the Arctic region is entering a period of greatly accelerated
economic, social, strategic, and is political change. The driving
force behind the changes taking place resource development
activity, and although the present scale of this activity is not
inconsequential, it is small in comparison to its projected growth
in the next two decades. In short, the Arctic is about to come
alive. However, knowledge of the Arctic and experience in the
Arctic is comparatively limited. Moreover, competing interests and
differing val ues exist among national groups and between countries
in the Arctic, just as they do in the lower latitudes."
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