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Atomic parameters for transitions involving Rydberg states of singly ionized alkaline earths

Mohamed Djerad

To cite this version:

Mohamed Djerad. Atomic parameters for transitions involving Rydberg states of singly ionized alkaline

earths. Journal de Physique II, EDP Sciences, 1991, 1 (1), pp.1-9. �10.1051/jp2:1991135�. �jpa-

00247496�

(2)

J.

Phys.

II1

(1991)

1-9 JANVIER1991, PAGE

Classification

Physics

Abstracts

32.70C

Atomic parameters for transitions involving Rydberg states

of singly ionized alkaline earths

Mohamed Tahar

Djerad

Dkpartement

de

Physi#ue,

Facultk des Sciences, 1060 Tunis, Tunisia

(Received

it

July,

1990,

accepted

8 October,

1990)

Rksumk. En utilisant des fonctions d'onde de la thkorie du dkfaut

quantique,

nous avons

caiculk les kikments de matrice radiaux mettant en jeu les ktats de

Rydberg

des atomes alcalineux

terreux une fois ionisks. Dans le but de tester les rksultats, nous avons calculk les

probabilitks

de

transitions, ies forces d'oscillateurs et ies durkes de vie radiative des ktats S, P, D et F

jusqu'i

n ~

30

( *).

Les

probabilitks

de. transitions sont en bon accord avec ies rksultats

disponibles.

Nous

prksentons

les durkes de vie eh terrre de lois d'kcheiles du type r~i

=

ro(n*)~.

La variation des forces d'oscillateurs en fonction du nombre

quantique

effectif n* est discutke.

Abstract.

Using quantum-defect theory

wave functions, we have computed

dipole

radial matrix elements

involving Rydberg

states of the

singly-ionized

alkaline-earth atoms. In order. to test the results, we have calculated a set of transition

probabilities, absorption

oscillator strengths and radiative lifetimes for S, P, D, and F states up to n 30(**). Transition

probabilities

are in

good agreement

with available data. We report the lifetimes in terms of scaling relations of type r~i =

r~(n*)~.

The variation of oscillator

strengths

with respect to the effective

principal quantun~

number n* is discussed.

1. InUoducdon.

Study

of the

properties

of atomic

Rydberg

states is of current interest. Excited atomic states are

pertinent

to

applications

in diverse fields such as

astrophysics, plasma physics,

space

physics,

etc.

Knowledge

of transition

probabilities,

oscillator

strengths

and radiative lifetimes is often needed. When

available,

measurements of these parameters are

generally

limited to

low-lying

states.

Thus,

a theoretical treatment

including highly

excited-states is of interest.

The calculation of any of these

parameters requires dipole

radial matrix elements. Extensive

calculations, involving

the use of elaborate theoretical model

requires prolonged computation

(*)

L'ensemble des rksultats est

disponible

sur demande adresske I l'auteur.

(**)

These extensive data are available upon request from the author.

(3)

2 JOURNAL DE

PHYSIQUE

II M

times.

Therefore, only approximate

methods are

usually

considered. The main

problem

is to

develop

a method for

obtaining satisfactory

and convenient wave functions for the

highly

excited-states. The traditional way of

describing Rydberg-state

wave functions is

bj uie

of the

quantum-defect theory,

which was

inaugurated by

Bates and

Damagaard

in their classic paper

[I]. Using

a numerical

approach

to

Bates-Damagaard

method

Lindgard

and Nielsen

[2]

evaluated transition

probabilities

for the alkali isoelectronic sequences for states with

n w12. To our

knowledge,

the atomic parameters are not

presently

available for

high-n-

excited states of

quasihydrogenic systems,

except alkali atoms for which exist extensive

predictions [3].

We consider

singly-ionized

alkaline-earths. We have used

analytical

wavefunc- tions

[4],

which were shown to

provide

a

good compromise

for detailed atomic calculations and accuracy

[5].

The paper is

organised

as follows. In section

2,

we

briefly

summarise the method. In section

3,

we determine the

parameters required

for the

computations.

In the last

section,

we

comment on the results. All the results are not listed here but are available upon request from

the author. Atomic units are used

throughout

unless otherwise stated

explicitly,

2. Method.

Kostelecky

et al.

[4] proposed

an

exactly

solvable

potential

model

adapted

to the

problem

of one-electron atoms. We

briefly

summarise the main feature of the model and

give

the

working equations.

The outer electron is described

by

the

following

orthonormalized radial

wave

functions, expressed

in terms of gamma

(r)

functions

~

~~~~

i

P3r(n*

/* I

(/))

>'2

fir

j'.~-prj~n. ~ji,~>~, fir

~"'"

@

2

r(n*

+ I* + I

)

n* ~ n* '

where

p

= 2

z~,

~~ is the net

charge

of the

nucleus,

I*

= 3

~j +

I(1), 3~j

is the quantum defect of a state nl

)

and

I(I )

is a

phenomenological, non-negative integer

with the allowed range of variation determined

by

the

following

two conditions :

(a)

the kinetic and

potential energies

are

separately normalisable,

which

imposes

the constraint 3

(1)

-1-

<

I(I (b)

2

Laguerre polynomials L)I '"it'~,

exist

only

for

I(I)

w n~,~ l

I,

where n~~~ is the

principal

quantum number of the

ground

state.

For a transition from the level nj

ii

to the level n~

l~),

the radial

part

of the

dipole

matrix element is

given by

(n,*)~" (nf)~~~

Jo ~ q~4

(n~ /~(

r ni

/,)

= ~

F(I, f)

x

4

z~(nj* nf

x

(r(n,* /~*) r(n? It r(n~*

+ /~* + i

) r(n?

+

It

+

1))"2

~

p~jo ~o

PI q'

~

(~l

~~~~~~) ~ n/~~~~~~j

~~~~i*~~ /~)ll'~

q + 2 '

where

F(I,f) =2ni*nf/(n~*+nf).

These matrix elements are

completely analytic

and

therefore convenient for calculations. In the

Bates-Damagaard [I] model,

the radial matrix elements are obtained

by

numerical

integration.

Moreover,

they depend

on a cutoff radius.

Various research groups have been

implementing

various series cutoff criteria but no

precise

justification

could be

given.

(4)

M I RYDBERG STATES OF IONIZED ALKALINE EARTHS 3

3.

Applicadon

to

singly-ionized

alkaline-earth atoms.

Einstein

coefficients,

oscillator

strengths

and lifetimes have been calculated for several

quasihydrogenic

atoms

(ions).

In

general,

the calculations were limited to

low-lying

states of the

systems.

In the

present work,

we include transitions

involving Rydberg

states of the second

spectra

of the alkaline earths. For a

given ion,

the basic

parameters

of the method will

now be

specified.

3.I THE QUANTUM DEFECT. It is well known that the

singly-excited binding energies

of

monovalent atoms

(ions)

in state

(n/)

are

given by hydrogen-like

formula

~

Zj Zj

~~

2(n*

)~

2(n

3

~j)~

For a

particular angular

momentum

/,

the

quantum

defect &~i is

nearly independent

of

n. To evaluate the

3~i

of

high

n states and thus

E~j,

we have used a numerical fit and

employed

the extended Ritz formula :

&~,=a+hm~~+cm~~+dm~~

with

m=n-30.

For each nl

series, 30

is constant and its value is determined

according

to an

optimisation technique.

The initial value is. the

quantum

defect of the lowest ternJ. In most cases,

30

could be obtained

by rounding

the initial value to the nearest 0.I. As recommended

by

Martin

[6],

the present Ritz formula is more convenient than one

expressed

in powers of

n*,

which has been

frequently.

As

input data,

we have used available

experimental

excitation

energies [7] only experimental

data for lower levels have been considered. Since we

neglect

the fine structure of the

levels,

we have used the baricenter for each level associated with the two fine-structure

components.

In all cases, the fit

reproduces

the observed

energies

to better than I fb. For

instance,

for Ba

ion,

there exist accurate

experimental energies [8]

up to

n = 70 for ns, np,

nd,

and ng

Rydberg

series. We have verified that we

reproduce

these values with excellent agreement. We have listed the fit parameters in table1.

3.2 THE INTEGER

I(I). Recently, Kostelecky

etal.

[9] predicted

the fine-structure

splittings

for

quasihydrogenic

atoms

(ions).

These are relevant to the short-distance behaviour because

they

vary as r~ and r~ ~ and

depend

on the

integer

I

(I )

in the model.

First,

the authors of reference

[9]

showed that the model constitutes a

good approximation

for

large

r and is therefore convenient for

Rydberg

states.

Second,

the model

provides good

predictions

of the fine-structure

splittings

for

light

atoms.

Accordingly,

the

experimental

data for fine-structure

splittings

allow the determination of values of the

phenomenological integer I(/ ).

In our case, this

approach

works well for Be+

only.

For the other

ions,

we have selected the values of

I(/)

that

give

the best agreement with

accepted

values. Table II shows the

phenomenological integers

we have used for various values off and for ions studied

by

us.

4. Results and accuracy.

We have

performed

calculations on a Vax 785 computer. The

expectation

values of radial

integrals

are

expressed

in terms of r function

(see

Sect.

2).

The use of double

precision

limited the calculations to n = 15.

Quadrupole precision

was therefore

used, corresponding

to about 33 decimal

digits.

The radial wavefunction

depends

upon the energy

E~,

of its

corresponding

state and the

(5)

4 JOURNAL DE

PHYSIQUE

II N

Table I. Excitation

energies of

the

fit

parameters.

Ion

3~

a h c d

s 0.3 0.25826767 0.072383024 0.27282557 0.49940956

Be+ p

0.0'

0.049366057 0.016608201 0.30420470 0.73083270

d 0.0

0.00071538i12

0.062185451 0.97974998 4.8120747

f 0.0 0.00029005721 0.0051964801 0.0733184467 0.0

s

1[0 J.066)201

0.13960186

0.2898719§

0.91979468

p 1.0 0.69639760 0.14831746 0.020831158 0.0

d 0.6 0.045457553 0.094118074 0.024890661 0.33961356

f 0.0 0.0035436391 0.037342068 0.73627400 6.6747470

g 0.0 0.0037441782

0.40812709

40.203358 075.3479

s 2.0 1.7994976 0.29482222 0.67478645 1.7830194

p 1.9 1.4364885 0.29501835 0.0 0.0

Ca+ d 1.0 0.62281942 0.21231084 0.96863210 4.6014581

f 0.0 0.025947075 0.15336217 4.4063873 61.276630

g 0.0 0.006863834 1.1933397 43.406574 507.34344

s 3.0 2.7050006 0.30806586

0.278495f4

0.97451008

p 3.45 2.3297160 0.16261426 0.0 0.0

Sr+ d 1.40 1.4505944 0.51244223 2,1281478 >27.432442

f 0.0 0.061722245 0.19285420 5.8515310 48.552032

g 0.0 0.98785323 £ 0.28638694 7.2725739 64.667908

s 4.0 3.5765221 0.36527434 0.15957843 0.62172544

p 3.95 3.191788 0.37837729 0.0 0.0

Ba+ d 2.40 2.3716066 0.91275573 4.928298 60.386803

f 3.0 0.85638016 0.73997784 0.58487803 0.78243428

g 3.4 0.020221187 0.040776726 0.13081138 0.16473958

ionization

potential

of the ion. It is obvious that the results

depend

upon the accuracy of the

experimental

level data.

Obtaining

these data from the extended Ritz formula eliminates local

accidents.

In

assessing

the accuracy of atomic parameters it is necessary to consider whether the radial

integral

is sensitive to small

changes

in the wave functions. The

sensitivity

is

usually

determined

by

the

degree

of cancellation which occurs between

positive

and

negative

contributions to the radial

integral.

In order to obtain an indication about such

sensitivity

let us assume that all the excitation

energies

are determined within I fb this

corresponds roughly

to ad

uncertainty

An the

quantum

defect 0.03 w ha

~j w 0.30 for the studied range of

n. We have varied

arbitrarily

the

quantum

defects for initial or final states in the aforesaid range. We have observed that the radial

integrals

are stable within

roughly

I fb for all transitions. Of course, if we,take into

account final and initial states, the cancellation effects would have

larger

percentages.

The transition

probability

for

spontaneous

emission from the upper level (n~

l~)

to a lower

(6)

M I RYDBERG STATES OF IONIZED ALKALINE EARTHS 5

Table II. Values

of

the parameters

I(I),

a and To iR 10~ ~ s

(see

the text

)

and the

asymptotic

quantum

defects 3,(1) for

values

of

the quantum number I.

I Parameter Be+

Mg+

Ca+ Sr+ Ba+

1(0)

0 2 4 4

s a 2.94 2.95 2.91 3.02 2.95

To 5.97 9,19 0.13 0.06 0.07

3(0)

0.258 1.066 1.800 2.705 3.577

1(1)

0 2 2 3

p a 2.92 2.96 2.89 2.87 3.08

T~ 9.53 0.239 0.27 1.0 0.80

3(1)

0.049 0.697 1.437 2.329 3.192

1(2)

0 0 2

d a 2.97 3.00 3.00 2.93 2.93

To 3.05 0.156 7.90 0.073 0.884

3(2)

0.001 0.045 0.623 1.451 2.373

1(3)

0 0 0 0 0

f a 2.97 3.02 2.93 3.17

To 6.50 0.528 0.055 0.320

3(3)

0.000 0.004 0.026 0.062 0.855

g

1(4)

0 0 0 0

3(4)

0.000 0.003 0.006 0.988 0.020

level

(n~l~)

for excitation

energies E~,j,

and E~~j~,

respectively,

is

given

in units of

l0~s~'by

2.026 x

10'~ (~i ~

~

(~f~f~ '~

~~~ ~~~'~~~

A

(ni

l~ ~

n~l~)

=

~ ~ 2

(

+ '

where A

(in A)

is the

wavelength

of the transition involved. The line

strength

(n~

l~( r

(n~l~)

(~ is in atomic units. In

tablet @IIa), (IIIb)

and

(IIIC),

we list a set of our calculations fur the transition

probabilities

for

light,

medium and

heavy ions, namely, Be+,

Ca+ and

Ba+, respectively.

The results are

compared

with recent critical

compi- lation[10].

The

majority

of the

quoted

values are obtained

calculationally

rather than

experimentally. Typically,

these values are

expected

to be accurate to within about 25 fb in

the Be+ and Ca+ cases and within about 50 fb in the Ba+ case.

However,

we note certain poverty for ns ~ np and np ~ ns transitions. For

example

the coefficient for Be +

(4s

~

2p)

transition is 1.5 greater than the

accepted

one. This is

expected

because these transitions involve the

largest quantum

defects and should

provide

the most

stringent

test of the model.- Moreover the model does not take into account

polarisation

effects. The results

conceming

the other levels are in the error bars and in certain cases to

(7)

6 JOURNAL DE PHYSIQUE II lK°

within a fraction of

percent.

This is due to the fact

thjt

these levels are almost

hydrogenic,

even for the haviest ions. We

emphasize

that within the

present'model,

we model less

accurately low-lying

levels than those with

larger

values of n which are of

primary

interest in the

present

calculations.

Thus,

the

agreement

with

accepted

values may be seen as better than that shown in tables III.

Table III.

Comparison of

our transition

probabilities

with

accepted

values

for

the ions

of Be(IIIa), Ca(IIIb)

and

Ba(IIIC).

(a)

Transition Present

Accepted

(io8

~->)

(io8 ~-l)

6s ~

4p

0.146 0.102

5s

~

3p

0Al1 0.28

4s ~

2p

0.142 0.94

6p

~ 4s, 0.0228 0.0256

5p

~ 4s 0.0259 0.030

5p

~ 3s 0.107 0.142

4p

~ 3s 0.143 0.19

6d ~

4p

0.137 0.143

5d

~

3p

0.576 0.59

4d ~

3p

1.13 1-1

3d ~

2p

11.6 9.2

(b)

Transition Present

Accepted

(jo8

~->)

(jo8 ~->)

7s ~

4p

0.201 0.308

6s ~

4p

0A13 0.62

5s

~

4p

1.17 1.7

4p

~ 4s 1.32 1.47

7d ~

4p

0.227 0.265

6d ~

4p

0.422 0.354

5d ~

4p

0.968 0.97

4d ~

4p

3.62 3.6

(8)

lK° RYDBERG STATES OF IONIZED ALKALINE EARTHS

Table

III(c).

Transition Present

Accepted

(108 s-') (108 s-')

I ls

~

8p

0.0456 0.041

1Is ~

7p

0.0744 0.064

II s

~

6p

0.160 0.12

10s

~

6p

0.250 0.18

9s

~

7p

0.218 0.18

9s

~

6p

0.428 0.32

8s ~

6p

0.840 0.60

8p

~ 7s 0.0177 0.018

7p

~ 7s 0.181 0.20

7p

~ 6s 0.119 0.10

6p

~ 6s 1.04 1-11

8p

~ 6d 2.18 x 10-4 6.7 x 10-4

8p

~ 5d 0.0176 0.034

6p

~ 5d 0.176 0.332

10d

~

8p

0.0340 0.037

10d

~

7p

0.0584 0.058

10d ~

6p

0.138 0.13

9d

~

8p

0.0562 0.063

9d

~

7p

0.0929 0.093

9d

~

6p

0.214 0.20

8d ~

8p

0. I I1 0.13

8d ~

7p

0.164 0.16

8d ~

6p

0.360 0.40

7d ~

7p

0.361 0.44

6d

~

6p

1.77 1.80

9d ~ 5f 4.63 x 10-4 6.6 x 10-4

10f ~ 5d 0.0106 0.038

6f

~ 5d 0.124 0.22

The

absorption

oscillator

strength

is

given by

the dimensionless

quantity

303_75

(n~ lj

r

(n~l~)

~ max

((, l~)

~~~~ ~'~

~~~~~

A 2 l~ +

It has

long

been established that

spectral

series of

quasihydrogenic species

reveal

systematic

trends. A

relatively unique

aspect of

Rydberg

series is their

regularity. They provide

an

opportunity

for-

systematic

and self-consistent studies

by

virtue of the

n-dependence

of

(9)

8 JOURNAL DE

PHYSIQUE

II lK°

it

id

~f

~~.1

0 IO 20 30

n~

Fig.

I.

Systematic

trend off values witlfin the

Mg+ (nS

-

4P) (x)

and Sr+

(nS

- 5P)

(A~

series.

Plotted 18

(n*)~

f vs., the effective

principal

quantum number n*.

/ ,

virtually

all atomic

proprieties.

For

instance,

the oscillator

strengths

diminish as

(n*)~~

so

that

(n*)~

f is constant. An

example

of such an

expected systematic

trend is

provided

in

figure

I for the transitions

Mg+ (nS

~ 4P and Sr+

(nS

~ 5P

).

The mean lifetime of a

given (nl)

level that

decays spontaneously

is defined

by

I Tn< ~

£

A

(nl

~ n'l'

)

n'l'

where the sommation holds [or all states

in'l') (E~,,,

<

E~j)

that are

radiatively

connected to the level

(nl).

It is known that the mean lifetimes of

high-n-levels

of

quasihydrogenic

atoms are well

represented by

the

formula[11] T~j=To(n*)~.

Tablell shows the

To and a

parameters

we obtained from a numerical fit of our results

(10

w n w 30

).

All of the

a values are close to

3,

which is the value

expected

in the limit of n

large

from consideration

on the

oscillator-strength

sum-rules

[12].

5. Conclusion.

Primarily

radial matrix elements have been

computed

for

highly-excited alkaline-earth, singly-ionised

atoms. Transition

probabilities,

oscillator

strengths

and lifetimes between a wide range of orbital I and

principal

n

quantum

numbers have been. evaluated.. Our modest

objective

was -to

provide

values of these

quantities

in nr~er to assist

experimentalists

in

(10)

lK° RYDBERG STATES OF IONIZED ALKALINE EARTHS 9

estimating

the lifetimes of excited-states and the

importance

of relevant processes. It is our

hope

that the present

predictions

will stimulate further accurate

experimental investigations, especially

for

large

atomic numbers.

References

[1] BATES D. R. and DAMAGAARD A., Philos. Trans. R. Soc. London, Sect. A 242

(1949)

101.

[2] LINDGARD A, and NIELSEN S. E., Atom. Data Nucl. Data Tables 19

(1977)

533.

[3] THEODOSIOU C. E.,

Phys.

Rev. A 30

(1984)

2881;

GOUNAND F., J. Phys. France 40 (1979) 457 ;

LI B. et al., J. Phys. B: Atom. Mol. Phys. 21

(1988)

2205.

[4] KOSTELECKEY V. A. and NIETO M. M.,

Phys.

Rev. A 32

(1985)

3243 ; KOSTELECKEY V. A.,

private

communication.

[5] CLARK R. E. H. and MERETS A. L., JQSRT 38

(1987)

287.

[6] MARTIN W.

C.,

J. Opt. Soc. Am. 70

(1984)

784.

[7] MOORE C. E., Atomic Energy Levels », Nat]. Bur. Stand. Washington D. C.

(1971).

[81 BOULMER J., CAMUS P., GAGNt J.-M. and PILLET P., J.

Phys.

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