Chemical Physics 276 (2002) 45±68 www.elsevier.com/locate/chemphys Water adsorption and hydrolysis in the Si2O4, P2O5 and P4O10 systems ± essential roles of the phosphate system in biosynthesis J.R. Tobias Johnson a,*, Itai Panas b b a Department of Chemistry, Inorganic Chemistry, Goteborg University, S-412 96 Goteborg, Sweden Department of Inorganic Environmental Chemistry, Chalmers University of Technology, S-412 96 Goteborg, Sweden Received 9 July 2001; in ®nal form 24 October 2001 Abstract Successive water addition to the mononuclear species SiO2 g and PO2 OH g, as well as the corresponding binuclear Si2 O4 g and P2 O5 g molecules, is studied by means of density functional theory. Hydrolysis of HO3 SiOSi OH3 g is found to be slightly endothermic, and only an asymmetric energy minimum is found for this silicic acid dimer. Four stable conformations are determined for the pyrophosphoric acid system HO2 OPOPO OH2 g. Depending on the choice of reference structure and basis set, the hydrolysis energetics ranges from 14±26 kJ/mol exothermic to 3±7 kJ/mol endothermic. In general, the hydrolysis reaction is best described as a near zero-energy process. Signi®cant dierences in the water chemistry of the ®nal monomeric products, Si OH4 g and PO OH3 g, appear in the ®rst solvation shell. Connecting the P±OH and P@O groups by water bridges results in a greater tendency for proton delocalization in PO OH3 g, than is observed when water is used to connect two Si±OH groups in Si OH4 g. Taking the properties of pyrophosphoric acid as model for the P±O±P bridge in adenosine triphosphate (ATP), the results of the present study support the notion that this molecule and its hydrolysis products provide a nano-scale buer, which is essential for sustaining biosynthesis by controlling the proton and water activities. Ó 2002 Elsevier Science B.V. All rights reserved. 1. Introduction Silicon dioxide (SiO2 (s), silica) and phosphorus pentoxide (P2 O5 (s)) display intricate and important chemical behaviors with water. A common denominator for both groups comprises the hy- * Corresponding author. E-mail address: [email protected] (J.R.T. Johnson). drolyzed species, silicates and phosphates, of which particularly the former belongs to the most important and complex among all commercial bulk chemicals. Silica alone is known to have as many as 22 dierent phases [1], a majority of which base their structures on a SiO4 tetrahedron building block. Still, there exists also a six-coordinated high-pressure phase of SiO2 (coesite). The origin of the multitude of phases is found in the varied arrangements and connectivities of the silica tetrahedra in the bulk. Many silicates contain chains or 0301-0104/02/$ - see front matter Ó 2002 Elsevier Science B.V. All rights reserved. PII: S 0 3 0 1 - 0 1 0 4 ( 0 1 ) 0 0 5 5 1 - 1 46 J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 sheets of such tetrahedra, which are interconnected through Si±O±Si bridges. The industrially most used form of phosphorous is orthophosphoric acid, OP OH3 or equivalently H3 PO4 . One desired quality of this acid comprises its capacity to buer solutions at very dierent pH values (from strongly alkaline to acidic) [1]. Another important reason for the great applicability of phosphates originates from their role in biochemistry, e.g., in teeth and bones, as well as in the essential molecules adenosine triphosphate (ATP) and DNA. Thus many fertilizers and nutrients have phosphates as main components. Their chemical role in the cell is to participate in hydrolysis and condensation reactions. One crucial feature of the biochemical molecule ATP is associated with the release of a formal energy equivalent when P±O±P or P±O±C bridges are hydrolyzed. This ``energy release'' has been argued to drive biosynthesis. In its most naive form, the exothermicity of one chemical process is suggested to drive a second reaction in the wanted direction [2]. This scenario must be deemed exceedingly complicated, as it involves exact and quantitative intermolecular energy transfer. Here, support is presented for the signi®cantly simpler understanding of the biophosphate system constituting a ``micro-buer'', which controls the detailed thermodynamic conditions, i.e., the proton and water activities, in the immediate vicinity of the reaction site, thus determining the conditions for biosynthesis. Acknowledging the similarities in the water chemistry of the phosphates and silicates, it becomes interesting to learn of detailed similarities and dierences in their water chemistry by employing quantum chemical techniques. A comprehensive understanding of similarities and in the water chemistry among the oxides of the 3p, 4p and 3d elements is sought. Thus, the present study is bracketed by two parallel investigations on the water chemistry of the 3p oxides. The ®rst study concentrated on the binuclear hydroxides or a hydrated complexes of the AlO(OH) and Al2 O3 systems [3]. The second investigation is on the water chemistry of the highly covalent SO2 OH2 , ClO3 OH and ArO4 systems and the dehydrated binuclear species of the former two [4]. The principles for the present investigation were outlined in two previous works on the water chemistry of some transition metal oxides [5,6]. Two types of reactions are considered. The ®rst type comprises water addition to mononuclear species, which results either in the formation of hydrated complexes, or the conversion of an M@O group into a corresponding dihydroxide unit. The second type comprises degradation of a polynuclear oxide species by successive hydrolytic cleavage of M±O±M bridges. Here, M is taken to be Si or P, and both mononuclear and binuclear species, as well as the conversion between the two, are described. Results are presented for the reactions: SiO2 g H2 O g ! SiO2 H2 O g SiO2 H2 O g ! SiO OH2 g SiO OH2 g H2 O g ! SiO OH2 H2 O g SiO OH2 H2 O g ! Si OH4 g Si OH4 g nH2 O g ! Si OH4 H2 On g R1 Si2 O4 g H2 O g ! Si2 O3 OH2 g Si2 O3 OH2 g H2 O g ! Si2 O2 OH4 g Si2 O2 OH4 g H2 O g ! Si2 O OH6 g Si2 O OH6 g H2 O g ! 2Si OH4 g R2 PO2 OH g H2 O g ! PO2 OH H2 O g PO2 OH H2 O g ! PO OH3 g PO OH3 g nH2 O g ! PO OH3 H2 On g R3 P2 O5 g H2 O g ! P2 O4 OH2 g P2 O4 OH2 g H2 O g ! P2 O3 OH4 g P2 O3 OH4 g H2 O g ! 2PO OH3 g R4 2. Methods and computational details The B3LYP hybrid functional [7] was selected for the calculations in the present study. This J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 choice was made on the basis of the high-quality results obtained previously in analogous investigations. These comprise two studies on scandium oxides [8,9] and one on germanium oxides and hydroxides [10]. Most important though, for the present eort are the two investigations on water addition to transition metal oxides [5,6]. In all cases, the computational results were in very close agreement with available experimental data. This expected success of the B3LYP hybrid density functional approach requires some comments. Experience on a vast number of systems tells of the robustness of the particular choice on mixing exchange and correlation terms for this functional. Only when ambiguity in the occupation of the Kohn±Sham orbitals exists, results can be expected to become unreliable. This is because the conventional Kohn±Sham strategy is ill de®ned in cases where the proper electronic density description requires partial orbital occupations, as in bond forming and bond breaking regions on the ground state potential energy surface (PES). Such anticipated pathological systems are carefully avoided in our DFT investigations. While this constraint may appear troublesome, a similar warning ¯ag is associated with the applicability of non-degenerate perturbation theories, such as Mùller±Plesset 2nd order perturbation method (MP2), and indeed also coupled-cluster methods, such as CCSD(T), at times. As the accuracy of DFT has been demonstrated previously [5,6,8±10], the high-cost eciency very much favors it before any explicitly correlated wave function based method. The agreement with ab initio results is repeatedly shown here by comparisons to a number of high-level calculations on SiO2 g, using MP2 and CCSD(T). The B3LYP calculations were performed on the Si and P oxides, oxyhydroxides and hydroxides as outlined in the (R1)±(R4) reaction steps by employing the GA U S S I A N 98 program package [11]. Molecular structures were determined by calculating analytical Hessians, and characterized by their stabilities and vibrational spectra. The choice of basis set requires some comments. The mediumsized 6-311+G(d, p) basis set (denoted by (M)), used for all atoms, appears fully sucient for describing the energetics and structures in general. However, the description of Si±O and P±O bond- 47 ing can be improved by selecting larger basis sets. This is most important for the Si and P atoms, where calculations on important structures were complemented by full optimizations using the maximal 6-311+G(3df) basis sets on these atoms (denoted by (L)). For O and H, 6-311+G(d, p) describes the bonding suciently well. The smaller 6-311G basis sets for O and H atoms in conjunction with the 6-311G(d) basis sets for Si and P were employed (denoted by (S)) for predicting structures. Although these are reasonable, for some reactions the energetics becomes wrong. This occurs when the polarization around the core molecule is altered, e.g., by deprotonation. If this eect is taken account for, the (S) basis set can be employed on large clusters, in order to reduce computational costs. All calculations were carried out on closed shell singlet systems, i.e., the ground states of the investigated species in their highest oxidation state. 3. Results and discussion The present eort comprises a systematic investigation of a stepwise addition of molecular water to the mononuclear SiO2 g and PO2 OH g molecules, as well as to the corresponding binuclear Si and P oxide systems. One part of this investigation follows closely a similar study on the mononuclear transition metal oxides [5], as similar reactions of H2 O with Si@O and P@O bonds are considered. In addition, the present investigation includes the hydrolysis of Si±O±Si and P±O±P bridges. The latter reactions are in line with the corresponding study on binuclear transition metal oxide clusters [6], as these reactions increase the number of Si±OH or P±OH units by two in each H2 O addition step. A third issue regarding the initial steps towards micro-solvation is addressed as follows. Comparing the stability of any hydrated molecule to the corresponding system where the water molecule has been hydrolyzed involves full geometry optimization of all reactants and products. The structures are established as corresponding to local minima on the ground state PES by determining the vibrational spectra. Because two or 48 J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 more minima exist on the PESs for several of the model species, it becomes important for the chemical understanding to complement structural characteristics by determining interconnecting paths between the minima. Such calculations involve evaluating relative stabilities of local minima along possible reaction coordinates. Summaries of geometrical parameters and vibrational frequencies for the structures are provided in Tables 1±4, and illustrated in Figs. 1±4. 3.1. SiO2 g nH2 O SiO2 g (Fig. 1(a)) is a linear molecule of D1h symmetry. The largely covalent Si@O bond dis (M) and 1.51 A (L/XL), distances are 1.52 A playing only small basis set eects. Despite the small size of SiO2 g and the general importance of silicates, experimental and computational data are scarce in the literature. This is probably due to the high reactivity of the Si@O bonds in SiO2 g. The IR-active vibrational frequencies have been determined in Ar matrix to be 1416 and 273 cm 1 by Schn ockel [12] and by Andrews and McClusky [13]. Calculations on the Hartree±Fock (HF) level have been performed by Pacansky and Hermann [14] and by Ystenes [15], but no investigation appears to have been done using high-level ab initio techniques. A DFT study, using small basis sets of DZ quality, has been done by Brinkmann et al. [16]. This gap in the available data is bridged in this investigation by comparing our B3LYP results with bond distances and frequencies from MP2 and CCSD(T) optimizations. While the Si@O bond is somewhat longer using MP2 (1.53 A (M) and 1.52 A (L/XL)), the CCSD(T) results (M) and 1.515 A (XL)) follow the B3LYP (1.52 A data very closely. The vibrational frequencies display larger basis set eects for MP2 and CCSD(T) than was found for B3LYP, and apparently the (L) or (XL) basis sets are required for these two methods. All three methods appear to agree on the low frequency (299 cm 1 (B3LYP/ XL), 295 cm 1 (MP2/XL) and 297 cm 1 (CCSD(T)/XL)), and they come out around 25 cm 1 above the experimental value. This is expected for harmonic frequencies without matrix eects. However, there is some deviations for the high frequency (1445 cm 1 (B3LYP/XL), 1416 cm 1 (MP2/XL) and 1424 cm 1 (CCSD(T)/XL)). It appears that both the MP2 and CCSD(T) potentials are too shallow, as anharmonicity would lower the frequencies further. In general, all three methods reproduce the experimental results very well, which is not the case for e.g., HF (too short Si@O bonds and too high-vibrational frequencies, cf. Table 1). The computational cost eciency though strongly favors B3LYP, as the MP2 2nd derivatives are takes 12 times longer and the CCSD(T) frequencies as much as 72 times longer time, exploiting similar resources on the same parallel computer. The degree to which the covalence in the O@Si@O p-system is sub-optimal can be appreciated from the reactivity of SiO2 to water. Initial hydration involves the formation of the SiO2 H2 O g complex (Fig. 1(b)). A structure with C2v symmetry is adopted for the complex, (M) displaying a long Si OH2 bond (1.93 A (L)), equivalent Si@O bonds and a and 1.89 A 158±159° O@Si@O bond angle. Although complex formation is exothermic by 81 kJ/mol (M) and 88 kJ/mol (L), no intramolecular hydrogen bonds are formed. These ®gures are expected to have high accuracy, based on the above agreement on SiO2 g between the B3LYP, MP2 and CCSD(T) methods, and the close structural and energetical agreement between B3LYP and MP2 on the more loosely bonded SO3 H2 O g complex (S OH2 [4]. bond: 2.37±2.39 A) Subsequent addition of the adsorbed water molecule to one of the Si@O bonds produces SiO OH2 g (Fig. 1(c)), which is accompanied by a 175 kJ/mol (M) and 184 kJ/mol (L) energy gain. Although the reaction involves overcoming a transition state, the considerable stability of the SiO2 H2 O g complex makes oxydihydroxide production very likely once the intermediate hydrate has been formed. The total exothermicity of this reaction becomes 256 kJ/mol (M) and 272 kJ/ mol (L). Interestingly, SiO2 g displays a 60±100 kJ/ mol higher reactivity in this step than GeO2 g does when forming the corresponding GeO OH2 [10]. The dierences in reactivities between the (M) and (L) basis sets are mainly assigned to a poorer describtion of the energetics of the Si@O bond in (M). J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 49 Table 1 and bond angles A (deg.), and ranges of vibrational frequencies cm 1 , together with normal mode Summaries of bond lengths R (A) symmetries and the number of vibrations in each group, for the SiO2 nH2 O system SiO2 D1h (M) D1h (L) D1h (XL) D1h (HF/M) D1h (HF/L) D1h (HF/XL) D1h (MP2/M) D1h (MP2/L) D1h (MP2/XL) D1h (CCSD(T)/M) D1h (CCSD(T)/XL) R Si@O: 1.516 Pu 1 vib:: 286 R Si@O: 1.509 Pu 1 vib:: 281 R Si@O: 1.509 Pu 1vib:: 299 R Si@O: 1.478 Pu (1 vib.): 342 R Si@O: 1.473 Pu (1 vib.): 332 R Si@O: 1.473 Pu (1 vib.): 359 R Si@O: 1.526 Pu (1 vib.): 267 R Si@O: 1.521 Pu (1 vib.): 264 R Si@O: 1.522 Pu 1 vib:: 295 R Si@O: 1.520 Pu (1 vib.): 267 R Si@O: 1.515 Pu (1 vib.): 297 SiO2 H2 O C2v (M) R Si@O: 1.527 R Si O: 1.931 Cs (L) C2v (L) SiO OH2 H2 O C1 (1-M) C1 (2-L) rg=u 2 vib:: 999±1448 rg=u (2 vib.): 998±1445 rg=u 2 vib:: 1115±1604 rg=u (2 vib.): 1121±1604 rg=u (2 vib.): 1119±1599 rg=u (2 vib.): 974±1440 rg=u (2 vib.): 975±1428 rg=u 2 vib:: 966±1416 rg=u 2 vib:: 979±1434 rg=u (2 vib.): 980±1424 A O@Si@O: 180.0 A O@Si@O: 180.0 A O@Si@O: 180.0 A O@Si@O: 180.0 A O@Si@O: 180.0 A O@Si@O: 180.0 A O@Si@O: 180.0 A O@Si@O: 180.0 A O@Si@O: 180.0 A O@Si@O: 180.0 A O@Si@O: 180.0 A O@Si@O: 159.3 A O@Si O: 100.3 A H±O±H: 114.1 A1 A2 B1 B2 4 1 2 3 vib:: 158±1575 A1 B2 1 1 vib:: 3749±3872 R Si@O: 1.518 R O±H: 0.968 A O@Si@O: 157.7 R Si O: 1.893 A Si O±H: 119.6 A O@Si O: 101.1 A H±O±H: 113.9 A0 A00 6 4 vib:: 191±1566 A0 A00 1 1 vib:: 3733±3852 SiO OH2 C2v (M) C1 (2-M) rg=u (2 vib.): 992±1446 R O±H: 0.967 A Si O±H: 122.9 R Si@O: 1.525 R O±H: 0.963 R Si±O: 1.627 A Si±O±H: 116.9 A1 A2 B1 B2 4 1 2 3 vib:: 305±1274 R Si@O: 1.514 R O±H: 0.963 R Si±O: 1.615 A Si±O±H: 116.1 A1 A2 B1 B2 4 1 2 3 vib:: 311±1292 R Si@O: 1.534 R Si±O: 1.615±1.625 R O±H: 0.961±0.981 A (17 vib.): 71±1622 R Si@O: 1.537 R Si±O: 1.641±1.652 R Si O: 1.993 R O±H: 0.961±0.970 A (17 vib.): 153±1596 R Si@O: 1.527 R Si±O: 1.628±1.640 R O H: 1.906±1.987 A Si±O±H: 110.9±117.6 A Si±O H: 98.9 A O±H O: 142.0 A (4 vib.): 3541±3896 A Si±O±H: 115.4±116.2 A Si O±H: 105.4±117.0 A H±O±H: 109.6 A (4 vib.): 3730±3894 A Si±O±H: 114.8±115.6 A O@Si±O: 128.3 A O±Si±O: 103.5 A1 B2 1 1 vib:: 3875±3877 A O@Si±O: 128.0 A O±Si±O: 103.9 A1 B2 1 1 vib:: 3874±3876 A O@Si±O: 125.7±127.3 A O±Si±O: 106.9 A H±O±H: 107.4 A H±O H: 97.6±136.0 A O@Si±O: 125.0±126.8 A O@Si O: 98.4 A O±Si±O: 103.2 A O±Si O: 95.0±98.0 A O@Si±O: 124.8±126.4 A O@Si O: 98.0 50 J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 Table 1 (Continued ) R Si O: 1.966 R O±H: 0.961±0.971 A (17 vib.): 166±1595 Si OH4 S4 (M) S4 (L) Si OH4 H2 O C1 (M) C1 (L) Si OH4 2H2 O C1 (1-M) C2 (2-M) C1 (3-M) R Si±O: 1.646 R O±H: 0.960 A B E 4 5 4 vib:: 198±982 R Si±O: 1.634 R O±H: 0.960 A B E 4 5 4 vib:: 190±994 R Si±O: 1.631±1.667 R O±H: 0.960±0.974 R O H: 1.911±2.000 A O±Si±O: 105.0±117.2 A O±H O: 141.5±151.0 A H±O±H: 106.6 R Si±O: 1.716±1.724 R Si O: 2.091±2.107 R O±H: 0.961±0.968 A O±Si±O: 89.6±172.0 A O±Si O: 83.7±95.2 A O Si O: 177.9 A H±O±H: 108.0±108.8 A (31 vib.): 85±1596 A (8 vib.): 3750±3874 R Si±O: 1.630±1.671 A O±Si±O: 105.2±117.8 R O±H: 0.961±0.974 A O±H O: 141.8±152.4 R O H: 1.891±1.995 A H±O±H: 106.7 A (31 vib.): 28±1624 A (8 vib.): 3615±3894 R Si±O: 1.620±1.674 A O±Si±O: 103.4±118.0 R O±H: 0.960±0.984 A O±H O: 161.0±170.8 R O H: 1.739±1.832 A H±O±H: 106.5±106.9 A (8 vib.): 3408±3901 R Si±O: 1.613±1.671 R O±H: 0.960±0.997 R O H: 1.679±1.921 A (38 vib.): 50±1686 A O±Si±O: 104.2±118.0 A O±H O: 156.8±167.8 A H±O±H: 106.5±106.9 A H±O H: 100.8±123.5 A (10 vib.): 3174±3897 Proceeding further along this line, it is observed that there are two optional coordinations for the SiO OH2 H2 O g complex. Either, H2 O is allowed to bridge between one hydroxide and the Si@O, forming a nearly planar con®guration (Fig. 1(d)) or water is allowed to coordinate directly to Si (Fig. 1(e)). Despite the long hydrogen bonds the bonding energy for the former (1.91±1.99 A), A O±Si±O: 103.5 A O±Si O: 95.7±98.9 A O±Si±O: 106.4±115.9 A Si±O±H: 118.4 A B E 1 1 1 vib:: 3897±3900 A O±Si±O: 106.3±115.9 A Si±O±H: 117.8 A B E 1 1 1 vib:: 3898±3901 A (24 vib.): 39±1624 A (6 vib.): 3623±3900 R Si±O: 1.618±1.654 A O±Si±O: 105.2±116.9 R O±H: 0.960±0.974 A O±H O: 141.5±152.7 R O H: 1.890±2.023 A H±O±H: 106.6 A (24 vib.): 39±1620 A (6 vib.): 3625±3902 A (31 vib.): 35±1645 Si OH4 3H2 O C1 (M) A Si O±H: 101.9±116.2 A H±O±H: 109.6 A (4 vib.): 3714±3894 A Si±O±H: 117.0±118.2 A Si±O H: 109.7 A H±O H: 91.4±127.5 A Si±O±H:116.9±117.6 A Si±O H: 109.0 A H±O H: 90.5±128.3 A Si±O±H: 111.8±112.6 A Si O±H: 102.0±111.4 A Si±O±H: 116.7±117.5 A Si±O H: 110.0 A H±O H: 90.7±127.6 A Si±O±H: 115.4±123.5 A Si±O H: 126.5 A H±O H: 100.8±123.5 A Si±O±H: 115.7±119.5 A Si±O H: 115.7±122.2 complex is 42 kJ/mol (M), while the latter gives an additional 14 kJ/mol (M). The reason for the higher stability of the complex where water is (M) and bonded directly to Si (Si OH2 : 1.99 A 1.97 A (L)), as compared to the H bonded complex, is that for both systems the bond to the complex relaxes only the Si±OH bonds, not the Si@O bond. This relaxation eect becomes largest J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 51 Table 2 and bond angles A (deg.), and ranges of vibrational frequencies cm 1 , together with normal mode Summaries of bond lengths R (A) symmetries and the number of vibrations in each group, for the SiO2 2 nH2 O systems OSiO2 SiO D2h (M) R Si@O: 1.512 A O@Si±O: 135.7 R Si±O: 1.680 A O±Si±O: 88.6 Ag B1u B2g=u B3g=u 3 2 3 4 vib:: 110±1338 R Si@O: 1.502 A O@Si±O: 135.5 R Si±O: 1.666 A O±Si±O: 89.0 Ag B1u B2g=u B3g=u 3 2 3 4 vib:: 121±1356 D2h (L) HOSiO3 SiOH C2 (M) R Si±O: 1.602±1.737 R Si±Si: 2.071 A B 10 9 vib:: 128±1178 (HO)OSiOSiO(OH) Cs (1-M) Cs (2-M) OSiO2 Si OH2 C2 (M) R Si@O: 1.516±1.518 R Si±O: 1.620±1.650 R O±H: 0.964 R O H: 2.185 A0 A00 13 6 vib:: 38±1306 R Si@O: 1.517±1.527 R Si±O: 1.612±1.670 R O±H: 0.963±0.978 R O H: 2.045 A0 A00 13 6 vib:: 64±1306 R Si@O: 1.516 R Si±O: 1.619±1.706 R O±H: 0.960 A B 10 9 vib:: 104±1314 HOOSiOSi OH3 C1 (1-M) C1 (2-M) HO2 SiO2 Si OH2 D2 (M) HO3 SiOSi OH3 C2 (1-M) C2 (1-L) A Si±O±Si: 91.4 A Si±O±Si: 91.0 R O±H: 0.961 A Si±O±Si: 73.7±73.9 A Si±O±H: 123.3 A O±Si±O: 87.2±128.0 A B 1 1 vib:: 3897±3898 A Si±O±H: 118.3±118.4 A Si±O H: 107.0 A H±O H: 134.7 A0 2 vib:: 3769±3852 A Si±O±H: 118.3±120.4 A Si±O H: 120.4 A Si±O±Si: 145.4 A O@Si±O: 124.6±130.2 A O±Si±O: 102.4±107.5 A O±H O: 139.3 A Si±O±Si: 129.7 A O@Si±O: 120.3±129.9 A O±Si±O: 107.5±110.5 A O±H O: 146.9 A0 2 vib:: 3565±3860 A Si±O±H: 121.6 A O@Si±O: 135.0 A Si±O±Si: 91.4 A O±Si±O: 87.3±114.2 A B 1 1 vib:: 3910 R Si@O: 1.523 A Si±O±H: R Si±O: 1.602±1.646 116.2±119.8 R O±H: 0.960±0.963 A (1 vib.): 22i A (25 vib.): 30±1298 A (4 vib.): 3862±3904 R Si@O: 1.530 A Si±O±H: R Si±O: 1.611±1.676 117.6±119.5 R O±H: 0.960±0.969 A Si@O H: 94.8 R O H: 2.308 A (26 vib.): 38±1306 A (4 vib.): 3769±3852 R Si±O: 1.629±1.690 A Si±O±H: 119.2 R O±H: 0.960 A B1 B2 B3 7 6 7 6 vib:: 85±1016 A B1 B2 B3 1 1 1 1 vib:: 3909±3912 R Si±O: 1.639±1.654 A Si±O±H: 116.2±119.0 R O±H: 0.960±0.964 A Si±O H: 103.0 R O H: 2.599 A H±O H: 137.5 A (1 vib.): 9i A (32 vib.): 41±1080 A (6 vib.): 3839±3901 R Si±O: 1.628±1.642 A Si±O±H: 115.3±118.6 R O±H: 0.960±0.964 A Si±O H: 103.4 R O H: 2.489 A H±O H: 137.0 A (33 vib.): 34±1082 A (6 vib.): 3834±3903 A Si±O±Si: 161.9 A O@Si±O: 125.9±129.0 A O±Si±O: 104.2±115.0 A Si±O±Si: 129.6 A O@Si±O: 121.6±123.6 A O±Si±O: 103.4±108.9 A O±H O: 138.2 A Si±O±Si: 91.3 A O±Si±O: 88.7±118.5 A Si±O±Si: 133.6 A O±Si±O: 103.2±113.9 A O±H O: 129.8 A Si±O±Si: 131.5 A O±Si±O: 103.3±113.8 A O±H O: 131.8 52 J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 Table 2 (Continued ) C1 (2-M) C1 (2-L) HO3 SiOSi OH3 H2 O C1 (M) R Si±O: 1.630±1.658 A Si±O±H: 115.8±119.0 R O±H: 0.960±0.966 A Si±O H: 106.6 R O H: 2.222 A H±O H: 131.9 A (33 vib.): 25±1105 A (6 vib.): 3799±3904 R Si±O: 1.618±1.645 A Si±O±H: 115.2±118.6 R O±H: 0.960±0.966 A Si±O H: 106.6 R O H: 2.196 A H±O H: 132.9 A (33 vib.): 15±1112 A (6 vib.): 3800±3906 R Si±O: 1.628±1.665 R O±H: 0.960±0.980 R O H: 1.802±2.132 A (40 vib.): 35±1647 A Si±O±H: 114.9±118.8 A Si±O H: 108.3 A H±O H: 110.5±132.8 A H±O±H: 106.5 A (8 vib.): 3508±3901 for the second structure. It can be noted that the exothermicity for the formation of the Fig. 1(e) complex depends little on the choice of basis set (59 kJ/mol (M) and 60 kJ/mol (L)). The subsequent reaction, from the complex in Fig. 1(e) to Si OH4 g (Fig. 1(f)), becomes exothermic by 195 kJ/mol (M) and 199 kJ/mol (L). Thus the total energy release for the water addition to the second Si@O (254 kJ/mol (M) and 259 kJ/ mol (L)) becomes somewhat lower than for addition to the ®rst. In total the SiO2 g 2H2 O g reaction is exothermic by 509 kJ/mol (M), which is about 100 kJ/mol higher than found for the corresponding Ge system [10]. The product, orhtosilicic acid, has been subject to several quantum chemical investigations in the past [17±22], though the focus has mainly been on the orientation of the four Si±OH groups. In the optimal structure, these are arranged so that each H atom points toward an adjacent O atom, which result in S4 symmetry [21]. This was indeed also observed for the optimal structure of Ge OH4 [10]. Possibly more interesting is the fact that the structure of Si OH4 does not display a tetrahedral con®guration on the O atoms. Rather, the arrangement of O atoms around Si could be described as a ¯attened tetrahedron, which contains two dierent O±Si±O bond angles (106° and 116° (M) and (L)). This is again very similar to what was obtained for Ge OH4 [10]. This ¯attened tetrahedron coordination is in contrast to the Ti OH4 molecule, which despite the lower molecular symmetry displays a perfectly tetrahedral oxygen coordination around the cen- A Si±O±Si: 141.3 A O±Si±O: 103.5±114.8 A O±H O: 137.6 A Si±O±Si: 139.9 A O±Si±O: 103.9±114.7 A O±H O: 138.3 A Si±O±Si: 140.4 A O±Si±O: 101.8±115.0 A O±H O: 140.9±167.0 tral atom [5]. It is suggested that Td symmetry cannot be sustained among neutral mononuclear oxyhydroxides of the p-elements. In fact, the only exception to this rule comprises ArO4 [4]. Thus, the reason why systems such as SiO44 , PO43 , SO42 , ClO4 and ArO4 do display Td symmetry is rather found in the packing of four exactly equivalent ligands on a sphere. In contrast, the 3dshell of e.g., Ti does indeed possess the necessary ¯exibility to produce a truly tetrahedral covalent bonding. The dominant basis set eect for Si OH4 g is observed on the Si±O bond distances, which decrease with an enlarged basis set (M) vs. 1.63 A (L)). (1.65 A Introduction of additional H2 O molecules initiates the formation of a solvation shell around the orthosilicic acid molecule by hydrogen bonding to the Si±OH groups. For Si OH4 H2 O g (Fig. 1 (g)) there exists only one structure, namely the one where the H end of one Si±OH group binds to water, and where one H end of water binds to O in another Si±OH group. This, however, results in (M) and elongated hydrogen bonds (1.91±2.00 A 1.89±2.02 A (L)), which consequently are not very strong. The energy released upon binding is only 27 kJ/mol (M) and 26 kJ/mol (L). The reason for the poor binding will discussed further. Here, it is stated to be due to the lack of drive for proton (electron pair) delocalization, originating from the bridging between the two equivalent OH groups. Water does not assist in further relaxing any strain in the molecule. The only observed structural eect is seen in the O±Si±O bond angles. It is gratifying J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 53 Table 3 and bond angles A (deg.), and ranges of vibrational frequencies (cm 1 ), together with normal mode Summaries of bond lengths R (A) symmetries and the number of vibrations in each group, for the PO2 OH nH2 O systems PO2 OH Cs (M) Cs (L) PO2 OH H2 O C1 (1-M) C1 (1-L) C1 (2-M) C1 (2-L) PO OH3 C3 (M) C3 (L) P OH3 H2 O2 C1 (M) R P@O: 1.462±1.469 R P±O: 1.600 A0 A00 6 2 vib:: 391±1440 R P@O: 1.450±1.456 R P±O: 1.579 A0 A00 6 2 vib:: 404±1472 C1 (L) PO OH3 H2 O C1 R O±H: 0.969 A P±O±H: 112.1 R P@O: 1.468±1.474 A P±O±H: 112.2 R P±O: 1.605 A P O±H: R P O: 2.184 107.0±108.2 R O±H: 0.967 A H±O±H: 107.5 A 15 vib:: 154±1611 A 3 vib:: 3759±3860 R P@O: 1.456±1.462 A P±O±H: 111.6 R P±O: 1.584 A P O±H: R P O: 2.119 105.5±105.9 R O±H: 0.966±0.968 A H±O±H: 107.7 A (15 vib.): 181±1614 A (3 vib.): 3748±3848 R P@O: 1.464±1.478 A P@O H: 108.7 R P±O: 1.579 A P±O±H: 111.0 R O±H: 0.962±0.998 A O±H O: R O H: 1.694±2.195 124.9±159.7 A (15 vib.): 73±1609 A (3 vib.): 3221±3896 R P@O: 1.451±1.464 A P@O H: 108.2 R P±O: 1.558 A P±O±H: 111.0 R O±H: 0.962±1.000 A O±H O: R O H: 1.676±2.204 125.1±161.2 A (15 vib.): 83±1608 A (3 vib.): 3186±3894 R P@O: 1.476 R P±O: 1.606 A E 5 5 vib:: 171±1291 R P@O: 1.462 R P±O: 1.588 A E 5 5 vib:: 173±1323 A P±O±H: 112.2±114.0 A P±O H: 115.8 A H±O H: 109.8±119.5 A (5 vib.): 3461±3837 R P±O: 1.627±1.725 R O±H: 0.968±0.972 A (22 vib.): 120±1201 R P±O: 1.610±1.708 R O±H: 0.962±0.966 A (22 vib.): 112±1208 R P@O: 1.472 A O@P@O: 134.6 A O@P±O: 111.8±113.7 A0 (1 vib.): 3788 A O@P@O: 134.1 A O@P±O: 112.2±113.8 A0 1 vib:: 3787 A O@P@O: 132.8 A O@P±O: 111.3±113.6 A O@P O: 95.0±96.0 A O±P O: 93.8 A O@P@O: 132.2 A O@P±O: 111.6±113.4 A O@P O: 95.7±96.0 A O±P O: 94.7 A O@P@O: 132.0 A O@P±O: 113.7±114.3 A H±O±H: 107.7 A H±O H: 101.4±129.4 A O@P@O: 131.5 A O@P±O: 113.9±114.6 A H±O±H: 107.7 A H±O H: 99.9±129.0 R O±H: 0.965 A O@P±O: 116.3 A P±O±H: 113.0 A O±P±O: 101.9 A E 1 1 vib:: 3834±3837 R O±H: 0.965 A O@P±O: 116.1 A P±O±H: 112.5 A O±P±O: 102.1 A E 1 1 vib:: 3839±3841 R P±O: 1.613±1.706 R O±O: 1.450 R O±H: 0.964±0.984 R O H: 1.753±2.220 A (22 vib.): 44±1535 P OH5 C1 (M) R O±H: 0.968 A P±O±H: 112.9 A O±P±O: 94.5±101.5 A O±O±H: 101.3±101.8 A O±O H: 113.4 A O±H O: 161.9±166.3 A O±P±O: 88.0±176.5 A P±O±H: 109.4±113.4 A (5 vib.): 3796±3866 A O±P±O: 88.2±176.5 A P±O±H: 109.4±113.4 A (5 vib.): 3807±3867 A P±O±H: A O@P±O: 113.4±117.2 54 J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 Table 3 (Continued ) (1-M) C1 (2-M) C1 (2-L) PO OH3 2H2 O C1 (1-M) C1 (2-M) PO OH3 3H2 O C3 (1-M) C1 (2-M) C1 (3-M) R P±O: 1.581±1.631 R O±H: 0.962±0.987 R O H: 1.753±2.220 111.5±115.4 A P±O H: 112.3 A O±H O: 125.0±161.2 A (22 vib.): 43±1612 A (5 vib.): 3390±3896 R P@O: 1.488 A P@O H: 107.6 R P±O: 1.585±1.612 A P±O±H: R O±H: 0.962±0.989 110.2±113.7 R O H: 1.773±1.970 A O±H O: 138.2±154.8 A (22 vib.): 42±1618 A (5 vib.): 3367±3890 R P@O: 1.474 A P@O H: 107.0 R P±O: 1.566±1.5922 A P±O±H: R O±H: 0.962±0.989 111.0±113.4 R O H: 1.764±1.969 A O±H O: 139.6±155.2 A (22 vib.): 44±1619 A (5 vib.): 3360±3888 R P@O: 1.502 R P±O: 1.583±1.603 R O±H: 0.962±0.988 R O H: 1.780±1.974 A P@O H: 107.6±107.8 A P±O±H: 111.0±113.7 A O±P±O: 100.4±107.3 A H±O±H: 106.8 A H±O H: 97.0±132.3 A O@P±O: 114.0±117.0 A O±P±O: 100.8±106.0 A H±O±H: 107.2 A H±O H: 93.4±127.7 A O@P±O: 113.8±116.8 A O±P±O: 101.3±106.6 A H±O±H: 107.0 A H±O H: 91.64±127.2 A O@P±O: 112.9±116.2 A O±P±O: 101.4±108.4 A H±O±H: 107.2 A H±O H: 92.0±128.6 A O±H O: 139.3±155.2 A (29 vib.): 33±1622 A (7 vib.): 3377±3889 R P@O: 1.484 A P@O H: 128.7 A O@P±O: 111.2±119.2 R P±O: 1.573±1.620 A P±O±H: A O±P±O: 102.8±105.9 R O±H: 0.961±1.008 112.3±116.5 A H±O±H: 106.7±107.3 R O H: 1.603±1.770 A O±H O: A H±O H: 101.0±123.7 162.5±171.8 A (29 vib.): 31±1662 A (3 vib.): 2986±3498 A (4 vib.): 3827±3888 R P@O: 1.517 R P±O: 1.586 R O±H: 0.962±0.985 R O H: 1.817±1.996 A P@O H: 125.7 A P±O±H: 106.8 A H±O±H: 107.0 A H±O H: 92.9±128.0 A O@P±O: 113.2 A O±P±O: 105.5 A O±H O: 139.7±151.5 A E 12 11 vib:: 29±1617 R P@O: 1.483 R P±O: 1.563±1.646 R O±H: 0.962±1.042 R O H: 1.489±2.004 A E 3 3 vib:: 3436±3890 A P@O H: 121.6 A O@P±O: 111.0±120.5 A P±O±H: A O±P±O: 102.3±105.5 111.0±115.7 A H±O±H: 106.6±107.0 A P±O H: 118.9 A H±O H: 103.5±126.9 A O±H O: 152.8±172.2 A (36 vib.): 48±1667 A (9 vib.): 2428±3893 R P@O: 1.498 A P@O H: A O@P±O: 110.0±117.9 R P±O: 1.573±1.605 106.8±125.7 A O±P±O: 103.2±107.0 R O±H: 0.962±1.006 A P±O±H: A H±O±H: 106.7±107.3 R O H: 1.612±1.980 111.2±116.9 A H±O H: 92.0±128.9 A O±H O: 139.7±170.0 A (36 vib.): 32±1655 A (9 vib.): 3018±3890 to note that the energy dierence between the (M) and (L) basis sets has virtually disappeared for Si OH4 H2 O g. The deviations on energetics for larger complexes using (M) can thus be estimated to 2 kJ/mol, which anyway is within the expected accuracy for DFT methods. Still, an improved J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 55 Table 4 and bond angles A (deg.), and ranges of vibrational frequencies cm 1 , together with normal mode Summaries of bond lengths R (A) symmetries and the number of vibrations in each group, for the PO2 OH2 nH2 O systems OPO3 PO D3h (M) O2 POPO2 C2 (M) C2 (L) R P@O: 1.450 R P±P: 2.111 R P±O: 1.694 A O@P±O: 128.6 A01 A002 E0 E00 3 2 3 2 vib:: 237±1443 R P@O: 1.459±1.462 R P±O: 1.627 A B 6 4 vib:: 57±655 R P@O: 1.447±1.450 R P±O: 1.605 A B 6 4 vib:: 42±684 O2 POPO OH2 C1 (M) HOOPO2 PO OH C2v (1-M) C2h (2-M) HO2 OPOPO OH2 C1 (1-S) C1 (1-M) C1 (1-L) C2 (2-S) C2 (2-M) A P±O±P: 77.1 A O±P±O: 85.3 A O@P@O: 136.7 A P±O±P: 134.3 A O@P±O: 110.7±112.6 A B 2 3 vib:: 960±1461 A O@P@O: 136.3 A P±O±P: 132.6 A O@P±O: 111.0±112.6 A B 2 3 vib:: 996±1492 R P@O: 1.459±1.476 A P±O±H: 113.4±116.0 R P±O: 1.578±1.688 A P±O H: 105.2 R O±H: 0.966±0.977 A O±H O: 138.5 R O H: 2.000 A (22 vib.): 60±1429 A (2 vib.): 3613±3817 A P±O±P: 131.0 A O@P@O: 133.5 A O@P±O: 110.7±117.7 A O±P±O: 100.8±104.3 R P@O: 1.461 A P±O±H: 112.8 A P±O±P: 93.9 R P±O: 1.594±1.656 A O@P±O: 116.4±120.0 R O±H: 0.967 A O±P±O: 86.1±104.8 A1=2 B1=2 12 10 vib:: 100±1362 A1 B2 1 1 vib:: 3817±3818 R P@O: 1.462 A P±O±H: 112.9 A P±O±P: 93.9 R P±O: 1.592±1.656 A O@P±O: 116.5±119.9 R O±H: 0.966 A O±P±O: 86.1±104.8 Ag=u Bg=u 11 11 vib:: 100±1352 Ag Bu 1 1 vib:: 3817±3818 R P@O: 1.470±1.474 A P±O±H: 118.6±123.0 R P±O: 1.581±1.653 A P±O H: 112.4 R O±H: 0.969±0.977 A H±O H: 127.0 R O H: 2.064 A (29 vib.): 39±1332 A (4 vib.): 3632±3767 R P@O: 1.463±1.468 A P±O±H: 113.0±115.3 R P±O: 1.589±1.651 A P±O H: 111.2 R O±H: 0.965±0.966 A H±O H: 124.0 R O H: 2.301 A (29 vib.): 37±1340 A (4 vib.): 3780±3835 R P@O: 1.455±1.450 A P±O±H: 112.7±115.5 R P±O: 1.571±1.625 A P±O H: 109.9 R O±H: 0.965±0.967 A H±O H: 135.6 R O H: 2.463 A (29 vib.): 30±1372 A (4 vib.): 3806±3836 R P@O: 1.467 A P±O±H: 119.0±119.5 R P±O: 1.585±1.640 A P±O H: 111.4 R O±H: 0.969±0.981 A H±O H: 128.0 R O H: 1.973 A B 15 14 vib:: 69±1359 A B 2 2 vib:: 3541±3759 R P@O: 1.460 A P±O±H: 113.4±113.8 R P±O: 1.593±1.636 A P±O H: 109.9 R O±H: 0.965±0.973 A H±O H: 133.0 R O H: 2.060 A B 15 14 vib:: 60±1365 A B 2 2 vib:: 3693±3830 A P±O±P: 139.4 A O@P±O: 114.7±119.6 A O±P±O: 98.2±103.0 A O±H O: 138.5 A P±O±P: 134.3 A O@P±O: 113.8±118.6 A O±P±O: 98.8±106.8 A O±H O: 124.0 A P±O±P: 134.4 A O@P±O: 113.6±118.0 A O±P±O: 99.5±106.4 A O±H O: 117.2 A P±O±P: 133.9 A O@P±O: 116.4±117.2 A O±P±O: 96.7±105.5 A O±H O: 136.8 A P±O±P: 133.3 A O@P±O: 114.9±116.2 A O±P±O: 98.0±105.8 A O±H O: 138.4 56 J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 Table 4 (Continued) C2 (2-L) C1 (3-S) C1 (3-M) C1 (3-L) C2 (4-M) C2 (4-L) R P@O: 1.448 A P±O±H: 112.3±114.0 R P±O: 1.573±1.614 A P±O H: 108.2 R O±H: 0.966±0.971 A H±O H: 129.7 R O H: 2.071 A B 15 14 vib:: 54±1393 A B 2 2 vib:: 3708±3828 R P@O: 1.478±1.492 A P±O±H: 118.0±122.0 R P±O: 1.576±1.636 A P@O H: 105.7 R O±H: 0.969±0.987 A O±H O: 138.5 R O H: 1.974 A (29 vib.): 65±1346 A (4 vib.): 3443±3778 R P@O: 1.461±1.483 A P±O±H: 112.6±113.9 R P±O: 1.585±1.635 A P@O H: 105.0 R O±H: 0.965±0.982 A O±H O: 143.7 R O H: 1.947 A (29 vib.): 68±1353 A (4 vib.): 3523±3834 R P@O: 1.449±1.469 A P±O±H: 112.6±113.0 R P±O: 1.568±1.619 A P@O H: 104.2 R O±H: 0.965±0.983 A O±H O: 145.0 R O H: 1.902 A (29 vib.): 59±1381 A (4 vib.): 3501±3835 R P@O: 1.482 A P±O±H: 111.4±112.9 R P±O: 1.586±1.642 A P@O H: 104.0 R O±H: 0.965±0.977 R O H: 2.163 A B 15 14 vib:: 79±1274 A B 2 2 vib:: 3629±3832 R P@O: 1.468 A P±O±H: 111.8±112.6 R P±O: 1.567±1.621 A P@O H: 103.0 R O±H: 0.965±0.978 R O H: 2.103 A B 15 14 vib:: 75±1304 A B 2 2 vib:: 3605±3838 HO2 OPOPO OH2 H2 O C1 (M) R P@O: 1.464±1.485 A P±O±H: 112.5±119.9 R P±O: 1.561±1.667 A P@O H: 130.7 R O±H: 0.962±1.009 A H±O±H: 107.3 R O H: 1.594±1.772 A H±O H: 103.0±118.8 A (36 vib.): 39±1639 A (4 vib.): 2963±3881 P4 O10 Td (M) Td (L) P4 O6 Td (M) Td (L) P4 Td (M) Td (L) A P±O±P: 133.6 A O@P±O: 114.7±115.8 A O±P±O: 99.4±105.7 A O±H O: 138.6 A P±O±P: 125.9 A O@P±O: 116.0±118.6 A O±P±O: 95.9±105.9 A P±O±P: 124.9 A O@P±O: 110.0±118.5 A O±P±O: 96.6±106.4 A P±O±P: 125.8 A O@P±O: 110.6±118.0 A O±P±O: 98.2±106.5 A P±O±P: 117.0 A O@P±O: 109.0±119.0 A O±P±O: 101.0±104.5 A O±H O: 136.8 A P±O±P: 117.3 A O@P±O: 109.5±118.9 A O±P±O: 101.8±104.3 A O±H O: 138.3 A P±O±P: 137.7 A O@P±O: 109.8±117.9 A O±P±O: 101.9±113.6 A O±H O: 158.0±173.7 R P@O: 1.448 A O@P±O: 117.0 A P±O±P: 124.6 R P±O: 1.634 A O±P±O: 101.0 A1 E T1 T2 2 3 3 4 vib:: 239±786 A1 T2 1 2 vib:: 975±1420 R P@O: 1.435 A O@P±O: 116.7 A P±O±P: 124.0 R P±O: 1.612 A O±P±O: 101.3 A1 E T1 T2 2 3 3 4 vib:: 245±820 A1 T2 1 2 vib:: 1013±1453 R P±O: 1.676 A O±P±O: 99.0 A1 E T1 T2 2 2 2 4 vib:: 278±914 R P±O: 1.655 A O±P±O: 99.3 A1 E T1 T2 2 2 2 4 vib:: 284±940 R P±P: 2.220 A P±P±P: 60.0 A1 E T2 1 1 1 vib:: 360±597 R P±P: 2.204 A P±P±P: 60.0 A1 E T2 1 1 1 vib:: 367±608 A P±O±P: 127.7 A P±O±P: 127.3 J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 57 Fig. 1. Structures in the SiO2 g 5H2 O g system: (a) SiO2 g D1h , (b) SiO2 H2 O g C2v , (c) SiO OH2 g C2v , (d) and (e) SiO OH2 H2 O g C1 , (f) Si OH4 g S4 ,(g) Si OH4 H2 O g C1 , (h), (i) and (j) Si OH4 2H2 O g C1 and (k) Si OH4 3H2 O g C1 together with relative stabilities and energetics for some hydrolysis reactions. quality on bond distances can be obtained if a larger basis set is used. There are three dierent possibilities for binding a second solvating water molecule. The least favorable coordination type for Si OH4 2H2 O g is the binding of all six O atoms to Si (Fig. 1(h)). Typical features include elongated bond distances Si OH2 : 2.10 A). Forming this (Si±O: 1.72 A, strained structure is endothermic by 127 kJ/mol (M), as compared to the monohydrate, but it is a local energy minimum. This structure is thus taken to exemplify a six-coordinated Si con®guration, elsewhere known only in high-pressure phases of SiO2 (s) [1]. The second type of dihydrate complex (Fig. 1(i)) has each of the H2 O bonded to two Si±OH groups and displays C2 symmetry. Binding the second water molecule is as exothermic (27 kJ/mol (M)), as was the ®rst. The hydrogen bonding in the Fig. 1(i) structure is rather poor though, as re¯ected in the in rather long O H bonds (1.89± The hydrogen bonding is signi®cantly 2.00 A). improved if the second water molecule is allowed to connect to the ®rst, thus forming a water dimer 58 J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 ligand (Fig. 1(j)). The O H bond distances are and this structure notably shortened (1.74±1.83 A), is 12 kJ/mol (M) more stable than the structure in Fig. 1(i). The total binding energy for the second water ligand thus becomes 39 kJ/mol (M). From this energy gain it can be concluded that the H2 O dimer is a better ligand to use for modeling the solvation shell, than a single water molecule. It can also be hypothesized, that binding four monomer or dimer ligands to the Si OH4 core will preserve its original symmetry. The ®nal water complex in this study is the trihydrate, Si OH4 3H2 O g (Fig. 1(k)). It is included as a reference structure to compare with similar trihydrates for e.g., perchloric acid, which display deprotonation and the formation of an ion pair [4]. The complex in Fig. 1(k) does not display such a behavior, and although the central O H bond is shortened, some others are elonagated This is re¯ected in the (range: 1.68±1.93 A). binding energy for the third water molecule, which again becomes 27 kJ/mol (M), typical of adding one H2 O g monomer. The main point with this structure is though to show that nano-scale acidity does not appear in Si OH4 g, which is in agreement with its Brùnsted alkalinity. 3.2. Si2 O4 g nH2 O The Si2 O4 molecule consists of a central Si2 O2 ring and two terminal Si@O bonds. O@SiO2 Si@O is planar (Fig. 2(a)), analogous to Ge2 O4 [10], and it is formed when dimerizing the SiO2 molecule (Fig. 2(b)). The fusion of two Si@O bonds into a ring is exothermic by 341 kJ/mol (M) and 378 kJ/mol (L). The energy released by this reaction is approximately 90±130 kJ/mol higher than what was found for the corresponding Fig. 2. Structures in the Si2 O4 4H2 O system: Si2 O4 : (a) OSiO2 SiO D2h , (b) 2 SiO2 D1h ; Si2 O5 H2 : (c) HOSiO3 SiOH C2 , (d) and (e) HO SiOO SiOOH Cs , (f) OSiO2 Si OH2 C2 ; Si2 O6 H4 :(g) and (h) HO SiOOSi OH3 C1 , (i) HO2 SiO2 Si OH2 D2 , (j) 2 SiO OH2 C2v ; Si2 O7 H6 : (k) HO3 SiOSi OH3 C2 and (l) C1 ; Si2 O8 H8 : (m) 2 Si OH4 S4 and (n) HO3 SiOSi OH3 H2 O C1 together with relative stabilities and energetics for some hydrolysis reactions. J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 dimerization of GeO2 [10], which seems reasonable due to the better bonding between Si±O than Ge±O. The 37 kJ/mol basis set eect on reaction energies, which is also observed through the shorter Si±O bond lengths using the (L) basis set (M) vs. 1:50 1:67 A (L)), corre(1:51 1:68 A sponds to the eect on the SiO2 g H2 O g reaction (2 16 kJ/mol). It is thus reasonable to assign this eect to description of SiO2 g, where the insuciency of (M) really aects the energetics. However, earlier investigations at the HF [14,22] and pseudo-potential levels [23] on the dimerization of SiO2 found much higher reactivities, i.e., in the range 450±520 kJ/mol. A somewhat later paper [24] compared results from MP2, DFT-GGA and experiment. Both theoretical methods were found to be in agreement with the experimental results, and the formation energy for Si2 O4 was calculated to be 354 kJ/mol, using DFT-GGA. A similar consistency between MP2 and B3LYP results was also found for the germanium oxides [10]. There are two dierent types of reactive sites for water addition to OSiO2 SiO, comprising the Si±O±Si bridges and the terminal Si@O bonds. Cleavage of one bridge results in a planar HO± O@Si±O± Si@O±OH chain, which displays one structure (Fig. 2(d)) similar to that found for its Ge analogue [10]. In contrast though, the intramolecular hydrogen bond between the two Si±OH groups is signi®cantly weaker (O H: 2.19 than what was found for the Ge system, and the A) Si±O±Si bond angle is rather open (145°). A second type of planar chain structure was found for (OH)OSiOSiO(OH). It displays a geometry, where the proton of one Si±OH group points toward one Si@O unit (Fig. 2(e)). The hydrogen bond is and the Si±O±Si bond somewhat shorter (2.04 A) angle more acute (129°). These eects stabilize the latter structure by 7 kJ/mol (M), as compared to the former. While hydrolysis of one Si±O±Si bridge in Si2 O4 , to form the most stable chain structure, is exothermic by 162 kJ/mol (M), the high reactivity of the terminal Si@O bonds determines the O@SiO2 Si OH2 cluster structure (Fig. 2(f)) to be the global minimum for Si2 O5 H2 . In fact, the Si2 O2 ring based cluster is 130 kJ/mol (M) more stable than the chain, making water addition to one 59 of the terminal Si@O bonds in Si2 O4 exothermic by 292 kJ/mol (M). The 27 kJ/mol lower exothermicity, that is observed when comparing the conversion from the ®rst Si-chain type to the cluster to the similar conversion of the Ge systems [10], is attributed to the higher reactivity of the Si@O bond, as compared to the Ge@O bond. Previous studies on the Si2 O5 H2 system suggested it to be a triplebridged HO±SifO3 gSi±OH cluster (Fig. 2(c)) [25,26]. However, this structure is the least stable of the three (2 kJ/mol above the ®rst chain type). This is in agreement with the stability ordering obtained for the structures found for Ge [10]. The principal sites for addition of a second water molecule comprise the remaining Si@O groups. Consequently, the reactivities become rather independent on reactant structure, and the relative stability ordering from seen for the Si2 O5 H2 systems remain. There exist two chain structures for OH± Si@O±O±Si OH3 . Reacting one Si@O group in the ®rst Si2 O5 H2 chain structure (Fig. 2(d)) releases 281 kJ/mol (M), and produces a structure (Fig. 2(g)) with a very wide Si±O±Si bond angle (161°). No hydrogen bonding remains in this system, and it turns out to be a transition state. Allowing for one ± OH2 Si±OH group to interact with the Si@O gives a 5 kJ/mol (M) stabilization, and produces an energy minimum (Fig. 2(h)), which has a bonding situation reminiscent of that in Fig. 2(e). Indeed, the rather acute Si±O±Si bond angle (130°) is recovered, despite the fact that the O H bond distance (2.30 must be deemed too long to be classi®ed as a A) hydrogen bond. Surely, such ``intramolecular hydrogen bonds'' have only negligible in¯uence on the bond angle of the Si±O±Si bridge. Rather, it is the overall ligand-backbone and ligand±ligand Pauli repulsions that become decisive for determining the Si±O±Si bond angles. The global minimum for Si2 O6 H4 comprises the Si2 O2 ring based cluster (Fig. 2(i)). This HO2 SiO2 Si OH2 cluster displays D2 symmetry. It resembles the corresponding Ge based system [10]. It is 114 kJ/mol (M) lower in energy than the chain structure (Fig. 2(h)), and consequently water addition to the Si@O bond in OSiO2 Si OH2 becomes exothermic by 265 kJ/mol (M). This tells of a somewhat lower reactivity of 60 J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 the second Si@O group, as compared to the ®rst, which is in agreement with the results on the monomeric systems using the (L) basis set. Interestingly, if the ring cluster is formed from two SiO OH2 molecules (Fig. 2(j)), 386 kJ/mol (M) is released, whereas the formation of the chain structure only releases 272 kJ/mol (M). Addition of a third water molecule, allows the reaction routes to converge to the single-bridged HO3 SiOSi OH3 molecule (Figs. 2(k) and (l)). This molecule is the silica dimer, and it is of great importance for understanding the chemistry of silicates. Consequently, several investigations have been conducted to establish structures and stability properties. The computational problem evolves mainly around the issues how to achieve a correct balance between ionic and covalent contributions to the Si±O bonds, in conjunction with a correct description of the intramolecular hydrogen bonding. Depending on the magnitude of each of these eects, dierent structures, and in particular different Si±O±Si bond angles, are obtained for the global energy minimum. In the study by Teppen et al. [21], three conformations, diering in the number of hydrogen bonds (1, 1.5 or 2), were investigated by employing HF and MP2 methods. A structure possessing two hydrogen bonds and C2 symmetry appeared to be the global energy minimum at the MP2 level. However, this structure was found to be a transition state at the HF level, whereas the two other structures came out as true minima. An optimal structure with C2 symmetry were and two intramolecular H bonds (2.08 A) also found for the Ge2 O7 H6 system [10]. Only little help in deciding on the global minimum on the Si system is obtained from this observation, since the strengths of such H bonds are signi®cantly smaller for the Si systems than for the Ge compounds. The Si±O±Si bond angles are also in general wider than the Ge±O±Ge angles (118° for Ge2 O7 H6 ). In the present study, the C2 structure of HO3 SiOSi OH3 (Fig. 2(k)), with a 134° Si±O±Si angle and is found to two very long O H bonds (2.60 A), be a transition state with a small symmetry breaking frequency using B3LYP and the (M) basis set. An energy minimum for the (M) basis set is obtained for a symmetry broken structure (Fig. 2(l)), which just has one long O H bond (2.22 Interestingly, the greater Si±O±Si bond angle A). (141°) is in good agreement with what is found in a-quartz (144°) [1]. The ®nding that the C2 structure is a TS on the B3LYP PES is in contradiction to a recent report by Pereira et al. [27] on silicate clusters. That work reports BLYP calculations, which have the C2 structure with a 132° Si±O±Si angle as the global minimum. As their structure seems quite similar to the TS with C2 symmetry obtained in the present work, it seems reasonable to doubt their conclusion. With the BLYP functional, we obtain two minima when employing the (S) basis set: one resembling the C2 , and another the C1 structure. The symmetry broken structure becomes the global minimum by 2 kJ/mol. Improvement of the basis set to (M) results in the C2 solution becoming a transition state also for the BLYP method. Thus, the C1 solutions produced by the B3LYP functional and HF cannot be deemed as artifacts due to HF exchange, as BLYP does not contain the HF exchange component. When ®nally the basis set in the B3LYP calculations is increased to (L), both structures come out as true energy minima. They are now equally stable, but still display two distinctly dierent Si±O±Si bond angles (134° and 140°, respectively). The H bonds in both systems are still very long, so it becomes obvious that the two conformers are the result of two equally important arrangements of SiO4 -tetrahedra in the silica dimer. In bulk silicates, it is the connectivity to the counter-cations that determines which type of chain, twisted (C1 ) or straight (C2 ), will form the material. It is interesting to note that a-quartz is built up by helical chains of SiO4 -tetrahedra, an arrangement based on the above C1 structure, and that it is the handedness of the chains that renders quartz its optical activity [1]. There are two ways to introduce the fourth water molecule to the Si2 O4 g system, starting from the single-bridged HO3 SiOSi OH3 molecule (Fig. 2(l)). One route involves the bridging of two Si±OH groups e.g., as indicated in Fig. 2(n), while the second possibility comprises hydrolysis of the remaining Si±O±Si bridge. While hydration is trivially exothermic (42 kJ/mol (M)), the formation of two Si OH4 g (Fig. 2(m)) from HO3 SiOSi OH3 g H2 O g is endothermic by J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 24 kJ/mol (M) and 19 kJ/mol (L). The relevance of this value for fully solvated species can though be questioned. However, the energy gain in Si2 O7 H6 H2 O g is to a large extent cancelled by hydrogen bonding between the two Si OH4 g fragments, although the water ligand renders the chain species some extra stability. The eect of further solvation is also expected to be quite similar both for Si2 O7 H6 H2 O g and the two fragments, as both systems have eight OH groups available for hydrogen bonding to surrounding H2 O. The remaining argument pro or con bridge cleavage is the shape of the space in water occupied by the solvated species. The ellipsoid that encloses the elongated Si2 O7 H6 H2 O g chain might be a smaller distortion to the structure of 61 water than the two spheres around the Si OH4 g fragments. In that case, the polymer gains additional stability. It can be noted that the formation of Si2 O7 H6 H2 O g is much too exothermic (81 kJ/mol) using the (S) basis set, despite a quite good structure. The origin of this eect lies in the two short H bonds that are formed in Si2 O7 H6 H2 O g, which require polarization functions on O for correct energetics. It can also be noted that the assymetric Si2 O7 H6 H2 O g molecule has a wide Si±O±Si bond angle (140°). 3.3. PO2 OH g nH2 O The structure of PO2 OH g, metaphosphoric acid, is planar (Fig. 3(a)). The O@P@O bond angle Fig. 3. Structures in the PO2 OH 3H2 O system: (a) PO2 OH g Cs , (b) and (c) PO2 OH H2 O g C1 , (d) PO OH3 g C3 , (e) P OH3 H2 O2 g C1 , (f) P OH5 g C1 ,(g) and (h) PO OH3 H2 O g C1 , (i) and (j) PO OH3 2H2 O g C1 , (k) PO OH3 3H2 O g C3 , (l) and (m) C1 together with relative stabilities and energetics for some hydrolysis reactions. 62 J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 of 134±135° (M) and (L) is signi®cantly greater than that of the puckered vanadium analogue VO2 OH (112°) [5], which tells of the greater ¯exibility in accommodating electron pairs of local p symmetry (in M@O), when 3d orbitals on M are available for bonding. Similar to the O@Si OH2 system, two kinds of complexes can be formed with water. A slightly smaller exothermicity (42 kJ/ mol (M) and 43 kJ/mol (L)) is observed when forming the four-coordinated PO2 OH H2 O g complex (Fig. 3(b)). The P OH2 bond is though (M) and 2.12 A (L)), despite rather long (2.18 A that no hydrogen bonds are observed. This long bond and the reduced reactivity are both results of the better covalent bonding in the two P@O groups, as compared to an Si@O unit. The threecoordinated complex (Fig. 3(c)) formally contains two hydrogen bonds, but the bond to the P@O (M)). The good unit is long (O H: 1.69±2.20 A H bonding to the P±OH group gives this complex a stability that is marginally (3 kJ/mol (M) and 4 kJ/mol (L)) below the complex in Fig. 3(b). Water addition to one of the P@O bonds of the PO2 OH H2 O g complex in Fig. 3(c), forming orthophosphoric acid OP OH3 (Fig. 3(d)), results in a further 108 kJ/mol (M) and 118 kJ/mol (L) stabilization. Thus the total addition reaction from meta- to orthophosphoric acid becomes exothermic by 153 kJ/mol (M) and 165 kJ/mol (L). This is about 100 kJ/mol less than what was found in the corresponding vanadium system [5]. This dierence is probably due to the lower stability of the V@O bonds in VO2 OH g, as compared to P@O in PO2 OH g, which generates the higher water anity for the former system. While the latter system displays a close to tetrahedral oxygen coordination, the PO OH3 g molecule displays signi®cant symmetry breaking, i.e., 116° and 102° (M)/(L) for the O@P±O and O±P±O bond angles, respectively. This observation is in accord with the proposed eect from 3d orbitals on ligand coordination, i.e., symmetry broken coordination in the 3p systems Si OH4 g and OP OH3 g, whereas the 3d systems Ti OH4 g and OV OH3 g both display close to tetrahedral coordination around the central atom. The overall symmetry of PO OH3 g is C3 , which also is lower than for the V system. The remaining P@O bond in PO OH3 g can react further with water. Two reactions are envisaged, one where water acts as reducing agent to form P OH3 H2 O2 g (Fig. 3(e)) and a second where P OH5 (Fig. 3(f)) is produced. The water induced reduction is endothermic by as much as 429 kJ/mol (M), re¯ecting the stability of P(V) as compared to P(III). In contrast, the formation of P OH5 is endothermic only by 42 kJ/mol (M) and 34 kJ/mol (L), which can be directly translated to an activation energy for oxygen exchange on phosphates in water. Furthermore, in as much as water can be understood to model a more general nucleophile with hydroxyl groups, this energy estimates the barrier height for activating phosphate transfer between two nucleophiles. Employing the second H2 O in hydrogen bonding produces PO OH3 H2 O g complexes, which are all more stable than forming the P OH5 g molecule. There are two structures for this complex, due to that there are two possible sites for binding water in PO OH3 g. The water molecule can either form a bridge between two P±OH groups (Fig. 3(g)) or between the P@O unit and one P±OH group (Fig. 3(h)). Despite that one of the hydrogen bonds in the former complex is rather long, it is 71 kJ/mol (M) more stable than P OH5 g. If water addition to PO OH3 g is considered, the reaction to form the PO OH3 H2 O g complex in Fig. 3(g) becomes exothermic by 29 kJ/mol (M). This value is very similar to the reaction that gives Si OH4 H2 O g, which displays a similar bonding situation. An additional 13 kJ/mol (M) energy gain can be obtained for PO OH3 H2 O g if the complex in Fig. 3(h) is allowed to form. The higher stability results from the function of the bridging water molecule as an equilizing agent between the P@O and P±OH units. This works as water partially provides a proton to the former and partially removes the proton from the latter. This tendency for local water mediated P±OH to P@O proton delocalization, which is seen already when employing a single H2 O g as bridge, is typical for Brùnsted acids. This type of local proton delocalization is most pronounced in the strong acids H2 SO4 g and HClO4 g, and is treated further in the same context [4]. J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 Allowing a second water molecule to bridge between two P±OH groups, and forming the PO OH3 2H2 O g complex depicted in Fig. 3(i), is found to release an additional 39 kJ/mol (M). However, an even more stable structure is achieved by the formation of a water dimer ligand. This is consistent with what was observed for the Si system, and the dimer complex (Fig. 3(j)) is an additional 10 kJ/mol (M) lower, thus resulting in a net 49 kJ/mol (M) exothermicity for the addition of the second water molecule. Here, it is gratifying to note the signi®cant shortenings of the O H bond distances and how these are accompanied by the corresponding elongations of the O±H bond distances (see Table 3). Finally, some representatives for the addition of a third water ligand to PO OH3 g are included in 63 the discussion. The PO OH3 3H2 O g complex in Fig. 3(k) preserves the C3 symmetry of the parent molecule by using each water ligands to bridge between the P@O group and one P±OH unit. However, water monomers are not optimal ligands. Equally stable to the structure in Fig. 3(k) is the complex in Fig. 3(l), which has the same con®guration of H bonds between the core molecule and ligands as does SO2 OH3 3H2 O g complexes that display deprotonation [4]. Using the (S) basis set, proton transfer is indeed observed for this structure. However, at the improved and more reliable (M) level the PO±H bond distance but stays atbecomes rather elongated (1.04 A), tached to the PO OH3 kernel. The energy release on binding the third water is only 27 kJ/mol (M), which indicates that this position represents a Fig. 4. Structures in the P2 O5 3H2 O system: P2 O5 : (a) OPO3 PO D3h , (b) O2 POPO2 C2 ; P2 O6 H2 : (c) 2 PO2 OH Cs , (d) O2 POPO OH2 C1 , (e) HOOPO2 PO OH C2v , (f) HOOPO2 PO OH C2h ; P2 O7 H4 :(g) HO2 OPOPO OH2 C2 , (h) C1 , (i) C2 and (j) C1 ; P2 O8 H6 : (k) 2 PO OH3 C3 and (l) HO2 OPOPO OH2 H2 O C1 together with relative stabilities and energetics for some hydrolysis reactions. 64 J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 sub-optimal site in PO OH3 2H2 O g. The global energy minimum for PO OH3 3H2 O g is shown in Fig. 3(m), and it contains one water dimer and one monomer as ligands, each bridging between the P@O and one P±OH group. This structure is 14 kJ/mol (M) below the complex in Fig. 3(l), an eect that is caused by the favorable combination of two water bridges to P@O in conjunction with a H2 O2 ligand. The fact that all PO OH3 3H2 O g complexes do not form ion pairs suggests that PO OH3 is a weaker acid than SO2 OH2 , even in the nano-scale clusters. 3.4. P2 O5 g nH2 O There are two important structures for P2 O5 g of which the least stable is a triple-bridged O@PfO3 gP@O cluster of D3h symmetry (Fig. 4(a)). The molecule is structurally related to similar molecules with three oxygen bridges that have been determined for the Sc, Ti, V, Al, Si and Ge systems [3,6,10]. In the majority of cases, this structure lies somewhat above the global energy minimum, as is also the case for P2 O5 g. Hence, the single-bridged O2 POPO2 molecule (Fig. 4(b)) is 97 kJ/mol (M) more stable than the D3h cluster. Interestingly, this ordering is opposite to what was found for V2 O5 g. Repeatedly, the origin of this dierence is most likely found in the greater capacity of the early 3d elements, as compared to 3p, to accommodate electron rich ligands. Hydrolytic cleavage of the P2 O5 chain, with its rather open P±O±P bond angle (134°), can be employed to model the general cleavage of such single bridges, as was done in case of the oxygen bridged binuclear transition metal oxyhydroxides [10]. Here, hydrolysis results in the formation of two of metaphosphoric acid molecules, PO2 OH g (Fig. 4(c)), and the reaction is exothermic by 48 kJ/mol (M). This comparatively large value is caused by the general instability of the two P@O groups in each metaphosphate unit Fig. 5. Structures related to P2 O5 2 : (a) P4 g Td , (b) P4 O6 g Td and P4 O10 g Td together with the energetics for oxidation processes, dimerization of P2 O5 g and hydrolysis of P4 O10 g. J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 toward reaction, which result in elongated P±O bonds in the P±O±P bridge. Indeed, molecular P2 O5 g is generally known to dimerize, forming P4 O10 g (Fig. 5(c)) with Td symmetry [1]. This molecule has a P4 O6 core (i.e., the P(III) oxide shown in Fig. 5(b), which also has Td symmetry), in which each P atom has three P±O bonds, completed by one P@O on each P. This dimerization reaction reduces the number of P@O groups, and is consequently highly exothermic (491 kJ/mol (M) and 536 kJ/mol (L)). However, the P4 O10 g molecule contains six P±O±P bridges that can be hydrolyzed. This results in the formation of four PO OH3 g molecules, a process that is associated with rather small reaction energies. Due to the repulsion between the individual P units in the P4 O10 g cluster, does the reaction though come out quite exothermic (215 kJ/mol (M) and 244 kJ/ mol (L)). From the fact that P4 O10 g does not represent a ®nal product of hydrolysis, it can be concluded that a discussion concerning binuclear clusters is just as informative on hydrolysis. The P4 O10 g molecule still serves as a good test on the quality of the computational results. A comparison with experimental data shows very close agreement with results obtained using the large (L) (M) and 1.43 A (L) vs. 1.43 basis set (P@O: 1.45 A exp.; P±O: 1.63 A (M) and 1.61 A (L) vs. 1.60 A A exp.; P±O±P: 125° (M) and 124° (L) vs. 123° exp.) [28]. Similar agreement is also found for the P4 O6 g molecule, as well as for the P4 g molecule (Fig. 5(a)). By looking at the energetics for the oxidation P4 g and P4 O6 g, the stability of the P(V) oxides becomes apparent (cf. Fig. 5). As a consequence of the reactivity of the P@O groups, the energetically favored alternative to dissociative water addition comprises reaction with one of the P@O bonds. This process is exothermic by 186 kJ/mol (M) for formation of the chain structure O2 P±O±PO OH2 (Fig. 4(d)). The central P±O±P bond angle (131°) is quite insensitive to this addition, but the two P±O bond distances are aected in an unsymmetrical fashion as an intramolecular H bond is (1.59 and 1.69 A), formed (O H: 2.00 A). Despite the extra stabilization, clusters based on hydrated P2 O2 rings are more stable than the hydrated chains. There exists two isomers for the 65 HOOPO2 PO OH cluster. The C2v structure (Fig. 4(e)) is 42 kJ/mol (M) more stable than the chain, and it can be viewed as the product of water addition to one of the P±O±P bridges in OPO3 PO g. The latter reaction comes out exothermic by 131 kJ/mol (M). The C2h structure (Fig. 4(f)), which displays inverted ligand arrangements on the P atoms, is found to be 1 kJ/mol (M) more stable than the C2v cluster. Dimerization of two PO2 OH g molecules, forming the P2 O6 H2 g structure in Fig. 4(f), is exothermic by 181 kJ/mol (M), which repeatedly re¯ects the instability of the P@O units in metaphosphoric acid. Addition of a second water molecule yields the pyrophosphoric acid, P2 O7 H4 . Similar to the silica system, this species is of great importance. In this case it is due to the fact that it is the primary condensation product of orthophosphoric acid. This reaction has been the topic of several studies during recent years [29±31]. However, all investigations so far have failed to describe the full structural complexity of the pyrophosphoric acid system. In the present work, we ®nd four unique energy minima, which dier in the orientations of the OH groups with respect to the P±O±P bridges. All structures dier in the P±O±P bond angles, and their reactivity towards hydrolysis dier. The least stable structure (Fig. 4(g)) displays one P±OH OH±P alignment and no symmetry ele is too ments. The H O bond distance (2.30 A) long for it to be classi®ed as a hydrogen bond. The structure is quite similar to the symmetry broken form of Si2 O7 H2 g, and the P±O±P bond angle is consequently quite open (139°). 2 kJ/mol (M) is gained if another pair of P±OH groups are allowed to interact. This gives the structure (Fig. 4(h)) C2 symmetry with two long hydrogen bonds (2.06 A). The P±O±P bridge is slightly more acute (133°), due to the changed bonding. Again, the structure has similarity to the Si2 O7 H2 g system, and more precisely its symmetric form. If the ligands on one P atom are rotated so that an P±OH O@P bridge is allowed to form, then an additional 14 kJ/ mol (M) is gained. In this structure (Fig. 4(i)), a is formed, while proper hydrogen bond (1.95 A) negligible interaction remains between the pair of As a result, the P±OH groups (O H: 2.38 A). P±O±P bond angle becomes somewhat more bent 66 J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 (125°). The unsymmetrical arrangement of the ligands with respect to the bridge gives the structure no overall symmetry. An additional 5 kJ/mol (M) is gained if two P±OH O@P bridges are formed (Fig. 4(j)). The two hydrogen bonds come out ra despite the fact that the P±O±P ther long (2.16 A), bond angle is reduced even further (117°). Thus, the bond angle is close to the previously reported range of values (113±119°) [30,31]. In contrast to the present study, signi®cantly longer hydrogen were found in these bond distances (2.28±2.39 A) investigations. Formation of the fourth and most stable HO2 OPOPO OH2 structure in Fig. 4(j) from the P2 O6 H2 g cluster in Fig. 4(f) is exothermic by 132 kJ/mol (M). It is noted that continued polymerization of this P2 O7 H4 g structure through condensation of the terminal P±OH groups is straight-forward, as there is one such non-hydrogen bonded group available on each P atom. Naturally, polymerization can occur starting from any of the four structures, but these processes are expected to result in lower stability for those polymers. A main ®nding of this investigation comprises the window of energies associated with the hydrolysis reaction for the four isomers (Figs. 4(g)± (j)). While hydrolysis of the P±O±P bridge comes out exothermic by 15 kJ/mol (M) in case of the ®rst P2 O7 H4 structure (Fig. 4(g)), the reaction turns endothermic by 7 kJ/mol (M) when considering the most stable binuclear isomer (Fig. 4(j)). This span in energy values re¯ects the values previously published in the literature, as obtained using a variety of methods and basis sets. One straightforward conclusion, which can be drawn from this observation, is that the relative stability of pyrophosphate molecule as compared to the mononuclear H3 PO4 molecules entirely determined by the amount of water available. The ®nding that the condensation±hydrolysis processes are determined by the reaction conditions on a nanometer length scale is not unique to the phosphorous system, but was also found for several transition metal systems [6]. Indeed, the energetics for the water chemistry of the phosphate system is not very dierent from the silica system, although the latter system displayed a somewhat higher endothermicity upon hydrolysis of the corresponding Si±O±Si bridge. In contrast, it is noted in bypass that hydrolytic cleavage of the oxygen bridge in disulfuric acid was found to be exothermic [4]. Finally, all four isomers of pyrophosphoric acid have enantiomeric forms, and are consequently optically active. The possible importance of the handedness of phosphoric acid chemistry to biochemistry remains to elucidate. 4. Conclusions The water chemistry of the mononuclear species SiO2 g and PO2 OH g, as well as the binuclear systems Si2 O4 g and P2 O5 g, has been investigated. The stabilities and reactivities of Si@O and P@O groups, as well as Si±O±Si and P±O±P bridges toward hydrolysis were studied. Systematic investigation of structures and stabilities of hydrolysis products was performed by means of a consecutive addition of molecular water, starting with anhydrous forms the binuclear compounds, and ending up with the corresponding mononuclear hydroxides. The formal oxidation states +IV and +V were maintained throughout this study, as neither the Si nor the P systems were found prone to reduction by water. The most stable monomeric products were concluded to be the four-coordinate Si OH4 g and PO OH3 g molecules or hydrated forms of these. Higher coordination numbers were also studied, as these could be of fundamental importance as reaction intermediates in e.g., phosphorylation processes. In particular P OH5 g, which has a trigonal bipyramid structure, was found to be 42 kJ/mol (M) above the H3 PO4 g H2 O g asymptote. Again, local conditions are expected to in¯uence these relative stabilities signi®cantly. Particularly stable compounds of Si OH4 g and OP OH3 g with water is obtained for water dimer ligands. Interestingly, a tendency toward intramolecular proton delocalization could be noted for PO OH3 if the ligand bridges between the P±OH and P@O groups. This tendency for delocalization is hardly seen for the H2 O2 bridging between two Si±OH. The use of a trimer water ligand increased the degree of proton J.R.T. Johnson, I. Panas / Chemical Physics 276 (2002) 45±68 transfer in the PO OH3 system, although complete deprotonation did not occur. A much smaller eect was noted for the Si OH4 system. This difference between the Si and P systems is taken to relate to the relative micro-acidity of the two core compounds. It is implied that this drive for water mediated intramolecular proton delocalization occurs according to a common mechanism for the acids H3 PO4 , H2 SO4 , and HClO4 . The cause for this is an eort to reduce the potential dierence between the acidic M±OH and the electron rich M@O groups. By using this functionality, the phosphates can provide nano-scale buering systems, and thus allow for an ecient control of proton activity. The structures of the binuclear systems HO3 Si±O±Si OH3 g and HO2 OP±O±PO OH2 g were addressed in detail, and the ordering of isomer stabilities were discussed based on intramolecular interactions. Both systems were global minima along the water addition reaction coordinate. Thus cleavage of the oxygen bridges through hydrolysis were found to be endothermic for both systems, and reversely the condensation of two Si OH4 g or PO OH3 g exothermic. The P±O±P bridge displayed close to 17 kJ/mol lower stability toward hydrolysis than the Si±O±Si bridge, which renders the former near zero reactivity. The understanding that the P±O±P bridge in the biphosphates does not display particular exothermicity upon hydrolysis has been around for several years in the context of biosynthetic chemistry [30]. This is further emphasized here as gas phase hydrolysis of the four most stable isomers of OH2 OP±O±PO OH2 were found to display energetics that vary in the range )14 to +7 kJ/mol. This indeed implies that water activity and the relative hygroscopicity of reactants versus products comprise decisive factors for the equilibrium concentrations of the two. Thus, extreme constraints must be imposed on the nano-scale reaction conditions for hydrolysis of the P±O±P bridges in ATP, if these bridges were to be the ``energy currency'' of the cell. Having said this, one possible function of the ATP hydrolysis mechanism, which would be consistent with the above ®ndings, is the precise control of local water ac- 67 tivity e.g., in the vicinity of an active site in an enzyme. Indeed, condensation reactions are central in biosynthetic processes, and the removal of the released water must be considered vital to the function of the enzyme. In conclusion, the results of the present study cannot be employed to support the simplistic understanding of the P±O±P bridge in ATP as a carrier of an exact energy quantum for release at a particular reactive site. More profoundly, quantum chemical calculations suggest the pyrophosphate and phosphate pairs to be decisive in providing a nano-scale buer for both water and proton activity. Indeed, it is strongly suggested that consumption of ATP during biosynthesis re¯ects precisely this micro-buering function, and that this role of ATP and its hydrolysis products can be translated into a Gibbs free energy equivalent. Acknowledgements This work was supported by the Swedish Natural Sciences Research Council (NFR). The National Supercomputer Center (NSC) in Link oping is acknowledged for allotment of computer time. References [1] N.N. Greenwood, A. Earnshaw, Chemistry of the Elements, second ed., Butterworth-Heinemann, Oxford, 1997. [2] Van Holde, Biochemistry, second ed., ButterworthHeinemann, Oxford, 1997. [3] J.R.T. Johnson, I. Panas, Phys. Chem. Chem. Phys., in press. [4] J.R.T. Johnson, I. Panas, J. Phys. Chem. A, in press. [5] J.R.T. Johnson, I. Panas, Inorg. Chem. 39 (2000) 3181. [6] J.R.T. Johnson, I. Panas, Inorg. Chem. 39 (2000) 3192. [7] A.D. Becke, J. Chem. Phys. 98 (1993) 5648. [8] J.R.T. Johnson, I. Panas, Chem. Phys. 248 (1999) 161. [9] C.W. 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