Possible RT superconductivity from Pb3CO5-Ag2O (PACO) system

Possible RT superconductivity from Pb3CO5-Ag2O (PACO) system

Physica ELSEVIER C 341-348 (2000) 723-725 www.elszvier.nl/locate/physc Possible RT superconductivity from Pb,CO,-Ag,O (PACO) system D. Djureka,...

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Physica

ELSEVIER

C 341-348

(2000)

723-725 www.elszvier.nl/locate/physc

Possible RT superconductivity

from Pb,CO,-Ag,O (PACO) system

D. Djureka, Z. Medunic”, A. Tonejcb and M. PaljeviCC aA. Volta Applied Ceramics (AVAC), Kesten brijeg 5, HR-10000 Zagreb, Croatia bFaculty of Sciences, Physics Dept., BijeniEka 32, HR-10000 Zagreb, Croatia ‘Ruder BoSkoviC Institute, BijeniEka 54, HR-10000 Zagreb, Croatia Some interesting results that could be eventually explained as coming from superconductivity Pb,CO,-AgrO (PACO) system are reported. Samples prepared at 340-350 OC in combined CO,-0,

(SC) in

atmosphere

exhibit low resistance states at room temperature (RT) with resistivity three orders of magnitude lower than that of silver. In addition, characteristic threshold current density dependence of electric resistance together with the DC susceptibility data obtained on balance support the idea of superconductivity

1. COMPONENTS

More efficient preparation is achieved by the use of PbC0,.2PbO

The most common superconductors

property

of high Tc

plane.

Pb,OCO,

PbCO,.PbO

(Pb,CO,

which exhibits

modification

important for reproducible

structure and electric conductivity in some preferred shannonite

(PC2P, CO,/PbO=1/3)

only one crystallographic

synthesized so far is their layered

crystallographic

in PACO system.

the fact

preparation. PC2P may

be prepared [3] by carbonization of tetragonal PbO ,

in l-3 bar flowing CO, at 3OO’C for 24 hours and

or PCP) with CO,/PbO=O.5

exhibits

X-ray diffractions

at d=3.01 A (I=lOO),

consists of PbCO, - PbO... layers [I,21 and doping

d=2.96 A (1=24), d=2.94 8, (1=31), d=2.88 li (1=49),

with Ag,O (Ag,CO,) may result in a number of novel

d=2.87 8, (Ial),

d=2.78 A (1=26).

metals. One modification of PbCO ,.PbO (a-PCP) may be obtained by carbonization of tetragonal PbO (lith-

2. PREFTRJNG AND ANNEALING

arge) at 3OOOCin 3-5 bar of flowing CO, with characteristic (1=32),

X-ray diffractions d=4.05

8, (1=54),

(CuK, ) at d=4.17 8, d=3.24

The powders of PC2P and Ag,O (PACO) are

8, (I=lOO),

mixed in corresponding

d=3.21 8, (I=lOO), d=2.87 8, (1=58), d=2.58 8, (1=34). Carbonization of tetragonal PbO at 300°C by 8-30 bar flowing

and prefired for 24 hours in 4-5 bar of flowing CO,

in j3-PCP with

at 33OOC. The mixture was then cooled to RT and

characteristic X-ray diffractions at d=3.29 8, (I=lOO),

reground to powder subsequently pressed in pellets

d=2.68 8, (1=41), d=2.37 A(I=10.6), d=2.32 8, (1=20).

by the use of 2 tons press between adequate hardened

For CO, pressures

CO, results

atomic Ag/Pb proportions

in a magnetic stirrer with ethanol as mixing agent

higher than 50 bars cerussite

steel dies. The usual dimensions of pellets are 5x5x0.3

PbCO, is obtained at 3OOOC.The mixing of p-PCP

mm’. For better estimation

as well as of a-PCP with Ag,O or Ag,CO, resulted

temperature in CO,-0,

in no metallic phases so far.

situ electrical

092

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PI1 SO92

matter

0 2000

Elsevier

Science

B.V.

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of optimal annealing

atmosphere

resistance

we measure in

of the pellets

during

D. Lljurek et al./Pl~_vstca C 341-348 (2000)723-725

124

annealing by the use of two probe 50 microns gold wires glued on the pellet with silver paint. During the heating stage in CO,-0,

atmosphere

at a rate

‘,‘t

PACO 512

megaohms

8

followed by an abrupt decrease to ten .

ohms at 340-345OC

which is actual annealing

1.0

;

&)=60 bar pfZO,)=45 bar

.“‘.

I”“‘.

0

00



0

OS

Pb,CO,+Ag,O

0

“--

B

1=1mA

oI=lA

temperature.

...

l

SK/mm the resistance of pellet usually exhibits 20

* ’ D e 0

l

0

20

40

60

80

100

t("C)

Figure 2.TGA decomposition

0”‘.

.I’..

0

.‘.

SO ~(0,)

‘.

100

.’

of PACO 5 12.

In addition, the undissolved Ag,O is visible in X-

1%I

(bar)

ray diffraction pattern and this sounds for provided

Figure 1. Phase diagram of PC2P-Ag,O system.

doping concentration of Ag in PCP to be less than Ag/Pb=1/5. TGA decomposition performed

in vacuu

(fig.2.) on PACO 5 12 sample (annealed under 60 bar 0, and 35 bar CO,) stresses CO ,/Pb0=0.58 which is

3. PHASES

somewhat higher than ideal PCP value 0.5 as a reThe study of PC2P-Ag,O system with atomic

sult of decomposed PbCO, and Bystrom phases.

Ag/Pb=0.20 (PACO 512) annealed for 24 hours at 345OC for various

pressures

CO,-0,

results

in

diagram shown in fig. 1. and sketched on the basis of resistive

properties.

Open

circles

represent

insulating state resulting from higher oxycarbonates with CO,/PbO > 0.5, while metallic samples which result from Ag doped intermediate Bystrom phases [4,5] are denoted correspond

by full circles.

Full squares

to samples which show SC properties

stable for several weeks or months. Empty squares belong to samples with SC properties disappearing after several days. X-ray diffraction pattern recorded on samples denoted by full squares reveals the presence of a-PCP, intermediate Bystrom phases as well as PbCO! as underlying compound.

4. RESISTIVE AND MAGNETIC PROPERTIES The samples for the measurement of electric resistance were prepared in two ways. Firstly, for higher measuring

currents ranging up to several

amperes we use four probe method with 100 microns gold wires pressed together

before

with prefired

annealing

powders.

procedure

The contact

resistance is several milliohms. Secondly, for lower measuring currents four probe measurements

are

provided by the use of 30 microns gold wires and silver paint with contact resistance

ranging from

3-50 ohms. The ultimate accuracy of in-phase signal

D. Djurek

et al./Physica

C 341-348

(2000)

125

723-725

resistance measurement for measuring current of one ampere in 1lo-235

Hz frequency range by the use of

52 IO lock-in amplifier is 1O-8ohms. The out-of-phase component of ac voltage signal never exceeded 10 percents of in-phase signal in normal resistance state and is usually half an order of magnitude higher low

resistance

resistance

state giving

measurements

rise to uncertainty

up

in

of

/

0

ZFC

-5

_lo _-_____L>

PACO512

t

to 5.10 -8ohms.

I

I

100

200

300

400

Figure 4. DC susceptibility of PACO 512. As it is shown on curve (a) of fig.4. The sample was p(O,)=60

bar

cooled in zero field down to 100 K and reheated in

p(CO,)=35 bar

magnetic field which is

followed by suppression

of the weight up to 290 K and an increase by further heating up to 70°C. The

-8

average magnetic field

gradient was - 120 gausscm -I and sample dimensions 5x5 mmr. The magnetic field estimated in the center of sample was -20-35 gauss. The accurate measure0

100

200

300

400

500

600

ments of dc susceptibility are limited by ferromagnetic

700

contribution of Fe

t(%

impurities extended in some

samples up to 300 ppm. In addition, in several samples tested SC properties are confined to thin layer Figure 3. Temperature dependence of electric

(2-5 microns) which was estimated by fine grinding.

resistance of PACO 5 12 sample.

Interior of samples is found to be semiconducting.

The measurement of electric resistance for sample

REFERENCES

PACO 512 annealed at 345OC for 24 hours under p(O,)=60

bar and p(CO,)=45

bar reveals

the

transition to SC state (fig.3.) with onset at nearly 70°C for measuring current 1 mA. An enhancement

of

electric resistance by application of 1A measuring current is evident. At 20°C for measuring current of 0.5 A the resistivity is about 10-l pohmcm which is three orders of magnitude less than that of silver. The only materials known so far to exhibit resistivities less than that of silver are superconductors. DC magnetic susceptibility measurements were performed on balance with sensitivity of 0.1 mg on sample of mass 113 mg.

1. D. A. Grisafe and W. B. White, Am. Mineral. 49 (1964) 1184. 2. A. C. Roberts, J. A. R. Stirling, G. J. C. Carpenter, A. J. Criddle, G. C. Jones, T. C. Birkett and W. D. Birch, Mineral. Mag. 59 (1995) 305. 3. G. Pannetier, S. Fenistein and G. DjegaMariadassou, Bull. Sot. Chim. Fr. (1964) 701. 4. A. Bystrom, Arkiv. Kemi Min. Geol. 20Al No 11 (1945). 5. J. S. Anderson and M. Stems, J. Inorg. Nucl. Chem. 11 (1959) 272.