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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Example 2.2Measuring enthalpies of reaction

Sodium reacts spontaneously and vigorously with oxygen to form Na 2O. The heat given off by this reaction is the enthalpy of formation ΔH ƒof Na 2O. Suppose that you react 23 g of Na metal with oxygen in a calorimeter that has the effective heat capacity of 5 kg of water. The heat capacity of water is 75.3 J/mol K. If the calorimeter has a temperature of 20°C before the reaction and a temperature of 29.9°C after the reaction, what is Δ H ƒof Na 2O? Assume that the Na 2O contributes negligibly to the heat capacity of the system.

Answer: The heat capacity of the calorimeter is

The heat required to raise its temperature by 99 K is then which is the - фото 144

The heat required to raise its temperature by 9.9 K is then

which is the enthalpy of this reaction Our experiment created 05 moles of Na - фото 145

which is the enthalpy of this reaction. Our experiment created 0.5 moles of Na 2O, so ΔH is −414.16 kJ/mol.

2.8 HEAT CAPACITY

It is a matter of everyday experience that the addition of heat to a body will raise its temperature. We also know that if we bring two bodies in contact, they will eventually reach the same temperature. In that state, the bodies are said to be in thermal equilibrium. However, thermal energy will not necessarily be partitioned equally between the two bodies. It would require half again as much heat to increase the temperature of 1 g of quartz by 1°C as it would to increase the temperature of 1 g of iron metal by 1°C. (We saw that temperature is a measure of the energy per degree of freedom. It would appear then that quartz and iron have different degrees of freedom per gram, something we will explore below.) Heat capacity is the amount of heat (in joules or calories) required to raise the temperature of a given amount (usually a mole) of a substance by 1 K. Mathematically, we would say:

(2.66) Geochemistry - изображение 146

However, the heat capacity of a substance will depend on whether heat is added at constant volume or constant pressure, because some of the heat will be consumed as work if the volume changes. Thus, a substance will have two values of heat capacity: one for constant volume and one for constant pressure.

2.8.1 Constant volume heat capacity

Recall that the first law states:

Geochemistry - изображение 147

If we restrict work to PV work, this may be rewritten as:

Geochemistry - изображение 148

If the heating is carried out at constant volume (i.e., d V = 0), then d U = d Q (all energy change takes the form of heat) and:

(2.67) In an ideal gas each atom has three degrees of translational freedom A mole - фото 149

In an ideal gas, each atom has three degrees of translational freedom. A mole of such gas will have N Asuch atoms and 3N Adegrees of freedom. According to the kinetic theory of gases, the energy, U , of this gas is 3/ 2N Ak T . Thus (d U /d T ) V= 3/ 2N Ak, or 3/ 2R where R is the gas constant. Molecular gases, however, are not ideal. Vibrational and rotational modes also come into play, and heat capacity of real gases, as well as solids and liquids, is a function of temperature.

For solids, motion is vibrational and heat capacities depend on vibrational frequencies, which in turn depend on temperature and bond strength (for stronger bonds there is less energy stored as potential energy, hence less energy is required to raise temperature), for reasons discussed below. For nearly incompressible substances such as solids, the difference between C Vand C Pis generally small.

2.8.2 Constant pressure heat capacity

While heat capacities at constant volume are readily measured for gases, they are difficult to measure for solids and liquids. In nature too, temperature changes tend not to take place at constant volume, so constant pressure heat capacities are of greater interest. equation 2.61states that Geochemistry - изображение 150. Substituting this expression in to eqn. 2.66we have:

(2.68) Geochemistry - изображение 151

Thus, enthalpy change at constant pressure may also be expressed as:

(2.69) Geochemistry - изображение 152

2.8.3 Energy associated with volume and the relationship between C vand C p

Constant pressure and constant temperature heat capacities are different because there is energy associated (work done) with expansion and contraction. Thus how much energy we must transfer to a substance to raise its temperature will depend on whether some of this energy will be consumed in this process of expansion. These energy changes are due to potential energy changes associated with changing the position of an atom or molecule in the electrostatic fields of its neighbors. The difference between C Vand C preflects this energy associated with volume. Let us now determine what this difference is.

We can combine relations 2.67and 2.68as:

(2.70) From this we may derive the following relationship 271 and further - фото 153

From this, we may derive the following relationship:

(2.71) and further 272 It can also be shown that for a reversible process - фото 154

and further:

(2.72) It can also be shown that for a reversible process 273 U V Tis - фото 155

It can also be shown that, for a reversible process:

(2.73) U V Tis the energy associated with the volume occupied by a substance - фото 156

(U/V) Tis the energy associated with the volume occupied by a substance and is known as the internal pressure ( P int, which we introduced earlier in our discussion of the van der Waals law, e.g., eqn. 2.17). It is a measure of the energy associated with the forces holding molecules or atoms together. For real substances, energy changes associated with volume changes reflect potential energy increases associated with increased separation between charged molecules and/or atoms; there are no such forces in an ideal gas, so this term is 0 for an ideal gas. Substituting eqn. 2.73into 2.72, we obtain:

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