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    CHEM 155 Basic Physical Chemistry(2, 1, 2)

    1

    Introduction to Physical Chemistry: Defnition,Structure o Science, Classifcations; Laws,y!otheses, "heories an# $o#els%

    States of Matter I& Classifcation; Structure an#Pro!erties o matter; "y!es o systems; State 'arialesan# *uations o state%

    Thermodynamics I& "he +irst law, eat Ca!acity,nthal!y an# "hermochemistry%

    Chemical Kinetics I& lementary Chemical -inetics,Basic Laws, .ect o "em!erature an# the /rrheniuse*uation%

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    MATTE

    States o $atter, Structure (the waysomethin0 is !ut to0ether) an# Pro!erty

    State an# ariales o a System

    *uation o State

    as Laws

    -inetic theory o ases

    3eal ases

    !

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    States o matter

    Matter " #e$nition:

    /00re0ation o atoms4ions4molecules which come withinthe sco!e o human e5!erience i%e% any sustance thathas mass an# occu!ies s!ace%

    States of Matter:

    $atter e5ists in one o the ollowin0 si5 states #ue to theener0y o its !articles& Gaseous, Liquid, Solid, Plasma,Bose-Einstein an# Filament. "he states o matter are also

    6nown as !hases o matter or states o a00re0ation%

     "he #i'ision o matter into states is not always sim!le%ow, or e5am!le, shoul# chocolate s!rea# e consi#ere#%Some scientists elei'e that the so calle# colloi#s shoul#

    e consi#ere#%

    %

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    /ssi0nment&

    1) 7hat is Physical Chemistry8

    2) 7hat are the classifcations in science8

    9) :sin0 a #ia0ram illustrate the structure oscience

    ) 5!lain the ollowin0 terms&

     Laws  y!otheses  "heories  $o#els

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    +our states o matter

    Base# u!on !article arran0ement

    Base# u!on ener0y o !articles

    Base# u!on #istance etween!articles

    5

    $atter is ma#e u! o !articles which are in

    continual ran#om motion

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    State #eterminant Structureas

    (sim!lest

    state o

    matter)

    • -inetic ener0y is more

    im!ortant than !otential

    ener0y%

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    States o matter Soli#s

    •Particles o soli#s areti0htly !ac6e#, 'iratin0

    aout a f5e# !osition

    •Soli#s ha'e a #efnite

    sha!e an# a #efnite'olumeeat

    '

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    States o matter Li*ui#

    Particles o li*ui#s areti0htly !ac6e#, ut arear enou0h a!art to

    sli#e o'er one another%

    Li*ui#s ha'e an

    in#efnite sha!e an# a#efnite 'olume%

    eat

    (

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    States o matter as

    Particles o 0ases are'ery ar a!art an#mo'e reely

    ases ha'e anin#efnite sha!e an#

    an in#efnite 'olume

    eat

    )

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    Phase chan0es

    #escri*tion ofPhase

    Chan+e

    Term forPhase

    Chan+e

    Heat Mo,ement#urin+

    Phase Chan+e

    Solid toli-uid

    Meltin+Heat +oes intothe solid as it

    melts./i-uid tosolid

    0reein+Heat lea,es theli-uid as itfreees.

    12

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    Phase chan0es

    Descri!tiono PhaseChan0e

     "erm orPhase

    Chan0e

    eat $o'ementDurin0

    Phase Chan0e

    Li*ui# to0as

    a!ori?ation(oilin0 an#e'a!oration)

    eat 0oes into theli*ui# as it'a!ori?es%

    as to

    li*ui# Con#ensation

    eat lea'es the 0as

    as it con#enses%

    Soli# to0as

    Sulimationeat 0oes into thesoli# as it

    sulimates%

    11

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    States o matter Plasma

    / !lasma is anioni?e# 0as%

    / !lasma is a 'ery

    0oo# con#uctor oelectricity an# isa.ecte# y ma0neticfel#s%

    Plasmas, li6e 0ases,ha'e an in#efnitesha!e an# anin#efnite 'olume%

    Plasma

    1!

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    States o matter

    S@L

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    Pro!erty

    / !ro!erty is an essential or #istincti'e attriute (*uality) o somethin0; a *ualityor characteristics that somethin0 has

    / !ro!erty cannot e a unction o the!ast history (!re'ious con#itions un#erwhich it has e5iste#) o a system; it#e!en#s only on the con#itions at thetime o consi#eration

    1&

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    State unction

    State 0unction& /ny system !ro!erty (measurale!hysical characteristic o a system, in#e!en#ent o how)#etermine# e5clusi'ely y the 'alues o the initial an#fnal states% 5am!les are :, , /, ", P, etc

    Path 0unction& 3elate to the !re!aration o the state%5am!les, ener0y transere# as heat  an# work  that is#one in !re!arin0 a state

     "hermo#ynamic lea#s to the #efnition o a##itional!ro!erties that can also e use# to #escrie the states oa system, an# are themsel'es state 'ariales% /, , %%

    14

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    Basic conce!ts o thermo#ynamics

     "he stu#y o the ow o heat or anyother orm o ener0y into or out o asystem as it un#er0oes a !hysical orchemical transormation%

     "hermo#ynamics #eals with the inter

    con'ersion o 'arious -in#s o ener0yan# chan0es in !hysical !ro!erties thatare in'ol'e#%

    1'

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     "hree em!irical laws

     "he stu#y o thermo#ynamics is ase#on three roa# 0eneralisations #eri'e#rom well estalishe# e5!erimental

    results

     "hese 0eneralisations are 6nown as the

    +irst, Secon# an# "hir# law othermo#ynamics

    1(

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    Sco!e o thermo#ynamics

    $ost o the im!ortant laws o Physical Chemistrycan e #eri'e# rom the laws othermo#ynamics%

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    Limitations othermo#ynamics "hermo#ynamics is a!!licale to macrosco!ic

    systems consistin0 o matter in ul6 an# not to

    microsco!ic systems o in#i'i#ual atoms ormolecules%

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     "hermo#ynamic systems

    / !art o the !hysical uni'erse that isse!arate# rom the rest o the uni'ersey real or ima0inary oun#aries un#er

    consi#eration or #iscussion%

    !1

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    omo0eneous systems

    / homo0eneous System is the system that isuniorm throu0hout

    / homo0eneous system is ma#e o one !hase

    only

    5am!les are & a !ure sin0le soli#, li*ui# or 0as,mi5tures o 0ases, an# true solution o a soli# in

    a li*ui# / !hase is a homo0eneous, !hysically #istinct

    an# mechanically se!arale !ortion o a system

    !%

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    etero0eneous systems

    / hetero0eneous system is one whichconsists o two or more !hases%

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     "y!es o thermo#ynamic systems!5

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    Close# system

    / close# system is one which cannottranser matter ut can transer ener0yin the orm o heat, wor6 an# ra#iation to

    an# rom its surroun#in0s%

     "he oun#ary o a close# system is

    seale# ut not insulate#%

    !'

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    @!en system

     "hereore, an o!en system is one whichcan transer oth ener0y an# matter toan# rom its surroun#in0s%

     "he oun#ary o an o!en system is o!enan# uninsulate#%

    !(

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    5tensi'e !ro!erties

    / !ro!erty that #oes #e!en# on the*uantity o matter !resent in the system%

    Some e5am!les o e5tensi'e !ro!ertiesare 'olume, numer o moles, enthal!y,entro!y, an# is ree ener0y%

    %1

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    State o a system

    / thermo#ynamic system is sai# to e in acertain state when all its !ro!erties are f5e#%

     "he un#amental !ro!erties which #etermine

    the state o a system are !ressure (P),tem!erature ("), 'olume (), mass an#

    com!osition%

    Since a chan0e in the ma0nitu#e o such!ro!erties alters the state o the system, theseare reerre# to as State 'ariales  or Stateunctions or "hermo#ynamic !arameters%

    %&

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    State o a system

    / chan0e o system rom the initial stateto the fnal state (2n# state) will eaccom!anie# y chan0e in the state

    'ariales%

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    *uation o states

     "he eha'iour o a 0aseous system can e #escrie#an# !re#icte# mathematically as

    P f (",, n) (1)

     "he !ressure P, is the #e!en#ent 'ariale an# thereare three in#e!en#ent 'ariales, ", an# n% "heletter f  stan#s or the unctional relationshi!%

    *n (1) !henomeno0ically summari?es em!iricaloser'ation calle# laws or rules i%e% reect someas!ect o the eha'iour o nature an# must thereoree correct (within limits o e5!erimental error)%

    %4

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    *uation o states%'

     "he e*uation o state or one mole o a!ure 0as is&

    P 3"

    where 3 is 0as constant%

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    De!en#ent an# in#e!en#ent 'ariales

    %(

     "he 'ariales (such as P an# ") whichmust e necessarily s!ecife# to #efnethe state o a system, are calle#

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    *uilirium states

    %)

    / system in which the state 'ariales ha'econstant 'alues throu0hout the system issai# to e in a state o thermo#ynamice*uilirium%

    If the frictionless piston is stationar, the state of the!as can "e speci#ed " !i$in! the $alues of pressure

    and $olume.

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    Criteria or e*uilirium&1

     "he tem!erature o the system must euniorm an# must e the same as that othe surroun#in0s (thermal e*uilirium)

     "he mechanical !ro!erties must e uniormthrou0hout the system (mechanicale*uilirium)

     "he chemical com!osition o the systemmust e uniorm with no net chemical

    chan0e (chemical e*uilirium)

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     "hermo#ynamic !rocesses&!

    7hen a thermo#ynamic system chan0esrom one state to another, the o!erationis calle# a Process%

    / !rocess in'ol'es chan0e in con#itions(tem!erature, !ressure an# 'olume)%

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    /#iaatic !rocesses&&

     "hose !rocesses in which no heat owsinto or out o the system, are calle#a#iaatic !rocesses%

    /#iaatic con#itions can e a!!roache#y carryin0 the !rocess in an insulate#

    container such as Fthermos ottle% i0h'acuum an# hi0hly !olishe# suraceshel! to achie'e thermal insulation%

    +or an a#iaatic !rocess #* E

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    Basic thermo#ynamic !rocesses&'

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    Cyclic !rocess&(

    7hen a system in a 0i'en state 0oesthrou0h a numer o #i.erent !rocessesan# fnally returns to its initial state, the

    o'erall !rocess is calle# a cycle or cyclic!rocess%

    +or a cyclic !rocess # E, # E%

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    Cyclic !rocess&)

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    3e'ersile an# irre'ersile !rocesses

    52

    / thermo#ynamic re'erse !rocess is one thatta6es !lace infnitesimally slowly an# its#irection at any !oint can e re'erse# y aninfnitesimal chan0e in the state o thesystem%

    / re'ersile !rocess !rocee#s rom the initialstate to the fnal state throu0h an infniteseries o infnitesimally small sta0es%

    /t the initial, fnal an# all interme#iatesta0es, the system is in e*uilirium state%

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    3e'ersile an# irre'ersile !rocesses

    51

    7hen a !rocess 0oes rom the initial tothe fnal state in a sin0le ste! an#cannot e carrie# in the re'erse or#er, it

    is sai# to e an irre'ersile !rocess%

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    3e'ersile an# irre'ersile !rocesses

    5!

    (a) 3e'ersile e5!ansion occurs y #ecreasin0 the!ressure on the !iston y infnitesimal amounts

    ()

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    3e'ersile an#

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    =ature o heat an# wor65&

    /"& is a transer o ener0y as a resulto a tem!erature #i.erence etween thesystem an# the surroun#in0s

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    7or655

    7or6 is a transer o ener0y that can euse# to chan0e the hei0ht o a wei0htsomewhere in the surroun#in0

    @nly two ways in which the ener0y o aclose# system can e chan0e#& ytranserrin0 ener0y as wor6 or heat

    7e shall reer the term Fwor6 ormechanical wor6 which is #efne# as orceG #istance

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    :nits o heat54

    S< unit o heat is Houle ( I)

     "he unit o heat, which was use# or manyyears, is calorie (cal)

    / calorie is #efne# as the *uantity o heatre*uire# to raise the tem!erature o 1 0ramo water y 1J C in the 'icinity o 1K JC

    1 Houle E%29 calories

    1 calorie %1M I

    1 6cal %1M 6I

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    Si0n Con'ention o eat5'

     "he symol o heat is *

    *

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    Si0n con'ention or heat ow in a system

    5(

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    Si0n Con'ention o 7or65)

     "he symol o wor6 is w

    w

    Summary o Si0n

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    Summary o Si0nCon'entions

    42

    eat ows into thesystem, * is N'e

    eat ows out o thesystem, * is >'e

    7or6 is #one on thesystem, w is N'e

    7or6 is #one y thesystem, w is %$e

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    Pressure>olume 7or641

    $echanical wor6 is #efne# as orcemulti!lie# y the #istance throu0h whichthe orce acts

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    Pressure>olume 7or64!

    Consi#er a 0as containe# in a cylin#er ftte#with a rictionless !iston% "he !ressure (orce!er unit area) o the 0as, P, e5erts a orce onthe !iston% "his can e alance# y a!!lyin0

    an e*ual ut o!!osite !ressure rom outsi#eon the !iston (Pe5t)%

    3ememer that it is the e5ternal !ressure(Pe5t) an# not the internal !ressure o the 0as

    itsel which is use# in e'aluatin0 wor6% "his istrue whether it e e5!ansion or contraction%

    Pressure>olume 7or6

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    Pressure olume 7or6(5!ansion)

    7or6 orce G #istance

    w = f × l 16

    Since pressure is force per area,f = P

    ext  × A !6

    &here ' is the cross-sectionalarea of the piston,

    +rom (1) an# (2),

    w = Pext 

     × A x l 

    w = - Pext 

     ×

    78

    4%

    Since the system (0as) is #oin0 wor6 on the

    surroun#in0s (!iston), it ears a >'e si0n%

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    Pressure>olume 7or6 (Com!ression)

    Similarly, wor6 #one in com!ression o a 0as can

    also e calculate#%

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    Class e5ercise45

    Calculate the !ressure'olume wor6#one when a system containin0 a 0ase5!an#s rom 1%E litre to 2%E litresa0ainst a constant e5ternal !ressure o1E atmos!heres%

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    $a5imum wor6 #one in re'ersile e5!ansion

    '%

    (a) "he re'ersile wor6 o e5!ansion; () "heirre'ersile wor6 #one y the 0as when the e5ternal!ressure is at once #ro!!e# to the fnal 'alue %

    $a5imum wor6 #one in re'ersile

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    $a5imum wor6 #one in re'ersilee5!ansion

    '&

    7or6 #one is much less in theirre'ersile e5!ansion than in there'ersile e5!ansion%

     "hus mechanical wor6 is not a stateunction as it #e!en#s on the !ath ywhich the !rocess is !erorme# ratherthan on the initial an# fnal states%

     

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    $a5imum wor6 #one in re'ersilee5!ansion

    '5

    7or6 #one in the re'ersile e5!ansion o a 0as is thema5imum wor6 that can e #one y a system (0as

     "his is ecause&

    wor6 always #e!en#s on Pe5t; the lar0er the Pe5t the more

    wor6 is #one y the 0as% But the Pe5t on the 0as cannot e more than the !ressure

    o the 0as, P0as or a com!ression will ta6e !lace% "hus the

    lar0est 'alue Pe5t can ha'e without a com!ression ta6in0

    !lace is e*ual to P0as% But an e5!ansion that occurs un#er

    these con#itions is the re'ersile e5!ansion% "hus, ma5imum wor6 is #one in the re'ersile e5!ansion

    o a 0as%

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    Symol re!resentation o internal ener0y an# si0n con'entions

    ''

     "he internal ener0y o a system is re!resente#y the symol (Some oo6s use the symol :)%

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    Sy o e! ese a o o e a e e 0yan# si0n con'entions

    '(

    in

    O is N'e i   is 0reater than in an# >'e

    i   is less than in%

    / system may transer ener0y to or rom

    the surroun#in0s as heat or as wor6, or

    : it i t l

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    :nits o internal ener0y

    ')

     "he S< unit or internal ener0y o asystem is the Houle (I)%

    /nother unit o ener0y which is not an S<unit is the calorie,

    1 cal %1M I%

    +i t l th # i

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    +irst law o thermo#ynamics

    (2

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    +irst law o thermo#ynamics

    7hen a system is chan0e#rom state / to state B, itun#er0oes a chan0e in theinternal ener0y rom / to B%

     "hus,

    O B > /

     "his ener0y chan0e is rou0htaout y the e'olution orasor!tion o heat an#4or ywor6 ein0 #one y thesystem%

    (1

    +irst law o thermo#ynamics

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    +irst law o thermo#ynamics(!

    Because the total ener0y o the system mustremain constant, we can write the +irst Law as&

    O * > wwhere * the amount o heat su!!lie# to the system

      w wor6 #one y the system

     "hus +irst Law may also e state# as& the netener0y chan0e o a close# system is e*ual tothe heat transerre# to the system minus thewor6 #one y the system%

    @ther #efnitions o frst law o thermo#ynamics

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    @ther #efnitions o frst law o thermo#ynamics

    (%

    1) 7hene'er ener0y o a !articular ty!e#isa!!ears e*ui'alent amount o anotherty!e must e !ro#uce#%

    2)  "otal ener0y o a system an# surroun#in0sremains constant (or conser'e#)

    9)

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    Some s!ecial orms o frst law o thermo#ynamics

    (&

    $athematical statement o the +irst lawo "hermo#ynamics is

    O * > w

    Case 1 & +or a cyclic !rocess in'ol'in0

    isothermal e5!ansion o an i#eal 0as

    O E * w

    Some s!ecial orms o frst law o

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    !thermo#ynamics

    (5

    Case 2 & +or an isochoric !rocess (no chan0ein 'olume) there is no wor6 o e5!ansion i%e%w E% ence O *'

    Case 9 & +or an a#iaatic !rocess there is nochan0e in heat 0aine# or lost i%e% * E%ence

    O > w i%e%, the #ecrease in internal ener0y is e5actly

    e*ual to the wor6 #one on the system ysurroun#in0s%

    Some s!ecial orms o frst law o

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    !thermo#ynamics

    (4

    Case & +or an isoaric !rocess there isno chan0e in !ressure, i%e% P remainsconstant%

    ence

    O * > w

    O * > PO

    nthal!y o a system

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    nthal!y o a system

    ('

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    :nits an# si0n con'entions o enthal!y

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    :nits an# si0n con'entions o enthal!y

    ()

    O 2 > 1

    O is !ositi'e i 2  Q 1  an# the !rocess or

    reaction will e en#othermic%

    O is ne0ati'e i 1 Q 2 an# the reaction will

    e e5othermic%

    22(0) N @2(0) 2@(l) N RM%92 6cal

     "he *uantity o heat RM%92 6cal on the ri0hthan# re!resents > O o the reaction%

    3elation etween O an# O

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    3elation etween O an# O)2

    O O N PO

    O O N On3"

    +or the reaction ,

    2+2(0) 2(0) N +2(0)

    O > 1%2 6cal4mole at 2KJ C

    Calculate O or the reaction%

    $olar heat ca!acities

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    $olar heat ca!acities

    )1

    eat ca!acity o a system is the heatasore# y unit mass in raisin0 thetem!erature y one #e0ree (- or J C) at as!ecife# tem!erature%

    7hen mass consi#ere# is 1 mole, we can

    write

    where C is #enote# as $olar heat ca!acity%

    $olar heat ca!acities

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    $olar heat ca!acities)!

     "he molar heat ca!acity o a system is#efne# as the amount o heat re*uire# toraise the tem!erature o one mole o thesustance (system) y 1 -%

     "hus the molar heat ca!acity may e#efne# as the ratio o the amount o heatasore# to the rise in tem!erature%

    :nits o heat ca!acity

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    :nits o heat ca!acity

    )%

     "he S< unit is Houles !er #e0ree !er mole

    (I - >1mol>1)%

    eat is not a state unction, neither is heatca!acity%

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    $olar heat ca!acity at constant 'olume (C')

    )&

    heat ca!acity at constant 'olume is#efne# as the rate o chan0e o internalener0y with tem!erature at constant'olume%

    #* # N P#

    Di'i#in0 oth si#es y #", we ha'e

    /t constant 'olume # E, we 0et

    dT

    PdVdE

    dT

    dq   +=

    V

    vdT

    dEC    

     

     =

    $olar heat ca!acity at constant !ressure, Cp

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    $olar heat ca!acity at constant !ressure, C p

    )5

    But, N P

    Di.erentiatin0 w%r%t% ",

    Com!arin0 (i) an# (ii)

    .....(i)dT

    PdV

    dT

    dEC   +=

    ....(ii)dT

    dVP

    dT

    dE

    dT

    dH

     p p p

       

      + 

      

      = 

      

      

    P

     pdT

    dHC    

      

      =

    3elation etween C! an# C'

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    3elation etween C! an# C'

    )4

    /t a constant !ressure !art o heat asore# y thesystem is use# u! in increasin0 the internal ener0yo the system an# the other or #oin0 wor6 y thesystem%

    7hile at constant 'olume the whole o heatasore# is utilise# in increasin0 the tem!erature othe system as there is no wor6 #one y the system%

     "hus increase in tem!erature o the system woul#e lesser at constant !ressure than at constant'olume% "hus C! is 0reater than C'%

    3elation etween C an# C

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    3elation etween C! an# C')'

     "hus, C!  is 0reater than C'  y a 0asconstant whose 'alue is M%91 I - >1 mol>1%

    +or n moles o an i#eal 0as,

    O n 5 C! 5 ("2  "1)

    R CC v p   +=R CC v p   =−

    v

     p

    C

    Cγ  =

    /#iaatic e5!ansion o an i#eal 0as

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    # aa c e !a s o o a #ea 0as

    )(

    / !rocess carrie# in a 'essel whose walls are!erectly insulate# so that no heat can !assthrou0h them, is sai# to e a#iaatic%

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    /#iaatic e5!ansion o an i#eal 0as

    ))

    +or a#iaatic e5!ansions,γ

    2

    1

    1

    2

    V

    V

    P

    P   

      

     =

    γ

    22

    γ

    11   VPVP   =

    k PV

    γ

    =

    Com!arison etween isothermal an# a#iaatic e5!ansions

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    ! !

    122

     "he #i.erence etween the two !rocesses is &in an isothermal !rocess, tem!erature o asystem remains constant while in an a#iaatic!rocess, tem!erature must chan0e%

    P constant (Boyles law)

    PS  constant (/#iaatic

    e5!ansion)

    7or6 #one in a#iaatic re'ersile e5!ansion

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    !

    121

    7ma5  P(2 > 1)

    7hen "2 Q "1, wma5 is ne0ati'e ecause 1 > is

    ne0ati'e% "his means that wor6 is #one on the0as%

    7hen "2  T "1, wma5  is !ositi'e which means

    that wor6 is #one y the 0as%

    γ1

    )TT(R nW   12mx −

    −=