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Journal of the Brazilian Chemical Society

Print version ISSN 0103-5053On-line version ISSN 1678-4790

J. Braz. Chem. Soc. vol.19 no.1 São Paulo  2008

http://dx.doi.org/10.1590/S0103-50532008000100015 

ARTICLE

 

Hydration properties of Al3+ ion using empirical ion-water potential by Monte Carlo simulation

 

 

Vania Elisabeth BarletteI, *; Luiz Carlos Gomide FreitasII; Paulo Henrique GuadagniniIII; Celso Aparecido BertranIV

ICentro Universitário Franciscano, Rua dos Andradas 1614, 97010-032 Santa Maria-RS, Brazil
IIDepartamento de Química, Universidade Federal de São Carlos, CP 676, 13565-905 São Carlos-SP, Brazil
IIIUniversidade Estadual do Rio Grande do Sul, Rua Gal. João Manoel 50, 90010-030 Porto Alegre-RS, Brazil
IVInstituto de Química, Universidade Estadual de Campinas, CP 6154, 13083-970 Campinas-SP, Brazil

 

 


ABSTRACT

In this work, hydration properties of Al3+ ion are investigated by statistical mechanics Monte Carlo simulations in the NpT ensemble at 298.15 K and 1 atm using an effective ion-water potential model whose parameters were developed through empirical search in configurational energy space during the course of simulations to fitting structural experimental data of the first hydration shell. Computed structural results for coordination numbers and ion-water oxygen distances for both first and second coordination shells are obtained in very good agreement with experimental observations. The hydration enthalpy predicted from this simple model is also in very good agreement with experimental values and it is quite similar to the one obtained by Wasserman et al. from the hydrated ion model. Many-body contributions investigated for an [Al(H2O)6]3+ cluster using the density functional theory in ab initio quantum mechanical calculations provide support to the effectiveness of the ion-water pair potential developed concerning many-body effects of water molecules around the ion incorporated in the fitted parameters.

Keywords: aluminum ion hydration, ion-water interaction, aluminum aqueous solution, empirical potential, Monte Carlo simulation


RESUMO

Neste trabalho, propriedades de hidratação do íon Al3+ são investigadas por simulações mecânico-estatísticas de Monte Carlo no ensemble NpT a 298,15 K e 1 atm usando um modelo de potencial efetivo de pares íon-água cujos parâmetros foram desenvolvidos por meio de busca empírica no espaço de fase configuracional durante o curso das simulações para reproduzir dados experimentais da estrutura da primeira camada de hidratação. Resultados estruturais obtidos a partir das simulações para números de coordenação e distâncias íon-oxigênio da água, correspondentes às camadas de hidratação primeira e segunda, estão em muito bom acordo com dados experimentais. A entalpia de hidratação predita a partir deste modelo também está em muito bom acordo com resultados experimentais e é bastante similar ao resultado obtido por Wasserman et al. a partir do modelo de íon hidratado. Contribuições de muitos corpos investigadas para um cluster [Al(H2O)6]3+ usando a teoria do funcional de densidade em cálculos mecânico-quânticos de primeiros princípios fornecem suporte à efetividade do potencial de pares íon-água desenvolvido quanto aos efeitos de muitos corpos incorporado nos parâmetros ajustados.


 

 

Introduction

Trivalent aluminum ion in aqueous media has mainly been studied due for its effects on living systems and to for its technological applications. In the last decades, many studies have demonstrated that Al3+ is toxic in plants, animals and humans, causing a negative impact on the environment.1-3 Concerning technological interests, there are some indications that the competition between typical Al3+ ligands, such as acetyl acetonates, urea, carboxylic acids and water molecules, by the coordination of the Al3+ in the hydration shells could be related to the control of the [Al(H2O)6]3+ hydrolysis rate, which could have a decisive influence to the improvement of interesting properties of advanced materials.4-6 The knowledge on the nature of the interactions of hydrated metal ions is one of the most fundamental interests in physical chemistry of inorganic solutions.

Experimental data of aqueous ionic solutions7,8 produced in the last decades have improved our knowledge on aqueous chemistry of the Al3+. At theoretical level, molecular simulations are powerful tools which have contributed with insights on the properties of aqueous ionic solutions. This methodology is based on a microscopic description of the system in which potential energy surfaces play a central role. For highly charged ions in water, such as Al3+, pairwise additive potential functions have been employed as approximations to total potential energy functions, aiming low cost simulations. Within this scope, different potential models have been extracted either from ab initio quantum mechanics or empirical procedures with varying degrees of success.

Potential models have been investigated from ab initio quantum mechanical calculations using the hydrated ion concept in molecular dynamics studies by Sánchez Marcos and co-workers9-11 for Cr3+, Be2+, Mg2+ and Al3+, by Bleuzen et al.12 for Cr3+, and by Wasserman et al.13 for Al3+. The potential models proposed by these authors, in different ways, allow some flexibility to water molecules of the first coordination shell. In these models, however, water molecules of the first shell can not be exchanged with ones of the second shell. Ortega-Blake and Bernal-Uruchurtu,14 using pairwise additive potentials which permit water release from the first shell, as well as polarization of water molecules, have performed Monte Carlo simulations of the hydration of Ca2+ and Mg2+. All of these pair potentials, with varying degrees of accuracy and extent in accounting for many-body effects, have been produced improvement in the description of aqueous ionic solutions.

As many-body effects of molecules are not pairwise additive, their inclusion to construct pair potentials has also been done, but in an effective way, by using empirical procedures.15 Empirical ion-water potentials were successfully parameterized by Curtiss et al.16 for Fe2+ and Fe3+ in water using molecular dynamics, and by Åqvist17 in his studies using free energy simulations for Mg2+, Ca2+, Sr2+, Ba2+, Li+, Na+, K+, Rb+ and Cs+ in water.

Empirical procedures take effectively into account the non additivity of many-body effects in pairwise potential functions, leading to most accurate results.18 This is achieved by considering solvent molecules of the solvation shells, as well as ones of the bulk, during the parameterization process. However, the main limitation of this approach is that it fails in generality, which implies in unknown starting parameters at each new system.18 Nevertheless, parameters such as electronegativity, atomic radius and hardness of the ions can be used for giving insights into empirical parameterization process.

In this work, a statistical mechanics Monte Carlo study of the hydration of the Al3+ ion is presented using an ion-water potential empirically parameterized to effectively account many-body effects in the fitted parameters using a search procedure in configurational energy space through Monte Carlo simulations of one Al3+ ion in water. The effectiveness of the ion-water potential developed in this work is discussed by evaluating the magnitude of interaction energies of two-, three-, four- and higher-body for an [Al(H2O)6]3+ cluster by means of ab initio quantum mechanical calculations using density functional theory. Concerning many-body contributions, the literature reports ab initio self-consistent field studies for [Al(H2O)6]3+ clusters performed by Probst19 for Na+, Mg2+ and Al3+, by Curtiss and Jurgens20 for Cu+ and Cu2+, and by Hermansson and co-workers21 which demonstrated that non-additive effects in hydrated clusters are much more important with increasing charge of the ion. Furthermore, it can be emphasized that there are many representative examples in which some dynamics aspects of interest between molecules of the coordination shells and ones of the bulk must be taken into account, such as in sol-gel process in materials research.4-6 Considering that an important feature of the present Al3+ ion-water interaction model is the flexibility which it allows to the water molecules of the first shell to exchange with the second shell, it is not of our knowledge that a simple Al3+ ion-water potential model including this feature has previously been studied.

 

Methodology

Ion-water and water-water potential functions

In an ionic hydration process within the pairwise additivity approximation at infinite dilution, the configurational energy can be partitioned into additive contributions of pairs of water-water and ion-water interactions. The functional form employed in this work for the ion-water interaction energy was applied in previous works for highly charged metal ions in aqueous solution,16,22,23 and it is composed by Coulomb plus short range terms,

In equation 1, summation is on sites j of a water molecule containing w sites, rIj is the distance between the ion I and the site j, and qj is the partial charge of the site j of the water molecule. For the present case, qI = +3|e|. To represent the water-water interaction, the TIP4P model developed by Jorgensen et al.15 was employed. Then, in this work, the short range part of equation 1 only concerns the oxygen site of the water molecule, in agreement with the TIP4P water model statement. The experimental geometry of water was used.24 The A, B, D, E and F parameters were fitted by empirical procedure as follows.

Parameter search through Monte Carlo simulation

To find an acceptable set of potential parameters to be used in simulation, a representative region of the configurational energy space for the particular system must be reached. To start the present optimization process, the input values used for the potential parameters were those empirically developed by Curtiss et al.16 for the Fe3+ in water. In order to perform preliminary investigations, these parameters were applied in equation 1 with distances in angstroms and partial charges in units of electron. The TIP4P water model15 and the experimental geometry for water24 were considered in these calculations. The Fe3+ ion-water curve obtained for interaction between the Fe3+ and one TIP4P water molecule is shown in Figure 1. A minimum energy value of -80.23 kcal mol-1 at 1.90 Å was found for the distance between the Fe3+ and the oxygen site of the water. Since the ionic radius25 of the hexacoordenated Al3+ (0.675 Å) is smaller than the one25 of the Fe3+ (0.785 Å), it is expected that the parameter B in equation 1 for the Al3+ be greater than the one for the Fe3+ (B(Fe3+) = 3.728 Å-1). Additional considerations on hardness also distinguish these ions26 (13.1 eV for the Fe3+ and 45.8 eV for the Al3+). To start the parameterization process, these tendencies were considered as well as the potential parameters for Fe3+ and the minimum energy value obtained for Fe3+ ion-water curve (Figure 1). Fe2+ ion-water curve is also plotted in Figure 1 using parameters developed by Curtiss et al.16

 

 

Simulations were run in the NpT ensemble at 298.15 K and 1 atm, using the algorithm of Metropolis et al.,27 in a modified version of the Diadorim program.28 Periodic boundary conditions and spherical cut-off radius were used. From a previously equilibrated pure water box containing a small system of 390 TIP4P water molecules plus one ion in a cubic cell, initial configurations were obtained in which the ion was placed near to the center of the box. From the spatial positions, the Metropolis criterion was applied to accepting new positions, as well as new volume moves, with an acceptance/trial ratio about 0.45. A water molecule changed its position by randomly rotating and translating it as a whole along a randomly chosen Cartesian direction, according to increments in the range ±15° and ±0.15 Å, respectively. Attempts to move the volume were made at each 103 configurations. Increments of volume were allowed in the range ±120 Å3. The ion was also allowed to move. Attempts to translate the ion were made at each 103 configurations and the allowed translation range was ±0.05 Å. In order to accelerate the convergence, the probability of attempting to move a water molecule around the ion was enhanced by the preferential sampling29 1/(rIO2 + c), where rIO is the distance from the ion to the oxygen site of a water molecule, and c is an empirical constant chosen in this work as 40 Å. The side length of the equilibrated simulation box containing the ion was 22.504 Å, which corresponds to a volume containing a solution of 0.146 mol dm-3.

To calculate the configurational energies, a full water-water interaction was considered whenever any site-to-site distance fell below spherical cut-off radius of 10 Å. Correspondly, the same value of spherical cut-off radius was used for the ion-water interaction specified by Equation 1, according to the procedure discussed above for any site-to-site distance rIj. Beyond the cut-off radius, energy corrections for non Coulomb terms due to the long range forces were done using the formalism discussed by Allen and Tildesley.30 For Coulomb terms, the same formalism was used to correct long range effects considering a scheme to calculate ion-water average energies beyond the spherical cut-off radius as a function of distance between ion and water. At every distance, 2×104 Monte Carlo steps were made considering movements for water molecule so that its orientation relative to the ion is changed by randomly rotating it as a whole along a randomly chosen Cartesian direction in the range -180° to +180°, until convergence in energy is achieved.

During the simulations, the A, B, D, E and F parameters were obtained by fitting experimental data for both hydration number and ion-water oxygen distance of the first hydration shell.7,8 The potential parameters obtained in the present process are listed in Table 1. Average properties were accomplished by generating 0.8×107 configurations. Periods of 0.4×107 configurations were discarded for equilibrium phase. Statistical uncertainties were calculated from separated averages over blocks of 0.4×106 configurations.

 

 

Many-body contributions to the total energy for an [Al(H2O)6]3+ cluster

The total energy of an aluminum trivalent ion I and n water molecules (w) can be expanded in a series of m-body energy terms,20

where Al3+ and water molecules are taken as particles of the interacting system composed by m = n + 1 particles, E([Al(H2O)n]3+) is the total energy of the system, E(1) are the energy terms of individual particles, E(2) are the two-body energy terms, E(3) are the three body energy terms, and so on. In equation 2, E([Al(H2O)n]3+) - E(1)(I)-E(1)(wi) is the binding energy BE([Al(H2O)n]3+).

In this work, the many-body contributions to the total energy for a cluster with one aluminum trivalent ion and six water molecules, ([Al(H2O)6]3+), were evaluated. To calculate each one of the terms of equation 2, the density functional theory (DFT) at the B3LYP/CC-pVTZ level31,32 was applied. All of the computational calculations were performed by using the GAUSSIAN 98 series of programs.33 The total energy E([Al(H2O)6]3+) was obtained from geometry optimization and frequency analysis at the Th symmetry. The frequency analysis shows the optimized geometry is a local minimum on the potential energy surface. Single point energy calculations were accomplished to calculate E(1), E(2), E(3), ... , E(7) terms at the optimized geometry of the [Al(H2O)6]3+ cluster.

To calculate energy terms in equation 2 for the [Al(H2O)6]3+ cluster at the Th symmetry, the summation E(1)(wi) reduces to 6 equivalent energy terms for one water molecule at the geometry of the cluster. For the summation E(2)(wiwj), there are 15 two-body interaction terms due to combinations of two water molecules which can be arranged in six spatial positions (C(6,2)) at the geometry of the cluster. In this combination, it were found 12 two-body terms in which the angle between water molecules is 90°, and 3 two-body terms in which this angle is 180°. Then,

where E90°(ww) and E180°(ww) are total energies for water dimers at 90° and 180°, respectively, at the optimized geometry of the [Al(H2O)6]3+ cluster. Subscripts for water molecules were omitted on the right-hand side of equation 3.

For the summation E(3)(wiwjwk) in equation 2, there are 20 three-body interaction terms (as a result of a C(6,3) combination) for the which 12 triplets correspond to water molecules at a same plane, Es(3)(www), and 8 triplets for the which waters do not, Ed(3)(www). Then,

where Es(www) are the total energies for water triplets in which the water molecules are at a same plane, and Ed(www) are the total energies for water triplets in which the water molecules are not in a same plane. All of these calculations were performed at the optimized geometry of the [Al(H2O)6]3+ cluster. Subscripts were omitted on the right-hand side of equation 4.

For the summation E(3)(Iwiwj) in equation 2, there are 15 energy terms (as a result of a C(6,2) combination) for the which 12 terms correspond to dimers of water molecules whose angle between them is 90° and 3 dimers for the which the angle is 180°. Then,

where E90°(Iww) and E180°(Iww) are the total energies for clusters composed by the ion and two water molecules whose water-ion-water angle is 90° and 180°, respectively, at the optimized geometry of the [Al(H2O)6]3+ cluster. In equation 5, E(2)(Iw) = E(Iw) - E(1)(I) - E(1)(w), where E(Iw) is the total energy of the ion and one water molecule at the optimized geometry of the [Al(H2O)6]3+ cluster.

For the summations in equation 2 including E(4), E(5), E(6) and E(7) terms, the calculations were performed following a similar procedure.

 

Results and Discussion

For a qualitative comparison, Figure 1 shows the Al3+ ion-water curve obtained for the interaction between the Al3+ and only one TIP4P water molecule when empirical parameters in Table 1 were applied in equation 1, as well as the ion water curves for the Fe3+ and Fe2+ ions using the corresponding parameters for these ions developed by Curtiss et al.16 It is clearly seen from this Figure that the expected behavior concerning size and hardness of the ions is reproduced, because (i) the ion-water minimum region is slightly shifted to smaller rIO values for the Al3+ (1.85 Å) in comparison with the Fe3+ (1.90 Å) and Fe2+ (1.97 Å) ions, (ii) in going from the ion-water minimum region to shortest distances, the ion-water energy values increase more quickly for the Al3+ than for the Fe3+ and Fe2+ ions, and (iii) the ion-water minimum region is deeper for the Al3+ (-109.66 kcal mol-1) than for the Fe3+ (-80.23 kcal mol-1) and Fe2+ (-48.55 kcal mol-1) ions. In what follows, results for structure and energetic refer to average properties from simulations.

The Al3+-O and Al3+-H radial distribution functions (rdf’s) and the corresponding Al3+-O and Al3+-H coordination numbers are presented in Figures 2 and 3, respectively. In Figure 2, a well defined peak for the Al3+-O rdf indicates strong interaction between the water molecules of the first coordination shell and the ion. The Al3+-O rdf goes to zero for distances between about of 2.15 Å to 3.14 Å, and a similar pattern is found for the Al3+-H rdf which goes to zero between 2.92 Å to 3.47 Å. Concerning the Al3+-O rdf in Figure 2, the first maximum centered at 1.92 Å identifies the contact average distance between the ion and the oxygen site of a water molecule in the first coordination shell. This result, defined as rIO(1), is presented in Table 2 along with the X-ray estimates of 1.87-1.90 Å for this distance.8 The running integration number calculated for the first peak of the Al3+-O rdf up to the first minimum at 2.15 Å is 6, identifying the average number of water molecules in the first coordination shell (defined as nIO(1) in Table 2). The hexacoordination of the Al3+ in water has been determined by measurements of hydration numbers from NMR spectroscopy8 and it is predicted by nIO(1) in the present ion-water model. This result is also supported by the running integration number calculated for the first peak of the Al3+-H rdf centered at 2.59 Å up to the first minimum at 2.92 Å, yielding an average number of 12 hydrogen sites in the first shell defined as nIH(1) in Table 2. These results can be seen by the Al3+-O and Al3+-H coordination numbers shown in Figure 3. Also, X-ray diffraction measurements have indicated a second hydration shell of 12-14 water molecules around the [Al(H2O)6]3+ specie.7,8 In this work, the running integration number calculated for the second peak of the Al3+ - O rdf up to the second minimum at 4.35 Å yields an average number of about 12 water molecules in the second coordination shell (defined as nIO(2) in Table 2), in favor of the lower X-ray experimental value. An average result of 14 water molecules was found by Sánchez Marcos and co-workers11 using the hydrated ion model.

 

 

 

 

 

 

Figure 4 refers to average configurational energies obtained from simulations considering the Al3+ ion-water and water-water interactions as a function of the distance of the ion to the oxygen site of the water molecules. It is clearly noted from this Figure that the average water-water interaction is repulsive in the first coordination shell, while the ion-water interaction is attractive until long distances due to major action of Coulomb forces. The ion-water minimum energy was calculated in -112.54 kcal mol-1 at average distance of 1.92 Å. Since average water-water interaction is repulsive in the first hydration shell, it is not surprising that this average distance is greater than the distance of 1.85 Å calculated for one ion and only one water molecule (Figure 1). The discontinuity in energy that appears for both Al3+ ion-water and water-water interactions from about 2.15 Å to 3 Å clearly distinguishes the first hydration shell from the second one, as indicated by the absence of water molecules in this region (Figure 2). After about 3 Å, a continuum in energy appears. It can be added that the ion and its first shell resemble an unity moving through the solution, in accord with hydrated ion concept. The repulsive water-water interaction energy in Figure 4 is less intense in the second coordination shell and operates until about 4 Å. A similar pattern is found for a divalent ion, such as Fe2+, as shown in this Figure (ion-water minimum energy of -48.546 kcal mol-1 at 1.97 Å).

 

 

Dependence of system size on energy results was assessed performing simulations with increasing number of water molecules. Then, two additional pure water systems containing 780 and 1560 TIP4P water molecules were constructed using cubic boxes. Two other systems containing 780 and 1560 TIP4P water molecules plus one Al3+ ion each one, were also constructed using cubic boxes and the simulation protocol discussed above. The corresponding side lengths of 28.296 Å and 35.824 Å, or 0.073 mol dm-3 and 0.036 mol dm-3 Al3+ solutions, respectively, were reached in the average period. Cut-off radii of 14 Å and 17.5 Å were used for these systems, respectively, as well as for those composed by pure water, to calculate ion-water and water-water energies. Table 3 presents results for average water-water potential energies per water molecule for both pure water and Al3+ in water systems. In this Table is included the potential energy value of -9.92 kcal mol-1 for liquid water estimated from experimental enthalpy of vaporization.34 Concerning the computed results for pure water presented in Table 3, it is observed that when the number of water molecules increases, the average water-water potential energy shows most accordance with the corresponding experimental estimative. The same pattern is found for the average water-water potential energies in the Al3+ in water systems, close to the experimental estimative for pure liquid water (-9.92 kcal mol-1) as the number of water molecules increases, which is expected for a solution approaching infinite dilution.

 

 

The hydration energy was also estimated for the systems containing 390, 780 and 1560 TIP4P water molecules plus one Al3+ ion each one. In these studies, the hydration energy (defined as DEhyd in Table 4) was calculated by EIw + Eww - , in which EIw and Eww are average configurational energies corresponding to ion-water and water-water contributions, respectively, and is the average configurational energy for pure water systems. Results obtained for these quantities are presented in Table 4. As showed in this Table, the calculated Eww and energy terms are very large values. The solvation relaxation energy, calculated as the difference between these values, Eww - , is shown in Figure 5 as function of Monte Carlo steps for N = 390, 780 and 1560 water molecules. This term shows large fluctuations depending on the Monte Carlo steps performed in the simulation until about 0.8×107 steps. After this quantity of steps, the convergence appears. The effect of the solvent relaxation term even far way from the ion can be observed inspecting the average results in Table 4 as a function of the system size. For the small system, N = 390, the calculated relaxation energy value (420 ± 4 kcal mol-1) is larger than the ones for the other two systems (375 ± 8 kcal mol-1 for N =780, and 372 ± 11 kcal mol-1 for N = 1560) indicating an insufficient number of water molecules in the small system to reproduce properly the hydration energy.

 

 

 

 

In Table 4, the EIw values were corrected for Coulomb contributions beyond the cut-off radii of 10 Å, 14 Å and 17.5 Å by, respectively, -18.45 ± 0.02 kcal mol-1, -9.64 ± 0.02 kcal mol-1 and -4.95 ± 0.02 kcal mol-1. Since the p DV terms were found negligible (-0.012 kcal mol-1 for 1560 water molecules), the hydration enthalpy (defined as DHhyd in Table 4) estimated by DEhyd + p DV was calculated to be -1107 ± 12 kcal mol-1 for the larger system. This result are in good agreement with experimental values of hydration enthalpy7,35 of -1115 kcal mol-1 and -1120 kcal mol-1. The hydration enthalpy calculated from the present ion-water model is also quite similar to the one obtained by the hydrated ion model, -1106 ± 6 kcal mol-1, by Wasserman et al.13 in a molecular dynamics study.

The good agreement between all structural and energetic results obtained in this work and the experimental observation is not surprising. They were derived from an effective ion-water potential model whose parameterization was performed taking into account not only water molecules of the first and the second hydration shells of the ion but also by considering water molecules of the bulk in spite of using a pair potential analytical function to modeling the interaction between ion and water. One emphasizes at this point the role of the water molecules of the bulk to obtain good results for hydration enthalpy, as revealed by our results showed in Table 4.

Another point to stress is that the effective ion-water potential model empirically fitted in this work differs from the fitting procedure used by the Rustad and Hay 36 and the Bakker et al.21 Rustad and Hay have obtained potential parameters from an ab initio procedure considering potential energy surface of one Fe3+ ion with a single water molecule to construct an ion-water pair potential. Bakker et al.21 have developed an ion-water pair potential and an water-ion-water three body potential by fitting ab initio interaction energies extracted from potential energy surfaces of two- and three-body, respectively. As discussed above, a different approach was used in this work for which contributions beyond three-body was effectively incorporated in the fitted potential parameters.

To support the afficacy concerning many-body effects of the ion-water potential developed in this work, many-body contributions were calculated for the [Al(H2O)6]3+ cluster using the density functional theory at the B3LYP/CC-pVTZ level. The geometrical parameters for the optimized structure at Th symmetry were found to be 1.935 Å for Al-O distance, 0.974 Å for the O-H distance, and 107.1 Å for the HOH angle. Table 6 shows the results for binding energy and many-body interaction energies for the [Al(H2O)6]3+ cluster calculated from the total energies for ion, water, water clusters, and ion and water clusters at the optimized geometry of the [Al(H2O)6]3+ cluster showed in Table 5. From Table 6, the interaction energies of tree-, four-, five-, six-, and seven-body for the cluster appear with alternating signs with the series converging very slowly, indicating that all these terms are important to reproduce the binding energy (BE) of the cluster. As an example, the summation over E(6) for water molecules resulting in -321.8 kcal mol-1 shows a large attractive value which can not be neglected to estimate the BE of the cluster. The summation over tree-body interaction terms, E(3), for example, are repulsive. It can be explained by the large value of the ion charge which polarizes the H-O bond in water molecules, increasing repulsive forces between water molecules. Adding one water molecule to the tree-body terms, at the geometry of the cluster, one found an attractive value as a result of the summation over interaction terms E(4), indicating a cooperative effect between water molecules. The summation over all these interactions from E(2) up to E(7) give the binding energy of -723.5 kcal mol-1 for the [Al(H2O)6]3+ cluster. Following an ab initio procedure in which the ion-water pair potential is extracted from a potential energy surface of one Al3+ ion with a single water molecule, it would expected an ion-water potential energy per water molecule of about -200 kcal mol-1, or 1/6E(2)(Iwi), as showed in Table 6, which is a very different result from that obtained by our empirical result of about -110 kcal mol-1 (Figure 4) for Al3+ ion-water interaction. In Figure 4, the average geometry of the Al3+-water pairs is not frozen with the minimum at rIO distance of 1.92 Å. The ab initio optimized distance rIO was found to be 1.935 Å at the structure of the [Al(H2O)6]3+ cluster with Th symmetry group. As the two values are quite similar, one can compare the interaction energies shown in Table 6 with the average configurational energy from simulation in Figure 4. The ab initio two-body interaction energy for ion-water, E(2)(Iwi) per water molecule of -200 kcal mol-1 presents an artificial stabilization which, in part, is due to the neglect of the three-, four- and higher order interaction energy terms.

 

 

 

 

Conclusions

In this work, a Monte Carlo study of the Al3+ ion hydration was performed using an empirical ion-water potential. Calculated results for coordination numbers and ion-water oxygen distances for the first and the second coordination shells of the Al3+ in water were found in very good agreement with experimentally derived X-ray and NMR measurements, although only the experimental results of structure of the first shell (coordination number and the ion-water oxygen distance) were fitted during the empirical optimization process. Furthermore, by using a large enough number of water molecules in the simulation box, the calculated hydration enthalpy was found in good agreement compared to experimental and theoretical results, without any additional optimization upon the potential parameters. These findings can be attributed in part by considering the molecules of the coordination shells and the ones of the bulk in the empirical optimization process, in which the many-body effects of water molecules around the Al3+ could effectively be incorporated in the fitted parameters. These conclusions are supported by ab initio quantum mechanical results for the magnitude of two- and higher-body interaction energy terms to the total energy for an [Al(H2O)6]3+ cluster which suggest that higher-body contributions are a significant part to be considered in constructing potentials for the Al3+ ion.

 

Acknowledgments

Partial financial support came from Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) and Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq), Brazil. The authors are grateful to reviewers for their useful comments and suggestions.

 

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Received: June 1, 2007
Published on the web: January 28, 2008
FAPESP helped in meeting the publication costs of this article.

 

 

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