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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(2.24) Geochemistry - изображение 73

2.5.3 Path independence, exact differentials, state functions, and the first law

We said earlier that state functions are those that depend only on the present state of a system. Another way of expressing this is to say that state functions are path independent. Indeed, path independence may be used as a test of whether a variable is a state function or not. This is to say that if Y is a state function, then for any process that results in a change Y1Y2 , the net change in Y , Δ Y , is independent of how one gets from Y1 to Y2 . Furthermore, if Y is a state function, then the differential d Y is said to be mathematically exact .

Let's explore what is meant by an exact differential. An exact differential is the familiar kind, the kind we would obtain by differentiating the function u with respect to x and y , and also the kind we can integrate. But not all differential equations are exact. Let's first consider the mathematical definition of an exact differential, then consider some thermodynamic examples of exact and inexact differentials.

Consider the first order differential expression:

(2.25) Geochemistry - изображение 74

containing variables M and N , which may or may not be functions of x and y . Equation 2.25is said to be an exact differential if there exists some function u of x and y relating them such that the expression:

(2.26) is the total differential of u 227 Lets consider what this implies - фото 75

is the total differential of u :

(2.27) Lets consider what this implies Comparing 226and 227 we see that 228 - фото 76

Let's consider what this implies. Comparing 2.26and 2.27, we see that:

(2.28) A necessary but not sufficient condition for 225to be an exact differential - фото 77

A necessary, but not sufficient, condition for 2.25to be an exact differential is that M and N must be functions of x and y .

A general property of partial differentials is the reciprocity relation or cross-differentiation identity, which states that the order of differentiation does not matter, so that:

(2.29) Geochemistry - изображение 78

(The reciprocity relation is an important and useful property in thermodynamics, as we shall see at the end of this chapter.) If eqn. 2.26is the total differential of u , it follows that:

(2.30) Geochemistry - изображение 79

which is equivalent to:

(2.31) Equation 231is a necessary and sufficient condition for 225 to be an exact - фото 80

Equation 2.31is a necessary and sufficient condition for 2.25 to be an exact differential; that is, if the cross-differentials are equal, then the differential expression is exact.

Exact differentials have the property that they can be integrated and an exact value obtained. This is true because they depend only on the initial and final values of the independent variables (e.g., x and y in eqn. 2.27).

Now let's consider some thermodynamic examples. Volume is a state function and we can express it as an exact differential in terms of other state functions, as in eqn. 2.17:

(2.17) Substituting the coefficient of thermal expansion and compressibility for VT - фото 81

Substituting the coefficient of thermal expansion and compressibility for ∂V/∂T and ∂V/∂P respectively, equation 2.30becomes equal to eqn. 2.18:

(2.18) According to eqn 231 if V is a state function then 232 You should - фото 82

According to eqn. 2.31, if V is a state function, then:

(2.32) You should satisfy yourself that eqn 232indeed holds for ideal gases and - фото 83

You should satisfy yourself that eqn. 2.32indeed holds for ideal gases and therefore that V is a state variable.

Work is not a state function, that is, the work done does not depend only on the initial and final states of a system. We would expect then that d W is not an exact differential, and indeed, this is easily shown for an ideal gas.

For PV work, d W = – P d V . Substituting eqn. 2.17for d V and rearranging, we have:

(2.33) Evaluating VT and VP for the ideal gas equation and multiplying through - фото 84

Evaluating ∂V/∂T and ∂V/∂P for the ideal gas equation and multiplying through by P, this becomes:

(2.34) but 235 We cannot integrate eqn 234and obtain a value for the work done - фото 85

but

(2.35) We cannot integrate eqn 234and obtain a value for the work done without - фото 86

We cannot integrate eqn. 2.34and obtain a value for the work done without additional knowledge of the variation of T and P because the amount of work done does not depend only on the initial and final values of T and P ; it depends on the path taken. Heat is also not a state function, not an exact differential, and is also path dependent. Path dependent functions always have inexact differentials; path independent functions always have exact differentials.

On a less mathematical level, let's consider how the work and heat will vary in a transformation of a system, say from state 1 to state 2. Imagine that we burn gasoline in an open container. In this case, in the transformation from state 1 (gasoline) to state 2 (combustion products of gasoline), energy is given up by the system only as heat. Alternatively, we could burn the gasoline in an engine and recover some of the energy as work (expansion of the volume of the cylinder resulting in motion of the piston). The end states of these two transformations are the same, but the amount of heat released and work done varies, depending on the path we took. Thus, neither work nor heat can be state functions. Energy is a state function, is path independent, and is an exact differential. Whether we burn the gasoline in an open container or an engine, the energy released will be the same. Herein lies the significance for thermodynamics of Joule's discovery: that the sum of heat and work is independent of the path taken even though, independently, work and heat are not .

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