Fluoridatedhydroqapatites synthesizedwith organicphosphate ester M.Okazaki Depaltment of Dental Technology, Osaka University Faculty of Dentistry. l-8 (Received 2 1 November 1989; accepted 22 November 1989)
Yamadaoka, Suita, Osaka 565, Japan
Fluoridated hydroxyapatites with various fluoride contents were synthesized with organic phosphate ester monomer as a source of P at pfl 9.5 and 80°C. The a-axis dimensions of the fluoridated hydroxyapatites decreased with the increase of the fluoride content in the same way as the fluoridated hydroxyapatites synthesized with inorganic phosphate under the same conditions. However, for the same calculated degree of fluoridation in the feed solution, fluoridated hydroxyapatites synthesized with organic P had higher fluoride contents than those synthesized with inorganic P. The crystallinity of the former decreased initially, then increased with increasing fluoride content; but on the whole it was lower than that of the latter. The apparent solubility at pH 4.0 and 37°C decreased dramatically and monotonically with increasing fluoride content and approached an almost constant value at a fluoride content above that of fluorapatite, at which value calcium fluoride was detected. Keywords: Hydroxyapatites, fluoride, organic phosphate ester, crystallinity
Organic phosphate esters such as ATP, phospholipid and nucleotide have various important roles in the human body’. Being present inside and/or just outside the cells or the matrix vesicles’, it is speculated that they may also be associated directly or indirectly with the formation of calcium phosphates. Some researchers3r4 have reported that organic materials promote crystal growth of hydroxyapatite and that hydroxyapatite was formed epitaxially along the c-axis of collagen. 0thers5-7, however, have reported that organic materials inhibit the diffusion of surrounding ions and finally the crystal growth of hydroxyapatite. Furthermore, these organic monomers and polymers sometimes interact with the crystal interface, may often be adsorbed or chemisorbed directly to the crystal surface and then are apt to inhibit crystal growth. However, the role of organic materials in apatite formation is not fully understood. In our previous study’, using mono(methacryloyloyxethyI) acid phosphate (PM), organic metallic monomer crystals were formed at below pH 10, and at above pH 10 hydroxyapatite was formed. The crystallinity of this hydroxyapatite was inhibited compared with that of hydroxyapatite synthesized with inorganic phosphateg, lo. Fluoride, on the other hand, may be associated with formation of hydroxyapatite as a reaction accelator in its initial stage, and also contribute to prevention of dental caries. Previous studiesg-” have indicated that the crystallinity of fluoridated hydroxyapatites (theoretical formula: CaIo(P04)s Correspondence to Dr M. Okazaki.
(OH), _ 2x FZx) showed unexpected behaviour with the increase of fluoride content, and that the pattern of crystallinity behaviour was sensitive to trace elements. Since the presence of organic materials sometimes inhibits crystal growth, the crystallinity of hydroxyapatite may be affected by phosphate ester. In this study, physicochemical properties of fluoridated hydroxyapatites synthesized with organic phosphate ester were examined.
MATERIALS
Reactions of calcium ions and phosphate ester were examined at 80°C under the various fluoride concentrations. A higher temperature for synthesis than the physiological 37°C was necessary to identify the precipitates as apatites. By a modification of the method used for fluoridated hydroxyapatitesynthesisg, 125 ml of 200 mM Ca(CH3C00)2 Hz0 was fed into 250 ml of mechanically stirred 1.3 M CH,COONH, solution containing 60 mM PM (Kyoeisha Yushi Co. Ltd. Japan) and O-40 mM HF. The calcium solution was supplied at 125 ml/h with a Tokyo Rikakikai microtube pump. The pH was maintained at 9.5 f 0.1 by occasional addition of concentrated NH40H solution. The suspension was stirred at 80 + 1 “C for 2 h, then filtered, and the precipitate was washed with distilled water and dried at 80°C for 2 d. X-ray diffraction was employed to identify precipitates. 0
46
Biomaterials
199 1, Vol 12 January
AND METHODS
1991
Butterworth-Heinemann
Ltd. 0142-9612/91/01DD46-04
FHAp
Measurements
were
made
diffractometer
with
graphite-monochromatized
radiation
on
a
Rigaku
Denki
synthewed
with
organ/c
P. M.
Okarak,
X-ray CuKa
35 kV, 23 mA.
Calcium absorption
concentrations
were
spectrophotometry.
trations
were
Fluoride
concentration
electrode
determined
(Model
by
were
407,
determined
Total the
method
determined
Orion
by atomic
phosphate
concen-
of
with
20
25
30
35
20
25
3c
35
20
25
30
35
20
25
3c
35
20
25
30
35
20
25
30
35
Eastoe13.
a specific
ion
Co. Ltd. USA).
RESULTS Products
synthesized
monomer
PM as a source
weak
alkaline
formed, pH 9.5,
due
similar
of P varied metallic
alkaline
was to
angle
that
organic
phosphate
with
pH, apatite
formed;
organic of about
of the apatite
and
no
compound
crystals was
4”.
This
formed
X-ray
as
diffraction
found
crystallinity with
and were
of PM. Above
were
synthesized
ester
pH. At acidic
monomer
7. This is due to the hydrolysis
apatite
diffraction than
at higher
in Figure
patterns
the
pH, organic
but
shown
with
at
was
inorganic
lower
Figure
P under
of
To examine
the
physicochemical
hydroxyapatites
(PM-FHAp), chemical Table
synthesized
the
synthesis
compositions
7. With
solutron,
concentrations apatites
similar
synthesized
(FHAp).
with
apatite,
was
to those
1.67.
expected
However, induced
the solution, fluoride
as will
content
2 mmol/g.
In
synthesized
with
equal
degree
fluoride
ratio,
the relatively
Ca/P,
be discussed
was the
case
inorganic
of fluoridation 2
I
L..
the
that
value,
of these
samples,
an ,ncrease
at about
to
hydroxyapat/tes.
half
of
floor/de
IS observed
Degree
content.
WI the peak
due
For to the
28.3”.
than the ratio
3
shows
of
the
(PM-FHAp)
PM-FHAp
rn
are
more organic
as compared
with
confirmed’that Crystallinity
was
1,
apatitic
fluoride
was
a- and
and
patterns
were
detected
with
inhibited
inorganic
inorganic
of F- ions
whole
organic
phosphate
(FHAp).
This indicates
hydroxyapatites,
is needed
phosphate.
as a source
It has already
of a-axis dimension into the OH initially,
then
as shown
with
of P been
is mainly
sites. increased
In Figure
as compared
of
with
fluoridated
phosphate
decreased
on the
dimensions
the same curves.
typical
of fluoridation,
c-axis
synthesized
the contraction
due to substitution the degree
hydroxyapatites content
X,
it, calcium
hydroxyapatites
although
fluorapatite,
fluoride
fluoridation,
fluorapatite.
that
Xr = 1, the
of
i.e. twice
of fluondated equal
Both sets of data gave almost
hydrolysis
Above
fluoridated
in the feed
shows
synthesized
of
than
phosphate,
to the expected
Figure products
higher
later.
patterns
numencally
Above
phosphate
hydroxy-
Fm/POd3-
of
observed. Figure
hydroxy-
was higher
high
is
of CaF2
fluondated
previously
of theoretical
content
diffract/on X,
and 2.15
degree
phosphate
value. This may be due to the incomplete
of PM, which
almost
molar
in
in the feed
and
phosphate
to that
The
shown
of fluoridated
inorganic
also similar
are
calcium
1.45
20:“)
phosphate pH 9.5.
of fluoridation
the
The calcium-phosphate
precipitates
at
X-ray
(1 1 1) reflection
of fluori-
organic
done
precipitates
degree
or below,
were
with
was
of the
a calculated
X,, of 0.5
properties
2
fluoridation,
X =
conditions.
dated
2 Gi”)
the
with
4, and was
that
of
FHAp.
I
I
1
the calculated
solution.
X-ray
diffraction
at a constant
patterns
of
Below
the
pH of 9.5.
0a
.,
.‘“-
5 6
6.92
-
6.87
1 0.5
0
b F/gun? organic at pH
1
Typical X-ray
Pat 7 4 lb)
various
pHs
d/ffraction (al. together
patterns wth
ofprecipitates that
synthesized
I
1
I
X synthesized wth
with
Inorganic
P
F/gure
3
synthesrzed
~-AXIS wth
and
c-ax/s
morgamc
dimensions (FHAp)
(CJ
of
fluoridated
and
organic
hydroxyapatites (PM-FHAp)
(0)
phosphates.
&omater/als
199 1, Vol
12 Januav
47
FHAp
synthesized
IO
0 T
-6
with
organic
PC M.
Okazakl
Table
I
--IN
I
1
Chemical
compositions
of precipitates
X‘
Ca(mmol/g)
P(mmol/g)
F(mmol/g)
Ca/P
0 0.02 0.04 0.10 0.16 0.20 0.50 1 2
9.57 9.74 9.65 9.74 9.37 9.19 9.06 8.81 8.70
5.73 5.89 5.84 5.80 5.65 5.56 5.19 3.80 3.32
0 0.170 0.280 0.538 0.845 1.07 1.39 2.90 4.30
1.67 1.65 1.65 1.68 1.66 1.65 1.75 2.32 2.62
X,: the calculated degree of fluoridation in feed solution.
Figure organic (300)
4
Ctystallinity P (PM-FHAp)
and
(002)
of shown
fluoridated
hydroxyapatites
as the inverse
synthesized
with
breadths
of the
of the half-value
reflections.
Transmission electron microphotographs supported in part the crystallinity behaviour as shown in Figure 5. The samples with the fluoride content below 2 mmol/g consisted of coagulated needle-like crystals and the crystal size seemed to increase with the increase of fluoride content. Above 2 mmol/g, spherical crystals, which were speculated to be CaF*, were observed in part. This was supported by X-ray diffraction analysis (Figure 2). Figure 6 shows the apparent solubility of PM-FHAp, represented by the dissolved calcium concentration in 0.5 M
acetate buffer at pH 4.0 and 37°C after one month. The solubility decreased dramatically with the increase of fluoride content until near 2 mmol/g, which is equal that of stoichiometrical fluorapatite. Above this content, the decrease was almost negligible, because calcium fluoride was formed. The absolute value of the solubility was higher than those of fluoridated hydroxyapatites synthesized with inorganic phosphate’ ‘.
DISCUSSION Hydrolysis With the acetate buffer used in this study, hydroxyapatite was formed at above pH 9.5, although in non-buffered aqueous system, the boundary pH rose and hydroxyapatite was formed at above pH 10. This tendency was also observed in a previous study’ performed at 60°C. Therefore, it may be said that hydrolysis of PM depends strongly on pH
a
d Figure
5
48
Biomaterials
Odprn
e
Transmission
electron
199 1. Vol
micrographs
12 January
of precipitates.
f Fluoride
content
fmmol/g):
0 (a); 0.170
(b); 0.538
(cl;
1.39
(d); 2.90
(e); 4.30
ff).
FHAp
apatites
PM-FHAp
60
0.5M acetate buffer
50
r
( pH 4.0.37”C
1
the
calcium
imperfection, content
20
conclusion,
1
and
Apparent
solubility
of the
I
4
precipitates
6
as the
calcium
strength.
complex
Below
(PM-Ca)
pH 9.0
the
following
organic
this solubility
behaviour
to the crystallinity crystal
growth
phosphate
was
behaviour.
soluble
by organic apatite
Although
because
of
substances.
crystals
thecrystallinity
in comparison
synthesized
with fluoride
In
ester can serve as a P source
of fluoridated
increased
with
under
highly
is inhibited
with
and
the fluoridated
inorganic
decreases
dramatically
at high fluoride
the strong
stabilizing
action of fluoride.
This
study
was
63570915
was formed: 0
yH3
of
P, the solubility
content
because
of
ACKNOWLEDGEMENTS
dissolved
concentration.
ionic
with
A
5
shown
dramatically
but the concentration
of crystal
alkalineconditions.
6
organic
This may be due to the degree
organic
hydroxyapatites
Ftgure
by the
under the
of crystal
the solubility
calcium
of
than that of FHAp
the apatite
in the formation
IO
content,
was not parallel
the inhibition
3 F(mmol/g)
be shielded
was higher
although
Probably,
2
Okazaki
F- ions. Also, the
of PM decreased
of fluoride
same conditions.
30
I
PC M
of the diffusion
POd3-, OH-,
may
solubility
increase
dissolved
(
by retardation
Ca”,
surface
The apparent
I
orgamc
Solubility
0 0
growth
with
compound.
40
E -
may be inhibited
the main components, crystal
t
synthesized
supported
in part by Research
from the Ministry
of Education
No.
Grant
of Japan.
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with
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almost
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