Solid State Ionics 18 & 19 (1986) 13-20 North-Holland, Amsterdam
13
STOICHIOMETRY, STRUCTUREAND CONDUCTIVITY OF NASICON A. CLEARFIELD, M.A. SUBRAMANIAN, P.R. RUDOLFand A. MOINI Department of Chemistry, Texas A&M U n i v e r s i t y , College Station, Texas, 77843, U.S.A. The crystal structures of two near stoichiometric NASICONS were determined from powder neutron d i f f r a c t i o n data. The compound prepared by Hong's s o l i d state reaction had a composition Na3.17ZrI.93Sil.9PI.IOI2 and a sol-gel preparation heated at I080°C gave Na3ZrI.93Si2P011.86. These compositions, obtained from refinement of the occupancy factors, were found to agree with elemental analysis carried out by X-ray fluorescence. The foregoing compositions are considerably d i f f e r e n t from that of a NASICON obtained by a hydrothermal route, Na3.2ZrI.68SiI.84PI.16011.54, and t h e i r unit c e l l parameters are somewhat larger. This difference results from the incorporation of approximately 0.32 moles of Na+ in the Zr 4+ sites f o r the hydrotherma] preparation. Solid state MAS NMR data are presented to support t h i s f i n d i n g , and in one sample, trapped electrons were detected. The hypothesis is proposed that the exact stoichiometry of NASICON cannot be represented by a simple s o l i d solution series, but r at her , depends on the method of preparation. 1. INTRODUCTION
of a rhombohedral NASICON by f l u x growth.
The discovery of NASICON was an important
They
determined the structure by X-ray d i f f r a c t i o n
development in the f i e l d of s o l i d e l e c t r o l y t e s
and obtained a nonstoichiometric composition,
because i t provided a superion conducting sys-
Na3.1ZrI.78Si1.24PI.76012, by refinement of occupancy factors. In a d d i t i o n , they found
tem in which conduction occurred over a three dimensional cavity network. 1'2
Thus the e l u c i -
that the end member with x = 3 contained a
dation of the mechanism of sodium ion trans-
zirconium deficiency with the charge being
port in this system became a high p r i o r i t y .
compensated by the presence of protons. I0
However, a vexing problem soon became evident.
suggested that the one dimensional NASICON
Several groups reported d i f f i c u l t y
formula proposed by Hong2
NASICON free of other phases. 3-6
in preparing The e l e c t r i c a l
They
and ceramic properties are affected by the accu-
(2) Nal+xZr2SixP3_xOl2 needs to be extended to a plane in the quaterna-
mulation of these other phases in the grain boun-
ry phase diagram.
daries of the sintered powders and reports on
should be
the i n s t a b i l i t y of NASICONS are undoubtedly i n -
(3) Nal+x+4yZr2_ySixP3_x012. 1 Meanwhile C l e a r f i e l d et a l . 1,12 prepared
fluenced by this factor. 7'8 The appearance of ZrO2 in the products made
The new general formula
monoclinic NASICON by a hydrothermal route
by high temperature s o l i d state reactions led
and found a single phase (by XRD) of t o t a l
von Alpen et a l . 6 to propose a second formula
composition given by X-ray fluorescence analysis
f o r the NASICON s o l i d s o l u t i o n , namely
as Na3.3Zrl.65Sil.9P1.I011.5. The s olid obtained from the i n i t i a l hydrothermal reaction had
(I) Nal+xZr2_x/3SixP3_xOl2_2x/3 . Although compositions of this type are known
a composition of Na4Zr2Si2PI.8015 and was stable
to e x h i b i t an X-ray pattern of a single NASICON
to about IO00°C. Above this temperature P205
phase, i t has recently been shown that these
s p l i t out to y i e l d the nonstoichiometric NASlCON.
solids also contain a glassy phase of low z i r -
Since i t is possible to have a single phase
conium content. 8 Kohler and Schulz 9 obtained single crystals 0 167-2738/86/$ 03.50 © Elsevier Science Publishers B.V. (North-Holland Physics Publishing Division)
appear in the X-ray pattern but to have glassy materials also present as a second phase, 8 we
14
A. ~Tearfield et al. / Stoichiometry, structure and conductivity o f NAS1CON
decided to solve the s t r u c t u r e o f our non-
prepared f o r neutron d i f f r a c t i o n
s t o i c h i o m e t r i c sample by powder neutron d i f -
sample of Alpha Inorganics NASICON was found
fraction
techniques.
Refinement of occupancy
studies.
to c o n t a i n l a r g e amounts of ZrO 2.
This sample
f a c t o r s should reveal the s t o i c h i o m e t r y of the
was reground and heated to IIO0°C f o r 20 hr
crystalline
and an a d d i t i o n a l 28 hr at 1150°C.
phase o n l y .
The r e s u l t 13 was a
A
This t r e a t -
f o r m u l a , Na3.2ZrL.68SiL.84P1.16011.54 , which i s very close to t h a t d e r i v e d from the a n a l y t i -
ment reduced the f r e e ZrO 2 to about 3-5 w e i g h t
cal data.
fully
The reason f o r t h i s strange s t o i c h i o -
%.
The hydrothermal p r e p a r a t i o n was described elsewhere 12 and i t s
s t r u c t u r e determina-
t i o n by neutron d i f f r a c t i o n
metry was also apparent; about 0.32 moles o f
r e p o r t e d e a r l i e r . 13
2.2 Neutron D i f f r a c t i o n
Na+ were found in the Zr 4+ s i t e s .
Neutron d i f f r a c t i o n
In c o n t r a s t to the above, Engell et a l . 14
Studies
time of f l i g h t
(TOF)
used a s o l - g e l technique to prepare s t o i c h i o m e -
data were obtained on the Special Environments
tric
phases which conformed to the Hong formu-
Powder D i f f r a c t o m e t e r (SEPD) a t the Intense
la.
This study stands in o p p o s i t i o n to the r e -
Pulsed Neutron Source (IPNS), Argonne National
s u l t s o b t a i n e d by Kuriakose e t a l . , 8 who found
L a b o r a t o r y . 17
that all
a t h i n - w a l l e d vanadium can under dry c o n d i t i o n s .
such p r e p a r a t i o n s contained ZrO 2.
We,
The samples were loaded i n t o
however, have prepared a s e r i e s of NASICONS in
Data p r e p a r a t i o n and r e d u c t i o n was conducted
which Sc3+ replaced p a r t o f the Zr 4÷.
on the 150 ° back s c a t t e r i n g banks.
The
In each
s t r u c t u r e o f two of these p r e p a r a t i o n s was de-
case the s t a r t i n g model f o r i n p u t to the R i e t -
termined by X-ray powder methods and r e f i n e d
veld program was t h a t of Hong2 f o r the composi-
by the R i e t v e l d technique. 15
t i o n Na3Zr2Si2P012.
No s i g n i f i c a n t
Refinement was c a r r i e d
change in composition over t h a t in the r e a c t a n t
out w i t h neutron TOF R i e t v e l d a n a l y s i s pro-
mix was observed.
grams 18 using a t h r e e - t e r m r e f i n a b l e background
That these p r e p a r a t i o n s are
s t o i c h i o m e t r i c lends support to the idea t h a t
f u n c t i o n and a two-term Gaussian peak shape
both s t o i c h i o m e t r i c and n o n s t o i c h i o m e t r i c forms
function.
of the compound are p o s s i b l e . 16
a s t o i c h i o m e t r i c s o l - g e l p r e p a r a t i o n (SG-AM56)
t h e s i s i s c o r r e c t , then i t the composition f i e l d exist.
I f t h i s hypo-
remains to d i s c o v e r
over which s t a b l e NASICONS
This paper i s a c o n t r i b u t i o n toward t h a t
Data were obtained f o r two samples;
heated a t 1080 ° f o r 20 hr and the reheated Alpha Inorganics N/~SICON (AI-NAS-1).
Programs
TPRMPH and TLSMPH were used to r e f i n e samples which contained ZrO 2 as they a l l o w simultaneous
end.
refinement of up to 4 phases. 19 cell profile
2. EXPERIMENTAL SECTION
Initially
and p o s i t i o n a l parameters of the
2.1 P r e p a r a t i o n o f NASICONS
NASICON p o r t i o n o f the data were r e f i n e d .
High temperature s o l i d s t a t e r e a c t i o n s were
was f o l l o w e d by o p t i m i z a t i o n o f the minor phase
c a r r i e d out in sealed p l a t i n u m tubes to prevent
parameters and in the f i n a l
the escape of v o l a t i l e
parameters were s i m u l t a n e o u s l y r e f i n e d .
c o n s t i t u e n t s . 11
The r e -
a c t a n t s c o n s i s t e d o f c a r e f u l l y weighed out quantities
o f Na3PO4, ZrP207, ZrO 2 and SiO 2 to give
In the case o f sample SG-AM56, the d i f f r a c contributing reflections
bed f u l l y
I.OA down.
paper. 11
were 20-50 hr. a t 1150°C.
Heating times
Sol-gel preparations
refinements a l l
t i o n peaks were extremely broad w i t h over 150
the d e s i r e d composition and t r e a t e d as d e s c r i in an e a r l i e r
per data p o i n t from
No ZrO 2 was detected in the p a t t e r n
However, the broadness o f the peaks was respon-
f o l l o w e d the procedure given by Engel114 w i t h
s i b l e f o r a slow approach to convergence.
minor v a r i a t i o n s .
final
Two s p e c i a l samples were
This
The
d i f f e r e n c e p l o t showed t h a t the problem
A. Clearfield et al. / Stoichiornetry, structure and conductivity o f NASICON
15
with peak asymmetry could not be eliminated.
tained.
These were phase I , Na5Zr(P04) 3 and
Therefore, the refinement was not as complete
y-Na3PO4.
This l a t t e r phase is probably s t a b i -
as f o r other samples and consequently the esd's
l i z e d by the presence of Zr 23 and has the compo-
are s l i g h t l y l a r g e r .
As part of each refinement
s i t i o n Na ~ Z r . . . . Z.JJ
(PO,)~ previously represent-
2~
U.tO/
the occupancy factors were released and only
ed as Na7Zro.5(P04) 3. ~
s i g n i f i c a n t changes retained.
monoclinic NASICON obtained.
Elemental analysis was carried out by X-ray
In no case was a single Therefore, in
order to obtain some idea of the stoichiometry,
fluorescence (Micron, In c ., A n a l y t i c a l Services
we prepared a sample (AI-NAS-1) whose s t a r t i n g
Laboratory).
composition was close to Na3Zr2Si2POt2.
Because
a large amount of sample was required f o r the 3. RESULTS
neutron study we reheated a commercial product
In the high temperature platinum tube reac-
(Alpha Inorganics NASICON) u n t i l no f u r t h e r
t i o n s , we explored a range of compositions giv-
reduction in the ZrO2 content was observed.
en by eq.(3) in which x = 0-3 and y = 0-0.3.
Full d e t a i l s of the structure determination
The results are shown in Figure 1 as a p l o t of
and results w i l l be published elsewhere. 24
x versus y.
the portions pertinent to this discussion are
A completely open c i r c l e indicates
Only
that only a single phase (rhombohedral NASICON)
given in Table 2.
was observed in the X-ray pattern and a t r i a n -
unit c e l l dimensions are almost i d e n t i c a l to
gle indicates the monoclinic phase.
I t is to be noted that the
Partial
blackening on the l e f t hand side of the t r i a n -
No1+4y+xZr2-yS1xP3-x012
gle or c i r c l e indicates the presence of ZrO2 and
ZrO~
on the r i g h t hand side of the f i g u r e , a phase
~)
other than ZrO2 or NASICON. This was usually
L~ Monoclinic Rhombohedral
phase I , a sodium zirconium phosphate with a composition range Na4.8_4.52ZrI.12_1.05(P04)3 .20'21 I t is seen that only a small number of the compositions consisted of a single phase and none of these were compositions in the high conduction region.
~.o~'~
xf
1.5(
In some cases the samples were reground
and reheated f o r up to 100 hr with only a small decrease in the amount of minor phases.
Howev-
er, i t is i n s t r u c t i v e to examine the u n i t c e l l
,o( )
O
@
@
@
@
@
072
o13
parameters of the NASICON phases which are col-
o.C)
lected in Table i . Along the j o i n represented by y = O, the unit c e l l dimensions increase in much the same way as given by Hong2 except that in the high Si region our a axis is considerably larger.
This
has also been found to be the case by others. t4'22
As y increases, in the region of i n -
terest f o r high conduction (x = 1.5-2) ZrO2 as well as sodium zirconium phosphates were ob-
oC Y
FIGURE 1 Phases formed by high temperature solid state reactions
16
A. Clearfield et al.
/ Stoichiometry, structure and conductivity o f NASICON
TABLE 1 Unit Cell Parameters and Phases Obtained f o r D i f f e r e n t NASICON Preparations Exp. No.
Composition
Other* Phases Present
MAS-13
Nal.5Zr2Sio.5P2.5012
WW-122
NaI.9ZrI.9Sio.5P2.5012
L a t t i c e Parameters a(A)
b(A)
c(A)
~(deg)
None
8.8792(7)
-
22.768(1)
-
ZrO 2 + I
8.8804(6)
-
22.771(1)
-
ZrO 2 + I
8,8863(6)
-
22,775(1)
-
ZrO 2
8.9426(7)
-
22.838(2)
-
-
22.849(2)
-
WW-120
Na2.3Zr1.8Sio.5P2.5012
MAS-12
Na2Zr2SiP2012
MAS-18
Na2.2Zr1.95SiP2012
MAS-15
Na2.4ZrI.9SiP2012
ZrO 2 + I + U
8.9485(5)
N~AS-17
Na2.8ZrI.8SiP2012
ZrO 2 + U
8.9625(5)
-
22.866(2)
-
ZrO 2
8.9904(5)
-
22.901(3)
-
MAS-23
ZrO 2 + U
MAS-24
Na2.5Zr2Sil.5Pl.5012 Na2.7Zrl.95Sil.5PI.5012 Na2.9ZrI.90Sil.5PI.5012 Na3.3Zrl.8oSil.5PI.5012
MAS-26
Na2.8Zr2Sil.8Pi.2012
MAS-21 MAS-19
MAS-25 MAS-11
Na3.4ZrI.85SiI.8PI.2012
15.5807(6)
8.9978(5)
9.219(4)
123.86(2)
15.591(1)
9.003(I)
9.208(1)
123.76(2)
15.6065(9)
9.0216(12)
9.2219
123.61(2)
ZrO 2 + I
15.605(2)
9.020(1)
9.212(1)
123.61(1)
ZrO 2 + I + U
15.646(2)
9.048(1)
9.214(1)
123.60(2)
ZrO2
15.654(2)
9.050(1)
9.212(1)
123.58(2)
ZrO 2 + U ZrO 2 + U + y-Na3PO 4
Na3Zr2Si2POI2
* I = S o l i d S o l u t i o n (see t e x t ) U = Na5Zr(P04) 3 those of MAS-11 in Table I which was obtained
t h i s formula is t h a t c a l c u l a t e d to j u s t s a t i s f y
from the platinum tube r e a c t i o n of the required
a l l the cation charge.
initial
elemental analysis in t h i s case is not as good
stoichiometry.
The formula f o r t h i s
Agreement with the
monoclinic NASICON phase, derived from the occu-
as f o r the previous sample but t h i s is to be
pancy f a c t o r s of the r e f i n e d neutron d i f f r a c t i o n
expected as the neutron peaks were broadened
data, is N a 3 . 1 7 Z r l . 9 3 S i l . 9 P i . 1 0 1 2 . This formula f i t s the scheme presented in e q . ( 3 ) , t h a t i s ,
ever when t h i s sample was heated to 1150°C,
a zirconium d e f i c i e n c y compensated by 4Na+.
a small amount of ZrO 2 formed accompanied by
El-
so t h a t the refinement was less accurate.
How-
emental a n a l y s i s f o r t h i s phase (XRF) is given
a considerable sharpening of the X-ray powder
in Table 3 along w i t h that c a l c u l a t e d from the
reflections.
neutron d i f f r a c t i o n
data.
We note t h a t except
Another i n t e r e s t i n g f e a t u r e of t h i s prepara-
f o r the low c a l c u l a t e d Zr value the agreement
t i o n is the almost complete segregation of
is e x c e l l e n t .
the s i l i c o n in T2 s i t e s and the phosphorus
However, we estimated from the
refinement t h a t about 4 weight % ZrO 2 was also
in T1 s i t e s .
present in the s o l i d .
segregation is real is found in a c o n s i d e r a t i o n
When allowance is made
f o r the ZrO 2, the best f i t
to the elemental ana-
Corroborating evidence that t h i s
of the bond distances.
The range of values
l y s i s o v e r a l l is found f o r 3 weight % ZrO 2 (Na,
f o r the P-O bonds (in T1) is 1.518(11)-1.537(9)A
12.4%; S i , 9.8%; P, 6.3%; Zr, 35.5%).
and f o r the Si-O bonds (in T2) 1.616(14) to
S i m i l a r l y refinement of the neutron data f o r
1.683(17)A.
The accepted average values f o r
the s o l - g e l sample (SG-AM56) y i e l d e d the formula
Si-O t e t r a h e d r a l bond distances are 1.620(2)A
Na3ZrI.93Si2P011.86.
and f o r P-O 1.520(3)A. 25
The amount of oxygen in
By way of contrast
A. Clearfield et al. / Stoichiornetry, structure and conductivity of NASICON
17
TABLE 2 Crystal Structure Data f o r Several NASICONS Prepared by D i f f e r e n t Synthetic Methods AI-NAS-I Space Group
SG-AM56
C2/c
C2/c
Hydrothermal C2/c
SCH(-x=2) C2/c
o
a(a)
15.6451(4)
15.643(4)
15.6209(8)
15.6407(6)
b
9.0491(2)
9.0484(7)
9.0326(5)
9.0498(3)
c
9.2151(2)
9.2214(22)
9.2172(5)
9.2102(4)
B(deg)
123.74(1)
No. of c o n t r i b u t i n g reflections
123.87(1)
123.67(1)
123.71(3)
977
975
997
R wp Rp
0.0334
0.0443
0.0285
-
0.0539
0.0765
0.0664
*
Re
0.0183
0.0200
0.0124
0.0528
0.0622
Occupancy f a c t o r Zr
1.93(1)
1.93(1)
1.67
2
P1
0.48
0.95
0.30
0.75
Sil
0.51
0.05
0.70
0.25
P2
0.61
0.05
0.86
0.26
Si2
0.39
1.95
1.13
1.74
Nal
0.27(1)
0.22(2)
0.265
1.00
Na2
1.00(1)
1.00(3)
1.00
0.732
Na3
1.90(6)
1.77(9)
1.608
1.268
Na(Zr)
-
0.326
• Not given the comparable Si-O and P-O distances
n AI-
treatment the s o l i d had a blue c o l o r a t i o n .
NAS-1, where s i l i c o n and phosphorus atoms are
Therefore we obtained i t s esr spectrum and
more randomly dispersed, are T I , 1.586-I.606A
t h i s revealed the presence of a radical with
o
and T2, 1.569-I.602A, respectively.
Data f o r
the NASICON prepared by a hydrothermal route are also given in Tables 2 and 3.
For t h i s sam-
ple we note that the sodium content is higher
g
= 2.047.
Reheating the sample in vacuum
removed some of t h i s species leaving free electrons in the l a t t i c e defects as shown by a signal at g = 2,0023.
and the zirconium content s i g n i f i c a n t l y lower
Preliminary NMR data also indicates that
than f o r the other samples as required by the
the hydrothermal preparation d i f f e r s from the
formula Na3.2ZrI.68SiI.84PI.16011.54. Furthermore the a and b axes are s i g n i f i c a n t l y smaller
near stoichiometric ones. In NaZr2(P04) 3 the 31p chemical s h i f t is -24.2ppm r e l a t i v e to
than f o r the other samples.
H3PO4 and the peak is narrow.
To confirm the s t o i -
chiometry we prepared a sample of the above comp o s i t i o n by the sol-gel method and unlike the
S i m i l a r l y in the stoichiometric compound Na3ScZrSiP201215 a much broadened 31p peak is observed at -12.4ppm,
contain ZrO2 even on s i n t e r i n g at 1200°C f o r 20
However in the hydrothermal preparation a simil a r 31p peak is observed at -11.7ppm but a
hr.
second much weaker (and broader) one is also
previous sol-gel sample (SG-AM56) i t did not However, we noticed that a f t e r t h i s heat
18
A. Clearfield et al. / Stoichiometry, structure and conductivity o f N A S I C O N
TABLE 3 Comparison of Observed Elemental Analysis (XRF) and Calculated Values from Neutron Refined Data Element
Obs.(XRF) %
Na
AI-NAS-1 Calc.(Neutron Data)
SG-AM56 Obs. % Calc.
Hydrothermal Obs. % Calc.
13.8
13.8
14.2
13.2
14.8
14.7
Si
9.9
10.1
10.2
10.8
10.8
10.3
P
6.3
6,4
6.4
5.9
7.2
7.2
Zr
34.8
33.3
34.5
33.7
29.8
30.9
obtained at +6.07ppm.
At this stage of our stu-
dy we tend to a t t r i b u t e this resonance to the
4. DISCUSSION There would appear to be no doubt, on the
influence of Na+ in the Zr 4+ sites acting on
basis of this study, that a nonstoichiometric
the phosphorus nuclei.
form of NASICON exists.
In fact the scandium
The stoichiometry
compound also gave a resonance at +5.8ppm, but
based on the refinement of the neutron d i f f r a c -
i t was so weak as to be barely perceptible. An 23 Na
t i o n data and elemental analysis carried out
NMR spectrum f o r Na5Zr(P04) 3 showed that
caused large s h i f t s in the 31p resonance.
There
by an independent laboratory agree w i t h i n the experimental error of the procedures.
Further-
were c l e a r l y v i s i b l e resonances of -4.36,
more, t h i s agreement rules out the presence
-0.97, +1.67 and +4.94ppm.*
of an amorphous or glassy phase in the hydro-
This compound has
a NASICON-Iike structure26 in which a l l of the
thermal preparation.
cavities are f i l l e d as well as half the Zr4÷
from the synthesis of the nonstoichiometric
sites.
phase by a sol-gel rather than a hydrothermal
The varied interactions of 23Na coupled
to 31p cause the m u l t i p l i c i t y of resonances. A similar anomaly was observed in the 29Si MAS NMR spectra.
The stoichiometric scandium
The f i n a l proof stems
technique. The sol-gel product was stable even to s i n t e r i n g at 1200°C without the appearance of a second phase. The key feature ex h ib it e d by the nonstoichio-
compound gave a single resonance peak at -90.3ppm while the hydrothermal preparation not
metric NASICON is the presence of 0.32 Na+ in
only gave this resonance (-90.1ppm) but another
the Zr 4+ sites.
very broad one of about I/3 intensity at -101.9.
ten (from refinement of the neutron data)
This l a t t e r resonance is indicative of a conden-
Na2.88(Zrl.68Nao.32)Sil.84Pl.16011.54 . This formula requires a deficiency of 0.23 moles
sed s i l i c a t e group such as pyrosilicate.
Thus, the formula can be w r i t -
3.1 Conductivity Data
of ZrO2 and 0.09 moles of Zr 4+ compensated
Conductivity data for the hydrothermally pre-
by 0.36 moles of Na÷.
In contrast the high
pared NASICON12 and the near stoichiometric sam-
temperature s o l i d state reaction and the sol-
ple, AI-NAS-1, are not too d i f f e r e n t even though
gel technique y i e l d products with more Zr,
the l a t t e r sample contained some ZrO2.
However,
i.e.,
1.93 moles and l a r g e r a and b unit c e l l
t h e i r corrosion behavior in contact with molten
parameters.
Their stoichiometries can be ration-
sodium may prove to be somewhat d i f f e r e n t and
a l i z e d as follows.
this aspect needs to be explored.
formula Na3Zr1.93Si2POiL.86, is d e f i c i e n t in
The sol-gel preparation,
0.07 moles of Zr02; f o r the s o l i d - s t a t e reaction NMR data collected by A. K. Cheetham and N. Clayden, University of Oxford.
the formula Na3.17Zr1.93SiI.9P1.I012 requires that the deficiency of 0.07 moles of Zr be
A. Clearfield et al. / Stoichiometry, structure and conductivity of NASICON
19
i n d i v i d u a l Si-O and P-O distance.
compensated by by 0.28 moles of Na+. One may question the stoichiometries just
There is a l -
most no difference in bond lengths between atoms
presented, but there are several factors which
in the T1 and T2 sites.
indicate they are accurate w i t h i n about 3 times
SG-AM56, where the Si and P atoms are segregated
the given esds.
i n t o sites T2 and TI , r e s p e c t i v e l y , the bond
F i r s t the agreement between
However, f or sample
the composition as determined from neutron d i f -
lengths are those of nearly pure Si-O and P-O
f r a c t i o n and XRF (obtained from an independent
distances, respectively.
laboratory) is e x c e l l e n t .
For sample AI-NAS-I
the difference in Zr values in fact predicts the presence of 4% ZrO2.
We also note that
I t is impossible at this time to t e l l whether the near stoichiometric NASICONS have any Na+ in the Zr 4+ sites.
We believe t h i s information
Schioler 22 carried out a neutron d i f f r a c t i o n
w i l l eventually arise from a d e t a i l e d NMR study
study of a stoichiometric NASICON sample of ex-
now underway.
pected composition Na3Zr2Si2P012 and we have
presence of free electrons in the nonstoichiome-
included her results in Table 2.
t r i c NASICON prepared by the sol-gel method.
The cell d i -
mensions of S c h i o l e r ' s preparation are almost
A surprising discovery is the
This could arise from an oxygen deficiency com-
i d e n t i c a l to those of AI-NAS-1 and SG-AM56 and
pensated by electrons in the oxygen sites.
the s o l i d also contained a small amount of ZrO2.
aspect also needs f u r t h e r i n v e s t i g a t i o n particu-
This
Therefore the composition of her NASICON should
l a r l y as to the nature of the u n i d e n t i f i e d ra-
be very close to that of AI-NAS-I.
dical and the e f f e c t on the c onduc t iv it y .
However,
Schioler constrained her t o t a l Na occupancy to equal 3 and that of Zr to be 2.
The refinement
I t is i n t e r e s t i n g that the conductivity of the near stoichiometric and nonstoichiometric
on t h i s basis produced several non-positive tem-
NASICONS are also i d e n t i c a l .
perature factors and poorer agreement factors.
not too surprising as the number of conducting
In our refinements, a l l the temperature factors
ions d i f f e r by only about 10% and t h e i r s i t e
were p h y s i c a l l y reasonable.
occupancy is nearly the same. Apparently the
Unfortunately
However, t h i s is
S c h i o l e r ' s data suffered from the presence of
bottleneck sizes also do not d i f f e r by much as
an impurity, probably Ti metal, and i t is not
the a c t i v a t i o n energies f o r conduction are also
known how much t h i s affected her results.
almost the same. F i n a l l y , we have proposed 13'15 that NASICON
We also note that our d i s t r i b u t i o n of sodium ions in the three c a v i t y sites d i f f e r s consider-
does not precisely conform to the s o l i d solu-
ably from that presented by Schioler.
t i o n formulas such as those represented by eqs.
She in-
dicates complete occupancy of the Nal s i t e
(1)-(3).
Rather the f i n a l composition is to
whereas we f i n d t h i s p o s i t i o n only 1/4 f i l l e d .
some extent path dependent; that i s , depends up-
In contrast in our study the Na2 s i t e was a l -
on the experimental conditions.
ways f i l l e d ,
the Na+ ions v ib r a t e so e n e r g e t i c a l l y at the
but Schioler found that s i t e to
We believe that
temperature required f o r NASICON formation that
be approximately 3/4 f i l l e d . Another feature i n d i c a t i n g the r e l i a b i l i t y
they tend to disrupt the l a t t i c e framework.
By
of our refinement is the way the Si-O and P-O
capturing some of these ions in t i g h t l y held oc-
bond distances r e f l e c t the d i s t r i b u t i o n of the
tahedral sites ( i . e . Zr-O distances are smaller
s i l i c o n and phosphorus atoms.
than Na-O bond distances) part of the stress is
When the d i s t r i -
bution is nearly random, the average bond dis-
alleviated.
tance l i e s close to the weighted mean of the
w i l l develop with f u r t h e r study by the methods
No doubt other r a t i o n a l i z a t i o n s
A. CTearfield et al. / Stoichiometry, stn~cture and conductivity o / N A S I C O N
20
indicated here including studies at elevated tem-
12.
A. C l e a r f i e l d , M. A. Subramanian, W. Wang and P. Jerus, Solid State lonics 9/10 (1983) 895.
13.
P. R. Rudolf, M. A. Subramanian, A. C l e a r f i e l d and J. D. Jorgensen, Mat. Res. B u l l . 20 (1985) 643.
14.
J. Engell, S. Mortenson and L. Moller , Sol i d State lonics 9/10 (1983) 877.
15.
M. A. Subramanian, P. R. Rudolf and A.
peratures. 5. ACKNOWLEDGEMENT Part of t h i s work was supported by the National Science Foundation under grant no. DMR 8025184 and by the Center f o r Energy and Mineral Resources of Texas A&M University f o r which grateful acknowledgement is made. We also thank Drs. Anthony K. Cheetham and Nigel Clayden, Universi-
C l e a r f i e l d , J. Solid State Chem., in press 16.
A. C l e a r f i e l d , Solid State lonics 9/10 (1983) 823.
17.
J. D. Jorgensen and J. Faber, J r . , in Proc. 6th Mtg. Int. Collab. of Advan. Neutron Sources. Ed. J. M. Carpenter. Pp 105-114. Argonne National Laboratory, June 28 - July 2, 1982. (ANL publication ANL-82-80).
f o r the use of t h e i r f a c i l i t i e s .
18.
R. B. Von Dreele, J. D. Jorgensen and C. G. Windsor, J. Appl. Cryst. 15 (1982) 581.
6. REFERENCES
19.
Programs from Materials Science and Technology D i v i s i o n , Argonne National Laborat o r y , Argonne, l l l i n o i s .
Hong, Mat. Res. B u l l . , 11 (1976)
20.
A. C l e a r f i e l d , R. Guerra, A. Oskarsson, M. A. Subramanian and W. Wang, Mat. Res. Bull. 18 (1983) 1561.
3.
M. L. Bayard and G. G. Barna, J. Electroanal. Chem. 91 (1978) 201.
21.
S. J. Milne and A. R. West, Mat. Res. Bull. 19 (1984) 705.
4.
J. P. B o i l o t , J. P. Salanie, G. Desplances and D. Le P o t i e r , Mat. Res. Bull. 14 (1979) 1469.
22.
L. J. Schioler, Ph.D. d i s s e r t a t i o n , Mass. Inst. Tech., Feb. 1983.
5.
R. S. Gordon, G. R. M i l l e r , B. J. McEntire, E. D. Beck and J. R. Rasmussen, Solid State lonics 3/4 (1981) 243.
23.
S. J. Milne and A. R. West, J. Solid State Chem. 57 (1985) 166.
24.
6.
U. von Alpen, M. F. Bell and H. H. Hoefer, Solid State lonics 3/4 (1981) 215.
P. R. Rudolf, A. C l e a r f i e l d and J. D. Jorgensen, J. Solid State Chem., in preparation.
7.
H. Schmid, L. C. De Jonghe and C. Cameron, Solid State lonics 6 (1982) 57.
25.
C. T. Prewitt and R. D. Shannon, Trans. Amer. Cryst. Assoc. 5 (1969) 51.
8.
A. K. Kuriakose, T. A. Wheat, A. Ahmad and J. Dirocco, J. Am. Ceram. Soc. 67 (1984) 179.
26.
J. P. B o i l o t , G. C o l l i n and R. Comes, Sol i d State lonics 9/10 (1983) 829.
9.
H. Kohler and H. Schulz, Solid State lonics 9/10 (1983) 795.
ty of Oxford, f o r taking the NMR data and Dr. James D. Jorgensen, Argonne National Laboratory f o r assistance with the neutron d i f f r a c t i o n data. The Intense Pulsed Neutron Source (IPNS) is operated under the auspices of the U. S. Department of Energy to whom thanks are extended
i.
J. B. Goodenough, H. Y.-P. Hong and J. A. Kafalas, Mat. Res. B u l l . I I (1976) 204.
2.
H, Y . - P .
173.
i0.
H. Kohler, H. Schulz and O. Melnikov, Mat. Res. B u l l . 18 (1983) 589.
Ii.
A. C l e a r f i e l d , P. Jerus and R. N. Cotman, Solid State l o n i c s , 5 (1981) 301.