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Chemistry 434. A Brief Review of Thermodynamics. Internal Energy and the First Law. The infinitesimal change in the internal energy . For a general process. The First Law of Thermodynamics. The Constant Volume Heat Capacity. Define the constant volume heat capacity, C V. Enthalpy.
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Chemistry 434 A Brief Review of Thermodynamics
Internal Energy and the First Law • The infinitesimal change in the internal energy • For a general process The First Law of Thermodynamics
The Constant Volume Heat Capacity • Define the constant volume heat capacity, CV
Enthalpy • We define the enthalpy of the system, H
The Constant Pressure Heat Capacity • Define the constant pressure heat capacity, CP
Thermodynamic Definition • Spontaneous Process – the process occurs without outside work being done on the system.
Mathematical Definition of Entropy • The entropy of the system is defined as follows
The Fundamental Equation of Thermodynamics • Combine the first law of thermodynamics with the definition of entropy.
The Temperature dependence of the Entropy • Under isochoric conditions, the entropy dependence on temperature is related to CV
Entropy changes Under Constant Volume Conditions • For a system undergoing an isochoric temperature change • For a macroscopic system
The Temperature dependence of the Entropy • Under isobaric conditions, the entropy dependence on temperature is related to CP
Entropy changes Under Constant Pressure Conditions • For a system undergoing an isobaric temperature change • For a macroscopic system
The Second Law of Thermodynamics • The second law of thermodynamics concerns itself with the entropy of the universe (univS). • univS unchanged in a reversible process • univS always increases for an irreversible process
The Third Law of Thermodynamics • The Third Law - the entropy of any perfect crystal is 0 J /(K mole) at 0 K (absolute 0!) • Due to the Third Law, we are able to calculate absolute entropy values.
Combining the First and Second Laws • From the first law
Pressure Volume and Other Types of Work • Many types of work can be done on or by chemical systems. • Electrical work. • Surface expansion. • Stress-strain work. dw=-Pext dV+dwa where dwa includes all other types of work
The General Condition of Equilibrium and Spontaneity • For a general system
Isothermal Processes • For a systems where the temperature is constant and equal to Tsurr
The Helmholtz Energy • Define the Helmholtz energy A A(T,V) =U – TS • Note that for an isothermal process dA dw A w • For an isochoric, isothermal process A 0
The Properties of A • The Helmholtz energy is a function of the temperature and volume
Isothermal Volume Changes • For an ideal gas undergoing an isothermal volume change
Isothermal Processes at Constant Pressure • For an isothermal, isobaric transformation
The Gibbs Energy • Define the Gibbs energy G G(T,P) =U – TS+PV • Note that for an isothermal process dG dwa G wa • For an isothermal, isobaric process G 0
The Properties of G • The Gibbs energy is a function of temperature and pressure
Isothermal Pressure Changes • For an ideal gas undergoing an isothermal pressure change
Temperature Dependence of A • Under isochoric conditions
Gibbs Energy Changes As a Function of Temperature • The Gibbs energy changes can be calculated at various temperatures
The Chemical Potential • Define the chemical potential = G/n
Gibbs Energy and Spontaneity sysG < 0 - spontaneous process sysG > 0 - non-spontaneous process (note that this process would be spontaneous in the reverse direction) sysG = 0 - system is in equilibrium
Applications of the Gibbs Energy • The Gibbs energy is used to determine the spontaneous direction of a process. • Two contributions to the Gibbs energy change (G) • Entropy (S) • Enthalpy (H) G = H - TS
Thermodynamics of Ions in Solutions • Electrolyte solutions – deviations from ideal behaviour occur at molalities as low as 0.01 mole/kg. • How do we obtain thermodynamic properties of ionic species in solution?
For the H+(aq) ion, we define • fH = 0 kJ/mole at all temperatures • S = 0 J/(K mole) at all temperatures • fG = 0 kJ/mole at all temperatures
Activities in Electrolyte Solutions • For the following discussion • Solvent “s” • Cation “+” • Anion “=“ • Consider 1 mole of an electrolyte dissociating into + cations and - anions G = nss + n = nss + n+ + +n- - • Note – since = + + - = + + +- -
The Mean Ionic Chemical Potential • We define = / • We now proceed to define the activities = + RT ln a + = + + RT ln a+ - = - + RT ln a- = + RT ln a
The Relationship Between a and a • Since = / = + RT ln a = ( + RT ln a) Since = / • This gives us the relationship between the electrolyte activity and the mean activity (a)= a
The Relationship Between a , a- and a+ • We note that = + + +- - and = / • This gives us the following relationship ( + RT ln a) = n+ (+ + RT ln a+) + - ( - + RT ln a-) • Since = +++ -- (a) = (a+)+ (a-)-
Activities in Electrolyte Solutions • The activities of various components in an electrolyte solution are defined as follows a+ = + m+ a- = - m- a+ = + m+ • As with the activities () = (+)+ (-)- (m) = (m+)+ (m-)-
The Chemical Potential Expression • This can be factored into two parts Deviations from ideal behaviour The ideal part
Activity Coefficients As a Function of Molality Data obtained from Glasstone et al., Introduction to Electrochemistry, Van Nostrand (1942). CRC Handbook of Chemistry and Physics, 63rd ed.; R.C. Weast Ed.; CRC Press, Boca Raton, Fl (1982). CaCl2 HCl LaCl3 KCl H2SO4
Estimates of Activity Coefficients in Electrolyte Solutions • The are a number of theories that have been proposed to allow the theoretical estimation of the mean activity coefficients of an electrolyte. • Each has a limited range of applicability.
The Debye Hűckel Limiting Law • This is valid in the up to a concentration of 0.010 molal! Z+ = charge of cation; z- = charge of anion
Debye Hűckel Extended Law • This equation can reliably estimate the activity coefficients up to a concentration of 0.10 mole/kg. B = 1.00 (kg/mole)1/2
The Davies Equation • This equation can reliably estimate the activity coefficients up to a concentration of 1.00 mole/kg. k = 0.30 (kg/mole)