J. Chem. Phys., Vol. 121, No. 18, 8 November 2004
Structural and electronic evolution of aqueous As(OH)3
8981
Kirkwood theory,63 by the dipole-dipole interaction term re-
sulting from the hydrogen bonding association. Several stud-
ies have been dedicated to experimental estimation of water
permittivity60–62,64 and spectroscopic observation of hydro-
gen bonding in water ͑see Ref. 65 and references therein͒ at
high temperature and pressure conditions. For example, the
permittivity value ⑀͑0͒, which is around 80 at ambient con-
ditions, is about 40 at 200 °C, and about 20 at 300 °C, at
pressures in the 100–500 bars range.64 In the RMN study of
Hoffmann and Conradi,65 the authors measure the variation
of the mean number of hydrogen bonds in subcritical and
supercritical water. At 250 bars they found that, in compari-
son with room temperature, there are about 70% ͑60% and
45%͒ of hydrogen bonds at 100 °C ͑200 and 300 °C, respec-
tively͒. Their results are in very good agreement with previ-
ous NMR and Raman measurements of hydrogen bonding.
Those experimental studies also reveal a really weak pres-
sure dependence at these low temperature/high density con-
ditions. Many theoretical studies tend to support the experi-
mental observations.66–70 Jedlovsky and Richardi compare
different water models’ viability to reproduce water proper-
ties from ambient to supercritical conditions.66 Concerning
the permittivity value at HP/HT conditions, these calcula-
tions reveal, at 300 °C, a strong decrease of ⑀͑0͒ to 1/4 the
ambient value. In Ref. 69, a geometrical and topological
study of the hydrogen-bonding structure, based on RMC cal-
culations, indicates a notable modification of its tetrahedral
arrangement from 150 °C upwards. It is thus evident that the
hydrogen bonded network of water and the corresponding
value of the permittivity rapidly evolve with increasing tem-
perature mostly in the 30–200 °C range.
of the atomic partial charges magnitude. The changes in the
solvent structure, such as the weakening of the hydrogen
bonded network concomitant with the decrease of the solvent
dielectric constant, are invoked to explain the structural and
electronic modifications in the As͑OH)3 cluster with increas-
ing temperature: the interactions between the As hydroxide
complexes and water molecules originating from hydrogen
bonding weaken, thus releasing the molecule from the hydro-
gen bonded network. This release enables the molecule to
open its structure to a more tetrahedrallike configuration con-
sistent with the sp3 hybridization of the As electronic orbit-
als. At the same time, the decrease of the bulk water permit-
tivity justifies the reduction of the partial atomic charges. All
these effects take place at both concentrations (0.3m and
0.05m) as soon as the temperature is increased, the major
changes occuring between 30 and 200 °C. This is in agree-
ment with several theoretical and experimental studies on
water showing a strong reduction of its dielectric properties
in this temperature range. The combination of EXAFS analy-
sis with XANES realistic simulations is demonstrated to be a
powerful tool to get precise information on both geometrical
and electronic ͑partial charges͒ structures of aqueous com-
plexes and on the solvent itself, in high temperature/high
pressure fluids. This HP/HT study would not have been pos-
sible without the development of an efficient experimental
setup that allows to obtain high-quality transmission and
fluorescence spectra.30
ACKNOWLEDGMENTS
The authors thank J.-C. Soetens for his strong help with
the various GAUSSIAN 98 calculations, and J.-M. Beny for the
Raman calculations of the normal modes frequencies.
In our study, the increase of the O-As-O angle and the
decrease of the atomic charges occur below 200 °C, and do
not depend on pressure. That is in accordance with the rapid
evolution of the solvent properties mentioned just above. For
temperatures above 200 °C, changes in the XANES spectra
become undetectable. This might imply that either the struc-
tural and electronic evolution of As͑OH)3 stops, or a further
evolution of both angles and charges go on but is undetect-
able within the resolution of the methods. No unequivocal
conclusion can be drawn at this point.
1 A. G. Kalinichev, Reviews in Mineralogy and Geochemistry ͑Mineralogi-
cal Society of America, Washington, D.C., 2001͒, Vol. 42, p. 83.
2 A. Filipponi, S. DePanfilis, C. Oliva, M. A. Ricci, P. D’Angelo, and D. T.
Bowron, Phys. Rev. Lett. 91, 165505 ͑2003͒.
3 V. Simonet, Y. Calzavara, J.-L. Hazemann, R. Argoud, O. Geaymond, and
D. Raoux, J. Chem. Phys. 117, 2771 ͑2002͒.
4 A. J. Anderson, S. Jayanetti, R. A. Mayanovic, W. A. Bassett, and I.-M.
Chou, Am. Mineral. 87, 262 ͑2002͒.
5 G. Ferlat, A. S. Miguel, J. F. Jal, J. C. Soetens, P. A. Bopp, I. Daniel, S.
Guillot, J. L. Hazemann, and R. Argoud, Phys. Rev. B 63, 134202 ͑2001͒.
6 J. L. Fulton, D. M. Pfund, S. L. Wallen, M. Newville, E. A. Stern, and Y.
Ma, J. Chem. Phys. 105, 2161 ͑1996͒.
V. CONCLUSION
7 J. L. Fulton, M. M. Hoffmann, and J. G. Darab, Chem. Phys. Lett. 330,
300 ͑2000͒.
The structure of the As͑OH)3 covalent molecule in aque-
ous solutions was determined by X-Ray absorption spectros-
copy from ambient to supercritical temperatures. Both
EXAFS analysis and XANES simulations were used to ob-
tain information on the evolution of the geometry of As en-
vironment ͑distances, angles͒ and its electronic configuration
͑atomic partial charges͒ with temperature and pressure. The
EXAFS analysis shows the constancy of the As-O distance,
which remains about 1.77 Å in 0.3m solutions in the whole
temperature range 30–500 °C at 250 and 600 bars, and about
1.75 Å in 0.05m solutions in the temperature range 30–
375 °C, at 250 bars. These new data confirm that the As-O
bonding has a strong covalent character, which keeps up un-
der the supercritical temperature conditions. New XANES
simulations reveal an enlargement of the O-As-O angles
when temperature increases, coupled with a small reduction
8 J. L. Fulton, M. M. Hoffmann, J. G. Darab, B. J. Palmer, and E. A. Stern,
J. Phys. Chem. A 104, 11651 ͑2000͒.
9 M. M. Hoffmann, J. G. Darab, S. M. Heald, C. L. Yonker, and J. L. Fulton,
Chem. Geol. 167, 89 ͑2000͒.
10 M. M. Hoffmann, J. G. Darab, B. J. Palmer, and J. L. Fulton, J. Phys.
Chem. 103, 8471 ͑1999͒.
11 R. A. Mayanovic, A. J. Anderson, W. A. Bassett, and I.-M. Chou, Chem.
Phys. Lett. 336, 212 ͑2001͒.
12 R. A. Mayanovic, A. J. Anderson, W. A. Bassett, and I.-M. Chou, J. Syn-
chrotron Radiat. 6, 195 ͑1999͒.
13 D. M. Pfund, J. G. Darab, J. L. Fulton, and Y. Ma, J. Phys. Chem. 98,
13102 ͑1994͒.
14 T. M. Seward, C. M. B. Henderson, J. M. Charnock, and B. R. Dobson,
Geochim. Cosmochim. Acta 60, 2273 ͑1996͒.
15 T. M. Seward, C. M. B. Henderson, J. M. Charnock, and T. Driesner,
Geochim. Cosmochim. Acta 63, 2409 ͑1999͒.
16 S. L. Wallen, B. J. Palmer, D. M. Pfund, and J. L. Fulton, J. Phys. Chem.
101, 9632 ͑1997͒.
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