William M. White - Geochemistry

Здесь есть возможность читать онлайн «William M. White - Geochemistry» — ознакомительный отрывок электронной книги совершенно бесплатно, а после прочтения отрывка купить полную версию. В некоторых случаях можно слушать аудио, скачать через торрент в формате fb2 и присутствует краткое содержание. Жанр: unrecognised, на английском языке. Описание произведения, (предисловие) а так же отзывы посетителей доступны на портале библиотеки ЛибКат.

Geochemistry: краткое содержание, описание и аннотация

Предлагаем к чтению аннотацию, описание, краткое содержание или предисловие (зависит от того, что написал сам автор книги «Geochemistry»). Если вы не нашли необходимую информацию о книге — напишите в комментариях, мы постараемся отыскать её.

A Comprehensive Introduction to the “Geochemist Toolbox” – the Basic Principles of Modern Geochemistry In the new edition of William M. White’s
, undergraduate and graduate students will find each of the core principles of geochemistry covered. From defining key principles and methods to examining Earth’s core composition and exploring organic chemistry and fossil fuels, this definitive edition encompasses all the information needed for a solid foundation in the earth sciences for beginners and beyond. 
For researchers and applied scientists, this book will act as a useful reference on fundamental theories of geochemistry, applications, and environmental sciences. The new edition includes new chapters on the geochemistry of the Earth’s surface (the “critical zone”), marine geochemistry, and applied geochemistry as it relates to environmental applications and geochemical exploration.
● A review of the fundamentals of geochemical thermodynamics and kinetics, trace element and organic geochemistry
● An introduction to radiogenic and stable isotope geochemistry and applications such as geologic time, ancient climates, and diets of prehistoric people
● Formation of the Earth and composition and origins of the core, the mantle, and the crust
● New chapters that cover soils and streams, the oceans, and geochemistry applied to the environment and mineral exploration
In this foundational look at geochemistry, new learners and professionals will find the answer to the essential principles and techniques of the science behind the Earth and its environs.

Geochemistry — читать онлайн ознакомительный отрывок

Ниже представлен текст книги, разбитый по страницам. Система сохранения места последней прочитанной страницы, позволяет с удобством читать онлайн бесплатно книгу «Geochemistry», без необходимости каждый раз заново искать на чём Вы остановились. Поставьте закладку, и сможете в любой момент перейти на страницу, на которой закончили чтение.

Тёмная тема
Сбросить

Интервал:

Закладка:

Сделать

(2.40) and 241 As additive properties ln and ln Ω are - фото 100

and

(2.41) As additive properties ln and ln Ω are consistent with our other extensive - фото 101

As additive properties, ln картинка 102and ln Ω are consistent with our other extensive state variables (e.g., U , V ).

We want to know which energy distribution (i.e., values of e and E – e ) is the most likely one, because that corresponds to the equilibrium state of the system. This is the same as asking where the probability function, картинка 103( e ), is maximum. Maximum values of functions have the useful property that they occur at points where the derivative of the function is 0 . That is, a maximum of function ƒ(x) will occur where d ƒ(x) /d (x) = 0. *Thus, the maximum value of картинка 104in Figure 2.8occurs where d d e 0 The most probable energy distribution will therefore occur at 242 - фото 105/d e = 0. The most probable energy distribution will therefore occur at:

(2.42) we use the partial differential notation to indicate that since the system is - фото 106

(we use the partial differential notation to indicate that, since the system is isolated, all other state variables are held constant). Substituting eqn. 2.41into 2.42, we have:

(2.43) since C is a constant Then substituting eqn 240into 243we have 244 - фото 107

(since C is a constant). Then substituting eqn. 2.40into 2.43we have:

(2.44) so the maximum occurs at 245 The maximum then occurs where the function - фото 108

so the maximum occurs at:

(2.45) The maximum then occurs where the function lnΩe for each of the two blocks - фото 109

The maximum then occurs where the function ∂lnΩ/∂e for each of the two blocks are equal (the negative sign will cancel because we are taking the derivative ∂ƒ(−e)/∂e). More generally, we may write:

(2.46) Notice two interesting things the equilibrium energy distribution is the one - фото 110

Notice two interesting things: the equilibrium energy distribution is the one where ln Ω is maximum (since it is proportional to P) and where the functions ∂lnΩ/∂E of the two blocks are equal . It would appear that both are very useful functions. We define entropy, S , †as:

(2.47) † Geochemistry - изображение 111

and a function β such that:

(2.48) Geochemistry - изображение 112

where k is a constant (which turns out to be Boltzmann's constant or the gas constant; the choice depends on whether we work in units of atoms or moles, respectively). The function S then has the property that it is maximum at equilibrium and β has the property that it is the same in every part of the system at equilibrium .

Entropy also has the interesting property that in any spontaneous reaction, the total entropy of the system plus its surroundings must increase. In our example, this is a simple consequence of the observation that the final probability, картинка 113( E ), and therefore also Ω, will be maximum and hence never be less than the original one. Because of that, the final number of accessible states must exceed the initial number and:

(2.49) rearranging The quantities in brackets are simply the entropy changes of the - фото 114

rearranging:

Geochemistry - изображение 115

The quantities in brackets are simply the entropy changes of the two blocks. Hence:

(2.50) Geochemistry - изображение 116

In other words, any decrease in entropy in one of the blocks must be at least compensated for by an increase in entropy of the other block.

For an irreversible process, that is, a spontaneous one such as thermal equilibrium between two copper blocks, we cannot determine exactly the increase in entropy. Experience has shown, however, that the increase in entropy will always exceed the ratio of heat exchanged to temperature. Thus, the mathematical formulation of the second law is:

(2.51) Geochemistry - изображение 117

Like the first law, eqn. 2.51cannot be derived or formally proven; it is simply a postulate that has never been contradicted by experience. For a reversible reaction, that is, one that is never far from equilibrium and therefore one where d Q is small relative to T ,

(2.52) Geochemistry - изображение 118

(see Example 2.1). In thermodynamics, we restrict our attention to systems that are close to equilibrium, so eqn. 2.52serves as an operational definition of entropy.

2.6.2.1 Microscopic interpretation of temperature

Let's now return to our function β . The macroscopic function having the property of our new function β is temperature. The relation of temperature to β is

(2.53) Geochemistry - изображение 119

and

(2.54) Geochemistry - изображение 120

equation 2.53provides a statistical mechanical definition of temperature. We can easily show that T is the measure of the energy per degree of freedom . To do this, though, we need one other relationship, which we introduce without proof. This is that Ω increases roughly with E as:

картинка 121

where ƒ is the number of degrees of freedom of the system (which, in turn, is proportional to the number of atoms or molecules in the system times the modes of motion, e.g., vibrational, rotational, translational, available to them). Hence:

Читать дальше
Тёмная тема
Сбросить

Интервал:

Закладка:

Сделать

Похожие книги на «Geochemistry»

Представляем Вашему вниманию похожие книги на «Geochemistry» списком для выбора. Мы отобрали схожую по названию и смыслу литературу в надежде предоставить читателям больше вариантов отыскать новые, интересные, ещё непрочитанные произведения.


Отзывы о книге «Geochemistry»

Обсуждение, отзывы о книге «Geochemistry» и просто собственные мнения читателей. Оставьте ваши комментарии, напишите, что Вы думаете о произведении, его смысле или главных героях. Укажите что конкретно понравилось, а что нет, и почему Вы так считаете.

x