Journal of Molecular Liquids, 28 (1984) 191--204
191
Elsevier Science Publishers B.V., Amsterdam -- Printed in The Netherlands
COMPLEX F O R M A T I O N AND P H O S P M A T E - H 2 0 INTERACTIONS IN A CONCENTRATED
AQUEOUS Mg(H2P04) 2 SOLUTION.
RUGGER0 CAMINITI Istituto di C h i m i c a Generale, sit~ di Cagllari,
I n o r g a n i c a e Analitica,
Via 0spedale 72, 09100 Cagliari,
Unlver-
(Italy)
(Received 14 F e b r u a r y 1984) ABSTRACT X-ray d i f f r a c t i o n data from a solution of Mg(H2P04) 2 were examined,
the experimental d i s t r i b u t i o n curve shows peaks
at about 2.10,
2.7-2.9, 3.6, 3.9 and 4.25 ~.
The 3.6 A peak
reveals the formation of inner sphere m a g n e s l u m - p h o s p h a t e com+2-z in w h i c h oxygens from phosphate plexes M g ( H 2 0 ) 6 _ z ( H 2 P 0 4 ) z groups substitute z w a t e r m o l e c u l e s of the h y d r a t e d Mg(H20)~+v ions. Least squares refinements of the i(s) curve are consistent with a structural unit in w h i c h the phosphate
tetrahedron sha-
res a corner w i t h one m a g n e s i u m o c t a h e d r o n with Mg-0-P angle of 147 deg.
Each phosphate ion interacts with about eight wa-
ter molecules. INTRODUCTION Phosphate ion c o m p l e x i n g with various cations,
e.g. cal-
cium, m a g n e s i u m is important to an u n d e r s t a n d i n g of its behaviour in certain biological
systems;
the possibility of complex
formation b e t w e e n m a g n e s i u m and phosphate ion is of interest also in g e o c h e m i s t r y with regard to w a t e r and fresh water chemistry. While several solid m a g n e s i u m phosphates have been studied [la-d ] n o study by using X-ray diffraction has been done on the complex formation between m a g n e s i u m and phosphate ion in aqueous solution.
Now,
the X-ray diffraction technique has proved
0167-7322/84/$03.00
© 1984 Elsevier Science Publishers B.V.
192
to play an important role in the d e t e r m i n a t i o n of the coordination state of the metal ions in c o n c e n t r a t e d solutions.
Hydra-
tion and complex p h e n o m e n a can be deeply investigated by this me t hod
[2]
Previous diffractometrlc studies on trivalent
[3a-c] and b i v a l e n t
[4a-d I ions have shown the existence of di-
rect interactions b e t w e e n cation and sulphate anion. The existence of complex formation for the system MgH2P04 was shown by Havel and H~gfeldt
[6]
The techniques
used did not give direct evidence about the nature of the complexes but the values of the e q u i l i b r i u m constants strongly suggested an inner complex formation. A n a l y s i s of X-ray and neutron diffraction data from concentrated aqueous salt solutions gives details about the environment of the ions and information about the g e o m e t r y of the c o o r d i n a t i o n polyedra.
This is p a r t i c u l a r l y useful
in the ca-
se of direct interaction between the anion and the cation,
sin-
ce information about their relative o r i e n t a t i o n cannot be obtained through other experimental techniques than diffraction. A n o t h e r object of this w o r k was to study the h y d r a t i o n of phosphate anion.
The h y d r a t i o n of the oxyanlons has been
e x t e n s i v e l y studied in the case of sulphate solutlons while only a study has been done on the phosphate solutions
[5]
E X P E R I M E N T A L AND DATA TREATMENT The solution was p r e p a r e d by d i s s o l v i n g w e i g h e d amounts of M g ( H 2 P 0 4 ) 2 . 3 H 2 0 in water;
the compositions were determined
by standard volumetric methods. was o b t a i n e d by denslmeter.
The density of the solution
In table 1 we report the analyti-
cal data of the solution studied.
The temperature of the sam-
ple was 20ZI °C. TABLE 1 C o m p o s i t i o n of the solution in moles/liter, and ~
d is
the density
the linear absorption coefficient calculated for Mok~
radiation. [ M E 2+]
[ H2P0 ~]
1.5
3.0
[H20] 51.047
d(gcm -31
~(cm -11
1.2471
2.2459
193
The X - r a y ction
has b e e n
apparatus described
ducibility
of d a t a w e r e
each
were
point
was w i t h i n
1%
i(s) where
fi are
intensity puted
A
proposed mer
the
atomic
unit
and W a b e r
scattering
units.
The
[8~
for H 2 0
proposed
from
The
International
correlation
function
corrected
Ie.u.
factors
those
proposed factors
solution
com-
coefficients
[iO]
[ii]
in is the
were
the
et al.
of the
and
using
Tables
for a-
coefficients
scattering
by S t e w a r t
.
from
(i)
of atoms
and
obtained
)2
scattering
and P,
Details
to
amplitudes
formula
used.
[Sb-c,4a,7a-b] was
stolchimetrlc
m kinds
[9] for 0 atom.
taken
The
m ) / ( i=l ~ xifi
to an a n a l y t i c a l
those
by a F o u r i e r
according
for
reproducibility was
given
of r e p r o -
collected
the o v e r a l l
already
the
checks
) radiation
Ie.u.
x i are
for d a t a c o l l e -
counts
of the s o l u t i o n
containings
by H a J d ~
they w e r e
been
m _ i=l ~ xif~
in e l e c t r o n
H atom were
G(r)
have
intensities
according
The
(O.7107
function
seifert)
Continuous
Mok~
dispersion,
a structural
.
and
structure
= ( Ie.u.
nomalous
[7a-b]
performed. or m o r e
.
the n o r m a l i z e d
S. D.
iOOO00
of d a t a n o r m a l i z a t i o n The
( G.
by C r o -
for the
, for Mg a t o m
. was
calculated
transformation
= i + ( 2 ~2r
~Smax @o)-lJ si(s)sin(rs)ds
(2)
Smin here
@o
is the
s is the usual re ~ the
is h a l f
average
bulk
scattering
density
variable
the s c a t t e r i n g
angle
of s t o i c h i o m e t r i c
( s = ( 4~/l and
units,
) sin~
, whe-
A is the w a v e l e n g t h
of
radiation emploJed, Moka ) (0.65 ~-i ) and s ( 0 -i ' stain max ) are the l o w e r and u p p e r l i m i t s of the e x p e r i m e n t a l
15.5 A data.
In o r d e r
incoherent mator
was
stematic removal
radiation estimated
residual
up
the
reaching by
function,
the c o u n t e r
are c o r r e c t e d
peaks
in the
of c o r r e c t i o n
for i n a c c u r a t e
i(s)
a semi-empirlcal
errors
of s p u r i o u s
The m e t h o d makes
to e v a l u a t e
G(r)
through
procedure
fraction
curve
of
the m o n o c h r o I12]
by a m e t h o d
of s y s t e m a t i c
determination
the
•
based
Syon the
at low r [12] errors
.
generally
of the m o n o c h r o m a t o r
tran-
194 smission alters
factor
the
but
real
data normalization c
squares
Ic(S)
the c o r r e c t e d
=
xif
and
species.
tion
intensities
(s) +
~ xii i i=l
incoherent
In this
function
is a b s o r b e d constant
details
the m e t h o d
the
Ic(S)
~s
about
comparison
Habenschuss-Spedding short
distances
ction
c.f.
fitted
and
of 13a-
this
by
least
method
(3)
fi(s)
the
second
and
of
(3). For
functions identical
the
) obtained
The further
.
provide
( Fig.
IinC(s)i
discrimina-
~ = ( A + { B k )-I.
function
term
(3)
of the v a r i -
the m o n o c h r o m a t o r
gives
function
~ Bkexp( k=l
amplitudes
[13a-c]
methods
2, p o i n t s
In
correlation
in the G(r)
the si(s)
( Fig.
into
is g i v e n
of the
two n o r m a l i z a t i o n
analysis
Following
are
+
scattering
formulation
normalization
The
persists
the m e t h o d
and S p e d d i n g
u s e d here.
A , B k , C k and D k are p a r a m e t e r s .
are c o h e r e n t ous
was
error
curve
i 1 where
some
Therefore,
by H a b e n s c h u s s
[14] used,
to a s m o o t h
that
in the G(r).
proposed
and p r e v i o u s l y
procedure
it is p o s s i b l e
peaks
lower
shows
spurious
and so in the
l, p o i n t s with
that
results.
The
peaks
at
following
) and G(r)
this m e t h o d
have
funbeen
used. The p r o c e d u r e
based
on the
removal
present
in the G(r)
function
at small
fective
if a r a t h e r
extended
range
this
end
and so i n t r a m o l e c u l a r
in the p r e s e n t peak
at about
tributions tation
case
the O-H p e a k
1.50-1.55
are o b v i o u s
of the results.
for N - 0 solutions
( in n i t r a t e
A
) were
and not The
peaks
at a b o u t also
very
ef-
can be u s e d
appearing
at
to
low r (
1.0 A and the P-0
removed
important
) [15]
and for P-O
peaks
of r is m o r e
of d i s t a n c e s
same p r o c e d u r e
solutions
) [3c,4c,16]
[ 5 ] distances.
real
of u n p h y s i c a l
values
was
since
these
for the used
, for S-0
( in p h o s p h a t e
con-
interpre-
elsewhere
( in s u l p h a t e solutions
)
195
si
1.C
0.~
0.(
-02
-1.0 '
0
Fig.
~
'
i
'
4
i. E x p e r i m e n t a l
lution
(points)
(solid
line)
I
6
obtained
ANALYSIS
OF THE R E S U L T S
lue
at 2 . 1 A
is c o m p a r a b l e
solutions
[la-d] [17a-c]
scribed
to 0-O
-bonded
water
in the
i
si(s)
i
I
10
I
12
I
s,k I ,
14
I
16
for 1.5 M M g ( H 2 P O 4 ) 2 so-
the s y n t h e t i c
the best
,
fit
structure
function
( parameters'
values
functions
In the e x p e r i m e n t a l
structures
with
from
2 ).
centered
~}
structure
compared
in T a b l e
Correlation
i
cation
G(r)
( see
is a s c r i b a b l e
Fig.
with
the M g - O
distance
and
in a g r e a t
number
The
double
2 ) the
to the M g - O
peak
nearest
neighbours
molecules,
which
hydration
shells;
found
crystal aqueous
2.8 A is to be
interactions
are p r e s e n t
peak this va-
in the
of m a g n e s i u m
at about
further
first
distance;
both
between
hydrogen
in the b u l k
contributions
a-
and
to this
196
peak
come
from
interactions
te ion and a n i o n i c tributions inside
could
among
hydration
also
come
the p h o s p h a t e
oxygen
water
from
atoms
molecules
of the p h o s p h a [5,18a-c]
0-0 d i s t a n c e s
(about
; con2.56 A
)
ion. o
A large In the
composite
solution
peak
is v i s i b l e
are v i s i b l e
three
in the
components
range
3.3-4.5
at about
3.6,
A.
3.9
o
and 4.25 H20II
A ascribable
interactions,
essentially
to the Mg-P,
respectively.
In the
P-H20
solid
and Mg-
structures
4c
o
the
distance
the
aqueous
Mg-P
is b e t w e e n
solutions
3.4-3.5
previously
A;
the P - H 2 0
studied
5
was
distance found
in
in the
o
range the
3.75-3.91
second
range
A;
the
distance
coordination
4.1-4.25
shell
Mg-H20II
(water
) has b e e n
found
molecules [17a-c]
in
in the
A.
G(r)
1.0
I
1
Fig.
2.
2
I
3
Experimental
Mg(H2P04) 2 solution the s t r u c t u r e
I
I
4
5
correlation (points)
function
with
r,A
6
function
compared
obtained
I
with
I
7
G(r)
for 1.5 M
that
calculated
the p a r a m e t e r s
from
of Table
2.
197
Model For a q u a n t i t a t i v e analysis we tested a synthetic function w h i c h was refined by least squares, tal structure function.
against the experimen-
The c h a r a c t e r f s t i c s of the approach
used and the c o m p u t a t i o n p r o c e d u r e are the same as those employed in previous papers
~b,5,17c]
.
For calculating the i(s)
theoretical function we used the w e l l - k n o w n formula m n i(s) = i=l~ J=l~ixififj
m ( i=12 xifi
)-2 exp ( -1/2 o 21j s2 )x
m
x sin(srij)/srij
x exp ( -1/2
+ 4~@o
~9]
~ i=l
m
m
~ xixiflfj J=l
(
• xifi )-2 i=l
aoi j s 2 ) x ( S r o i j C O S ( S r o l J ) - s i n ( s r o i J ) )
x i/s 3
(4)
where m is the number of atoms in the stolchiometric unit, n i is the n u m b e r of atoms with discrete structure origin atom of the i type;
" seen " by an
rij is the mean radial distance of
the jth atom from an origin atom of the i type;
o ij is the
r o o t - m e a n - s q u a r e d e v i a t i o n for rij; roi j is the mean radius of the discrete structure of the J atoms around one of the i type; and Coi j is the r o o t - m e a n - s q u a r e deviation for roi j.
In eq.
(4) the first term derives from the discrete interactions, while the second is the c o n t r i b u t i o n deriving from the continuous d i s t r i b u t i o n of distances. The model used was based on the h y p o t h e s i s that first and second n e i g h b o u r w a t e r m o l e c u l e s around the cation have a discrete structure. noncorrelated.
The h y d r a t e d ions were considered spatially
The discrete structure of anions only extends
up to the first neighbours. A c c o r d i n g to these assumptions,
the model used has the
f o l l o w i n g features: i) M a g n e s i u m in octahedral g e o m e t r y was d e s c r i b e d by three independent parameters:
the distance rMg_w I and two root-mean
-square d e v i a t i o n s O M g _ w I
ando
Wl-W 1
198
2) For
the p h o s p h a t e
assumed, ters
with
the usual
tetrahedral
r0p_O P d i s t a n c e
and
interactions
M g - O 7, Mg-08, are
Only
three
arising
Mg-09
correlated
orientation
from
the oomplex,
was
parame-
between
octahedron
independent
and
tetrahedron
parameters
one m e a n - s q u a r e
deviations
for all
into
interactions
account.
groups
the d i s c r e t e
around
cations
Mg-w 2 interactions
independent
parameters:
root-mean-square
z,
interact-
deviation
the
(Mg-w2)
were
distance
aMg_w 2 and
were
described rMg_w
taby
, the
the c o o r d i n a t i o n
nMg_w 2 .
number
5) W l - W 2 i n t e r a c t i o n s shells
belonging
of the cation.
mean-square dent
to d e s c r i -
phosphate
the Mg-O6-P.
4) S e c o n d - o r d e r
three
is fixed.
are n e c e s s a r y
of b o n d e d
and
Mg-P,
(Wl)i=6_z-(0P03H2)z ( see Fig. 3), ^ to the M g - O 6 - P angle, once the r e c i p r o c a l
the n u m b e r
ions,
namely,
and
the complex:
ken
structure
the ~ 0 p _ 0 p
to be refined.
3) The
be
ion,
the
The
deviation
parameters,
a
while
to two s u b s e q u e n t
distance
hydration
r
and the rootWl-W 2 a s s u m e d to be i n d e p e n -
were Wl-W 2 the c o o r d i n a t i o n
number
n
is r e l a t e d Wl-W 2
to n M g _ w 2 by No
fixed
the
orientation
6) No g e o m e t r i c a l and
the
was
number
for w 2 m o l e c u l e s .
was made rip_w
as an i n d e p e n d e n t
and r o o t - m e a n - s q u a r e
nwl_w 2 = nMg_w2/(6-z)w I .
chosen
assumption
frequency
troduced ces
relationship
about
of P - w
parameter
deviations
anionic
hydration
interactions together
with
for 0 p - w
is indistan-
and P-w
inte-
ractions. 7) In a d d i t i o n nuum for
region loss
Only
four
to d i s c r e t e - s t r u c t u r e
interactions,
was
each
introduced
of p o s i z i o n a l distances
ir r o o t - m e a n - s q u a r e O-H20
and H 2 0 - H 2 0
rameters.
around
correlation
of the
start
deviations pairs
were
species
at h i g h e r
a contito a c c o u n t
distances.
of the c o n t i n u u m
for
the Mg-H20,
considered
and the-
P-H20,
as i n d e p e n d e n t
pa-
199
9
)6
Fig.
3.
The
phosphate unit
has
bridging angle
resulted
being the
plane
06, in
model
assumed
the h y d r a t e d
the
147
for
magnesium
the b o n d i n g ion.
containing
the
M g 2+
P atom
the
oxygen
and
The
ion,
of
the w l,
07 .
the
structural
The
the
Mg-0-P
degrees.
least
squares refinements were o_ 1 0.65-15.5 A , the f u n c t i o n
s intervall
U = ~ s
to
a mirror oxygen
The
s
geometrical
group
carried
out
using
the
max . mln
i(S)ob s _ i(S)calc
minimized
classical
Marquardt
by means Gauss-Newton
[20] .
This
of
)2
the
(5)
LSHS
program;
linearization
program
this
method
is a p e r s o n a l
is b a s e d
on
as m o d i f i e d
by
version
in F o r t r a n
200
IV, that allows the simultaneous fitting of the parameters with a calculation time lesser than the least-squares programs previously used. Results In Figs.
1 and 2, the structure functions and the corre-
lation functions obtained from the best fit are compared with the experimental data.
The final values of the most signifi-
cant p a r a m e t e r s are listed in Table 2. Table 2.
P a r a m e t e r values [r = distance
squares deviation viations
(A), o = root-mean-
° (A), n = frequency factor
(in parentheses)
]
and standard de-
obtained from least squares fitting
and used in the final c a l c u l a t i o n of the synthetic structure function;
z = the average number of phosphate bonded to magne^
slum. Mg-06-P angle in degrees. Cation
Anion
rMg_Wl = 2.11(1)
rOp_Op= 2.58(1)
OMg_Wl 0.126(8)
OOp_Op=0.05(1)
=
rwl_w 2 = 2.76(1) =
o Wl-W2
0.118(8)
rMg_w2 = 4.28(6) o
Mg-w 2
nMg_w 2
= 0.47(4) =
9.5(5)
rOp_ w = 2.878(8) o Op-W rp_ w o
P-w
np_ w
=
Complex z
=
1.0(i)
o = 0.189(5) Mg-O6-P
= 147(2)
0.135(7)
= 3.87(2) = 0.33(1)
= 8.8(4)
The consistency of the model with experimental data is supported by the very good agreement obtained and also by the low value of R = 0.15
R is an agreement factor expressed by
R = ( ~ (si(S)ob s - si(S)calc)2) ~ /( Z ( s i ( s ) o b s ) 2 )
~
(6)
commonly used in crystallography. Obviously the agreement between model and experimental
201
data
is n o t b y
rect.
The
necessary
condition
is i m p o s s i b l e only
itself
difficulty
for
the
respect
is to s p e c i f y
that
an u s e f u l o f this
basis
The function This
AND
experiment
shown
in line w i t h
te c o m p l e x in the
Coordination
lecules
procedure
or phosphate
[17a-o]
is c o n f i r m e d
bing
ions
phase.
selected
Moreover,
[3a-c,4a-c,~
it c o u l d
that p o i n t s
it
prove
that on the
be c o n s i d e r e d
correlation conctacts.
to c a t i o n - p h o s p h a -
o f the p a r a m e t e r s some
obtained
conclusions:
presence
) arranged
the p r e c i s i o n
of a second
solutions
shell
and
around
bonding
mo-
The v a l u e is
in s o l u t i o n the c a t i o n
among
o f the p a r a m e t e r s are
confirm
( from water
o f the m e t h o d ,
Jim-d]
shell
of hydrogen
The v a l u e s
hydration
atoms
octahedrally.
structures
coordination
in o t h e r
the c a t i o n
by six oxygen
in s o l i d
by a network
Cation-phosphate As
describing
molecules.
the s e c o n d
se f o u n d
suggest
Mg-w I within
found The
outer water
( see Fig.
in fact
of cation-phosphate
161
The v a l u e s
is s u r r o u n d e d
as
the p h o s p h a t e
of c a t i o n
o f the d i s t a n c e the same
for
o f the e x p e r i m e n t a l
the e x i s t e n c e literature
The p a r a m e t e r s that M g ( I I )
analysis
in d e t a i l .
o f the m o d e l ,
only
This
ones.
analysis
formation.
fitting
work
it
employed
CONCLUSIONS
qualitative has
studies
but
data.
structural
It w a s
in s o l i d
f o r the c h o i c e
single
valid,
o f the c a t i o n
ones.
the p r e v i o u s
one o f the m a n y p o s s i b l e DISCUSSION
if the
is c o r -
only a
" o f the m o d e l
orientation
possible
o f the s t r u c t u r e
to be
Judged
diffractometric
to the o c t a h e d r a l
on the g r o u n d
ground
to be
the m o d e l
of course,
in the p r e s e n t
selected
3 ) is one o f the m a n y
that
is,
" uniqueness
especially
the
two
the m o d e l s
discussed
For example,
proof
the
of our single
is s e r i o u s
the m o d e l s
anion with
between
to a s s e s s
on the g r o u n d
treats
a conclusive
consistency
in a g r e e m e n t
inner and descriwith
tho-
[l?a-c]
complex
f a r as r e g a r d i n g
the a v e r a g e
number
of phosphate
gro-
202
ups d i r e c t l y ments
bonded
gives
ment with
final values
those
ty constants centration
to the cations, of z about
calculated
[8]
range used
in the present
the m a g n e s i u m - O - P
is very
similar
stance
is,
angle
to that found
solid
[idl
is similar
lid c o m p o u n d
1 .
on the average,
given
analysis.
and c o n s e q u e n t l y
is agree-
to be valid
obtained
in the con-
As far as re-
in our solution,
also
fragment
determined
it
of
the cation-P
and solid structure.
of phosphate
refine-
for the stabili-
in c o r r e s p o n d i n g
in solution
the n u m b e r
This value
by the values
, if these are assumed
garding
MgHPO4-3H20
the least-squares
di-
In the so-
groups b o n d e d
toscation
by the s t o i c h i o m e t r y ~ f r ~ h e
substance. What
seems
to persist
( solid and liquid clusion phate
in the two different
) is the b u i l d i n g
is in line with
the findings
solutions[3a-c,4a-c]and
and also
in p h o s p h a t e
of a structural ctures
and c o m p l e x e s
[5~
between
itself.
in several
in nitrate
solutions
continuity
unit
This con-
cases
solutions
, in which fragments
in c o n c e t r a t e d
conditions
of sul-
[21a-b]
the existence
of solid
solution
stru-
has been confir-
med. Moreover, be consistent Phosphate
the a g g r e g a t i o n
with
~roups
and anionic
From the final value sible
to calculate
geometry
for the phosphate with
those
solutions
nic h y d r a t i o n
of the Op-0p distance of P-0 by assuming
group;
. Regarding
they are different
ned in the p r e v i o u s
the value
found in the crystal
[5]
study.
complexes
the p a r a m e t e r s respect
to the values
in the solution
tions
p H in our solution [22].
in which,
studied.
should have
It w o u l d be interesting on increasing
should be present.
and in
of the anio-
We think that the average
prevailing cies H2PO ~
it is pos-
1.58 A is in a-
around the anion obtained,
species
to
constants.
a tetrahedral
structures
of w a t e r m o l e c u l e s and 3.0,the
proved
from e q u i l i b r i u m
hydration
the value
greement aqueous
of these
the one o b t a i n e d
depends
obtainumber on the
Being w i t h i n
2.0
the p r e d o m i n a n t
spe-
to study other ~solu-
the pH, also the species P0~-
In such a way we may check
if, also in
203 _
aqueous number
solution
( pH 710),
of 12 as f o u n d
studies
may
in s o l i d
contribute
ral p r o b l e m .
We
the PO
to c l a r i f y
are w o r k i n g
ion has
structure this
in this
a coordination
~l~a-c]
aspect
Further
of the s t r u c t u -
direction.
ACKNOWLEDGMENTS This work ma della All
was partially
Sardegna
the c a l c u l a t i o n s
tronico,
supported
( Assessorato
Universit&
were
done
b y the R e g i o n e
della Pubblica at the C e n t r o
Autono-
Istruzione).
di C a l c o l o
Elet-
di C a g l i a r i .
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