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Valence Transition in Yb Hydrides*

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by

R.

Oldenbourg Verlag,

-0044-3336/89

Valence

Transition

in Yb

Hydrides*

Stefan

Biichler,

Rene Monnier and Leo

Degiorgi

Laboratorium fur

Festkorperphysik,

ETH Zurich,CH-8093Zurich,Switzerland Louis

Schlapbach

Universite de

Fribourg,

Perolles,CH-1700

Fribourg,

Switzerland

Ybexhibitsanunstable4f

configuration

in certain

compounds.

Ithas been shown

experimentally

and

theoretically

that 3d core-level

spectra

ofsome rareearthions exhibit satellite features which canbe

quantitatively

relatedtothe4foccupancyin the

ground

state. We

present

3d

photoelectron

spectra of various

Yb-hydrides,

measured with Si Kcc radiation at 1740 eV

photon

energy. The results indicate divalent Yb in

YbHi.8<x<2and mixed

valency

in the

trihydrides

(YbH2<x<2.6)-Introduction

At moderate pressure and temperature Yb forms a solid solution

phase

with

hydrogen,

anonmetallic

dihydride phase

(YbHi g<x<2.o)

andametallic

trihydride

phase

(YbH.j02.5n).

The

dihydride

is orthorhombic and

nonmagnetic,

whereas the

trihydride

has

been

reported

tobe of feestructureand

magnetic

/l/.

Apparently

theamountof

hydrogen

uptake

is relatedtovalence

changes,

which havenotbeen studied

previously.

Photoelectron spectroscopy has been shown to be a

powerful

tool for

studying

valence transitionsinrareearthmaterials

/2,3,4,5,6,7/

including hydrides

/8,9,10,11/.

Photoemissionspectraof valence band andcorelevels ofsome rareearth ions

(La,

Ce,

Sm, Yb,

Lu)

show features whichcan be understood ina

many-electron

picture

only.

* Presentedatthe International

Symposium

onMetal

Hydrogen

Systems,

Fundamen-tals and

Applications,

Stuttgart,

FRG,

September

4—9, 1988.

(2)

Model calculations

11,5,61

based on the

degenerate

Anderson

impurity

hamiltonian describe

spectroscopic

data

quite

well. These models involve initial and final states of

mixed 4f occupancy andas

important

interaction a

hybridisation

termbetween 4fand valencestates. Inthecaseof Yb the

groundstate lg>

is the

superposition

oftwo states

with13 and 14 4f

electrons,

respectively:

The firstterm

corresponds

to

divalent,

the secondtodivalent Yb.

Similarly,

the final statelf> of the 3d

photoemission

process is writtenas :

For the sake of

brevity

we usethe obvious abbreviations

4f13

and

4f14,

respectively,

for thetwocontributionstothe final and the

ground

state.

Alocalized4felectronscreensa3d holemuchbetter thanacontinuumstate.Inthe

photoemission

process the

outgoing

electron is much stronger

coupled

to a

poorly

screened ion thantoonewithafull 4f orbital. Therefore the kineticenergyof the former is lower andin the 3d

photoemission

experiment

the

4f13

finalstateappearstobemore

strongly

bound than the

4f14.

In thecaseof the Yb

hydrides

the difference in

binding

energyis almost 10eV,

making

it

possible

toseparatethetwocomponentsof the final statein thespectra. A

comparison

of

experimental

intensities of the

4f13

and

4f14

final

states with model calculations allowstheextraction of theparametersof the modified Anderson

hamiltonian,

in

particular

the4f

binding

energyand the

hybridisation strength.

With theseparametersone cancalculate the

ground

state

lg>

and thusthe 4f occupancy.

The relative intensities of the different 4P final states contributions in the

photoemission

spectraare adirectmeasureof the 4f occupancyinthe

ground

state as

Gunnarsson and Schonhammer/3/have shown in thecaseof

Ce,

and Monnieretal.161in

thecaseof Yb

/12/.

InYb the

missing

ofafinalstatecontribution

implies

the

missing

of the

corresponding ground

state. Therefore 3d

photoemission

is a strong tool for

determining

the Yb

valency.

Experimental

The XPS spectra were taken in a VG Escalab 5 spectrometer ata base pressure 1 •

10"lu

mbar. Si Ka radiationwasused and the overall resolution

was 1.6 eV FWHM

lg>

=

ocg

I4fl33dl°val3>

+

(3g

Ufl43dl°val2>

(1)

(3)

of the Au

4fj/2

peak

at 84.0 eV.

Kcc3

4 satellites were

numerically

corrected in the

spectra. The nonmetallic

YbH.2.0

showeda shift in

binding

energy due to

charging

effects. The

energies

werecalibrated witha

gold

wireonthe surface of the

hydride.

Yb metal

(99.9%,

Research

Chemicals)

wascleanedinthe

preparation

chamber of the spectrometer

by repetitive

Ar+

bombardement,

filing

and

outgassing

at 400°Cat

p=

10"9

mbar.

Hydrogenation

was

performed

in a

specially designed high

pressure

cell inside the spectrometer. The

hydriding

conditions are summarized in Table 1.

Hydrogen

wasfirst cleaned

by

a

LN2

cooledtrapandagetterstation downtoabout

lppm

contamination level. Table 1:

Hydride

YbHi.g

YbH2.Q

YbH2.2

YbH2,6

YbD2,6

pressure

(bar)

50-->1 50 50 50 50 temperature

(°C)

400

4C0.12°C/h>375

400.1.0°C/h>350

400

2A°9/.i1>

250

4002l°_9/_h>

250 exposure time

(hours)

10 24+4

Hydridingconditionsofseveral hydrides. InYbHjjjthepressurewas50 barsduring30 minutes. The hydrideswerepreparedinahighpressurecell inside thespectrometer,the deuteride inaseparate reaction

cell.

The

samples

wereof

cylindrical shape

with about 1 cmof diameter. The

hydride

samples

wereof dark grey colour and

brittle,

but didnot

disintegrate

into

powder.

To

reduceoxygendiffusiontothe surface the

samples

werecooled with

liquid nitrogen

to=

100K in the

analyzing position.

The

hydrides

werecleaned with adiamond file in situ

immediately

before

taking

thespectra. Thecontaminationasdetermined from

Ols, Cls,

and

Yb4p peaks

measured with

MgKa

radiationwasbelow 2%.

Structure,

composition

and

homogeneity

of the

samples

werechecked after

photoemission

measurements

by

X-ray diffraction and volumetric determination of the

hydrogen

liberated upon dissolution of partsof the

samples

in dilute acid.

The deuteridewas

prepared

intwosteps.Afterafirst deuteration of the Yb

metal,

it was

pulverized

inanargon

atmosphere

and deuterated

again.

The

powder

wasthen filled

in a copper coated vanadium vessel. Neutron measurements were

performed

at the multidetector

powder

diffractometer DMCatS APHIR. The

wavelength

was 1.708

A.

(4)

Results

Fig.

1 shows the Yb

3ds/2

XPS spectra of Yb

metal,

several Yb

hydrides

and Yb+ 100L

O2 (1

L= 1 s at

10~6 Torr).

The

hydride

spectra arecharacterized

by

two

main features. The first is at about 1522 eV

binding

energy and

corresponds

to a

Ufl43d9val2>

finalstate

(4f14).

It isa

single

line and is broadened

only by

lifetime and instrumental effects. The second is centered around 1530 eV and

corresponds

mainly

toa

I4f133d9val3>

finalstate

(4f13).

The3d and 4f holes

produce

a

multiplet

structure,which

significantly

broadens this contribution. This

multiplet

ismost

clearly

seen asthestrong

peak

in the Yb+100L

O2

spectrum, which is included in the

figure

as areference .

Yb2C>3

is knowntobe divalent

having

4f13

configuration.

The small

4f14

finalstate

signal

is due to

remaining

divalent

Yb,

resulting

from poor oxidation kinetics at room

temperatures.

Themost

interesting

andclearest result is the increase of the

weight

ofthe

4f13

peak

fromaboutzeroin the

dihydrides

toabout 50 %in

YbH2.6-

The intermediate

compound

YbH2.2,

which isatwo

phase

mixture of

YbH.2

and

YbH.2.5,

shows somescatterof the

4f13

finalstaterelative

intensity

arounda meanvalue of 30%.

Thespecdaof thetwo

dihydrides,

YbHi.g

and

YbH.2.0,

aredominated

by

the

4f14

finalstate.Inthe

region

of the

4f13

finalstatethere isaverybroad

peak

of low

intensity.

Thecenterof this feature is at

significantly

higher binding

energythan that ofthe

4f13

final state,

suggesting

avery low

4f13

finalstate

intensity.

This broad

peak

may be caused

by

banddansition losses of the

4f14

finalstate.The

backscattering

elecdon energyloss specda

(EELS)

ofthe

dihydrides

show broad losses

starting

4.5eV below the elastic

line,

withamaximumat 14eV.

The divalent Yb metal exhibitsa

pronounced

4f14

finalstate

peak.

Between 1525 and 1535 eV elecdon losses from the

4f14

finalstatedominate thespectrum.Abulkanda

surface

plasmon

5.4eV and 9.4

eV,

respectively,

below the

4f14 line,

overlap

witha

broad

peak

caused

by

band dansition losses.

Again

these losses have beenseeninrecent

EELS

experiments

/13/.

The

experimental

results

clearly

showavalence dansition from divalent

YbH.2

with

4f14

configuration

tomixed valent

YDH2.6

with

4f13/4f14

configuration.

Our calculations of the 3d core level

spectrum

of

YbH.2.6

based on the Gunnarsson-Schonhammer formulation of the

degenerate

Anderson

impurity

model agrees

qualitatively

and

quantitatively

very well witha50 %

4f13

/ 4f14

mixed valent

configuration

/l 1/.

Magnetic properties, specially

the absence of

magnetic ordering

atlowtemperature

(5)

XPS SiKrx

I

I

1540 1530 1520 1510

M-

BINDING ENERGY

(eV)

fig.1: Yb-W5/2corelevel spectraofYbmetal. Ybhydridesand Yb+100LO2.A cleartransitionfrom

divalent Ybll2

(4f14)

tomixed valenlYbll2.6

{4fl3l4f14)

occurs.Si

KC134

satellitestructureshave been

numericallysubtracted.4findicatesa

4fx3d9val3

finalstaleconfiguration.Indie Yb spectrumabulk and

(6)

Inorderto

clarify

the

question

of

homogeneous

or

inhomogeneous

mixed valencea

structurerefinement ofneutrondiffractionpatternsof

YDD2.6

wasstarted. Some

peaks

in

addition to the pattern of the fee structure suggest a

larger

unit cell due to small

displacements

of the Yb ions anda

possible

smearing

outofsomeoctahedralDsites/14/. It isa

pleasure

tothank J. Schefer and P. Fischer from theneutrondiffraction group at Paul Scherrer Institut for the

preliminary

structure

results,

T. Greber and

H.C.

Siegmann

for fruitful

discussions,

the Swiss National

Energy

Research Foundation

(NEFF)

and the National ScienceFoundation

(NF)

for financialsupport.

References

1 P.

Knappe,

andH.

Miiller,

J. Less-Common Met.

124,

263

(1986)

2 J. W.

Allen,

S.J.

Oh,

O.

Gunnarsson,

K.

Schonhammer,

M. B.

Maple,

M.S.Torikachvili and I.

Lindau,

Advancesin

Physics

35,

275

(1986)

3 O. Gunnarsson andK.

Schonhammer,

Phys.

Rev. B

28,

4315

(1983)

4 W. D.

Schneider,

B.

Delley,

E.

Wuilloud,

J.M. ImerandY.

Baer,

Phys.

Rev. B

21,

6819

(1985)

5 J.C.

Parlebas,

T. Nakano andA.

Kotani,

J.

Physique

48 , 1141

(1987)

6 R.

Monnier,

L.

Degiorgi

and D.D.

Koelling,

Phys.

Rev. Letters

56,

2744

(1986)

7 J. C.

Fuggle,

F. U.

Hillebrecht,

Z.

Zolnierek,

R.

Lasser,

Ch.

Freiburg,

O.

Gunnarsson,

K.

Schonhammer,

Phys.

Rev. B

22,7330

(1983)

8 J.

Osterwalder,

T.

Riesterer,

L.

Schlapbach,

F. VaillantandD.

Fruchart,

Phys.

Rev. B

31,

8311

(1985)

9 J.

Osterwalder,

Z. fur

Physik

B

6_L

113

(1985)

10 M.

Gupta

and L.

Schlapbach,

in

Topics

in

Applied

Physics,

Vol.

63,

L.

Schlapbach,

ed.,

Springer

Heidelberg

(1988),

p. 139

11 St.

Biichler,

L.

Schlapbach,

R.

Monnier,

L.Degiorgi,

J.

Physique

12,

C9

-947

(1987)

12 seealso

fig.7

,p. 4322 of Ref.3

13 A.

Stenborg,

E.

Bauer,

SurfaceScience

66,

561

(1988)

Figure

fig. 1: Yb -W5/2 core level spectra of Yb metal. Yb hydrides and Yb+100 L O2. A clear transition from

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