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Brad Gietman's List: 3rd part of chem

    • Altering the mechanism of a reaction so that the activation energy is lower is the second major way to speed up the reaction. A catalyst can do this by participating in the activated complex for the rate-limiting step, even though the catalyst itself is neither a reactant nor a product in the overall stoichiometric equation.
    • The currently accepted mechanism for this catalyzed reaction involves three steps:


                       ½ I2 \rightleftharpoons I

            I + cis-C4H8 → C4H8I trans-C4H8 + I

                            I \rightleftharpoons ½ I2

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    • Our previous discussion has concentrated on catalysts which are in the same phase as the reaction being catalyzed. This kind of catalysis is called homogeneous catalysis.
    • Many important industrial processes rely on heterogeneous catalysis, in which the catalyst is in a different phase. Usually the catalyst is a solid and the reactants are gases, and so the rate-limiting step occurs at the solid surface. Thus heterogeneous catalysis is also referred to as surface catalysis.

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    • It does so efficiently enough that only a few kilograms of enzyme are necessary to fix about 44 × 1012 g of nitrogen worldwide each year. Other enzymes carry out other reactions with comparable efficiencies.
    • All enzymes are large protein molecules whose molar masses exceed 20 000 g mol–1. They are condensation polymers of amino acids,

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    • thermochemical equations, such as


      CH4(g) + 2O2(g) → CO2(g) + 2H2O(l)(25°C, 1 atm pressure)


      ΔHm = –890 kJ mol–1      (1)


      Here the ΔHm (delta H subscript m) tells us whether heat energy is released or absorbed when the reaction occurs and also enables us to find the actual quantity of energy involved.

    • By convention, if ΔHm is positive, heat is absorbed by the reaction; i.e., it is endothermic. More commonly, ΔHm is negative as in Eq. (1), indicating that heat energy is released rather than absorbed by the reaction, and that the reaction is exothermic.

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    • Perhaps the most useful feature of thermochemical equations is that they can be combined to determine ΔHm values for other chemical reactions
    • On paper this net result can be obtained by adding the two chemical equations as though they were algebraic equations. The CO produced is canceled by the CO consumed since it is both a reactant and a product of the overall reaction

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    • By now chemists have measured the enthalpy changes for so many reactions that it would take several large volumes to list all the thermochemical equations. Fortunately Hess' law makes it possible to list a single value, the standard enthalpy of formation ΔHf, for each compound
    • The standard enthalpy of formation is the enthalpy change when 1 mol of a pure substance is formed from its elements. Each element must be in the physical and chemical form which is most stable at normal atmospheric pressure and a specified temperature (usually 25°C).

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    • the law of conservation of energy is therefore referred to as the first law of thermodynamics.
    • The total of translational, rotational, vibrational, and electronic energies is the internal energy of an atom or molecule.

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    • Here we must consider changes in the kinetic and potential energies of electrons in the atoms and molecules involved, that is, changes in the electronic energy.
    • As a simple example of a chemical change, let us consider an exothermic reaction involving only one kind of atom, the decomposition of ozone, O3:

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    • System. The term system is used to describe any sample of matter in which we are particularly interested
    • Initial and final states. In thermodynamics our principal concern is with the initial state before any changes begin, and the final state, when no more changes occur

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    • When a change occurs at constant pressure, there is another energy factor we must consider in addition to the heat absorbed and the change in internal energy. This is the expansion work wexp which the system does as its volume expands against the external pressure.
    • qp = ΔU + wexp 

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    • t is therefore often necessary to convert a measured ΔU value to a ΔH value.
    • Though enthalpies of formation are easy to find, equivalent tables of internal energies are nonexistent. In many ways this insistence on ΔH rather than on ΔU is a pity. In particular, it suggests that somehow the enthalpy H has more fundamental significance on the molecular level than the internal energy U. It is important to realize that this is not the case. It is the internal energy which has a simple molecular interpretation, namely, the total energy of all the molecules in the system. By contrast the enthalpy includes not only the total energy of the molecules in the system but the potential energy of the atmosphere outside the system as well. We use the enthalpy so often because of its convenience rather than because of its molecular significance.

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    • The bond enthalpy DX–Y of a diatomic molecule X—Y is the enthalpy change for the (usually hypothetical) process:


      XY(g) → X(g) + Y(g)      ΔH°(298 K) = DX―Y      (1)

    • We have already used the term bond energy to describe this quantity, though strictly speaking the bond energy is a measure of ΔU rather than ΔH. As we have already seen, ΔU and ΔH are nearly equal, and so either term may be used.

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    • If less energy is needed to break up the reactant molecules into their constituent atoms than is released when these atoms are reconstituted into product molecules, then the reaction will be exothermic
    • In summary, there are two factors which determine whether a gaseous reaction will be exothermic or not: (1) the relative strengths of the bonds as measured by the bond enthalpies, and (2) the relative number of bonds broken and formed. An exothermic reaction corresponds to the formation of more bonds, stronger bonds, or both

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    • The entropy of a substance depends on two things: first, the state of a substance—its temperature, pressure, and amount; and second, how the substance is structured at the molecular level.
    •    As we saw in the last section, there should be only one way of arranging the energy in a perfect crystal at 0 K. If W = 1, then S = k ln W = 0; so that the entropy should be zero at the absolute zero of temperature. This rule, known as the third law of thermodynamics, is obeyed by all solids unless some randomness of arrangement is accidentally “frozen” into the cryst

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    • There are two aspects of the molecular structure of a substance which affect the value of its entropy: (1) The degree to which the movement of the atoms and molecules in the structure is restricted—the less restricted this movement, the greater the entropy. (2) The mass of the atoms and molecules which are moving—the greater the mass, the larger the entropy.
    • Thus when a solid melts, the molar entropy of the substance increases. When a liquid vaporizes, the restrictions on the molecules’ ability to move around are relaxed almost completely and a further and larger increase in the entropy occurs. When 1 mol of ice melts, for example, its entropy increases by 22 J K–1, while on boiling the entropy increase is 110 J K–1
    • we still find an increase of entropy with complexity when we compare molecules of very similar masses:

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