Scaling, renormalisation and accuracy of perturbation calculations

Scaling, renormalisation and accuracy of perturbation calculations

CHEhiICAL Volume 105, number 3 SCALING, RENORMALLSATION PHYSICS AND ACCURACY 16 hlarch 1984 LETTERS OF PERTURBATION CALCULATIONS M. COHEN an...

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CHEhiICAL

Volume 105, number 3

SCALING,

RENORMALLSATION

PHYSICS

AND ACCURACY

16 hlarch 1984

LETTERS

OF PERTURBATION

CALCULATIONS

M. COHEN and S. KAIS Deportment

ofPhysical

Received 2 January

Chemistry,

The

Hebrew

Universiry.

Jerusalem

93904,

Israel

1984

l-or certain eigenvalue problems whrch lead to dkergent Rayleigh-Schrbdinger perturbation series, enegy estimates oi acceptable accuracy may be obtzined casrly m first order by optn-nlsing a vanahonal scale factor. Some simple calculations on the quartic anharmonic osc2lator and on the quadratic Zecman effect shorn errors xxhich are generally quite %mdl over a very wide range of perturbation pammeter valuer

ly, for a given hamiltonian

I_ Intrculuc tion Following the pioneering

work of Bender and Wu

[l]

and of Simon [2] on the anhxmonic oscillator, has been a great deal of recent interest m largeorder perturbation theory, particularly for systems whose Rayleigh-Schriidinger (RS) perturbation series are known to be divergent or asymptotic. A major aim has been to devise successful summation techniques for such series; the work of &Zek and Vrscay [3] and of Silverman [4] provide just two recent examples, and many references. What emerges clearly from these treatments is that different procedures must be used in order to obtain highly accurate results for different systems, and there appears to be no L llversal solution applicable to all problems. Moreove. _Jthough it is now possible to calculate RS energy coefficients accurately up to order 100 (or beyond) for some model there

systems, it remains unlikely that this will become the norm. A generally applicable alternative is clearly desirable. Now, as has been emphasized by Banejee [5] and Killingbeck [6], it is often possible to rescule or tenormaIise a perturbation series. In fact, certain widely used “summation procedures” have their origins in an appropriate change of scale, or equivalently, in a different choice of reference (zero-order) hamiltonian Hb in place of the more natural (physical) operator Ho _ (The celebrated screening approximation of Dalgarno and Stewart [7] is a very good example of this.) Specifical0 009-26 14/84/S 03.00 0 Elsevier Science Publishers B.V. (North-Holland Physics Publishing Division)

H(J)

= Ho + XH,

(1)

in which h S a ~~ahtrul perturbation parameter, and H,,, H, are mdependent of h, it will often be more convenient to write H(X)=H(X;p=

1).

(2)

where

and Hi, Hi may be (explicitly or imphcltly) h dependent. The formal perturbarion parameter p will be set equal to unity at the end of the calculation. so that ir is sufficient for our purposes if convergence of the pperturbation series can be established only for a rather limited range, 0 < _u< 1; the range of the physical parame ter h is frequently unbounded (0 < X < -)_ Since H&A) may be chosen differently for differenr ranges of h, it becomes possible ro treat in zero order the leading effect of the physical penurbation, AH, _ Moreover, if this X dependence is introduced by means of variational parameters, these may be optimlsedfir my partidar X by appeal to the variation theorem: there is no need to have recourse ro the asymptotic (WKBJ) approximation for large h, although this is a well-documented procedure [1,5] _ In this letter, we reconsider the ground-state energies of two popular “problematic“ hamilronians, the one-dimensional (quartic) anharmonic oscillator and 295

Volume

10s. number

the twodimensional

PllYStCS

CHEMICAL

3

(quadratic)

cffcct. De-

Zccman

Table I

spite

the simplicity of’ both calculations. we obtain energies which arc remarkably accurate over almost tbc

Ground-state

eniite ranges OSboth pcttutbartons.

A -.

2. The qmic

anharmonic

oscillalor

‘The complct e hanultonlan

d2/d.2

H(A) 7

IS

+ r* + xx4

(A > 0)

(4)

and If(A) is anatlytically soluble when A ; 0. hut not for large A. WC make the sln~ple choice II&A) = -.d2/dx2 H;(h).

(I

Where

o(A)

.

+ ,2x2

.0*)x*

+ xx4

.

iS a A&!pCndCnt

transformation

If@)

l

oj-4~:dx2

palamCtC,

SO

thJt , f0,

$9 ”

-

My

Iv”’

F(ya) ‘n

5tdC

= (2n

+

l)o

+ (A/d)x4]

.

(‘I)

- a) + 2,(2n2

+ 2n t

1) A/o2

state (n = 0) and for any A, the perturbation sum E;“)(o) t ICAt) prondes a rtgorous upper bound to the energy. Variation of a now leads to the follawinR equations for oor,, and the corresponding optimiscd CllClgy Eopt : E=$(k-

mum to

CllUI

100,

ol

whereas

k(o*r

) Jars

I)+

l/Za.

(9)

not C.xcecr\ 2 2%

the Q 7 1 wties

is clearly

fat h up

divcr@g. The same proccrlure may be used for excItLY1 states (n 2 1) &hot&t EA”) + EF) now furnishes an upper

296

_-YLT

1.06917 1.2.5x02 1.41606 1.63943 I.80651 1.94377 2.06196 2 50286 3 07s51 4.089jt 5 10458 _

t 04529 174185 I .I39235 t .60754 I .769S9 1.90114 1.01 u34 2 44917 3.009’94 4.UOiY9 4.99942

181

if the variat wn of o 1s suitably if the variatmn

constraints,

It ts easily

whik

for large A and laige

,tsUh

Wa.S obtail,ed

is carried

seen

cons.

th,oup,h

rained. with-

1 when

that a

A = 0,

Ihls latter

n, 0%: (3nX)1/3;

by ktaIlCt)CC [ fi ] 011 the

ptCViOUtiy

basis of a WKBJ

treatment,

hut

3. The quadratic

Zeeman

effect

charge

% placed

z direction.

this

is unncccssacy.

f{(7)

of a one-Clcctron

in a magnetic

the non-rclativistlc

field

atom

of nuclca,

of strength

hamdtonian

H III the

(in atomic

is CffCct ivcly =

- Z/r t g+7?r2 silt30 .

j F2

(10)

(tlerc, 7 IS a dirncnsionlcss constant B/Ho. where Ho = 23505 X 10y G.) ‘Ihts problem is clearly two4ur,Cnsional. and may be therefore expected to hr mo~c dtfficult to treat than the one4imensional oscillator probkin. On the other cally

Table 1 contains mnnerical resulti based on eqs. (7) (9) both for a = I and for aopt,together with accurate values from the work of Biswas et al. 181; the maxi-

.

out

units)

results,

For the ground

l)~3A.

__

(6)

09

~*(a-

oscdta~or

.-

-_- mkJg,r) -

values I’rom ref.

For rn = 0 states

,

= :(211 + I)(l/a

onharmonic

-

1.075 1 375 1.75 2.5 3.25 4 0 4.75 H.S 160 38 5 ‘16.0 -

Nevertheless,

,

and usutg standard E;)(a)

leads to

n

Wli”(X)

(quarlic)

the

.-_

- Eb .-- 1)

0.1 0.5 I.0 2.0 7.0 4.0 5.0 10.0 20.0 50.0 100.0 -

bound only

t0 hC dCtC,-

the well-known propsolutions A simple

x’) ,

1)x2

iIi (A) _ l o[( I /02

of

(5)

x + x/at12 +

rncrey

.-.

a) Accurate

mmed; this allows us to exploit erties of the harmonic oriljator scaling

16 March 1984

LI;‘I-I’ERS

soluble

clearly

hand,

desirable

to choose

correctly

at both

It{:’

cxp[

=N

the hamiltontan

for srnall7

tmrh

limits.

where a : 4-y). fl-

a model ifI

Ihcrcforc.

(ar t ipr2

H(7)

is analyti-

and for large 7, and ,t is

sin%)]

N-y) with the

which

bchnvCs

we choose

(11)

, expectztron

that

at y

-O,o-%andp~Owhileas7-.m,a-rOandP-b~7 Corrcqtonding iq

r -* r/,2)

to this

$‘,o’.

WC have (aftc,

transform-

Volume

105. number 3

H&)-d-iv*

-

Iq(y)-4[p/r-

CHEMICAL

l/r + Gr + $A*)

~r+~zJr2)sin~0]

where we w&e /l=fi/S,

sin%]

PHYSlCS

(12)

for convenience

p=(a-q/a,

v=g

+2/cr4

_

(13)

Here both air) and /I(T) may be varied independently with 7, although it is also possible to vary only a single parameter, either II(~) or p(r) In this case also, all energy integrals may be evaluated analytically and we obtain the results E~qcr,

@) = a’(-

+ + p) ,

[exp(--t)P/(l

+pt)J

dt _

Table 2 contains four sets of results based on eqs. ((Y and j3 fHed, one parameter varied, both parameters varied) together with the most accurate energies available [3,4]. We have taken 2 = 1 for comparison with results of other workers. Even with cr and p tixed (note that our results correct and extend rhose of U-ardt [lo]) there is no divergence, a consequence of the correct behaviour of the trial function at both small and large field strengths. Indeed, only at y = 2 where the correcr energy changes sign, is the error in this simplest calculation unacceptably large. With j3 fured and (Yvaned (these results extend and improve (14)

(14)

(15)

isfactory

where = s

integrals are most easily generated recursively

from

Ground-state Y

results.

We have no reason to beheve that these examples

0 These

integral

those of Rau et al. [ll]) and with Q fned and fl varied, we obtain some improvement for all fLyed strengths although unexpectedly, variation of Q is more effective for large y and of fl for small y_ Independent variation of both (Y and /3 yields generally sat-

E~)(~,~)=d[PC~-~(c~-cC1)-~~(C~-2C2)]/C1,

C, = C,@)

16 March 1984

where X= l/p and I51 (X) is the exponential (see, for example, ref. [9])_

)

)

LETTERS

energy of a hydrogen atom in a magxtic

=)

are in any way exceptional, and conclude that other systems may be treated no less successfully by the same merhcds.

field (in atomic units) Accurarc

Presentcalculations

b)

(1)

(2)

(3)

(5)

(4)

0.1

-0.49579

-0.49659

-0.49743

-0 49747

-0.49

0.2 0.5

-0 48530 -0.43 170

-0.40747 -0.43716

-0.49036 -0.44681

-0.49027 -0.44683

-0.4903 -0.44721

10

-0.30’762

-0.3

-0.3’934

-0.32956

-0.01560

-0.01763

-0.33117 -0.02223

1003

2.0

0.02262

0.01685

3.0 4.0 5.0

0.39239 0.78629 1.1961

0 38885 0.78466 1.1956

10.0 20.0 100

3 3707 7.9771 46.826

3.3678 7.9508 46 536

034785 0.73837 1.1428 3.2939 7.9211 46.789

c)

753

0 3429s 0.72946 1.1324

0.33539

3.2756

3.2564

7.8245 46.361

200 300 1000

96.248 145.89 495.78

95.684 145-10 49297

96 220 145.88 494.77

95.433 144.82 492.72

2000 .____~_

994.12

991.42

994.11

99122

8

0.71913 1.1198 7.7847 46.211 9 5273 144.65 492.36 990.70

__

‘) 7=BjBo where B. = 2 3505 x 10’ G. b’(1)rr=l.~=y/2;(2)~vvaried.~=~~2;(3)cr=1.pvaried;(4)aand~varied. Cl (5) From refs

[3,41_

297

Volume

105. nurnbcr

CliEMlCAL

3

PllYSIcS

Referma 1 I ] CM.

Ucndcr

111 J. ?i7ck

and 1.T. Rev. l&l

121 B. Simon,

Ann

Wu. Yhys. Hcv. I CI~CI~ 21 (1968)

(1969)

Phyr. NY

and ):.H. Vrwxy.

K. Hancrjec.

Phyr

YIoc

Inlrrn.

SOC A368

161 1. Killm~hrxk Rcpl. Prop. Phyr. Al4 (1981) 1005,.

298

5.8 (1970)

J ~uuntum

(:hrm.

498

(19791

PhyL 40(

1977)

I SJ. Y63, J.

21

K. IMta.

V.S. Varma, J. Math lYj

76

Rev. A28 (1981)

Roy.

181 S.N. Birwaq.

1231.

27.

141 J.N. SlIverman. ISI

I6 March

171 A. IJal+?arno and A.I.. (1960) 534.

406,tnyr

i1982)

LErrERS

I IO] I I1 I

M. Ahramowlz

SIcwr1.

I’roc.

R.P. Saxcrw. Phyr

I4 (1973)

and I. !&pm.

malhcmalical luncttons(I)ovcr, W. Ekardt, Solid Slate Commun. A R P. RJU. R.0 All

(lY75)

1865.

Murllcr

edr.

Ray,

SOC.

1984

A257

P.K. Snvzvt;lv;r ;lnd 1190. Iiandb,ok

New York I6 (1975)

and I.. Spruch.

of

1972). 233. Phys

Rev