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87 Cards in this Set

  • Front
  • Back

Adiabatic

Extremely fast


Ideal process



Q = constant



P × V^gamma


T×V^(gamma - 1)


T×P^(1-gamma/gamma)



Cv = R / (gamma - 1)



Work


W = mR (T1-T2)/gamma - 1


W= (P1V1 - P2V2) /gamma - 1

Isenthalpic

H = constant



Throttling



Its an expansion through a narrow restricted passage, without doing any external work, under adiabatic condition

Isentropic

S = constant



Adiabatic + reversible

Lewis Randell rule

It states that fugacity of a component in an ideal solution is directly proportional to molar fraction of the component in the solution



f"i proportional to xi



f"i = xi fi



f"i = fugacity of i in ideal solution


xi = mole fraction of i the solution


fi = fugacity of i in pure state

Raults law


Ideal solution


PMP of solution = MP of solution



Law


P"i = xi Psi



Partial pressure of the component in the ideal solution is directly proportional to mole fraction in the solution



P"i = yi P



yi P = xi Psi

Henry's law

For dilute ideal solution, the fugacity of component is directly proportional to the mole fraction of the component in the solution.



f"i proportional xi



f"i = xi Hi



xi →0, f"i = xi Hi


xi →1, f"i = xi fi



xi =1, f"i = fi



Activity in solution


Effect of T and P

Ratio of fugacity of the component in solution to the fugacity of component in the standard state



ai = f"i/f°



üi -üi(id) = RT (lnai)



For ideal solution


f"i = xi f°i ;


So ,ai = xi



For real solution


fi≠f°i


ai proportional to xi


ai = Yi xi ; Yi = Activity Coeff (indicates extent to which solution is non ideal)



For real solution


f"i = Yi xi fi



For ideal solution


Yi = 1



Effect of Temp on Yi


d/dT (lnYixi) = (H"i - Hi)/RT²


Gibbs Duhem eqⁿ general form



And other derived form

€ ni dM"i = 0



Others


€ ni dG"i = 0 or € ni düi = 0



x1 dü1/dx1 - x2 dü2/dx2 =0



x1 dV"1/dx1 - x2 dV"2/dx2 =0



x1 dlnf"1/dx1 - x2 dlnf"2/dx2 =0



x1 dlnY1/dx1 - x2 dlnY2/dx2 =0


Property change of mixing general form

∆M = € xi (M"i-Mi)



Free Energy change of mixing

∆G = RT € xi lnxi



For ideal solution, ai = xi


∆G = RT € xi lnai



For pure solution; xi→1


∆G = 0

Volume change of mixing

Below differentiation is partial



∆V = RT € xi d/dP (lnai)



For ideal solution,ai = xi


,


ai = xi



∆V = RT € xi d/dP (lnxi)



For pure solution


∆V = 0

Enthalpy Change of mixing

At constant P



∆H = - RT² €xi ( d/dT (lnai))



For ideal solution, ai = xi


∆H = - RT² €xi ( d/dT (lnxi))



For pure solution, xi →1


∆H = 0

Entropy change of mixing

∆s = -R € xi dlnai/dlnT -R €xi lnai



For ideal solution


ai = xi = constant


∆s = - R € xi lnxi



For pure solution


∆s = 0

Excess Property

M(E) = M(Real) - M(ideal)



How much the real mixture deviating from ideality



M(E) >0 +ve deviation from ideality


M(E) <0 -ve deviation from ideality


Excess change of mixing

∆M(E) = ∆M (real) - ∆M(id)



∆M(E) = M (real) - M(id) = M(E)

Excess Gibbs free energy

∆G(E) = RT ln(Yi)

Extent of reaction £

yi = ni/n



ni = nio + Vi£



Vi = coefficient of product - coefficient of reactant



n = no + V£



no = €nio


V = €Vi

Gibbs phase rule or phase rule

F=C-P+2



C= no. of chemical species..



F<0 ; system is in disequilibrium



F= C-P+2-r



r = no. of independent chemical rxn

1st law

In a closed system going any thermo cycle, cycle integral of work and cycle integral of heat are proportional to each other



proportional = when expressed in their own unit



Equal to = when expressed in consistent units



$Q - $W , $ = partial derivative

Independent path


Point function


Thermo property

dU=

$Q - $W



All function are perfect differential

Isothermal

T = constant


Extremely slow process


Ideal process


∆U = 0


Q=W


∆H = 0



Work


W = P1V1 ln (V2/V1) = RT ln(V2/V1)


= RT ln(P1/P2)

Iso baric

P = constant


Q = ∆H


Work


W = P (V2-V1)

Isochoric

V = constant


W =0


Q = U

Polytropic

PVⁿ = constant


TV^(n-1) = c


TP^ (1-n)/n = c



Work = (P1V1-P2V2)/ n-1

For air Cp, Cv and R

Cp = 1.005 kJ/kgK


Cv = 0.718 kJ/kgK


R = 0.287 kJ/kgK

For compression

W(irreversible) = W(reversible)/n

For expansion

W(irreversible) = W(reversible) × n



n = efficiency

U and H

H used in open system


Sum of internal energy and flow energy



U used in closed system

For open system 1st law

dH + d(K.E.) +d(P.E.) = $q - $Ws

WD in open system and adiabatically

W (a to b) = int (a to b) {-VdP}



W (1 to 2) = gamma (P1V1- P2V2) / gamma - 1

Relationship b/w open system and closed system WD

WD(ops) = gamma WD(cls)



WD(ops) = WD(cls) + net flow of system



- int (1to2)VdP = int (1to2)PdV +(P1V1-P2V2)



Clausis statement

Heat can't flow from low T to high T naturally

Kelvin Planck's

It is impossible to have 100℅ n of a engine

Heat engine

n (efficiency) = o/p÷i/p


n = energy aimed at / energy that costs


= Net WD / Heat Supplied



Net WD = Qh - Ql


Net WD = W(by turbine) - W(by pump)



n = Qh - Ql / Qh



Its an expansion process, work is obtained heat must be supplied



Its a compression process, work is required heat should be rejected out



Carnot engine

WD = Qh - Ql


= P1V1ln(V2/V1) - P3V3 ln(V3/V4)



n(carnot) = Th-Tl/Th = Qh - Ql/Qh

C.O.P. of Refrigerator and Heat pump

Reciprocal of efficiency

Clausis Inequality

If Th = constant



cyclic integration $Q/T ≤ 0



For actual system ie


Irreversible system due to friction



cyclic integration $Q/T = 0



For ideal system ie


Rev system or frictionless



cyclic integration $Q/T ≥ 0


Impossible





Entropy 's'

ds = $Q/T ( Extensive property )


ds' = $q/T (Intensive property )



s/m = s' & Q/m = q



Its a thermodynamic property that ↑ when heat is supplied, expansion takes place, work is obtained,T↓,


↓ when heat is rejected & vice versa


& remains constant if no heat is supplied or rejected



s'2 - s'1 = Cv ln (T2/T1) + R ln (V2/V1)



s'2 - s'1 = Cp ln (T2/T1) - R ln (P2/P1)



s'2 - s'1 = Cv ln (P2/P1) + Cp ln (V2/V1)



Isobaric


s'2 - s'1 = Cp ln (V2/V1)


= Cp ln (T2/T1)


Slope +



Isochoric Process


s'2 - s'1 = Cv ln (P2/P1)


= Cv ln (T2/T1)


Slope +



Isothermal process


s'2 - s'1 = - R ln (P2/P1) = R ln (V2/V1)


Slope 0



Adiabatic


.s'2 - s'1 = 0, s = constant


Slope ∞

Maxwell relation

V A T


-U -G


S H P

Volume Expansivity ß or Coeff. of thermal expansion



And Isothermal Compressibility K

Differentiation is partial



ß = 1/V (dV/dT) at constant P



K = -1/V (dV/dP) at constant T



Cp - Cv = TVß²/ K



For incompressible fluid


ß = K = 0



For an ideal gas


ß is fⁿ of T and ß = 1/T


K is fⁿ of P and K =1/P


h is fⁿ of T



For real gas


h is fⁿ of P,V


Joule-kelvin or jolue Thomson coefficient

Differentiation is partial



ü = (dT / dP) at constant H



ü = (dT / dP) at constant H


= 1/Cp [T dV/dT(at constant P) - V]



If ideal gas is throttled


ü = (dT / dP) at constant H = 0



Expansivity


ü = (dT / dP) at constant H = V/Cp(Tß-1)



ü + ; cooling


ü - ; heating


Clapeyron eqⁿ

dP/dT = s'g-s'f/Vg-Vf = hfg /{Ts(Vg-Vf)}



hfg = latent heat of vaporisation



dP(saturation)/ dT = ∆H/T∆V



Clausius Clapeyron Eqⁿ


3 forms

1. dP/P = hfg / RT² × dT



2. ln(P2/P1) = ( hfg / R) × (1/T1-1/T2) For liq. and vapor


For liq. and vapor



3. d(lnP)/d(1/T) = - hfg/R


Slope = -hfg/R = -ve

Dryness Factor

X = Mass of dry & sat. steam / (Mass of dry & sat. steam + Mass of saturated water )

Degree of super heat

= Tsup. h - Ts

Degree of super heat

= Tsup. h - Ts

hg, sg, and h(wet)

hg = hf+hfg



s'g = s'f + s'fg



h(wet) = hf+ xhfg



hg = enthalpy of sat. vapor


hf = enthalpy of sat. liq. (At exit)


h(wet) = enthalpy of sat. liq. (At enter)

hg, s'g, and h(wet)

hg = hf+hfg



s'g = s'f + s'fg



h(wet) = hf+ xhfg



hg = enthalpy of sat. vapor


hf = enthalpy of sat. liq. (At exit)


h(wet) = enthalpy of sat. liq. (At enter)

Virial EOS


Compressibility factor = Z

Z = volm of real gas / volm of ideal gas


Z = V’ /(RT/P) = PV’ /RT


Z = 1 + B°(T)/V’ + B¹(T)/V’² + ………



B°; 0 is not a power only denotation



Z = 1 + B°(T)/V’



B° = (RTc/Pc) (B'+WB")



W = accentric factor (Molecule shape, density, sphericity of molecule)



B' = 0.083 - (0.422/Tr ^1.6)



B" = 0.139 - (0.172)/Tr^4.2



Tr = Reduced temp.= T/Tc


Vander wall EOS



a, b, V'c, Zc

P = [RT/(V'-b)] - (a/V'²)


b → figure volume occupied by molecule


a/V'² → attractive



a = 3 Pc V'c²


b = V'c /3



a = 27/64 R² Tc²/ Pc


b = ⅛ R Tc/Pc


Zc = Pc V'c/R Tc = ⅜


Zc = compressibility at critical point.

Chemical potential

Change in entropy per unit mass is chemical potential of any system



üA = dS(T)/dnA



Differentiation is partial


T n A are in suffix

0th law

If A n B system are in thermal equilibrium with C system then A n C are in thermal equilibrium also

0th law

If A n B system are in thermal equilibrium with C system then A n C are in thermal equilibrium also

1st law

For any cyclic process


Change in IE is equal to the heat supplied to system - work obtained by the system

2nd law

HT can't be done from a cold region to hot region naturally, spontaneously (irreversible)




Reversible → quasi static → almost at rest

3rd law

At absolute zero temp , Abs entropy is minimum for all the systems

Chemical potential ü

It's a partial molar free energy



It is equal to change in total Gibbs fee energy power unit change of moles of any component.



ü = (dGt/dna)



T,P,n≠A

Reversible

Ideal case


Net change in ü is 0


∆G = 0

Irreversible

Spontaneous process in forward direction


∆G < 0

Not possible

∆G >0


Spontaneous process in backward directions

Thermodynamic equilibrium

Mechanical equilibrium


Thermal equilibrium


Chemical equilibrium



dG = 0


dP = 0


dT =0

dU

= Tds - PdV

dH

= Tds + VdP

dA

= -PdV - sdT

dG

= VdP - sdT

Irreversible

Spontaneous + Naturally

For open system

Fundamental relation for whole thermodynamics



dG= VdP - sdT + € üi dni



For n moles


dG= VdP - sdT + € üi dxi



Here


xi = ni/n


€ = summation

Phase equilibrium

üi (alpha) = üi (ß)

Molar property of i in pure substance (Mi) and


Partial molar property of ith in mixture (M'i)

1. Pure Substance


∆Mt = ∆ni × Mi



2. Mixture


∆Mt ≠ ∆ni × Mi



∆Mt = ∆ni × M'i



M'i = d(Mt) / d(ni)


At constant P,T,ni≠i



Denotation



Pure


Vi, ui, si, Hi, Gi



Mixture


V'i, u'i, s'i, H'i, G'i



Relation Btw PMP and MP

dMt = €(iton) M'i dni



Mt = € M'i ni



M = € M'i xi (similarly for H,U and V)



M = M'1 x1 + M'2 x2



M = Mt /n



Below differentiation is in partial form


M'1 = M + (n1+n2) dM/dn1


M'1 = M - x2 dM/dx2



M'2 = M + (n1+n2) dM/dn2


M'2 = M - x1 dM/dx1




x1 dM'1/dx1 + x2 dM'2/dx2 = 0



When chemical potential


x1 dG'1/dx1 + x2 dG'2/dx2 = 0



At ∞ dilution of 1, x1→0


then H'1 = H'1^∞



At ∞ dilution of 2, x2→0


then H'2 = H'2^∞

Chemical potential and G



Effect of T on ü and Effect of P on ü

Here ü (act as PMP) & G (act as MP)



dG = € üi dxi



dG = € (dG/dni) dxi


{ inside brackets differentiation is partial } at constant P,T,ni≠i



Effect of T


dü/dT = -(dst/dni) at constant P


= - s'i



Effect of P


dü/dP = (dVt/dni) at constant T


= V'i

Ideal gas and real gas

Id : there is no interaction between molecule



Real : molecular interaction is there but behaves as ideal at low P and high T

Fugacity

Ideal gas


dG = RT d(lnP)


P = pressure of ideal gas



Real gas


dG = RT d(lnf)


f=effective pressure exerted in case of real gas



Ideal gas


∆G = G2 - G1 = RT ln(P2/P1)



Real gas


∆G = G2 - G1 = RT ln(f2/f1)



For ideal gas f=P


For real gas f≠P



Standard state for fugacity


Low pressure P°


f°=P°



G - G° = RT ln(f/f°)



If p°→0


f/p = 1



If p↑,f↑ real condition exist


f≠p


Fugacity coefficient ∅

= fugacity of gas / pressure of ideal gas



∅ = f/p



Real gas approaching towards ideality


∅→1


f→p


p° →0



Gas is far from ideality


∅ → 0


f↑ , p°↑



If p→0


f°=p°


∆G = -∞

Calculation of fugacity using compressibility factor Z

Z= volm of real gas / volm of ideal gas



d(lnf/p) = (Z-1)/P dP



ln∅ = Int (0toP) (Z-1)/P dP

Calculation of fugacity using Residual Molar Volm (alpha)

Alpha = volume of gas - volume occupied by ideal gas



Alpha = V - RT/P



V = ZRT/P



Alpha = (Z-1) RT/P



As P↑,Z low


& P↓,Z high



Int(0toP) alpha dP = RT ln(f/p)

Calculation of fugacity using H and s

ln(f/f°) = (H-H°)/RT - (S°-S)/R



f=∅p, f°=p°



H → real case


H° → ideal case



Effect of T


dlnf/dT = H°-H/RT²


Here f° not comes because its constant



T↑,H↑,(H°-H) ↓, f↓



Effect of p


dlnf/dP = V/RT

Standard case of fugacity

G-G° = RTln(P/P°) + RT ln∅



Change in Gibbs free energy for real gas =


Change in Gibbs free energy for ideal gas + RT ln∅



RT ln∅ → Due to intermolecular forces



∅ = 1, f=p


RT ln∅ = 0


∆G=∆G°



∅ <1


∆G < ∆G°



p→0, ∅→1,real gas → ideality


p→∞, ∅→0,real gas far from ideality

Fugacity in solid and liquid

∆G = Gs - Gv = RT ln (fs/fv)



At equilibrium


∆G = 0


Gs =Gv


(fs=fv)



For liquid


(f l=fv)

Calculation of fugacity in solids and liquids

At low VP


P→ low


Pv → low


At equilibrium


P=Pv


fv = Pv = f l



At low VP,


ln(f/fs) = V/RT (P-Ps)


Activity or Relative fugacity



ai

Ratio of fugacity to the fugacity in standard state for pure substances



ai = f(i)/f°(i)



∆G = RT ln(a)



Effect of T


dlna/dT = H°-H/RT²



Effect of P


dlna/dP = V/RT


Or


lna = V/RT(P-P°)

Fugacity in solution



f" = f cap


G' = G bar

For pure solution


dG = RT d(lnf)



For real mixture


dG' = RT d(lnf")



f"i = dfti/dni



fi = fugacity in pure solution


f"i = fugacity in real mixture



düi = RT d lnf"i, for real solution




düi = d G"i = RT dlnf"i


dlnf"i = V/RT dp"i



On integrating


ln f"I = P/RT Int (0to1) Vdyi



dln(f"i/P) = (Vyi/RT-1/p) dp ------(1)



ln(f"i/P) = Int (0top) (Vyi/RT-1/p) dp




From eq (1)



P = P"i/y and V = V"i/yi



Then


dln(f"i/P"i) = (Vi/RT-1/p) dp



For ideal mixture

Pure mixture


V"i = Vi



Ideal pure mixture


Vi = RT/P



ln ( f"i/p'i) = 0


f"i = p'i


fugacity of i in mixture = partial pressure of i for ideal mixture

Volumetric property of fluid

dV/V (differentiation is partial) = ßdT - KdP

Actual flame temp

<Theoretical Flame Temp


<Adiabatic Flame Temp

Troutons ratio

K= ∆Hn/RTn ≈ 10



Here 10 is troutons no.