William M. White - Geochemistry

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Geochemistry: краткое содержание, описание и аннотация

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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.

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Substituting β for ∂ln Ω ( E )/d E ( eqn. 2.48), we have:

and 280 Since the total energy of the system E is fixed Ω E must - фото 170

and

(2.80) Geochemistry - изображение 171

Since the total energy of the system, E , is fixed, Ω( E ) must also be fixed, so:

(2.81) Geochemistry - изображение 172

Substituting 1/k T for β ( eqn. 2.53), we have:

Geochemistry - изображение 173

We can deduce the value of the constant C by noting that Geochemistry - изображение 174, that is, the probabilities over all energy levels must sum to one (because the system must always be in one of these states). Therefore:

(2.82) Geochemistry - изображение 175

so that

(2.83) Geochemistry - изображение 176

Generalizing our result, the probability of the system being in state i corresponding to energy ε iis:

(2.84) This equation is the Boltzmann distribution law and one of the most - фото 177

This equation is the Boltzmann distribution law * , and one of the most important equations in statistical mechanics. Though we derived it for a specific situation and introduced an approximation (the Taylor series expansion), these were merely conveniences; the result is very general (see Feynman et al., 1989 for an alternative derivation). If we define our system as an atom or molecule, then this equation tells us the probability of an atom having a given energy value, ε i.This is the statistical mechanical interpretation of this equation; it can also be interpreted in terms of quantum physics. The basic tenet of quantum physics is that energy is quantized: only discrete values are possible. The Boltzmann distribution law gives the probability of an atom having the energy associated with quantum level i .

The Boltzmann distribution law says that the population of energy levels decreases exponentially as the energy of that level increases ( energy among atoms is like money among men: the poor are many and the rich few ). A hypothetical example is shown in Figure 2.9.

2.8.4.2 The partition function

The denominator of eqn. 2.84, which is the probability normalizing factor or the sum of the energy distribution over all accessible states , is called the partition function and is denoted Q :

(2.85) The partition function is a key variable in statistical mechanics and quantum - фото 178

The partition function is a key variable in statistical mechanics and quantum physics. It is related to macroscopic variables with which we are already familiar, namely energy and entropy. Let's examine these relationships.

We can compute the total internal energy of a system, U , as the average energy of the atoms times the number of atoms, n . To do this we need to know how energy is distributed among atoms. Macroscopic systems have a very large number of atoms (∼10 23, give or take a few in the exponent). In this case, the number of atoms having some energy ε iis proportional to the probability of one atom having this energy. So to find the average, we take the sum over all possible energies of the product of energy times the possibility of an atom having that energy. Thus, the internal energy of the system is just:

Figure 29 Occupation of vibrational energy levels calculated from the - фото 179

Figure 2.9 Occupation of vibrational energy levels calculated from the Boltzmann distribution. The probability of an energy level associated with the vibrational quantum number n is shown as a function of n for a hypothetical diatomic molecule at 273 K and 673 K.

(2.86) The derivative of Q with respect to temperature at constant volume can be - фото 180

The derivative of Q with respect to temperature (at constant volume) can be obtained from eqn. 2.85:

(2.87) Comparing this with eqn 286 we see that this is equivalent to 288 It - фото 181

Comparing this with eqn. 2.86, we see that this is equivalent to:

(2.88) It is also easy to show that so the internal energy of the system is 289 - фото 182

It is also easy to show that so the internal energy of the system is 289 For 1 mole of substance n - фото 183, so the internal energy of the system is:

(2.89) For 1 mole of substance n is equal to the Avogadro number N A Since R N - фото 184

For 1 mole of substance, n is equal to the Avogadro number, N A. Since R = N Ak, eqn. 2.89, when expressed on a molar basis, becomes:

(2.90) We should not be surprised to find that entropy is also related to Q This - фото 185

We should not be surprised to find that entropy is also related to Q . This relationship, the derivation of which is left to you (Problem 13), is:

(2.91) Since the partition function is a sum over all possible states it might appear - фото 186

Since the partition function is a sum over all possible states, it might appear that computing it would be a formidable, if not impossible, task. As we shall see, however, the partition function can very often be approximated to a high degree of accuracy by quite simple functions . The partition function and Boltzmann distribution will prove useful to us in subsequent chapters in discussing several geologically important phenomena such as diffusion and the distribution of stable isotopes between phases, as well as in understanding heat capacities, discussed below.

2.8.4.3 Energy distribution in solids

According to quantum theory, all modes of motion are quantized. Consider, for example, vibrations of atoms in a hydrogen molecule. Even at absolute zero temperature, the atoms will vibrate at a ground state frequency. The energy associated with this vibration will be:

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