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A Brief Review of Thermodynamics Internal Energy and the First Law The infinitesimal change in the internal energy dU dq dw For a general process U dq dw q w c The First Law of Thermodynamics The Constant Volume Heat Capacity Define the constant volume heat capacity, CV dq U CV dT V T V Enthalpy We define the enthalpy of the system, H H U PV The Constant Pressure Heat Capacity Define the constant pressure heat capacity, CP dq H CP dT P T P 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 dq rev dS T The Fundamental Equation of Thermodynamics Combine the first law of thermodynamics with the definition of entropy. dq rev 1 dS dU PdV T T The Temperature dependence of the Entropy Under isochoric conditions, the entropy dependence on temperature is related to CV CV S T T V Entropy changes Under Constant Volume Conditions For a system undergoing an isochoric temperature change CV dS dT T For a macroscopic system T2 CV S dT T T 1 The Temperature dependence of the Entropy Under isobaric conditions, the entropy dependence on temperature is related to CP CP S T T P Entropy changes Under Constant Pressure Conditions For a system undergoing an isobaric temperature change CP dS dT T For a macroscopic system T2 CP S dT T T 1 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 dU dq dw T surr dS dU dw 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 dU Pext dV dw a T surr dS 0 Isothermal Processes For a systems where the temperature is constant and equal to Tsurr dU TdS dw 0 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 A A dA dT dV T V V T A T S V A V P T Isothermal Volume Changes For an ideal gas undergoing an isothermal volume change V2 V2 A A dV PdV V1 V T V1 V 2 nRT ln V1 Isothermal Processes at Constant Pressure For an isothermal, isobaric transformation dU TdS Pext dV dw a 0 dU TdS PdV dw a 0 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 G G dG dT dP T P P T G T S P G P V T Isothermal Pressure Changes For an ideal gas undergoing an isothermal pressure change P2 V2 G G dP VdP P1 P T V1 P2 nRT ln P1 Temperature Dependence of A Under isochoric conditions A dA dT SdT T V T2 T2 A A dT SdT T1 T V T1 Gibbs Energy Changes As a Function of Temperature The Gibbs energy changes can be calculated at various temperatures G T 2 G T1 T2 T S dT 1 G T2 G T1 S T 2 T1 The Chemical Potential Define the chemical potential = G/n P2 G 2 G1 RT ln n n P1 G P2 2 1 RT ln P1 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 RT ln m 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 = ns s + n = ns s + 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 , aand a+ We note that = + + + - - and = / This gives us the following relationship ( + RT ln a) = + (+ + 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- = - ma+ = + m+ As with the activities () = (+)+ (-)(m) = (m+)+ (m-)- The Chemical Potential Expression RT ln a RT ln m RT ln m RT ln m RT ln RT ln m RT ln RT ln This can be factored into two parts RT ln m RT ln The ideal part RT ln Deviations from ideal behaviour 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! log 0.510 z z Im 1 2 Z+ = charge of cation; z- = charge of anion I m Ionic strength ½ j z j m j 2 Debye Hűckel Extended Law This equation can reliably estimate the activity coefficients up to a concentration of 0.10 mole/kg. log 0.510 z z I c 1 B I c B = 1.00 (kg/mole)1/2 1 2 1 2 The Davies Equation This equation can reliably estimate the activity coefficients up to a concentration of 1.00 mole/kg. log 0.510 z z 1 2 I m kI m 1 1 I m 2 k = 0.30 (kg/mole)