MOLECULAR PHYSICS, 20 May 2003, VOL. 101, NO. 10, 1501–1510 Solvation properties of Li+ and Cl in water: molecular dynamics simulation with a non-rigid model ZHENHAO DUAN1,2* and ZHIGANG ZHANG1 1 Chinese Academy of Sciences, Institute of Geology and Geophysics, Beijing 100029, China 2 Department of Chemistry, 0340, University of California, San Diego, La Jolla, CA 92129, USA (Received 18 December 2002; revised version accepted 5 February 2003) Molecular dynamics (MD) simulations were carried out to investigate the solvation properties of Li+ and Cl ions in water with a relatively accurate but rarely used non-rigid model, RWK2, in this study. A new set of ion–water interaction parameters was evaluated from the experimental data and first principles calculation results of stable clusters, Li+(H2O)n (n ¼ 1–6) and Cl(H2O)n (n ¼ 1–4). With the ion–water potential parameters evaluated from the data of the clusters and the water–water potential predetermined from the non-rigid RWK2 model, the structural (radial distribution functions, angular distribution functions, spatial distribution functions, coordination number), dynamical (residence time) and energetic properties of the ionic solvations in bulk water were studied through a comprehensive analysis of our MD simulation outputs. These results not only agree well with experimental data and first principles calculations, but also reveal some new insights into the microscopic ionic solvation processes. 1. Introduction Ionic solvation is a fundamental property of aqueous electrolyte solutions associated with biological and chemical processes. The knowledge of ionic solvation structure, the dynamics of water molecules around ions and the interaction energy of ions with water are of great importance for the deep understanding of microscopic mechanisms such as DNA stability [1] and the speciation of ore-forming elements in hydrothermal processes [2]. There are generally three approaches to the study of ion solvations: experimental measurements, first principles molecular dynamics simulation and classical molecular dynamics simulation. Extensive experimental work (such as X-ray and neutron diffraction) has been carried out to derive the ionic solvation structure, the energy and the coordination number of water molecules around ions over the past 30 years. These works were comprehensively reviewed in [3]. However, experimental techniques often yield an incomplete description of ionic solvation or hydrogen bonding [4] because of such difficulties as the lack of suitable isotope substitutions in neutron diffraction, or the difficulties in separating the atomic correlations of different species in diffraction tests. Usually experiments are carried out in such high *Author for correspondence. e-mail: duanzhenhao@yahoo. com concentration solutions that ion–ion interactions may significantly alter the solvation structure [5]. Thus the solvation mechanism of ions in dilute systems must be an approximate extrapolation from concentrated solution measurements. Recently first principles (FP) molecular dynamics (MD) calculations have played an important role in the study of microscopic properties [5–9]. These simulations have led to a much better understanding of the solvation mechanism. However, FP calculations are about 4000 times slower than the classical MD simulation. This prevents many researchers from studying relatively large systems. Most researchers still use a system size of less than 100 water molecules with a less than 5 ps period of molecular motions. Such a small system size may be too small to reproduce meaningful properties in bulk. A few picoseconds of molecular motion time may be insufficient for collecting dynamic data under the equilibrium state. For example, the residence time of water molecules around an ion can be several dozens of picoseconds or longer; a time of a few picoseconds is obviously too short to study the residence time and the equilibrium process between the ion and the water molecules. In addition, it is usually hard to estimate the quantitative accuracy in the structural and thermodynamic properties calculated by FP calculations. In many cases, the classical simulation can reproduce experimental data with an accuracy not much different from FP Molecular Physics ISSN 0026–8976 print/ISSN 1362–3028 online # 2003 Taylor & Francis Ltd http://www.tandf.co.uk/journals DOI: 10.1080/0026897031000099907 1502 Z. Duan and Z. Zhang calculations as long as the interaction potential is well parameterized. Therefore, the simulations based on the pairwise additive potentials are still justified. In this study, we carry out MD simulations to investigate the solvation properties of Li+ and Cl ions in bulk water with a non-rigid model for water– water interactions and an ion–water interaction model evaluated from the data of ion–water clusters. In the past, researchers employed rigid water molecule models to simulate various bulk properties. However, some results [10, 11] indicate that intramolecular forces markedly modified the liquid structure and the liquid– vapour equilibrium and that flexible potentials yield better predictions. The non-rigid water potential model RWK2 (Reiners, Watts and Klein, 1982) yields remarkably good predictions of steam, liquid water and ice, and liquid–vapour phase equilibria but receives much less attention [11]. Through this study, we should like to find the Li+ and Cl solvation structure, the coordination number of water molecules around the ions, the solvation energy and the solvation dynamics at different temperatures and pressures. We present this article as follows. The predetermined water–water potential RWK2 and the evaluation of the ion–water potential will be introduced in Section 2. With the interaction potentials determined, the ion solvation properties in water clusters are investigated, as reported in Section 3. The ion solvation properties in bulk water predicted by MD simulation are discussed in Section 4. Finally, conclusions are drawn in Section 5. 2. Interaction potential The interaction potential plays a crucial role in the results of MD simulations. There are three kinds of interaction in the water–salt binary solutions: water– water, water–ion and ion–ion interactions. Since our objective in this study is to find the single-ion solvation behaviour, the ion–ion interactions can be ignored here. Over the past two decades, more than 30 water potential models have been proposed to simulate water properties. They can be approximately classified into three categories [12]: pairwise two-body additive rigid models (e.g. SPC/E [13, 14], TIP4P [15], ST2 [16]), pairwise additive non-rigid models (e.g. RWK2 [17]), and models which explicitly include the effects of polarization and many-body effects. Although the polarization models are theoretically sound, they have in general not led to more accurate predictions than the two-body potentials in the prediction of such important properties as liquid–vapour phase equilibria [11]. The rigid twobody potentials have found wide use in the study of microscopic liquid structure and thermodynamic properties. However, some research results suggest that flexible models, which allow intramolecular motions, are Table 1. Interaction Li+–H2O Cl–H2O Parameters for the water–ion interaction. "IW (kJ mol 1) 0.3108 0.5187 IW (Å) 2.72 3.635 superior in the prediction of mean force potential and vapour–liquid equilibria [10, 11]. Therefore, we choose RWK2, which predicts gas, liquid and ice properties with remarkable accuracy for the water–water interactions in this study. The RWK2 potential function and its parameters can be found in the appendix of [18]. The ion–water interaction can be modelled in two parts: uIW ¼ uCoulomb þ uShort IW IW , ð1Þ where I denotes an ion, W stands for a water molecule, uCoulomb represents the Coulombic interaction and uShort IW IW is the short-range interaction. In the Coulombic interaction, the partial charges for oxygen and hydrogen atoms are: 2qH ¼ qO ¼ 1.2, which are consistent with the RWK2 model. The pairwise potential function for the short-range interaction is modelled as the Lennard-Jones (LJ) form: " 12 6 # IW IW LJ uShort , ð2Þ IW ¼ uIW ðrIW Þ ¼ 4"IW rIW rIW where rIW is the distance between the centre of the ion and the partial negative charge of the water molecule (its position can be found on the bisector of the HOH angle, see the appendix of [18]); "IW and IW are the energy and size parameters, respectively. Using a trial and reducing error procedure, the parameters (table 1) for the Li+–H2O and Cl–H2O interaction potentials are best obtained by reproducing the binding energy of one ion associated with two- or three-water-molecule clusters, since the multi-body interactions need to be taken into account for the study of bulk properties. 3. The solvation properties of clusters The minimum energy structures of the clusters Li+(H2O)n (n ¼ 1–6) and Cl(H2O)n (n ¼ 1–4), were obtained from MD simulated annealing and the steepest descent method [12]. The initial configuration was generally taken from a previous simulation. The system was annealed gradually with a scaling factor (Ti+1/Ti ¼ 0.90). When the temperature reached a few kelvins, we quenched the systems to 0 K with the steepest descent method and obtained the minimum Solvation properties of Li+ and Cl in water energy structures. It is found from our simulation that different initial configurations may generate several stable isomers with little energy differences. These isomers are all possible minimum energy structures occurring in the real physical world and each contributes to the probability distribution of the cluster according to its Boltzmann factor [19]. The enthalpy (H ) of the formation of a cluster at a specific temperature T can be calculated from: H ¼ U þ pV ¼ Ucluster Uintra nRT, ð3Þ where Ucluster is the internal energy of the cluster, n is the number of water molecules and R is the ideal gas constant. Uintra is the intramolecular energy of water molecules and is always a very small variable with a magnitude of 104 kJ mol1 in the minimum energy structure (in the rigid model, it is actually equal to zero), so it can be ignored in the calculations. -20 Energy (kcal/mol) -40 -60 -80 -100 Simulated Exp. -120 -140 0 1 2 3 4 5 6 7 Number of water molecules Figure 1. Simulated enthalpies of Li+(H2O)n and corresponding experimental data [20] (1 kcal ¼ 4.18 kJ). Table 2. 1503 3.1. Li+–(H2O)n Figure 1 and table 2 show the simulated enthalpies and structures of stable Li+(H2O)n (n ¼ 1–6) clusters. In general, our simulated results agree well with the experimental data [20] with deviations of less than 5%, except for the one-water cluster, Li+(H2O), with a deviation of 15%. We could fit the potential parameters to the one-water cluster data with an error of less than 5%. However, our objective is to find the ion solvation properties in the bulk water, where more than one water molecule surrounds the ion, and thus we fit the effective pair potential to the multi-water cluster data. The simulated distances between Li+ and oxygen in different clusters, rLi–O, vary from 1.84 to 1.92 Å (table 2), except for the long distance of rLi–O in Li+(H2O)5 or Li+(H2O)6. These results are consistent with the results of quantum calculations [9]. The stable minimum energy structures of Li+(H2O)n clusters are displayed in table 2. Li+(H2O)2 is linear, Li+(H2O)3 is triangular planar, Li+(H2O)4 is a tetrahedron, Li+(H2O)5 is a trigonal bipyramid, and Li+(H2O)6 is an octahedron. These structures are consistent with the results of prior workers [19] and quantum mechanical calculations [9]. 3.2. Cl(H2O)n Table 3 shows the possible stable structures for Cl(H2O)n (n ¼ 1–4) clusters. It can be seen that multiwater clusters, Cl (H2O)n (n > 2), generally have two isomers: a symmetric ion-centred structure and an asymmetric pyramidal structure. The symmetric ioncentred structures always have slightly higher energies than the corresponding asymmetric pyramidal structures. These calculated energies are very close to the experimental results [20]. The ion–oxygen distances, rCl–O, for different clusters are also listed in table 3, showing the close agreement with the quantum simulation results [9]. Structures and energies of Li+(H2O)n. (a) n ¼ 1 (b) n ¼ 2 (c) n ¼ 3 (d) n ¼ 4 (e) n ¼ 5 (f ) n ¼ 6 120.8 142.2 1.84 1.86 235.5 250.1 1.84 1.87 339.7 336.7 1.87 1.90 426.7 405.3 1.91 1.94 485.6 463.5 1.92, 3.60 2.02 542.5 514.1 1.92, 3.63 2.08 Geometry Enthalpy (kJ mol 1) rLi–O (Å) Simulated Exp. [20] Simulated FP [9] 1504 Z. Duan and Z. Zhang Table 3. Structures and energies of Cl (H2O)n. (b) n ¼ 2 (c) n ¼ 3 (d) n ¼ 4 (a) n ¼ 1 I II I II I II 51.9 54.8 3.24 3.30 108.3 107.9 3.24, 3.42 — 102.1 107.9 3.24 3.31 171.5 156.9 3.39 — 150.6 — 3.25 3.34 236.3 203.3 3.25, 3.44 — 210.4 203.3 3.23, 3.39, 4.08 3.37 Geometry Enthalpy (kJ mol 1) rCl–O (Å) Simulated Exp. [20] Simulated FP [9] I, pyramidal structure; II, symmetric ion-centred structure. Compared with Li+(H2O)n, Cl(H2O)n clusters are preferable to the asymmetric pyramidal structures. According to the analysis in [19], the discrimination between the ion-centred structure and the pyramidal structure is directly related to the size of the ion. Smaller ions tend to have stronger interactions with water molecules and cause more distortions on the water clusters. Therefore, a larger ion can accommodate the pyramidal configuration more easily than a small ion [19]. 4. The solvation properties of ions in bulk aqueous solutions With the interaction potentials determined above, the solvation properties of Li+ and Cl in bulk water were studied by canonical ensemble MD simulations. The simulations were carried out at 298 K and 573 K, respectively. A total of 230 water molecules and a single ion are used in the cubic simulation box with a length of 19.03 Å, which is equivalent to a volume of 18.0 cm3mol1. Another simulation was performed at 573 K and 22.0 cm3 mol1 for the study of pressure impact on the solvation structure. The conventional periodic boundary conditions and minimum image conventions [21] were used in the simulations to treat out-of-box atoms and to calculate interatom distances. Long-range electrostatic forces and energies were calculated with the Ewald sum. In all runs, the time step was set as 31.25 au or 0.75 fs. Initial configurations were selected from the final configurations of previous simulations. Each simulation began with 10 000 step pre-equilibrium runs followed by 40 000 subsequent steps for data collection. However, for the study of the residence time of water molecules around ions, a run of 400 000 steps is carried out for the data collection. We did not notice an observable difference for the solvation structure derived between the run of 40 000 steps and the run of 400 000 steps. The trajectories of the particles were calculated using the Verlet algorithm [21] and the intermediate configurations were saved at certain intervals. Through the analysis of the trajectory configurations as a function of time, the solvation structures, the coordination number of water molecules around ions, the solvation energy and the dynamics are investigated. 4.1. Radial distribution functions and the coordination number in the ionic solvation shell Li–oxygen and Li–hydrogen radial distribution functions (rdfs) from our simulations and those from the FP molecular simulations [7] are shown in figure 2. It is remarkable that our results are in excellent agreement with the corresponding FP calculation results. Two prominent maxima can be found in the Li–oxygen rdf, indicating that two solvation shells exist. The first maximum is especially sharp, suggesting that the first hydration shell is well established in the vicinity of the lithium ion. The clearly delineated peaks in the Cl–O and Cl–H radial distribution functions (figure 3) indicate hydrogen bonding to the chlorine ion, as was found also by Hanke et al. [22]. Table 4 lists the structural properties of the first solvation shell from this study and compares them with the corresponding results from some previously reported simulations and experiments. Three parameters are used to describe the characteristics of the first ionic hydration shell: RIO, RIH and the coordination number. RIO is the position of the first maximum in the ion–oxygen rdf and RIH is the corresponding position in the ion–hydrogen rdf. These two parameters calculated by our program agree well with the experimental data [26–28]. Furthermore, our results are in good agreement with the most recent quantum mechanical calculations and experimental data [7, 29]. As for the coordination number, various simulations have produced a range of results from four to six for the lithium ion and from Solvation properties of Li+ and Cl in water Table 4. 12 g(r) 8 6 4 2 0 1 2 3 4 5 6 r(A) Figure 2. Radial distribution functions of Li–O and Li–H from our simulations and those from the FP simulations [7] at 298 K. 5 Cl-O Cl-H 4 Structural properties of the first solvation shell. Li+ Cl RIO (Å) This work Chandrasekhar et al. [23] Heinzinger [24] Mezei and Beveridge [25] X-ray [26] Neutron diffractiona 1.93 1.95 2.13 2.10 1.95–2.25 1.95 3.25 3.21 3.22 3.25 3.10–3.35 3.20–3.34 RIH (Å) This work Chandrasekhar et al. [23] Heinzinger [24] Mezei and Beveridge [25] Neutron diffractiona 2.62 2.60 2.68 2.70 2.55 2.25 2.25 2.24 2.25 2.22–2.26 Coordination number This workb Chandrasekhar et al. [23]b Heinzinger [24] Mezei and Beveridge [25] X-ray [26] Neutron diffractiona 4.6 (9.2) 4.9 (10.6) 6.1 5.97 4–6 5.5 7.2 (7.4) 7.4 (7.0) 8.2 8.36 5–11 5.3–6.2 Source Li-O: This work Li-O: FP results Li-H: This work Li-H: FP results 10 1505 a Reference [27] for lithium and reference [28] for chloride. On the basis of ion–oxygen rdfs; values for ion–hydrogen rdfs in parentheses. b g(r) 3 2 1 0 0 1 2 3 4 5 6 7 8 9 r(A) Figure 3. Radial distribution functions of Cl–O and Cl–H at 298 K. seven to eleven for the chlorine ion [23–25, 30, 31]. There also exists a discrepancy between different experiments with different methods of measurement and different definitions [32]. In this study the coordination number is calculated with the most commonly used definition: Z rmin h ¼ 4p0 gðrÞr2 dr, ð4Þ 0 where g(r) is the rdf of ion–oxygen or ion–hydrogen, 0 is the density of water molecules and rmin is the first minimum position (after the first peak) of the rdf. Two sets of coordination numbers are reported in table 4 on the basis of the ion–oxygen rdf as well as the ion–hydrogen rdf (in the parentheses). These coordination numbers compare favourably with experiments [26–28, 33]. They are also consistent with the MD simulation results based on non-additive potentials [34], polarizable model [35] and quasi-chemical organization of solution theory [36]. It can be seen from figures 4 and 5 that temperature has a striking impact on the ion–oxygen rdf. As the temperature increases, the first peak decreases significantly but accompanies a broadened width. At the same time, the intensity of the first minimum increases and the second peak almost vanishes to the average bulk distributions at high temperatures. These features indicate that the hydration shell around ions becomes less prominent when the temperature increases, as displayed by figures 4 and 5. However, the coordination number is almost unchanged. This is consistent with the simulation results of [37] that suggest very little temperature effect on the hydration number in the Na+ solvation shell. The impact of pressure on the solvation structures is found to be small as shown in figures 6 and 7, which compare the ion–oxygen rdfs under different pressures (corresponding to two different volumes and pressures: 18.0 cm3 mol1 (4966 bar) and 22.0 cm3 mol1(714 bar)). In these two figures, the curves of rdf remain almost unchanged for different pressures except for a small difference in the intensities of the first peaks. In fact, the calculated coordination number (using equation (4)) remains the same when the 1506 Z. Duan and Z. Zhang 12 573K 298K 10 n(r) 30 4.0 25 3.5 3.0 20 6 15 4 10 2.5 g(r) g(r) n(r) 8 g(r) 18 cm3/mol 22 cm3/mol 2.0 1.5 2 0 0 1 2 3 4 5 6 7 8 5 1.0 0 0.5 9 r(A) Figure 4. 0.0 Li–O radial distribution function and coordination number at 298 K and 573 K. 0 1 2 3 4 5 6 7 8 9 r (A) Figure 7. The Cl–O radial distribution functions at two different volumes (18 cm3 mol1 and 22 cm3 mol1). 5 50 573K 298K 4 pressure increases (equivalent to the decreasing of the volume). 40 n(r) n(r) 30 g(r) 3 g(r) 2 20 1 10 0 0 0 1 2 3 4 5 6 7 8 9 r(A) Figure 5. Cl–O radial distribution function and coordination number at 298 K and 573 K. 10 18 cm3/mol 22 cm3/mol 8 g(r) 6 4 2 0 0 1 2 3 4 5 6 7 8 9 r(A) Figure 6. The Li–O radial distribution functions at two different volumes (18 cm3 mol1 and 22 cm3 mol1). 4.2. Angular structural properties in the ionic hydration shell Although the widely used radial distribution function can provide useful insights into solvation structures, it only reveals the two-body structural information and the important properties involving orientations and angular distributions may be lost by averaging. A straightforward way to get more detailed structural information of the ionic hydration shell is through the study of the probability distributions of some angular properties. These distributions reveal the rigorous probability densities over the entire angular range. As an example, figure 8 shows two kinds of angular distributions in the first hydration shell of the lithium ion. It can be seen that there are two maxima in the O–Li–O angle distribution: the first is centred around 105 with a fluctuation of about 30 and the second around 170 with a smaller fluctuation of about 10 . The distribution of the dipole–ion angle, which is defined as the angle between the HOH bisector and the direction from oxygen to ion (as illustrated in figure 8), indicates that the lithium ion lies around 160–165 away from the HOH bisector with the most probability. In order to present a more vivid image of the spatial distribution of the hydration shell, we used a convenient routine, the spatial distribution function (sdf ), which is a three-dimensional function with a definition mentioned in [38]. This function can be visualized into impressive graphics by some well-established software such as the gOpenMol package [38, 39]. Figure 9 shows the sdf of the lithium ion relative to a water molecule in the first hydration shell. The origin of the local Solvation properties of Li+ and Cl in water 1507 0.07 0.06 O-Li-O angle Dipole-ion angle Distribution 0.05 0.04 + O Li H 0.03 Dip H ole -io n 0.02 an gle 0.01 0.00 0 20 40 60 80 100 120 140 160 180 Angle Figure 10. Spatial distribution of water molecules relative to the Li+ ion in the first hydration shell. A coordinate system is introduced where the ion defines the origin, one oxygen of the hydration shell water molecules defines the z-axis, and a second such oxygen defines the xz-plane. Figure 8. Distribution of the O–Li–O angle and the dipole– ion angle of Li–water in the first hydration shell at 298 K. 0.08 O-Cl-O Angle Dipole-ion Angle 0.07 - Cl H 0.05 O H Di n -io le po gle an Distribution 0.06 0.04 0.03 0.02 0.01 þ Figure 9. Spatial distribution of the Li ion relative to a water molecule in the first hydration shell. The origin of the local coordinate system lies on the centre of the oxygen atom, the HOH bisector defines the x-axis and the water molecule plane defines the xz-plane. coordinate system lies on the centre of the oxygen atom, the HOH bisector defines the x-axis and the water molecule plane defines the xz-plane. In this figure, dark shading indicates high intensity of the sdf and grey corresponds to lower intensity. It can be found that the maximum of the lithium ion distribution lies approximately on the plane perpendicular to the water molecule plane. Figure 10 shows the sdf of water molecules in the first hydration shell relative to the Li+ ion. This figure provides a more impressive image of the strucuture of the first hydration shell of the lithium ion. Here is introduced a coordinate system where the ion defines the origin, one of the oxygens in the hydration shell defines the z-axis, and a second oxygen the xz-plane. The two water molecules defining the frame are plotted as two oxygen atoms in this figure. We can easily find that four water molecules in the first hydration shell of the lithium ion lie around the vertices of a distorted tetrahedron, which corresponds to the first peak of the O–Li–O distribution in figure 8. In addition, we can also find 0.00 0 20 40 60 80 100 120 140 160 180 Angle Figure 11. Distribution of the O–Cl–O angle and the dipole– ion angle of Cl–water in the first hydration shell at 298 K. another two smaller areas almost opposite the two axis oxygen atoms and obviously these areas constitute the second peak of the O–Li–O distribution in figure 8. It can be noticed in figure 8 that the intensity of the second peak is far smaller than that of the first peak, indicating that these areas can be visited by water molecules with lower probabilities or shorter residence times. This will be further demonstrated in the following analysis on the dynamical residence time of water molecules. Similar analysis is made on the hydration shell of the Cl ion. Figure 11 shows the O–Cl–O angle and the dipole–ion angle distributions. Compared with the lithium ion, the hydration shell in the vicinity of the chlorine ion is not so well featured, which is revealed by the relatively flat distribution of the O–Cl–O angle. However, a well-defined peak at around 60 can be found in the dipole–ion angle distribution. This can be interpreted from figure 12, which indicates that the chlorine ion prefers positions approximately in the 1508 Z. Duan and Z. Zhang Table 5. Average number of acceptors and donators of hydrogen bonds per water molecule with different distances from the ions (298 K). Li+ Distance (Å) Figure 12. Spatial distribution of Cl ion relative to a water molecule in the first hydration shell. The local coordinate system is defined as the same as figure 7. 0.10 + Donator Acceptor Donator 0.118 0.374 1.586 1.785 1.756 1.793 1.765 1.743 1.707 1.707 1.717 1.744 1.763 1.737 0 1.786 1.685 1.723 1.767 1.678 1.706 0 0.863 0.934 1.714 1.739 1.724 1.731 4.0 3.5 0.06 Number of H-bonds Distribution Acceptor 0–2 2–3 3–4 4–5 5–6 6–7 7–8 Li Cl Bulk 0.08 Cl 0.04 0.02 3.0 2.5 + Li Cl Pure water 0.00 2.0 80 90 100 110 120 130 Angle 1.5 Figure 13. The HOH angle distribution of water in the first hydration shell of ions and that in the bulk. direction of the O—H bond of a water molecule in the first hydration shell, indicating hydrogen bonding to the chlorine ion. The use of such a flexible water model permits an investigation of the influence of an ion on the geometry of water molecules. Figure 13 demonstrates this influence by a comparison between the HOH angle in the first hydration shell of ions and the angle of bulk water molecules. The effect turns out to be tiny but measurable: the HOH angles of the water molecules around the lithium ion are shrunk by about 0.5 while the negative charge of chlorine increases the HOH angle by about 1.0 . 4.3. Hydrogen bonding analysis Hydrogen bonds were evaluated with the conventional geometric criteria: if a hydrogen atom of one water molecule, A, is within the distance of 3.5 Å of the oxygen atom of another water molecule, B, and the H—O H angle is greater than 140.0 , a hydrogen bond is assigned [5, 40]. We count an ‘acceptor’ for B and a ‘donator’ for A. According to our calculations, the 2 3 4 5 6 7 Distance(A) Figure 14. Average number of hydrogen bonds per water molecule with different distances from the ions. average numbers of acceptors and donators per molecule in pure water at 298 K have the same value of 1.73. Table 5 lists the average number of acceptors and donators of hydrogen bonds per water molecule with different distances from the ions at 298 K. From this table, one can see that the acceptors and donators of water molecules are distinctly affected by the ions: in the vicinity of a Li+ ion, the acceptors are significantly reduced while the donators keep an average value around that of pure water. On the contrary, a Cl ion reduces the donators of the water molecules around it. This can be understood from the sdfs in figures 9 and 12, which indicate that the position of a hydrogen bond acceptor is firmly bonded by a positive ion (Li+) while that of a donator is bonded with a negative ion (Cl). Figure 14 displays the number of hydrogen bonds as a function of distances from the ions. The horizontal dot– dashed line is the average number of hydrogen bonds per molecule in pure water with a value of 3.47. The solute ions reduce the number of hydrogen bonds in the Solvation properties of Li+ and Cl in water areas close to them. Nevertheless, this influence is only noticeable when the distance is less than 4.5 Å. Beyond this distance the numbers of hydrogen bonds remain at about the same value as in the pure water (3.47), which indicates that the ions have almost negligible effects on the hydrogen bonds of water molecules in this region. 4.4. Dynamical residence time The question of how long a water molecule stays in the hydration shell is interesting, but is very difficult to answer with experimental approaches [3] or with short ab initio simulations. An approximate measurement with the nuclear magnetic resonance (NMR) spectroscopy technique reveals that the residence time of water molecules in the first hydration shell of the Li+ ion should be a little greater than 30 ps [3]. Such a long residence time is obviously originated from the well-established hydration shell around the lithium ion. It seems that a water molecule inside the shell has to overcome a strong energy barrier to exchange with outside molecules. An analysis of the dynamical residence time of water molecules in the first hydration shell over a long (300 ps) MD simulation shows consistent but somewhat surprising behaviour of the water molecules. The four water molecules at the vertices of the distorted tetrahedron (see figure 10) have a relatively long residence time of 15–57 ps, while another two molecules in the hydration shell are always exchanging with the outside molecules frequently, with a residence time of 1–8 ps. The chlorine ion has much less influence on water molecules and in its first hydration shell there are more residents but none dwells there for a long time. The lifetime of the water molecule in the first hydration shell of the chlorine ion varies from 1.0 to 12.0 ps, which is consistent with the data in [3]. The lifetimes of hydrogen bonds are even shorter. The average lifetime of a hydrogen bond is less than 0.4 ps. Occasionally there exists a hydrogen bond that lasts for a relatively long time of several picoseconds. 4.5. Solvation energies Solvation energy is defined as the energy for the process of transferring the solute from the ideal gas phase into the solvent. It can be obtained from the simulations on the pure solvent and the dilute solution [23]: Esol ¼ Esolution Epure , ð5Þ where Esolution is the configurational energy in the dilute solution and Epure is the energy of pure water under the same conditions. Our calculated solvation energies of lithium ions and chlorine ions in water are 1509 486.5 kJ mol1 and 358.1 kJ mol1, respectively. These results are in good agreement with the experimental data [41]. 5. Conclusion In this study, the RWK2 model is proven to be able to predict the solvation structures and dynamical properties of Li+ and Cl ions in water with an accuracy close to experiments and the first principles calculation results. A new set of parameters for ion–water short-range interaction potentials has been evaluated by fitting binding energies and geometries of gas-phase clusters to experimental data. Several stable structures for the clusters Li+(H2O)n (n ¼ 1–6) and Cl(H2O)n (n ¼ 1–4) have been obtained. These structures and their corresponding energies are generally in good agreement with experimental data and quantum mechanical calculation results. On the basis of the obtained parameters for the interaction potentials, the solvations of Li+ and Cl ions in bulk water have been extensively investigated with molecular dynamics simulations in this study. The detailed solvation structures of lithium and chlorine ions in water have been revealed through the analysis of our simulation results. These structures are strikingly influenced by temperature but not much by pressure. Dynamical properties of water molecules in the hydration shell and the solvation energies have also been investigated. These results not only agree well with experimental data and first principles calculation results, but also disclose some new insights into the microscopic ionic solvation processes. We thank Dr Ruth Lynden-Bell and a reviewer for their constructive suggestions. This work is supported by Zhenhao Duan’s ‘Hundred Scientists Project’ funds awarded by the Chinese Academy of Sciences and his Outstanding Young Scientist funds (#40225008) awarded by the National Science Foundation of China. This work is also partially supported by the National Science Foundation (USA): Ear-0126331. References [1] URABE, H., KATO, M., TOMINAGA, Y., and KAJIWARA, K., 1990, J. chem. Phys., 92, 768. [2] BARNES, H. L., 1997, Geochemistry of Hydrothermal Ore Deposits (New York: John Wiley & Sons). [3] OHTAKI, H., and RADNAI, T., 1993, Chem. Rev., 93, 1157. [4] CHIALVO, A. A., and CUMMINGS, P. T., 1994, J. chem. Phys., 101, 4466. [5] WHITE, J. A., SCHWEGLER, E., GALLI, G., and GYGI, F., 2000, J. chem. Phys., 113, 4668. 1510 Solvation properties of Li+ and Cl in water [6] RAMANIAH, L. M., BERNASCONI, M., and PARRINELLO, M., 1998, J. chem. Phys., 109, 6839. [7] LYUBARTSEV, A. P., LAAKSONEN, K., and LAAKSONEN, A., 2001, J. chem. Phys., 114, 3120. [8] TONGRAAR, A., LIEDL, K. 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