Graphical and Computational Analysis of
the Vibrations of Triatomic Molecules.
by
Nicholas G. Fulton
A thesis subm itted to the
U N IV ER SITY OF LONDON
for the degree of
DOCTOR OF PHILOSOPHY
ProQuest Number: 10016820
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A b stra ct
T h e v ib ra tio n a l m o tion s of tria to m ic m olecules a t low energies are well s tu d ie d
b o th e x p erim en tally and th eoretically. A dvances in co m p u te r c ap a b ility hav e
m a d e it possible to perform fully q u a n ta l calcu lation s a t ever higher energies,
w here th e m otions are less well know n an d often classically chaotic. E x p e rim e n ts
a t th e se energies freq u en tly give very co m plicated resu lts, for ex am p le th e p h o
to d isso ciatio n s p e c tru m of w hich has yet to be fully exp lained. T ra d itio n a lly
m uch th e o re tic al effort has been co n ce n trate d in rep ro d u cin g tra n sitio n energies
seen ex p erim en tally. G rap h ical an d c o m p u ta tio n a l tech n iq u es p resen ted h ere are
aim ed a t th e analysis of th e w avefunctions, w hich are often calcu la ted w ith th e
eigenenergies, b u t n o t stu d ie d so thoroughly.
A d iscrete variable re p re se n ta tio n (D V R ) m e th o d for c alcu la tin g large a m p li
tu d e v ib ratio n s in sy m m e trised R ad au co ord inates is p resen te d an d ap p lied to
w ater. T h e eigenenergies are com pared w ith o th e r calcu latio n s, and w avefunc
tions analysed g rap h ically to find th e im p o rta n t m otion s. Possible convergence
pro blem s are th e n discussed w ith reference to th e local m od e 0 - H s tre tc h .
A nalysis of n o rm al an d local m ode v ib ratio n al b eh av io u r of H3 an d D3 is p re
sen ted w ith discussion as to how topological con sid eration s of th e con fig uration
p o te n tia l can p re d ic t th e likely typ es of m otion a t low energies. W avefunctions
are ex am in ed g rap h ically an d lo calisation is co m pared to th a t of a sim ilar clas
sical sy stem .
M etho ds for stu d y in g high a m p litu d e v ib ratio n s are p resen ted an d ap p lied
to H ^. New typ es of w avefunction localisation are show n, an d th e ir lifetim es
and period s in v estig ated . A new fu n ctio n is defined w hich gives a m easu re of
th e degree of lo calisatio n an d th e way in w hich w avefunction a m p litu d e m ay
tra n sfe r betw een different m odes of localisation.
C lassical analysis of is perfo rm ed in 2D an d co m p ared to q u a n ta l cal
cu latio ns. T h e b eh av io u r of th e sy stem at different energies is discussed an d
b ifu rcatio n d iag ram s are ex am in ed , showing th e a p p e a ra n c e of new m otions.
I m p o rta n t m otio ns are th e n discussed an d considered in th e e x p lan atio n of th e
C o n ten ts
A b stra ct
3
List o f F igures
7
List o f Tables
11
A ck n ow led gem en ts
12
1 In trod u ction
13
1 . 1 M odern A pproaches to T h e o r y ... 13
1.2 M olecular S p e c tro s c o p y ... 14
1.3 V ib ratio n al S p e c t r a ... 16
1.4 C a l c u la t io n s ...18
1.5 Hg an d th e C a rrin g to n -K e n n ed y s p e c tru m ...22
1 . 6 C o m p u ta tio n a l A d v a n c e s ... 28
2 Q uantum M eth o d s
30
2.1 V ib ra tio n a l S ep aratio n an d C oo rd in ates ... 302.2 F B R H a m i lto n i a n ... 31
2.3 Basis F u n c t i o n s ...32
2.4 F B R to D V R T r a n s f o r m a t i o n ... 33
2.5 Solution S c h e m e ...35
2.6 Q u a n ta l P h a se S p a c e ...36
3.2 P h ase S p a c e ...40
3.3 Lyapunov E x p o n en ts ... 41
3.4 Successive C rossing P l o t s ...42
3.5 B i f u r c a t i o n s ... 42
3.6 R e tu rn M aps ... 43
4 W ater
44
4.1 I n t r o d u c t i o n ... 444.2 B a c k g r o u n d ... 45
4.3 A S y m m etrised R ad au D V R ... 46
4.4 R esults an d D is c u s s i o n ...49
4.5 C o n c l u s i o n s ... 75
5
Hg and D j N orm al and Local M odes
76
5.1 I n t r o d u c t i o n ... 765.2 B a c k g r o u n d ... 77
5.3 T h e o r y ...79
5.4 R esults a n d D is c u s s i o n ...81
5.5 C o n c l u s i o n s ... 89
6
Q uantum P h a se Space S tru ctu res
91
6.1 W avepacket D ynam ics, C o rrelatio n F unctions an d Pow er S p ectra. 91 6.2 Jacobi H a m i l t o n i a n ... 936.3 R e s u l t s ...94
6.4 P h ase Space S tru c tu re , C orrelatio n F unctions an d Power S p ectra. 95 6.5 B and W a v e f u n c t i o n s ... 99
6 . 6 R ep ea ted P h ase Space F e a tu re s... 107
6.7 S y m m e try C on sideratio ns ... 108
6 . 8 R o bu stn ess of P o t e n t i a l s ... 109
7 R ecu rren ce and T ransport fu nction s
115
7.1 I n t r o d u c t i o n ... 115
7.2 T h e o r y ...116
7.3 R e s u l t s ...116
7.4 R ecu rrence F u n ctio n as a L ocalisation Searching Tool ... 117
7.5 O dd P a rity E ig e n sta te A n a l y s i s ...123
7.6 T ran sp o rt an d D issociation M echanism s ... 130
7.7 B ending M otions an d Q u a n tu m B if u r c a t i o n s ... 133
7.8 C arrin g to n -K e n n ed y S p e c t r u m ...137
7.9 C o n c l u s i o n s ... 141
8 C lassical C alculations: B ifu rcation and R etu rn M aps
143
8.1 T ra je c to ry P ro g ra m ... 1438.2 P oincare Surfaces of S e c t i o n ... 144
8.3 B ending P erio dic O rb its an d B i f u r c a t i o n ...151
8.4 T ra je c to ry R e tu rn M a p s ...159
8.5 Q u an tal-C lassical C o r r e s p o n d e n c e ...160
8 . 6 P o te n tia l R o b u s t n e s s ...166
8.7 C o n c l u s i o n s ... 168
9
Further P o ssib ilities
169
9.1 Q u an tal C a l c u l a t i o n s ...1699.2 Q u a n ta l P h ase S p a c e ...169
9.3 C lassical an d Q u a n ta l B i f u r c a t i o n s ... 170
9.4 C lassical C a lc u la tio n s ... 171
9.5 S u m m a r y ...171
List o f F igu res
1 . 1 C arrin g to n -K en n ed y H3 p h o to disso ciation e x p e rim e n ta l a p p a ra tu s , 23
2 . 1 G eneral co o rd in a te s y ste m ...31
4.1 F in ite D V R grid p r o b l e m s ...50
4.2 B ending s ta te s of w a t e r ...69
4.3 S y m m etric s tre tc h sta te s of w a t e r ...69
4.4 O dd an d even p a rity a n tisy m m e tric stre tc h s ta te s of w ater . . . . 70
4.5 Even p a rity local m ode s ta te s of w a t e r ... 71
4.6 O dd p a rity local m ode w avefunctions of w a t e r ...72
4.7 C om parison of D V R grid r a n g e s ... 74
5.1 C lassical m otio ns in th e H enon-H eiles s y ste m ...78
5.2 C om bined D j w avefunctions showing I li,2 , 3 lo calisation: iV = 4 . 83 5.3 C om bined D j w avefunctions showing IIi,2 , 3 lo calisation: TV = 5 . 85 5.4 C om bined D j w avefunctions showing IIi,2 , 3 lo calisation: TV = 6 . 85 5.5 D3 w avefunctions w ith circu lar localisation: TV = 5 ...8 6 5.6 D3 w avefunctions w ith circu lar localisation: TV = 6 ... 87
5.7 D3 (0, 4^) F p a ir w avefunctions...87
5.8 D3 (1,3^) E p a ir w avefu nctio ns...8 8 5.9 D3 co m b in atio n of (1,3^) an d (0, s ta te s ...8 8 5.10 D3 co m b in atio n of (0,6~^) an d (0,6^) s ta te s ... 89
6.1 H usim i d is trib u tio n an d w avefunction of a horseshoe sta te . . . 96
6.3 C o rrelatio n functio ns of w avepackets cen tred on horseshoe a n d
elep h an t foot m o tio n s ... 98
6.4 Power s p e c tra of w avepackets cen tred on horseshoe an d elep h an t
foot m o tio n s...1 0 0
6.5 B an d w avefunctions of horseshoe an d elep h an t foot b end ing m o tio n s 101
6 . 6 H usim i d is trib u tio n a n d w avefunction of a sy m m e tric s tre tc h s ta te 103
6.7 C o rrelatio n fun ctio n an d pow er sp e c tru m of sy m m e tric s tre tc h
m o tio n ...104
6 . 8 B an d w avefunctions showing sy m m e tric s tre tc h m o t i o n ... 105
6.9 C o rrelatio n fu n ctio n an d pow er sp e c tru m of th e o re tic a l sy m m e tric
s tre tc h m o tio n ...106
6.10 H usim is an d eigenfunctions of four sta te s in a pow er sp e c tru m b an d . 107
6.11 H usim i d is trib u tio n an d w avefunction of a ele p h a n t foot band
w avefu nction...108
6.12 Power s p e c tra for sy m m e trised horseshoe ben d in g m o tio n ...110
6.13 S y m m etrised horseshoe b en d in g m o tio n w avefu nction s...I l l
6.14 C o rrelatio n fu n ctio n an d pow er sp e c tru m of D IM elep h an t foot
m o tio n ...1 1 2
6.15 B and w avefunctions of DIM p o te n tia l elep h an t foot m otion. , . .1 1 3
7.1 H3 recu rren ce fu n ctio n plot arou nd th e ab so lu te m in im u m ...119
7.2 H3 co rrelatio n fu n ctio n and pow er sp e c tru m of horseshoe m o tio n 120
7.3 D iagram to show how localisation increases w ith fin ite m o m en tu m . 120
7.4 H3 recu rren ce fu n ctio n plot for po int n ear d isso ciation channel. . 121
7.5 H3 co rrelatio n fu n ctio n an d pow er sp e c tru m of e le p h a n t foot m o tio n 122
7.6 H3 co rrelatio n fu n ctio n an d pow er sp e c tru m of unknow n m otio n. 124
7.7 H3 b an d w avefunctions of a new m o tio n ... 125
7.8 H3 recu rren ce fu n ctio n plot for p o in t n ear eq u ilib riu m po in t. . . . 126
7.9 H3 co rrelatio n fu nctio ns and pow er s p e c tra of tw o m o tio n s...127
7.10 H3 b an d w avefunctions of ex cited horseshoe m o tio n s ...129
7.12 b a n d w avefunctions of in v erted h y p ersp h erical m o tio n ... 132
7.13 H3 tra n s p o rt fu n ctio n for ben ding m o tio n w avep ack ets...134
7.14 H3 co rrelatio n fu n ctio n an d pow er sp e c tru m of n o d al horseshoe
m o tio n ...135
7.15 H3 b an d w avefunctions of n o d al horseshoe m o tio n ... 136
7.16 T h eo re tic al sp e c tru m of horseshoe to n o d al horseshoe tra n sitio n s. 140
8.1 H3 P o in care surfaces of section a t T2 = 0, ^ = 90° for energies of
19600 an d 23200 c m “ ^... 145
8.2 H3 tra je c to ry a t 19600 c m “ ^ showing a ‘b ra id e d ’ horseshoe. . . . 146
8.3 H3 tra je c to ry a t 23200 c m “ ^ showing a ‘b ra id e d ’ horseshoe. . . . 147
8.4 H3 P o in care surfaces of section a t T2 = 0, 0 = 90° for energies of
26800 an d 30400 c m “ ^...148
8.5 H3 tra je c to ry a t 26800 c m “ ^ showing th e sim ple horseshoe m o tio n , 149
8 . 6 H3 P o in care surface of section a t t2 = 0, ^ = 90°... 150
8.7 H3 tra je c to ry a t 30400 c m “ ^ showing th e elep h an t foot m o tion . , 151
8 . 8 H3 P o in care surfaces of section at T2 = 0, 0 = 90° for energies of
34000 an d 37600 c m “ ^... 152
8.9 H3 tra je c to ry a t 37600 cm~^ showing th e b en t horseshoe m otio n. 153
8.10 H3 P o in care surface of section a t T2 = 0, ^ = 90° for an energy of
41200... 153
8.11 H3 P o in caré surface of section a t T2 = 0, ^ = 90°: en larged region
a t 41200 c m “ ^... 154
8.12 H3 successive crossing diag ram s at 38520 c m “ ^ an d 40210 cm ~ h . 155
8.13 H3 T -sh ap ed ben d in g tra je c to ry b ifu rcatio n d ia g ra m ...157
8.14 H3 tra je c to rie s a t 40000 c m “ ^ showing th e two ele p h a n t foot m o
tio n s... 158
8.15 H3 tra je c to rie s a t 48000 cm~^ showing th e Feshbach b en d in g m o
tio n s... 159
8.16 H3 T -sh ap ed b en d in g tra je c to ry re tu rn m a p ... 161
8.18 no dal horseshoe H usim i d istrib u tio n an d P S O S a t 33698 cm~^. 164
8.19 B ifu rcatio n m a p of th e recu rren ce fun ctio n for H j T -sh a p e d b e n d
ing m o tio n ... 165
List o f T ables
4.1 E x p erim en tal and th e o re tic a l even p a rity b an d origins of w ater . . 51
4.2 E x p erim en tal and th e o re tic a l odd p a rity b an d origins of w ater . . 60
4.3 Energies of th e 201-404 w ater even p a rity s ta te s ...67
4.4 Energies of th e 138-324 odd p a rity w ater s ta te s ...6 8
4.5 Energies of odd an d even p a rity local m o d e 0 -H s tr e t c h e s ... 72
5.1 C alcu lated b an d origins, in cm~^, for D3 below th e b arrie r to
linearity. H j b an d origins are given for a sim ilar energy region. . 82
5.2 Q uasi-deg enerate v ib ratio n al tria d s in th e s tru c tu re of ben ding
[ v i =0^V2= N ) polyads of H3 an d D3 ... 84
7.1 Energies of b an d centres in th e sm o othed pow er s p e c tra for th e
A ck n o w led g em en ts
I d like to s ta r t by th a n k in g J o n a th a n Tennyson for being a g re a t sup ervisor. His
en co u rag em en t a n d friendliness have m ad e m y P hD b o th fru itfu l an d enjoyable
an d allowed m e th e freedom to try ou t new techniques an d ideas.
I ’d also like to th a n k Jam es H enderson for supplying m e w ith his H3 w ave
fu n ctio n s w hich w ere th e invaluable source of d a ta for g rap h ic al and n u m erical
analysis. I also th a n k him for being th e m an on th e inside a t U LCC .
I w ould like to th a n k D im a Sadovskii for help in th e w ritin g of c h a p te r five
an d th e enjoyable co llab oratio n on th e non-linear m odes of Hj" and D3 . T h e
correspo nd en ce a n d results were co m m u n icated solely by e-m ail, and I hope one
day I will m eet h im face to face.
I w ould like to express m y th a n k s to all th e people th a t I have sh ared a
ro om w ith d u rin g m y P h D , and w ould especially like to th a n k R u th Le S ueur
w hose help an d advice on m an y different su b jects has been inv aluable, a n d for
proo f-read ing th e final d ra ft of th is thesis.
I w ould like to th a n k S E R C /E P S R C for a stu d e n tsh ip , an d several g ra n ts
th a t have helped m e to a tte n d conferences. I would also like to th a n k m y p a re n ts
w ho have helped m e to survive th e expense of London by keeping th e re n t on
th e ir flat a t a m inim u m .
F in ally I ’d like to th a n k G onzalo G arcia de P o lav ieja for help in w ritin g
c h ap ters 6 and 7. His visit to E ng land in 1993 led to a co llab o ratio n a n d a
frien d sh ip w hich has given m e m uch insight into th e d y n am ics of m o lecu lar
C h ap ter 1
In tro d u ctio n
1.1
M o d e r n A p p r o a c h e s to T h e o r y
In m an y fields of th e o re tic al physics an d ch em istry th e re has been a change of
em p h asis on how solutions to problem s are d eterm in ed . T h is change has been
fueled alm o st en tirely by th e availab ility of m o d e rn co m p u ters. In th e p a s t,
tim e was sp en t w ith ‘pen an d p a p e r ’ deriving a n aly tic solutions to p rob lem s,
an d proposing ap p ro x im atio n s th a t w ould m ake a calcu latio n possible. Now,
a lth o u g h m any of th e m e th o d s used are based heavily on th e a n a ly tic solu tion s,
we can often use th e sheer pow er of co m p u ters to ‘n u m b er c ru n c h ’ a solution
w ith o u t having to spend so m uch tim e deriving an efficient m e th o d .
T h e lim its of th e ap p ro x im atio n s th a t were m a d e are b eg in ning to b e reach ed
because calculatio ns are so a c c u ra te th a t com parison w ith ex p erim en ts show
slight d eviation s w hich can n o t be a ttr ib u te d to th e calculation s them selves. O ne
such ex am p le is th e failure of th e B o rn -O p p en h eim er a p p ro x im a tio n [1] in vi
b ra tio n a l calcu lation s on H j an d its isotopom ers [2 ]. Also we are now able to
p erfo rm calculatio ns u n d re a m t of in previous years, o pening up new fields of
research.
T h e new app ro ach has no t only given us m ore d a ta to w ork w ith b u t also th e
tools to analyse th e d a ta . In spectroscopy, w here originally th e aim of th e o ry
th e in ten sities of tra n sitio n s, an d assign te m p e ra tu re s an d p o p u la tio n d en sities
to a sp e c tru m .
T h e increase in c o m p u ter technology has also allow ed us to ta k e a far m o re
grap h ic al ap p ro ach in w hich a b s tra c t concepts such as w avefunctions can be
p lo tte d . T h is can give us m uch insight in to th e physical m ech an ism s w hich
m ak e tra n sitio n s occur th a t e x p e rim e n ta l an d sim pler calcu latio n s could only
p red ic t.
1.2
M o le c u la r S p e c tr o s c o p y
M olecular sp ectroscopy spans an enorm ous range of th e ele c tro m a g n e tic sp ec
tr u m d ep en d in g on th e typ es of tran sitio n s th a t th e sy stem of s tu d y is u n
dergoing. In th e high frequency rang e electron e x c ita tio n occurs, w ith s p e c tra
ran g in g from th e visible light ran ge for o u te r electron s to X -rays for e x c ita tio n of
th e in n e r shell electrons. A t in frared w avelengths m o lecular s p e c tra a re p re d o m i
n a n tly d u e to ro -v ib ratio n al tran sitio n s; a t m icrow ave frequencies th e tra n s itio n s
are m a in ly due to ro ta tio n s, an d a t lower energies still, changes in th e spin of th e
electro n s an d nuclei can be found in th e rad io frequency range. T h e tra n s itio n s
are usu ally due to e ith e r changes in th e overall dipole of a m olecule, or changes
in its polarisability . T h e second of these is know n as R am an sp ectro sco p y a fte r
its founder.
T h e m o tiv atio n s for p erform in g calculations an d m easu rin g th e s p e c tra of
m olecules com e from m any fields. P ro b ab ly th e first im p o rta n t use of sp e c tra l
d a ta was in m olecular s tru c tu re work. T h e way in w hich a m o lecule v ib ra te s
an d u nd ergoes tra n sitio n s is very d ep en d e n t on th e sy m m e try an d sh a p e of th e
m olecule, an d also on th e way in w hich it is bonded. By carefully stu d y in g th e
tra n s itio n frequencies an d overall p a tte rn s of th e s p e c tru m , in fo rm atio n a b o u t
th e m olecule can be e x tra c te d . For exam ple th e s tre n g th of a b o n d d ire c tly af
fects th e frequency of v ib ratio n al tra n sitio n s along th a t bond, an d th e s y m m e try
of th e m olecule can give c e rta in p a tte rn s in th e sp ectru m .
calcu la tio n an d co m parin g th e resu lt w ith e x p erim en tal d a ta . W h en th e tw o
m a tc h , average b o nd length s, fu n d a m e n ta l frequencies an d overall s tr u c tu re can
b e confirm ed.
O ne of th e n ex t m o st im p o rta n t uses of sp ectra l d a ta is in a tm o sp h eric m o d
eling. T h e s p e c tra of n itro g en , oxygen, carbon dioxide, w ater, and m an y tra c e
gases including su lp h u r dioxide, m e th a n e , ozone an d C F C s, are exten sively used
to e s tim a te op acities a t different heigh ts in th e atm o sp h ere. T his in fo rm atio n
helps in th e u n d e rsta n d in g of how h eat is tran sferred to an d from th e E a r t h ’s
surface.
T h e well know n greenhouse effect is caused essentially by th e dense s p e c tru m
of c arb o n dioxide. Light en terin g th e E a r th ’s a tm o sp h ere from th e sun, be
ing co n c e n tra te d m ainly in th e visible sp e c tru m and n ear-in frared , passes easily
th ro u g h th e atm o sp h ere and w arm s th e surface. T h e w arm surface th e n ra d ia te s
a t m u ch longer w avelengths, w hich do no t find th e a tm o sp h ere so tra n s p a re n t.
N itrog en an d oxygen, th e two m ost ab u n d a n t atm o sp h eric gases, are b o th di
a to m ic m olecules an d do no t have very dense s p e c tra giving th e m a low opacity.
C arb o n dioxide, w hich only accounts for ab o u t 0.5 % of th e atm o sp h ere, has a
m u c h denser ro -v ib ratio n al sp e c tru m w hich absorbs stron gly in th e far in frared .
T h is m akes it abso rb th e h e a t th a t th e surface ra d ia te s, tra p p in g th e energy
in th e atm o sp h ere. A ccu rate know ledge of th e ab so rp tio n sp e c tru m of carb o n
diox id e is essential in e s tim a tin g th e m echanism s of te m p e ra tu re balan ce an d
th e effects of changes in its abu n d an ce.
Spectroscopy is also used in d eterm in in g th e po llu tio n effects of m o to r v ehi
cles by ta k in g s p e c tra of th e gases released from ex h au st pipes. T his can a ctu ally
be d one from th e side of th e ro ad as cars drive p ast, by m o n ito rin g th e sig n a tu re
ab so rp tio n and em ission features of p a rtic u la r m olecules one can e s tim a te q u a n
titie s of th e b y -p ro d u cts of com b ustion . Sim ilar tech niqu es are also im p o rta n t
in th e design of engines an d fuels w here different o p e ra tin g te m p e ra tu re s and
fuel co n ce n tratio n s can affect th e efficiency of th e b u rn in g process.
In astro n o m y th e need for a c c u ra te m olecular spectroscopic d a ta has in
scarce in space, b u t ob servations have challenged th is id ea a n d m a d e it necessary
to form new th eories to accou nt for th e ab u n dance.
In th e stu d y of stellar s tr u c tu re it was assum ed th a t sta rs are to o h o t for
m olecules to be boun d, and m odels w ere based on th e o p acity of a to m s an d th e ir
ions. T h e op acity p ro jec t [3], w hich has now been co m p lete d , was an a tte m p t to
calcu la te all th e tra n sitio n s of th e possible ato m ic species w hich could exist in
stars. T his p ro jec t calcu la ted over a m illion tra n sitio n s an d is used ex ten siv ely
in s te lla r s tru c tu re m odels, how ever in cool sta rs m olecules are now know n to
ex ist, an d p relim in ary e stim a te s for w a te r alone in d ic a te th a t th e re m ay be as
m an y as 2 0 m illion im p o rta n t ro -v ib ratio n al tra n sitio n s, w ater being on ly one of
th e m an y sm all m olecules w hich m ay b e found [4].
In th e in te rste lla r m e d iu m th e re a re also rich sources of m olecules. T h e
large neb ulae which are found in th e space betw een sta rs a re of g re a t in te re st
to astro n o m ers as th ey are th e b irth place of new stars. T h e te m p e r a tu r e of
th ese clouds is betw een 5 a n d 100 K, so m any m olecules w ould be s ta b le if th e y
ex isted . So far m an y exo tic species h ave been fo und in th e se regions, in clu d in g
long chain carb on m olecules. K now ledge of th e c h em istry of th e se regions is still
very poor, and a m ore co m p lete know ledge can only be o b ta in e d by ex am in in g
th e ab so rp tio n , an d em ission s p e c tra of th e regions to search for th e fin g erp rin ts
of c e rta in m olecules.
A t high energies th e processes w hich lead to d isso ciatio n are of in te re s t to
scien tist in vestigating reac tio n m echanism s. S pectroscopy is a v aluab le tool in
th e stu d y of how it m ay b e possible to excite a p a rtic u la r m olecule to a s ta te
w here it will yield p red ic tab le p ro d u c ts as it breaks up. T h is stu d y m a y o p en th e
doors to p ro d u ctio n line tech n iq u es in w hich a series of ex c ita tio n s can control
th e progress of a reactio n.
1.3
V ib r a tio n a l S p e c tr a
In th e calculatio n of any m o lecu lar sp e c tru m , it is n ecessary to m ak e ap p ro x
Born-O p p en h eim er a p p ro x im atio n [1] is critica l in any v ib ra tio n a l c alcu la tio n since
it sep arates electro n m o tio n from th e nu clear m o tio n. E lectro n s are very m uch
lig h te r th a n nuclei, an d th erefo re tra v e l ‘fa ste r’. T h e a p p ro x im a tio n assum es
th a t for any nuclear m otion th e electro n s will always find a con fig uratio n w hich
m inim ises th e energy in such a sh o rt tim e th a t we need n o t w orry a b o u t th e ir
m o tio n . T h is ap p ro x im atio n m akes it possible to consider a p o te n tia l energy
su rface w hich rep resents th e energy of any configuration of th e ato m s for a
p a rtic u la r electronic state. T h e v ib ratio n al p ro blem can th e n be solved using
a p u rely n uclear m o tion H am ilto n ian w ith a p o te n tia l for th e given electro n ic
s ta te . T h e p o te n tia l can be derived from e ith e r nb initio calcu latio n s of th e
electro n ic energy of a given n u clear configuration, or by fittin g to ex p e rim e n ta l
d a ta .
T h e lim its of th is fu n d a m e n ta l ap p ro x im atio n are now being reached as cal
cu latio n s becom e m o re and m ore a cc u rate. In ex p erim en ts on HD'*' disso ciation
[5] th e am o u n t of and D"*" frag m en ts d etecte d was n ot th e sam e. T h is effect
is d u e to th e preference of th e electro n to be bound to th e d e u te riu m . W ith in
th e B o rn -O p p en h eim er ap p ro x im atio n th e electron does n o t feel a difference b e
tw een th e two ato m s. In fact th e resu lt is due to th e difference in th e ra tio of
m ass betw een th e electrons an d th e ato m s for hydrogen an d d e u te riu m . T h is
gives a slightly higher bind ing energy for D th a n H and so th e electro n prefers
th e d e u te riu m to th e hydrogen ato m .
In p o te n tia l fittin g of H j , w here for a tria to m ic th e ra tio of th e m ass of th e
electro n s to th a t of th e nuclei is sm allest, fitting a single v ib ra tio n a l p o te n tia l
to th e ro -v ib ratio n al sp e c tra of th e isotopom ers H j , H2D""", D2H''' an d D j has
failed [2] due to th e breakdow n of th e B orn O p p en h eim er ap p ro x im atio n . In
sim ilar work on fittin g a p o te n tia l to w ater [6] th e ap p ro x im atio n has also been
show n to breakdow n.
O th e r problem s can arise w hen th e electronic m otion is n o t sep arab le from th e
n u clear m otion. O ne case is th a t of th e p seu d o -ro tatio n of Nag. T h is m olecule
has a d eg en e rate electron ic gro un d s ta te from which it un derg oes a Ja h n -T e lle r
e x c ita tio n th e m olecule can ‘h o p ’ from one m in im u m to a n o th e r [8 ]. W ith in
th e B o rn -O p p en h eim er a p p ro x im a tio n th is is allowed, b u t becau se th e m olecule
suffers a Jah n -T eller d isto rtio n , th e assu m ed grou nd electro n ic s ta te is a c tu a lly
m ad e up of two electro n ic sta te s. If th e m olecule undergoes one p se u d o -ro ta tio n ,
i.e. m o tio n from m in im u m one, to tw o, to th re e an d back to one, th e m olecule
does n o t re tu rn to th e original electro n ic surface an d an ad d itio n a l p h ase facto r,
know n as B erry p h ase [9], m u st be in tro d u ced to correct for th is.
1 .4
C a lc u la tio n s
T h e re are m any m odels w hich are used to ap p ro x im ate v ib ra tio n a l a n d r o ta
tio n al b ehaviou r, an d allow sim ple s p e c tra to be ex plain ed. T h e co m m o n est of
th e se m odels is th e harm o n ic oscillator m odel w hich considers v ib ra tio n s as sm all
d isp lacem en ts of th e ato m s from a global m in im u m along th e re s u lta n t n o rm al
m odes. N orm al m odes can be th o u g h t as th e basic ty pes of v ib ra tio n th a t a
m olecule can undergo. Q u a n tu m n u m b e rs can th e n be assigned to th e se m odes
an d sp e c tra l lines assigned to ce rta in tran sitio n s. T h e ro ta tio n a l b eh av io u r can
be calcu la ted using th e rig id -ro to r a p p ro x im atio n w hich assum es sim p le q u a n ti
satio n of th e ro ta tio n a l levels, w hich is th e n sup erim p o sed o n to th e energies of
th e v ib ra tio n a l tra n sitio n s.
T h e idea th a t m o tio n is q u an tised along th e n o rm al m odes does n o t alw ays
apply, an d alth o u g h th e h arm o n ic ap p ro x im atio n is only ex p ec ted to w ork a t low
energies, for som e m olecules sy m m e try p ro p erties of th e p o te n tia l or reso nan ces
betw een linear n o rm al m odes m ake th is break dow n even a t th e en erg y of th e
fu n d a m e n ta l frequencies. In th ese cases it is useful to use a n o n -lin ear n o rm al
m o d e m odel [1 0] w here th e re is im p lic it coupling betw een th e n o rm a l m odes.
T h e a p p licatio n of th is m odel to th e v ib ratio n s of H j is in v e stig ated in c h a p te r
5. In a sim ilar fashion to th e no n-linear norm al m od e m od el, local m o des can
arise a t low energies w here th e h arm o n ic ap p ro x im atio n is assu m ed to valid.
T h is s itu a tio n arises in th e v ib ratio n s of w ater an d is discussed in c h a p te r 4.
was p e rtu rb a tio n theory. W ith in th e h arm o n ic o scillator-rigid ro to r m o d el for a
given v ib ratio n al m ode, or ro ta tio n , successive ex citatio n s give reg u larly spaced
energy levels. P e rtu rb a tio n theory, for v ib ratio n s, considers sm all a d d itio n a l
te rm s in th e p o te n tia l to account for an h arm o n icities. T hese are th e n ex p a n d e d
as a Taylor series aro u n d eq u ilib riu m to give force co n stan ts th a t can be fitte d to
observed sp ectra . In a sim ilar way ro ta tio n a l co n stan ts are fitte d to th e ro ta tio n a l
beh av io u r, to in clud e effects such as Coriolis coupling. T h e te rm s them selv es give
d irec t in fo rm atio n on th e form of th e p o te n tia l an d its deriv atives a ro u n d th e
eq u ilib riu m geom etry.
O ne of th e m a in problem s of p e rtu rb a tio n th eo ry is th e assu m p tio n th a t th e
corrections to o ur ap p ro x im ate H am ilto n ian are sm all an d so th e a m p litu d e s of
v ib ratio n s m u st rem a in sm all. For som e m olecules w hich are p a rtic u la rly ‘flo p p y ’
even a t low energies th e am p litu d e of v ib ratio n s can be large. A t higher energies
all m olecules m u st undergo high a m p litu d e v ib ratio n s and m ay ex p erien ce m ore
c o m p licated m o tion s. For th is reason o th e r m eth o d s, especially th e v aria tio n a l
m e th o d [1 1], have gained favour as m o re th a n ju s t th e fu n d a m e n ta l frequencies
are in v estig ated .
B y rep resen tin g th e w avefunctions as sum s of p ro d u c ts of basis fu n ctio n s,
an d th e n diagonalising a H am ilto n ian m a trix w hich couples th e basis fu n ctio n s
to g e th e r, solutions can be found. T h e v ariatio n al p rin cip le s ta te s th a t for a
given basis set, th e calcu lated grou nd s ta te energy is an u p p e r b ou n d to th e
ex ac t energy. An im p rov em en t in th e basis set, by inclusion of m ore fu n ctio n s or
o p tim isa tio n of th e fu n ctio n al form , will give a lower energy. T h is is th e n a lower
u p p e r b o u n d to th e ex act energy. It can also be shown th a t for a p p ro p ria te ly
fo rm u la te d pro blem s th e calcu lated ex cited s ta te energies are also u p p e r bo u n d s
to th e ir corresponding ex act energies [1 2].
F ro m th is we can say th a t th e en ergy always app ro ach th e correct energ y
from above. It is th erefore possible to o ptim ise convergence by im pro vin g th e
basis sets for a given size prob lem , i.e. nu m b er of basis fun ctio ns, u n til th e
c a lc u la te d energy is m inim ised. O nce an o p tim ised basis set is found m ore basis
converges no m ore, th e exact energy is assum ed to have b een reached. T h e re are
possible pitfalls if th e energy ap p ears to be converged b u t is in fact on a ‘k n ee’
of th e convergence curve. However th is situ a tio n is n o t n o rm ally th e case for th e
grou nd sta te .
For stric t variation al beh av io u r th e in teg ratio n of th e p o te n tia l an d basis
fun ctio ns m u st be exact. If th e p o te n tia l is very com p licated a n a ly tic in te g ra tio n
m ay n o t be possible and G aussian q u a d ra tu re is em ployed.
T h e m e th o d of using o rth og on al basis functions to rep resen t a w avefunction
is n o rm ally referred to as a finite basis rep resen tatio n (F B R ) [13]. O th e r m e th o d s
exist w hich use non -o rtho go nal basis fun ctio ns, such as th e d is trib u te d G aussian
basis (D G B ) m e th o d . T his rep resen ts th e w avefunctions as G aussian fu n ctio n s
on a grid of p oints. T h e ad van tage of th is is w hen th e p o te n tia l is n o t su ite d
to a set of basis functio ns for each coo rd in ate, e.g. if th e p o te n tia l has a lot of
coupling betw een co ordin ates. T h is m e th o d is also used to c alcu la te ap p ro x im a te
q u an tisa tio n values of classical p erio dic orbits by placing th e G aussians aro u n d
th e perio dic o rb it [15].
F in ite basis m e th o d s have had m uch success in calcu la tin g energies in m an y
different ty p es of problem s. H owever one lim ita tio n w ith th e ap pro ach is th a t
only th e ground s ta te an d a b o u t th e low est 5 % of th e eigenvalues o b ta in e d are
well converged. To converge m ore v ib ratio n al levels it is necessary to ad d m ore
basis fun ction s to rep resen t th e m o tio n b e tte r an d in crease th e to ta l n u m b e r of
eigenvalues. However, if th is is done th e H am ilto n ian m a trix becom es u n m a n
ageably large an d w ith th e cu rren t c o m p u te r technology, unsolvable. To p erfo rm
th e calculatio ns it is necessary to use a techn iq ue originally developed in o th e r
fields [14] based on a finite elem en t approach.
B y tran sfo rm in g th e basis fu n ctio n so th a t th e w avefunctions are now rep
resen ted as am p litu d es a t po in ts, one can approach th e pro blem s slig htly dif
ferently. T his m e th o d is known as th e discrete variable re p re se n ta tio n m e th o d
(D V R ) allows tru n c a tio n of th e w avefunction in regions w here it will have no
m a g n itu d e because th e p o te n tia l is very high, an d hence reduces th e overall size
w avefunctions, a n d up to 50 % of calcu la ted eigenvalues m ay be converged. O ne
d raw back of th e D V R m e th o d is th a t it is n ot stric tly v aria tio n a l since th e in te
g ra tio n is not ex ac t. T h e tru n c a tio n stag e m u st also be carefully p erfo rm ed since
th e re m ay be a te m p ta tio n to in tro d u c e m an y basis fun ctio n , i.e. D V R p o in ts,
th e n tru n c a te th e pro blem to a m an ag eab le size. T h is can increase th e in accu
racy of th e rep re se n ta tio n since som e regions of th e p o te n tia l will be ignored in
th e tru n c a tio n . T h e energies can th e n be un reliable an d w rongly converged.
C lassical calcu latio n s of m o lecular v ib ratio n s form a good com p lim en t to
q u a n ta l calcu latio n s since th e y allow different asp ects of th e physical sy stem to
be in v estig ated . H owever th e m ain reason for doing classical calcu latio n s is th a t
th e y are often a quick an d easy way to g et an in itia l id ea of th e b eh av io u r of a
system .
A t low energies th e classical-q u an tal correspondence p rin cip le is n o t stro ng,
b u t classical p erio d ic o rb its often reflect th e fu n d am e n tal m o tion s. T h e n o rm al
m o de to local m o d e tran sitio n s can be p red ic ted [16] an d n on-linear m o tio n
in v e stig ated [1 0].
A t higher energies th e q u a n ta l b eh av io u r m ore closely resem bles th e classical
b e h av io u r and it is h ere th a t classical p eriod ic m otions are im p o rta n t since th e y
‘s c a r’ th e w avefunctions [17], and can give rise to stro ng spectroscopic featu res.
In sy stem s w hich are classically chaotic th e stu d y of q u a n tu m featu res has been
n ick n am ed q u a n tu m chaology.
A co m plete u n d e rsta n d in g of th e m echanism s w hich give rise to w avefunc
tio n scarring has n o t yet been found. B erry [18] and Voros [19] proposed th e
m icro can on ical h y p o th esis to ex plain th e a m p litu d e e n h an c em en t. However, it
was found to fail since clear scars were found in a classical chao tic sy stem [2 0]. A
m ore co m p lete e x p la n a tio n was th e n p u t forw ard by Bogom olny [21] to ex plain
scars in th e w avefunctions. T h is was th e n ex ten d ed into p hase space by B erry
[2 2] using a W igner d istrib u tio n [23]. A m e th o d for q u an tify in g th e stre n g th of
scarrin g has been given by A gam and F ish m an [24].
For m ore a c c u ra te an d q u an tal-lik e stu dies classical m e th o d s often becom e
rep-resen tin g a w avepacket as an ensem ble of classical tra je c to rie s [25] [26] a n d th e n
stu d y in g th e recu rren ce to e x tra c t eigenenergies. In a 2D s tu d y of C O2 a classi
cal ap p ro ach too k 2 days to ru n , w hereas th e e s tim a te for a equ ivalent q u a n ta l
calcu latio n was 10 m in u tes [27] on th e sam e co m p u ter.
1.5
a n d th e C a r r in g to n -K e n n e d y s p e c tr u m .
T h e H3 ion was first d e te c te d in discharge ex p erim en ts by J .J . T h o m p so n [28]
who m e asu re d a p a rtic le w ith a m ass to charge ra tio of 3. T h e c u rre n t th e o ry a t
th e tim e could not exp lain th e discovery an d w hen d e u te riu m was discovered th e
p a rtic le was th o u g h t to be HD"^ [29]. L ater, when ab initio th e o ry h ad im p ro v ed ,
a s ta b le s tru c tu re of was p re d ic te d [30], an d it rep laced as th e likely
c u lp rit to exp lain th e earlier observations. Now we know a lot m ore a b o u t th e
m o lecular ion, an d th e ease w ith w hich it can form in gas discharges.
In its grou nd s ta te H j is an e q u ila te ra l trian g le, w ith ato m ic se p a ra tio n s
of 1.65ao' It is easily form ed by th e collision of H2 and H2 in an ex o th e rm ic
reactio n ,
H2 + H+ H+ + H + 1.7 eV
H3 is th o u g h t to be a very im p o rta n t m olecule in th e in te rs te lla r m e d iu m as
it is a p ro to n donor, read ily giving u p in chem ical reactio n s, an d m ay be
responsible for trig gerin g m an y of th e chains of reactio n s w hich occur in th e
diffuse clouds, an d n ebu lae betw een th e stars. So far, how ever, it has n o t b een
d e te c te d in th e in te rste lla r m ed iu m , b u t by chance was found on J u p ite r [31], an d
la te r U ranus [32], S a tu rn [33] and a su sp ected sighting in S up ernova 1987a [34].
T h e m o st well stu d ie d of these cases is J u p ite r, w here is form ed in a u ro ra e
a t th e n o rth an d so u th m ag n etic poles, w ith an e s tim a te d colum n d e n sity of
30 X 10^^ m olecules cm~^, and a te m p e ra tu re varying from 800K to 1200K [35].
In th e la b o ra to ry th e sp e c tru m of H3 was first observed by O ka [36], an d
now a large n u m b e r of im p o rta n t tra n sitio n s have been record ed an d c a lc u la te d
[37]. T h eo re tic al calculatio ns of th e sp e c tru m were first p erfo rm ed by C arn ey
Figure 1.1: C arrington-K ennedy H j photodissociation exp erim ental a p p ara tu s
[40]. This is a simplified diagram to show th e m ain experim ental
features. Ions enter on the left, are m ass/ch arg e selected and then
en ter th e drift cham ber. A tu nable laser excites the ions and if
they dissociate th e products can be m ass selected in th e ESA on
th e right and detected by th e two detectors which can also estim ate
their kinetic energy. M odulation of th e laser allows a red uction in
th e noise due to norm al dissociation and reaction processes.
leaser
Intennediate slit
Drift tube
D etector 1
Laser
Ion Beam M agnetic
ESA
Doctector 2
Ion Source
to very high energies [39], which have aided in the discovery of H j in astronom y.
In much of th e work presented here th e driving force has been an a tte m p t to
in terp ret th e results of the photodissociation sp ectru m of H3 first m easured in
1982 by C arrington et al [40].
T he C arrington-K ennedy photodissociation sp ectru m of was rem arkable
because in only a 220 cm “ ^ window, 870 cm “ ^ from the origin, they m easured
nearly 27000 absorption lines due to transitions leading to dissociation [41]. Even
m ore surprising was th e discovery th a t, on ‘roarse-graining’ about 2 0 0 0 of th e
strongest lines, th e sm oothed spectrum had 4 very d istinct peaks separated by
ab ou t 50 c m “ b Since th e original results much analysis and m any new results
have been published which investigate th e dependence of th e spectrum on th e
kinetic energy of the dissociating ions, the role of isotopic su b stitu tio n , and
the different dissociation m echanism s [41], [42].
T h e exp erim ental ap p aratu s in a simplified diag ram m atic form is shown in
figure 1 .1. H3 ions are produced by electron b om bardm ent, and then accelerated
up to th e m a g n e tic secto r w hich is tu n e d to tra n s m it ions. T hese th e n e n te r
th e d rift ch am b er w hich can accelerate th e ions fu rth e r. A m ech anically chopped
laser beam passes along th e d rift ch am b er an d is sw ept th ro u g h th e frequency
range from a b o u t 870 c m “ ^ to 1095 c m “ ^. P ro to n s, w hich are released from
dissociation, are d e te c te d by th e m u ltip lier. To s e p a ra te th e m from th e p a re n t
H J b eam an d frag m en ts a e le c tro sta tic an aly ser, or ESA , is used. T h e
ESA has sufficient m ass-to-velocity resolu tion th a t it can b e used to d e te rm in e
th e a p p ro x im a te k in etic energy of th e frag m ents. A bias voltage in th e d rift
tu b e can also b e set so th a t p ro to n s d e te c te d m u st have been p ro du ced in th e
d rift tu b e . W ith o u t th e laser b o th H"*" an d frag m en ts are d etecte d w hich
are g en era ted by collision ind uced d issociation [41], an d n o t by uni m o lecu lar
decay of th e H3 . W ith th e laser on a n d locked to th e m echanical chopping
frequency th e p re d o m in a n t ions d e te c te d are H'*’. A line is recorded w hen th e
frequency of th e laser causes an increase in th e r a te of d etectio n of p ro to n s,
co rrespo nd in g to e x c ita tio n from a sta b le or m e ta -sta b le s ta te , to a s ta te w hich
leads to dissociation.
T h e m ain featu res of th e sp e c tru m can be su m m arised as follows.
• 27000 lines observed in th e range 874 - 1094 cm "^. Each line was recorded
by d e te c tin g frag m en t pro d u ced by predissociatio n.
• ‘C o arse-g rain in g ’ of th e h ighest 1934 lines gave a sm o o th ed sp e c tru m w ith
four clear p eaks cen tred a t 875.65, 928.02, 978.45 an d 1033.62 cm~^.
• T h e sp e c tru m is d ep en d e n t on th e kinetic energy of th e H'*' frag m en ts
released. T h e k in etic energy of th e released frag m en t can be as high as
4000 c m “ ^. T his im plies th a t th e in itia l an d final sta te s which give th e
tra n s itio n are m e ta s ta b le states.
• T h e in itia l s ta te of H3 before e x citatio n m u st have a lifetim e longer th a n
lO '^ s for it to reach th e d rift tu b e , and th e final d issociatin g s ta te s m u st
have lifetim es sh o rte r th a n 7 x 10“ 's for dissociation to occur in th e d rift
• T h e s p e c tra of th e isotopom ers H2D''' an d D2H''' gave different resu lts w hen
m o n ito rin g e ith e r frag m en t p ro to n s o r frag m en t deu tero n s.
T h e first th e o re tic al m odel proposed to exp lain th e s p e c tru m was given by
C a rrin g to n an d K ennedy in th e ex p e rim e n ta l p a p e r [41]. T h e y d escribe th e
sy stem as a H2 • -H"*" com plex since th e four peaks corresp on d very closely to
j = 3 ^ 5 tran sitio n s for = 0 ,1 ,2 ,3 in th e g round electro nic s ta te of H2. Since
th e final s ta te s in th e tra n sitio n s w hich give th e sp e c tru m lead to dissociation,
th e y m u st be m e ta sta b le . T h ree m odes w ere discussed to ex p lain th e ex isten ce of
th e pred isso ciatio n m echanism . T h e first, tu n n ellin g th ro u g h a centrifugal b a r
rier, gives only low k in etic energy releases and n ot enough possible tra n sitio n s.
T h e second, ro ta tio n a l predissociation , in w hich th e H"*" is b o u n d to an ex cited
H2 m olecule, gives tra n s itio n frequencies in th e rang e 0-900 c m “ h F in ally vi
b ra tio n a l pred isso ciation , in a sim ilar fashion to ro ta tio n a l p red isso ciatio n , gives
energies th a t are high, betw een 2400 an d 5000 cm~^. T h e ir m odel gives values
for lifetim es in th e correct range, b u t by no m eans conclusively fits th e o bserved
d a ta .
A second m odel was proposed by Pfeiffer and C hild [43] b ased on th e H2 -H"''
com plex m odel of C arrin g to n an d K ennedy. T his rigid ro to r m odel ex p lain ed
th e lifetim es of th e p redissociation s ta te s as caused by tu n n e llin g and to ok th e
com plex to be loosely coupled b u t bo un d by a high ro ta tio n a l an g u lar m o m e n tu m
b a rrie r. T h is could account for th e n u m b e r of lines b u t n o t th e stru c tu re , a n d
w ith o u t assum ing sa tu ra tio n , could n o t exp lain tra n sitio n s above a b o u t 900
cm “^.
U sing classical tra je c to ry analysis on th e DIM p o te n tia l B erblinger et al [44]
fo und regions of bou nd p h ase space in 2D calculatio ns w ith J — 0. In 3D th e se
w ere found to be u n sta b le excep t th e periodic o rb it nickn am ed th e ‘h o rsesh o e’
o rb it, w hich was a ty p e of b ending m o tion . By considering ./ > 0 they s tu d ie d
th e an g u lar m o m en tu m b a rrie r effects w hich m ay account for th e long lifetim es.
T h ey found th e sy stem to be q uasi-periodic or chaotic d ep end in g on th e a n g u la r
w ith th o se of th e ex p erim en t.
U sing M on te C arlo in teg ratio n th e y calcu la ted th e volum e of p h ase space
available an d hence e s tim a te d th e d en sity of sta te s. T h is d en sity th e y found to
b e very high w hich fitte d w ith th e large n u m b e r of lines m e asu re d in th e e x p e ri
m e n t. G om ez L lorente an d P oliak [45] ex ten d ed th e analysis by c o n c e n tra tin g on
th e ro ta tin g horseshoe p erio d ic o rb it a n d found th a t a n tis y m m e tric e x c ita tio n ,
p e rp e n d ic u la r to th e horseshoe m o tion , w ith ro ta tio n a l tra n sitio n s could be used
to ex p lain th e four b ro ad peaks in th e ‘co arse-g rain ed ’ sp e c tru m , describ ed as a
R b ran ch .
T h e o bserv atio n of different resu lts w hen m o n ito rin g p ro to n or d e u te ro n re
lease for th e iso to po m ers was analysed by C arrin g to n et al [42] a n d fitte d th e
o retical p red ictio n s. T h e y observed th a t for D2H"^ th e H'*' was th e d o m in a n t
d issociatio n p ro d u c t a t low k in etic energies an d d o m in atin g a t h ig h er K .E .
T his could be ex p lain ed by considering th e an g u lar m o m e n tu m b a rrie r in b o th
cases w hich w ould favour H"'" p ro d u ctio n a t low an g u lar m o m e n tu m a n d D'*’ for
h igher values. T his was also th e case for H2D'*', b u t w ith a less p ro n o u n ced
energy selection.
O bviously to confirm th e classica] p red ic tio n it is im p o rta n t to find th e q uan-
ta l c o u n te rp a rts to th e horseshoe and ex cited horseshoe m o tio n . H ow ever th e
s ta te s th a t are involved in th e sp e c tru m are n ear to and above th e d isso ciatio n
th resh o ld , an d co rresp o n d to a b o u t th e 8 00 th -f s ta te s co u ntin g from th e gro u n d
s ta te . T h e calcu latio n of such highly ex cited s ta te s is frau g h t w ith difficulty, an d
for a tria to m ic m olecule was p ractically im possible u n til only a few years ago.
U sing G aussians s c a tte re d along th e classical p eriodic o rb it, G om ez L loren te
et al [15] confirm ed th e ex istence of th e horseshoe sta te s in a q u a n ta l c alcu la tio n
an d e s tim a te d th e energies. However, th e se were 2D calculation s an d relied h eav
ily on th e fact th a t any q u a n ta l horseshoe would be tig h tly localised along th e
classical p erio d ic o rb it. U sing a new ly developed d iscrete variable re p re s e n ta tio n
(D V R ) T ennyson, B rass an d P oliak found strong lo calisation of th e h orseshoe in
full q u a n tu m calcu latio n s in b o th 2D [46] and 3D [47]. T h ey also fo und o th e r
existence of a q u a n tu m ex cited horseshoe sta te .
M ore recen t calculatio ns by a few groups relying heavily on th e D V R m e th o d
have m an ag ed to converge sta te s up to th e dissociatio n lim it [39], [48]. A tte m p ts
are now being m a d e to recrea te th e sp e c tru m from pu rely q u a n tu m m ech an ical
grounds. However, th e re are q u ite a n u m b e r of different p a ra m e te rs w hich need
to be in clud ed in th e m odel to m im ic th e ex p erim en tally o bserved resu lts, e.g. ion
b eam te m p e ra tu re and s ta te lifetim es. For a fully th eo re tic al rep ro d u ctio n of th e
resu lts th ese facto rs will have to be in cluded, an d so th e p ra c tic a l lim ita tio n s
m ay n ot be defined only by th e pow er of co m p u ters.
O ne of th e m a in problem s w ith m olecu lar v ib ratio n calcu lation s is th e ac
cu racy of th e p o te n tia l available. For H j th e re now ex ist arg u ab ly th e m o st
a c c u ra te p o te n tia ls for a tria to m ic m olecule [49], [2], [50], b u t th ese are only
a c c u ra te to a b o u t 24000 cm~^ above th e g round electro nic s ta te . In th e p h o
to d isso ciatio n sp e c tru m , b o th th e in itia l an d final s ta te s w hich give rise to th e
ab so rp tio n are n ear to or above th e d issociation lim it. T h is occurs a t a b o u t
36000 cm~^, d ep en d in g on th e p o te n tia l used, and th e sta te s are th erefore b ad ly
rep resen ted in th e p o te n tial. In ch a p te r 8 th e ro b ustness of p o te n tia ls is discussed
an d it is arg ued th a t q u a lita tiv e form , r a th e r th a n q u a n tita tiv e accuracy, m ay be
enough to find th e m otions an d sta te s responsible for th e C arrin g to n -K e n n ed y
sp e c tru m .
T h e ex act value of th e dissociation energy of H j is n ot certain . E x p e rim e n ta l
tech n iq u es used to e s tim a te th e value do n o t give th e sam e resu lt as ab initio
calcu latio n s [51]. However, it is im p o rta n t to u n d e rsta n d th e different definitions
of th e value. C lassically it is norm al to q u o te th e difference betw een th e a b so lu te
m in im u m of th e p o te n tia l of in terest, an d th e energy a t w hich th e p o te n tia l is no
longer b ou nd . T h is is in d icate d by D^. Q u an tally zero p o in t energies m u st be
considered, an d for H j on th e M BB p o te n tia l this value is a b o u t 4400 c m “ F T h e
low est energy a t w hich th e m olecule can dissociate is also higher th a n th e energy
a t w hich th e p o te n tia l is no longer bo u n d since th e re is a zero p oint energy for
th e rem a in in g H2, if we assum e a p ro to n is given off. T h is zero p oint energy
Dq.
In th is thesis m o st energies are q u o te d referred to th e g ro u n d s ta te , i.e. w ith
th e zero p o in t energy. For convenient com p arison of th e classical an d q u a n ta l
resu lts, th e classical resu lts are also p resen te d on th is energy scale, so th e classical
d issociatio n energy is given w ith respect to th e q u a n ta l g ro u n d sta te .
O n th e M B B p o te n tia l energy surface, w hich is used for m o st of th e c alcu la
tio n s p resen ted h ere, H j has a classical d isso ciation energy of a b o u t 36400 cm "*
above th e grou nd s ta te . T h e DIM p o te n tia l has a value of a b o u t 35500 cm~^.
T h e second definition w hich needs to be discussed is th e energy a t w hich
th e H3 can go linear. C lassically this b a rrie r to lin earity has a value of a b o u t
14000 cm~^ from th e ab so lu te m in im u m of th e p o te n tia l. Q u an tally , tu n n e llin g
can occur, so th e effect of lin earity m ay b e felt as low as 9000 cm~^ ab ov e th e
g ro u n d sta te . S tric tly speaking th e energy should be a b o u t 2000 c m “ ^ above
th e b a rrie r before th e m o tion can be said to be freely m oving th ro u g h lin earity ,
giving a value of a b o u t 1 2 0 0 0 cm~^ above th e g ro u n d s ta te .
1.6
C o m p u ta tio n a l A d v a n c e s
O ne of th e m a in changes in science in th e last decade has n o t been fueled by
new e x p e rim e n ta l discoveries, or by th e o re tic a l in novation, b u t by th e en o rm o u s
advances in co m p u tin g technology b o th in sheer calcu latin g sp eed and user in te r
faces. A com m on id ea am o ng st co m p u ter scien tists, w hich is som etim es know n
as ‘M o ore’s law ’, s ta te s th a t th e co m p u ter pow er available for a ce rta in am o u n t
of m on ey will dou ble every 18 m on th s. T his has ce rta in ly been th e case for
th e la st two decades, an d th e increase does not look likely to slow for a t least
th e n e x t decade, an d m ay b e even la ter. F in ite lim its im po sed by th e p hysical
technology itself can be avoided by sim ply squeezing m ore processors in to one
box. T h e tra n s itio n from scalar to v ecto r arc h ite c tu re s gave power increases
of u p to 1 0 0 tim es, an d now p arallel m e th o d s w here each processor itse lf m ay
be v ecto r looks set to increase th e available pow er fu rth e r. However w ith th e
m em o ry lim its, w hich m ay n o t be able to increase to su p p o rt th e d e m a n d s of
th e processors them selves.
T h e definition of co m p u ter pow er is som etim es a little vague b u t can be
th o u g h t of as th e n u m b er of m a th e m a tic a l o p eratio n s p er second. T h e increase
has n o t only affected th e speed of calcu latio n s, b u t also g rap h ic al cap ab ility.
T h is im p ro v em en t in th e ab ility to visualise resu lts has spaw ned new research
of its own. W avefunctions w hich h ad o ften been th o u g h t of as m a th e m a tic a l
con cepts can now be p lo tte d on th e screen in seconds allow ing in -d e p th analysis
of th e in fo rm atio n th e y convey. For a tria to m ic m olecule th e v ib ra tio n s fill a
th re e dim en sion al configuration space, a n d th e w avefunctions h ave values a t all
p o in ts. It is th erefo re necessary to select a ‘slice’ th ro u g h th is co nfig uration
space, for in sta n c e by fixing a co o rd in ate, before a plot of th e w av efunction can
be displayed. T h is selection of co o rd in ates an d slice is im p o rta n t, as in fo rm a tio n
can be easily d isto rte d , for ex am p le by p lo ttin g dow n a n od al plane. However,
th e graph ics interfaces can use th e pow er of th e processor to tra n sfo rm p lo ts
in to o th e r co o rd in ates quickly and hence p erfo rm , in effect, m u ltid im en sio n a l
plots. For te tra -a to m ic m olecules th e p rob lem is increased fu rth e r as th e re are
six v ib ra tio n a l degrees of freedom . T h e choice of co o rd in a te ‘slice’ in th is case
m ay be critica l in conveying any useful in fo rm atio n a t all. In ch a p te rs 4, 5, 6
an d 7 th e v aria tio n of coord inates is used ex tensively to display different ty p e s
of m o tio n an d sy m m e try for w ater an d H3 .
P re d ic tin g w h at will be ‘th e s ta te of th e a r t ’ co m p u tin g te ch n iq u es in a
decad e is n o rm ally left to science fiction w riter. It is likely th a t th e 100 h o u r
‘jo b s ’ needed to converge 1 0 0 0 v ib ra tio n a l s ta te s m ay take no m ore th a n a few
m in u tes. B u t it is also likely th a t th e pro blem s being tack led will increase in
c o m p u ta tio n a l d em an d to m a tc h th a t available. C u rren tly ex act H am ilto n ia n
v ib ra tio n a l calcu lation s are n o rm ally re stric te d to tria to m ic m olecules, alth o u g h
rece n tly work on te tra -a to m ic m olecules has begun. P erh ap s th e te tra -a to m ic
work will becom e com m on place an d m olecules w ith five ato m s will also be
C h a p ter 2
Q u an tu m M eth o d s
2.1
V ib r a tio n a l S e p a r a tio n a n d C o o r d in a te s
A tria to m ic m olecule has nine degrees of freedom . To consider th e v ib ra tio n s
an d ro ta tio n s only it is possible to rem ove th re e dim ensions w hich co rresp o n d
to sim ple tra n s la tio n of th e cen tre of m ass of th e m olecule. R o ta tio n s can th e n
be se p a ra te d from th e v ib ratio n s by tran sfo rm in g from space fixed co o rd in a tes
to b od y fixed co o rd in ates, an d considering th e ro ta tio n s of th e b o dy fixed fram e
w ith in th e space fixed fram e. T his reduces th e n u m b e r of v ib ra tio n a l degrees of
freedom to th re e for a n on -linear tria to m ic and four for a lin ear tria to m ic . T h e
difference being th a t th e re can be no ro ta tio n along th e lin ear axis as th is has
an effective m o m en t of in e rtia of zero.
Sutcliffe and T ennyson derived a set of general co o rd in ates w hich d escrib e
configurations of th e ato m s, A i, A2 an d A3, w ith tw o len gth s, a n d T2, a n d an
angle, 0. T hese are shown in figure 2.1, w here th e p oints P i an d P2 are defined
using tw o factors ffi an d ^2,
By choosing different values of ffi an d §2 different sets of co o rd in ates can be
selected. Jacob i o r sc a tte rin g coord inates are defined w hen g\ = ^ — , ^ 2 = 0-
For b o n d len g th bond angle coo rdin ates gi = q2 = 0, an d for R ad au c o o rd in a tes
F ig u re 2.1: G en eral co o rd in ate sy stem for v ib ratio n s d escribed by tw o len g th s,
Ti a n d T2, an d a angle, 6, T h e p o sitio n of P i a n d Pg is defined by th e choice of co o rd in a te system s an d th e m asses of th e ato m s, A i,
Â2 an d A3.
A'
O f th ese Jaco b i an d R ad au co o rd in ates are th e m o st useful as th e y are o rth o g o n al
so th e re is no r%-r2 coupling in th e k in etic energy o p erato r.
2.2
F B R H a m ilto n ia n
U sing a finite basis rep resen tatio n (F B R ), for th e o rth o g o n al co o rd in ates de
scribed above, th e Sutcliffe an d T ennyson ro tatio n less H am ilto n ian m a trix can
be w ritte n [52]
( m ,n , j | P | m ' , n ' , j ') = {m\h^^^\m')6n,n'Sj,j' +
-f + {n\g^^^\n')6m,m') j ( j +
i - { m , n J \ V { r i , r2,0) \ m ' , n J ' ) (2 .2 )
w here |m ) an d \n) are th e basis fu nctions for an d T2 m o tio n respectively, an d
th e a n g u la r basis fun ctions \j) are L egendre polynom ials rep resen tin g m o tio n in
are th e k in e tic energy in tegrals for an d T2. a n d a re th e a n g u la r
k in e tic energy in teg rals. T hese are given by
( 4 « |< '> = (2.3)
an d
(2.4)
w here |f) = |m ) for i = 1 an d |() = |n ) for i = 2 , is th e a p p ro p ria te red u ce d
m ass in th e rad ia l co ordinates. T hese are d e term in e d by th e choice of co o rd in a te
sy stem s an d th erefo re d ep en d on g\ an d g2\
= ^ 2 ^ - 1 + 7722^ + (l+5r2)^m 3^ , = g l m2^ ^ m X ^ - \ - { l - \ - g i f m '^ ^ . (2.5)
2 .3
B a s is F u n c tio n s
T h e choice of basis fu nctions is of g re a t im p o rta n c e to o b ta in good convergence
tow ards th e ‘e x a c t’ solution. T h e p ro b lem size is u ltim a te ly d e te rm in e d by th e
n u m b e r of basis fun ctio ns needed, an d so it is useful to m in im ise th is n u m b e r by
using fun ction s w hich give a good re p re se n ta tio n of th e m o tio n in th e given coor
d in a te. In th e an g u lar co o rd in ate th e T-S H am ilto n ian is d eriv ed w ith L egendre
polynom ials im p licitly used.
For th e rad ia l co ord in ates m an y facto rs influence th e ty p e of fu n ctio n s used.
For coordinates in w hich m otions do n o t go linear, e.g. r i in Jaco b i co o rd in ates,
T ennyson an d Sutcliffe [53] defined a set of o rth o n o rm a l fu n ctio n s based on
solutions to a M orse o scillator H am ilto n ian . T hese can be w ritte n
\t) = H t { n ) = ^ î A f , „ e x p ( - | ) ÿ ^ i r ( ÿ ) (2.6)
y = A exp[-/9(r,- - He)] ,
w here
A = /3 = uje (2^ ) ’ ^ “ i n t e g e r ( A ) . (2.7)
N t a L t ( y ) ^re n o rm alised asso ciated L aguerre polynom ials. O p tim isa b le p a ra m