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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3.11.1 Redox in aqueous solutions

The simplest form of the chemical equation for the reduction of ferric iron would be:

(3.102) Figure 318 Electrode reactions in the Daniell cell where the subscript aq - фото 546

Figure 318 Electrode reactions in the Daniell cell where the subscript aq - фото 547

Figure 3.18 Electrode reactions in the Daniell cell.

where the subscript aq denotes the aqueous species. This form suggests that the energy involved might be most conveniently measured in an electrochemical cell.

The Daniell cell pictured in Figure 3.18can be used to measure the energy involved in the exchange of electrons between elements, for example, zinc and copper:

(3.103) where the subscript s denotes the solid Such a cell provides a measure of the - фото 548

where the subscript s denotes the solid. Such a cell provides a measure of the relative preference of Zn and Cu for electrons. In practice, such measurements are made by applying a voltage to the system that is just sufficient to halt the flow of electrons from the zinc plate to the copper one. What is actually measured, then, is a potential energy, denoted E, and referred to as the electrode potential , or simply the potential of the reaction.

If we could measure the potential of two separate half-cell reactions:

we could determine the energy gainloss in the transfer of an electron from an - фото 549 we could determine the energy gainloss in the transfer of an electron from an - фото 550

we could determine the energy gain/loss in the transfer of an electron from an individual element. Unfortunately, such measurements are not possible (nor would these reactions occur in the natural environment: electrons are not given up except to another element or species §). This requires the establishment of an arbitrary reference value. Once such a reference value is established, the potential involved in reactions such as 3.102 can be established.

3.11.1.1 Hydrogen scale potential, EH

The established convention is to measure potentials in a standard hydrogen electrode cell (at standard temperature and pressure). The cell consists on one side of a platinum plate coated with fine Pt powder that is surrounded by H 2gas maintained at a partial pressure of 1 atm and immersed in a solution of unit H +activity. The other side consists of the electrode and solution under investigation. A potential of 0 is assigned to the half-cell reaction:

(3.104) where the subscript g denotes the gas phase The potential measured for the - фото 551

where the subscript g denotes the gas phase. The potential measured for the entire reaction is then assigned to the half-cell reaction of interest. Thus, for example, the potential of the reaction:

is 0763 V This value is assigned to the reaction 3105 Table 33 EH - фото 552

is –0.763 V. This value is assigned to the reaction:

(3.105) Table 33 EH and pε for some halfcell reactions Halfcell reaction E H - фото 553

Table 3.3 EH° and pε° for some half-cell reactions.

Half-cell reaction E H ° (V) p ε°
Li ++ e –⇌ Li −3.05 −51.58
Ca 2++ 2 e –⇌ Ca −2.93 −49.55
Th 4++ 4e –⇌ Th −1.83 −30.95
U 4++ 4e –⇌ U −1.38 −23.34
Mn 2++2e –⇌ Mn −1.18 −19.95
Zn 2++ 2e –⇌ Zn −0.76 −12.85
Cr 3++3e –⇌ Cr −0.74 −12.51
CO 2(g)+ 4H ++ 4e –⇌ CH 2O*+2H 2O −0.71 −12.01
Fe 2++ 2e –⇌ Fe −0.44 −7.44
Eu 3++ e –⇌ Eu 2+ −0.36 −6.08
Ni 2++ 2e –⇌ Ni −0.26 −4.34
Pb 2++ 2e –⇌ Pb −0.13 −2.2
CrO 4 2−+ 4H 2O +3e –⇌ Cr(OH) 3+ H 2O −0.13 −2.2
2H ++ 2e –⇌ H 2(g) 0 0
N 2(g)+ 6H ++ 6e –⇌ 2NH 3 0.093 1.58
Cu 2++ 2e –⇌ Cu 0.34 5.75
UO 2 2++ 2e –⇌ UO 2 0.41 6.85
S + 2e –⇌ S 2− 0.44 7.44
Cu ++ e –⇌ Cu 0.52 8.79
Fe 3++ e –⇌ Fe 2+ 0.77 13.02
NO 3++ 2H ++ e –⇌ NO 2(g)+ H 2O 0.80 13.53
Ag ++ e –⇌ Ag 0.80 13.53
Hg 2++ 2e –⇌ Hg 0.85 14.37
MnO 2(s)+ 4H ++ 2e –⇌ Mn 2++ 2H 2O 1.22 20.63
O 2+ 4H ++ 4e –⇌ 2H 2O 1.23 20.80
MnO 4–+ 8H ++ 5e –⇌ Mn 2++ 4H 2O 1.51 25.53
Au ++ e –⇌ Au 1.69 28.58
Ce 4++ e –⇌ Ce 3+ 1.72 29.05
Pt ++ e –⇌ Pt 2.64 44.64

*CH 2O refers to carbohydrate, the basic product of photosynthesis.

and called the hydrogen scale potential , or E H, of this reaction. Thus, the E Hfor the reduction of Zn +2to Zn 0is −0.763 V. The hydrogen scale potentials of a few half-cell reactions are listed in Table 3.3. The sign convention for E His that the sign of the potential is positive when the reaction proceeds from left to right (i.e., from reactants to products). Thus, if a reaction has positive E H, the metal ion will be reduced by hydrogen gas to the metal. If a reaction has negative E H, the metal will be oxidized to the ion and H +reduced. The standard state potentials (298 K, 0.1 MPa) of more complex reactions can be predicted by algebraic combinations of the reactions and potentials in Table 3.3(see Example 3.11).

The half-cell reactions in Table 3.3are arranged in order of increasing картинка 554. Thus, a species on the product (right) side of a given reaction will reduce (give up electrons to) the species on the reactant side in all reactions listed below it. Thus, in the Daniell cell reaction in Figure 3.18, Zn metal will reduce Cu 2+in solution. Zn may thus be said to be a stronger reducing agent than Cu.

Electrochemical energy is another form of free energy and can be related to the Gibbs free energy of reaction as:

(3.106) Geochemistry - изображение 555

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