Synthetic Metals, 34 (1989) 157-162
257
FORMATION OF GRAPHITE OXIDE
M. MERMOUX Science des Surfaces et Mat~riaux Carbon,s, INP Grenoble,
BP 75, F-38402,
associ~ au CNRS (UA 413)
Saint Martin d ' H ~ r e s
(France)
Y. CHABRE Laboratoire de Spectrom~trie Physique, Universit6 Joseph ~ourier-Grenoble Saint Martin d ' H ~ r e s
associ~ au CNRS (UA 08)
I, BP 87, F-38402,
(France)
ABSTRACT Preparation of graphite oxide in nitric acid media has been performed and analyzed step by step. Evidence is given that graphite oxide is obtained by hydrolysis of an intermediary compound which is the result of an overoxidation of the second stage nitric acic GIC. A preliminary characterization
of
this intermediary compound is presented.
INTRODUCTION Interest
in graphite
oxide has
positive electrode material
increased
after
in lithium batteries
it has been proposed [I]. Electrochemical
as
tests
have clearly shown that it compares well with graphite fluoride in terms of electrical capacity,
as well as for energy and power density
[2].
From 13C NMR studies we have shown recently that graphite oxide contains covalently carbons
linked epoxy
[2,3].
An
(etheral) groups,
average
formula
close
hydroxy groups and sp 2 coordinated to C400H
has
been
agreement with the earlier hypothesis of Hofmann and coworkers It is generally accepted that graphite oxide
(hereafter
proposed,
in
[4].
G.O.)
can only be
obtained by oxidation of graphite acid salts, such as nitrate or bisulfate, with strong oxidizing agents such as KCIO 3, KMnO 4, CIO 2, sis
is enforced
electrochemical
when reminding way:
that G.O.
for example
can also be obtained
electrochemical
sulfuric acid leads to the formation of the first which givesG.O,
by overoxidation
etc...This hypothe-
oxidation
through
an
of graphite
in
stage graphite bisulfate
[5]. But very scarce information
has been
given on the mechanism of this overoxidation.
0379-6779/89/$3.50
© Elsevier Sequoia/Printed in The Netherlands
158 We focus our attention on these questions, mine how w e r e
particularly in order to deter-
formed the epoxy and hydroxy groups.
doing step by step synthesis with X-ray diffaction,
This has been obtained
in nitric acid, as in the Brodie process
FTIR spectroscopy,
[6],
13C NMR and DTA studies at differ-
ent steps to characterize the intermediary compounds. SAMPLES PREPARATION In our previous
studies
modified Brodie method
G.O.
preparation
[7]. In this study,
was carried out according
to a
in order to examine the different
steps of the synthesis we stopped the reaction before adding KClO 3 and before the washing
of the product.
For this,
from Madagascar,
10~m grain size)
is put in concentrated nitric acid,
anhydrous
KCIO 3 is added gradually.
then
and finally dried at room tempera-
Great care is taken to prevent atmosphere exposition dur-
ing all this process. atmosphere,
(natural,
Then it is washed several times with
nitric acid and filtrated,
ture under vacuum.
powder
The solution is heated at 70°C-80°C un-
til the powder turns to a green color. concentrated
the graphite
When treated with water,
or within hours at ambient
this green compound thus obtained turns to a yellow one which is
G.O.. Samples have also been prepared in this way but with heavy water
(D20)
in the latter step, for comparative studies by NMR and FTIR. RESULTS AND DISCUSSION X-ray diffraction In fig.l are shown the diffraction various
steps
of the G.O.
profiles
preparation.
It
of the products
is known
that
obtained
graphite
at
reacts
spontaneously with nitric acid to give a second stage graphite intercalation compound la),
(GIC) [8]. This GIC is observed with
in agreement
with previous
results.
an 11.15 A Ic parameter
The green compound,
potassium chlorate has been added to the solution, close to 8 A
(Fig
obtained when
has an Ic parameter value
(Fig. ib), whereas the yellow compound obtained after action of
the water or exposure to ambient ed in fig Ic, characteristic
atmosphere gives the X-ray profile present-
of G.O.,
with an Ic parameter value depending
on the water content of the sample [7]. A value close to 6 A is observed for the the well dried G.O. samples. FTIR Spectroscopy The FTIR spectra of the of the G.O. pellets
preparation
pressed
with
compounds obtained at the above mentioned
are presented
KBr,
in Fig 2. They
under an argon atmosphere.
were The
steps
recorded, spectrum
from
of the
159
50
40
30 20
20
10
i 50
4O
3O 20
I!
2O
10
!
~
I
,
i
,
~
50
J
,
i
,
I
I
4O
Fig.
I.
second
to
stage
nitric
O-H
groups.
,
J
I
Proof
of
and
hydrogen
chlorate
one obtains
ance of a new band at 1070 cm ported by Hadzi and Novak its
mode
the
I
,
i
in fig.2a:
the strong band
at 1375
the band at 3400 cm
can be assigned
bonding
different
between
the
at 2940 cm-i[8].
the spectrum -i
oxide.
presented
of the
the appear-
of C-O bonds,
as reon this
O-H
may be characteristic
After action
in fig.2b:
HNO 3
[9]. The band at 1375 cm -I is still present
intensity
of
,
c) graphite
is reported
of NO 3 ions
is given by the band centered
but
,
I0
green compound,
potassium
spectrum
i
of: a) second stage nitric acid GIC
molecules
stretching
,
20
patterns
acid GIC
zs characteristic the
,
20
X-ray diffraction b) intermediary
cm
,
3O •
c
has
increased,
groups.
The
as
compared
water-washed
to
that
compound
of
the
presents
the
FTIR spectrum 2c: it is that of G.O., characterized by another band at 1370 -i cm , due to the appearance of acidic tertiary C-OH groups. An increase of the
relative
amount
of the O-H groups
firmed by measurements
on D20 washed
bonds with a stretching that Hadzi
and Novak
tons in G.O. that
part
washing
of
samples,
in which
This
has been
case one observes
mode at 2560 cm -I. This must be compared
failed
can be replaced the
is also observed.
protons
to exchange
proton
with deuterium
by strong basic reagents of
step of the preparation,
the
G.O.
structure
only.
comes
conO-D
to the fact
in G.O.:
pro-
One can conclude
during
the
which rmlst be seen as a hydrolysis.
water-
160
~000
~0
3~80
a§ZO
Z~60
Z~O0
I~0
1~eo " I|20
#60
k~AVENUMBER
Fig. 2.
FTIR spectra of: a) second stage nitric acid GIC; b) intermediary green compound;
c) graphite oxide; d) deuterated graphite oxide.
13C high resolution NMR We have done preliminary 13C CPMAS measurements of the compound obtained by action of the potassium chlorate on the second stage nitric acid GIC. Spectra of this overoxidized second stage GIC are similar to that of G.O.. In both cases they are characterized by three lines, ppm from TMS, respectively sp
2
hybridized carbons
shifted by 60.2, 71.2 and 132
attributed to epoxy groups , hydroxy groups and
[3]. But
the
intensity
of
the
line due to the hy-
droxy groups is smaller in the intermediary compound than in G.O.. In agreement with the results of the FTIR,
this confirms that part of the protons
comes from the final water-washing step.
161 DTA analvsis
The thermal behaviors of the various samples are presented in fig.3. Concerning the second stage nitric acid GIC
(fig.3a) the presence of an endo-
thermic peak which begins at 50°C shows that the compound turns to a higher stage one on heating. The DTA of G.O. 100°C,
assigned
to its dehydration,
(fig.3c) shows an endothermic peak at and a strong exothermic
corresponding to its exfoliation. A similar behaviour in the case of the intermediary compound,
one at 240°C
(Fig.3b)
is observed
but one can notice that there is
no endothermic peak which could be attributed to dehydration or to nitric acid
deintercalation.
present
in this
It
seems
that
intermediary green
all
the
chemical
groups
compound are covalently
which
are
linked to the
carbon skeleton. Exfoliation f
so
Ex follation
~
IOO
200
~sfl
*
('C)
so
i I
,-4
50
a
Fig.
3.
~00
200
;SO
1fct
~
b
DTA o f : a) second s t a g e n i t r i c compound,
i~o
/~o~
75o T(c}
e
a c i d GIC, b) i n t e r m e d i a r y g r e e n
c) graphite oxide
CONCLUSIONS
The preliminary results reported in this paper show that action of the potassium chlorate on the second stage nitric acid GIC leads to an intermediary compound which is transformed in graphite oxide by an hydrolysis. new green compound contains covalent C-O bonds, have sp 3 coordinated carbons.
The observation we have done to date is
sufficient enough to have a clear picture of this compound. have not yet clearly Ic parameter
This
so its carbon skeleton must not
In particular we
identified the chemical groups which are present. The
(close to 8 A)
is consistent with a first stage compound in
which nitrate groups would be covalently bounded to a puckered carbon skeleton.
The
(i00) diffraction line leads to a 1.52 A value for the C-C dis-
162
tance, G.O.
as in G.O.. whereas
For the first time we were able to prepare deuterated
previous
reports
have clearly
shown that exchange
of proton
with deuteron does not occur when G.O. is simply put into heavy water. This confirms that part of the O-H groups present in G.O. comes from the hydrolysis final step in the formation process. So,
as proposed by Fischer and coworkers
[I0], it seems that the charge
transfer compounds which can be formed by reacting graphite with electron acceptors can be classified in two distinct groups:
the ones obtained from
weakly oxidizing species which give GICs in which the guest species is ionic and in which the transferredcharge is delocalized, leading to a metallic behavior;
the others obtained from overoxidation of the first ones which are
covalent insulator compounds in which the transferred c h ~ e s
are localized on
the C-O bonds. In this latter case the carbon skeleton is no more planar but puckered. According
to these
results,
chemical
overoxidation
graphite bisulfate GIC by potassium permanganate,
of the
second
stage
as done in the Staudenmai-
er or Hummers and Offeman synthesis method to prepare G.O.,
also would give
a covalent compound similar to the one that we described in this paper. Concerning this new green compound, phite nitrate,
that we think to be a first stage gra-
further studies are currently in progress in order to deter-
mine its stoichiometry and to get a detailed scheme of its structure.
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1
Ph. Touzain, R. Yazami and J. Maire, French patent 83.8266
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i0
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