Melting of Li, K, Rb and Cs at high pressure

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Melting of Li, K, Rb and Cs at high pressure R N Singh and S Arafin Abstract Lindemann s melting law has been used to develop analytical expression to determine the pressure (P) dependence of the melting temperature (Tm) of Li, K, Rb and Cs. The basic inputs are Grüneisen parameter and the bulk modulus. Tm P variations exhibit maximum melting temperature with concave downwards. The maximum in Tm for Cs is found to occur at pressure of 2.2 GPa whereas for Li, K and Rb it falls in the range of 7 to 9.5 GPa. The predicted values of Tm as a function of pressure, based on the present empirical relation, fit quite well with the available experimental data. The empirical relation can also be used to extrapolate Tm at higher pressure from the values available at lower pressures. Keywords Alkali metals, melting law, pressure, semi-empirical equations. A I. INTROUCTION LKALI metals (Li, Na, K, Rb and Cs) are highly reactive and have large number of industrial applications, including alkalides and biological roles as electrolytes. These fall under the category of low melting temperature metals varying in the range 301.59K (Cs) to 453.69K (Li) at ambient conditions. It is of great interest to investigate the effect of high pressure on the melting curve. The general character of the melting phenomenon at lower pressure is the same as for other substances i.e. melting curve rises with increasing pressure but the behavior at higher pressure is not well understood. Recent experimental results for Na and Li [1,2] suggest that at lower pressure, T m increases with P and then decreases with increasing pressure exhibiting a maximum for T m -P variation. In the present work we investigate the characteristics of melting curves of Li, K, Rb and Cs as a function of pressure and examine the maxima and the critical point of the curves. The comparative study of the behavior of these metals under pressure has special significance because the effects of pressure on these metals are excessively large, for example, Cs is by far the most compressible solid element. The energy density on compressions becomes comparable to the bonding energies resulting in significant changes in the electronic states, chemical bonding and the packing of condensed phases. Alkali metals are found [3-6] to transform at high pressure into structurally complex and poorly conducting states as a result of changes in the electronic structure due to s-p or s-d hybridization. Several authors [7-9] have experimentally determined the bcc-fcc transitions in Rb, K and Cs at higher pressure. epartment of Physics, College of Science, Sultan Qaboos University, PO Box-36, PC -123, Oman,( (corresponding author s phone: 0096824141464 ; e-mail: ram@squ.edu.om ). We used here an empirical approach based on Lindemann criterion of melting to determine T m as a function of pressure. Such an approach has been successfully applied to different class of materials [10-12]. The basic inputs are the Grüneisen parameter (ξ) and the bulk modulus (B). ξ and B have been expanded here in terms of pressure which allows us to obtain analytical relation for T m in terms of pressure. The computed results are in very good agreement with the available experimental data [2,13]. We observe that T m -P variation of all the alkali metals exhibits maximum at a pressure around which the bcc-fcc transformation occurs. Section 2 covers the formulation for obtaining the analytical relations for T m as a function of P. The computed values of the results are given and discussed in section 3 which is followed by conclusion in section 4. II. FORMALISM II.1 Melting temperature in terms of bulk modulus (B) and Grüneisen parameter (ξ) The present empirical method is based on Lindemann s melting law which has been extended by expressing the bulk modulus, B and the Grüneisen parameter, ξ as a function of pressure. Grüneisen parameter is a property of materials that establishes a link between thermal behavior and the elastic response to thermally induced stress of the material. It measures the anharmonic interactions and is of considerable interest for theoretical and experimental studies of materials whereas the bulk modulus determines the ability of the materials to undergo compression. It was proposed by Lindemann [14] that the amplitude of the atomic vibrations increases with increasing temperature and that melting occurs when the amplitude of vibrations reaches a critical fraction, y m, of the mean atomic radius R a. Lindemann's original formula, in association with the approximate expression of Mott and Jones [15] for the mean square amplitude of vibration of each atom, can be written in the form: 2 T y R Mk 3h m m a B 2 where Θ is the ebye temperature, R a is the atomic radius and M is the atomic mass. The variation of Θ with atomic volume can be expressed in terms of Grüneisen parameter (ln ) (ln ) On replacing R a [=(3M/4πρ) 1/3 and M in Eq. (1), carrying out some algebra with the help of Eq. (2) one gets an expression (1) (2) 167

for pressure variation of T m in terms of bulk modulus, B and Grüneisen parameter, ξ [10,11] To find the pressure, P m at which T m becomes maximum, we differentiate Eq. (6) with respect to P and set it equal to zero. This leads to the relation where and ξ in Eq. (3) are pressure dependent. is the bulk modulus of the material. B 2.1.1 Linear dependence of B and ξ on pressure For want of better analytical expression, B and ξ can be expanded in terms of P: For most metals ξ 0 is greater than 1/3. Hence the pressure derivative of Grüneisen parameter, a 1 must be negative. It suggests that Grüneisen parameter, ξ decreases with pressure which is in agreement with available results [16 ]. For most metals ξ 0 is greater than 1/3. Hence the pressure derivative of Grüneisen parameter, a 1 must be negative. It suggests that Grüneisen parameter, ξ decreases with pressure which is in agreement with available results [16 ]. II.1.2 Non-linear dependence of B and ξ on pressure In this case we retain up to 2 nd order terms (a 2 and b 2 ) of Eqs. 4 and 5 to compute T m as a function of pressure. Integration of Eq. (3) leads to B 0 and ξ 0 are the bulk modulus and the Grüneisen parameter at zero pressure. a n and b n (n=1, 2, 3,.) are the n th derivatives of Grüneisen parameter and the bulk modulus respectively. For linear dependence of B and ξ on P we retain terms up to 1 st order and neglect the higher order terms. Without going into derivation of the equation, which can be found in [10 12], T m (P) can be expressed as To solve the above integral equation analytically we substitute the first three terms of Eqs. 4 and 5 in Eq. (12) and get T 0, B 0 and ξ 0 are the melting temperature, bulk modulus and the Grüneisen parameter at ambient condition respectively; a 1 and b 1 are the pressure derivatives of Grüneisen parameter, ( ξ/ P) and the bulk modulus, ( B/ P) respectively. If the Grüneisen parameter is assumed to be independent of P, then Eq. (6) simplifies to Equation (8) is a simplified version to compute the pressure dependence of the melting temperature subject to the condition that the bulk modulus of the material depends linearly on pressure and the Grüneisen parameter remains invariant. It is of interest to compare Eq. (8) to one of the most important and extensively used Simon s empirical relation, It is possible to integrate I 1, I 2 and I 3 analytically for two conditions (i) and (ii). We provide below explicit expressions satisfying these two conditions: Solution for Condition I: If The integrals I 1, I 2 and I 3 (Eqs. 14-16) stand for: It suggests that the Simon s constants X and Y can readily be related to the bulk modulus and the Grüneisen parameter as, 168

The above integrals are to be evaluated between the limits 0 and P. After substituting Eqs. (17-19) in Eq. (13), we obtain an expression for the melting temperature, T m (P), Solution for Condition II: If The solutions for the three integrals (Eqs, 14-16) stand as: (20) and After substituting Eqs. (24-26) in Eq. (13), we obtain the expression of T m i.e. Computed values of T m are plotted in Figs. 1-4 and are compared with the experimental values [2,13] for Li, K, Rb and Cs. Both the values of T m (P) computed from Eq. (6) and Eq. (27) are plotted for the sake of comparison. The computed values from second order Eq. (27) are in excellent agreement with the experimental values. T m exhibits non-linear dependence on P. In the lower pressure region, Eq. (6) which includes only the linear terms of expansion of B(P) and ξ(p) gives good agreement except for the case of Cesium. For the latter, T m P variation computed from Eq. (6) is quite at variance in comparison to experimental values and the values computed from Eq. (27). T m P curves for alkali metals are found to be concave downwards. It is interesting to observe that the melting curves exhibit a point of inflexion in all the alkali metals. First, it increases with P, then flattens over a small range of pressure, and then starts decreasing with increasing pressure. The positive gradient dt m /dp is large at low pressure (indicating a sharp rise of the T m (P) curves) in comparison with the magnitude of negative gradient of high pressures. The point of inflexion is often interpreted as the sign of structural transformation. It may be noted that in case of Na, the synchrotron diffraction measurements of Na [1] suggest that a structural transition occurs around the point of inflexion from bcc to fcc phase. Recently Arafin and Singh [17] have used the empirical relation to compute T m -P variation for Na and found that the maximum occurs at 33GPa. It may be noted that at normal pressure and temperature Li, K, Rb and Cs possess bcc structure like Na at ambient conditions. For a given isobaric condition, the kinetic energy of atoms increases with increasing temperature, and the solid-liquid transition occurs when amplitude of vibration reaches a critical value which may vary between 0.11 and 0.23 [18] depending on factors such as the crystal structure and the nature of atomic bonding. For most of the alkali metals, the packing fraction (volume of cell/volume of rigid sphere) is found to be 0.47 [19] at normal melting temperature. From a thermodynamic point of view the melting point is simply the temperature at which the Gibbs free energy of the solid and liquid phase are equal, or III. RESULTS AN ISCUSSION The formalism of section 2 has been applied to compute Tm as a function of P for Li, K, Rb and Cs. The range of pressure in this investigation for K and Rb varies from atmospheric pressure to 16 GPa whereas for Li it goes up to 64 GPa and for Cs it it ranges up to 8GPa.The computational inputs are tabulated intable 1. Tab Table I : ξ0 and B0 are values at ambient conditions, a1 and a2 are the coefficients of expansion of ξ; b1 and b2 are the coefficients of expansion of B; Tmin and Pmin represent the point of inflexion of Tm P curves. Met als B 0 GPa b 1 b 2 GPa -1 ξ 0 a 1 Gpa - 1 x 10-2 a 2 GPa - 2 )x 10-2 T m in K P in GP a Li 12.13 6.25.3281.771-4.5.091 529 10. 0 K 2.85 5.02.1575 1.02-9.5 2.15 557 9.5 Rb 2.3 4.70 -.0811 1.02-9.0-1.13 559 7.0 Cs 2.43 1.79.1202 1.05-33.4 -.224 466 2.2 169

600 200 Lithium (39, 338) 250 200 150 100 (2.19, 465.63) Cesium 50 100 0 10 20 30 40 50 60 70 0 0 2 4 6 8 Fig. 1 Melting temperature (Tm) as a function of pressure, P for Li computed from Eq. (8) : open square; Eq. (27) : solid line; downward triangles represent experimental values [ref 2] and upward triangles represent experimental values [ref 13]. 550 (9.47, 557.22) Potassium 0 2 4 6 8 10 12 14 16 18 Fig 2 T m - P variation from K. open square represents values 600 550 (7.05, 558.56) Rubidium 0 2 4 6 8 10 12 14 16 18 Pressure, P (GPa) Fig 3 T m - P variation from Rb. open square represents values Fig 4 T m - P variation from Cs. open square represents values Recently Schaeffer et al [2] have investigated the melting curve of Li up to 64 GPa. At high pressures Li undergoes a series of structure phase transformation like Na [1]. Their experimental results suggest a maximum in the T m P curve around 10 GPa which compares well to our value of 10.5 GPa around which bcc-fcc phase transition [20,21] has been observed from diffraction study. Though our empirical relation does not exhibit a minimum in Li around 35 GPa as reported in reference [2], but computed values from empirical relation does give a point of inflexion at 39.34 GPa. Molecular dynamics calculation suggests a sharp decrease in melting at 60 GPa around which lithium structure changes from fcc to lower symmetry. Likewise ours, the differential thermal analysis [13,22] measurements suggest sharp drop in the melting temperature between 15 to 40 GPa. The maxima in the melting temperature of K, Rb and Cs are found to be 9.47 GPa, 7.05 GPa and 2.19 GPa respectively. We may recall [17] that Na exhibits the maximum in the T m -P variation at comparatively higher P 33 GPa. In comparison to other alkali metals, Cs is found to be quite different. The maximum in the melting curve of Cs occurs at a low pressure of 2.2 GPa. We also observed that the relation, Eq. 6 which is derived by virtue of linear dependence of ξ and B on P fails miserably to predict T m P variation for Na. But values [17] computed from Eq. (27) are in excellent agreement with the experimental observation. At ambient pressure, alkali metals are the best example of free electron system but at high pressure the quantum structure of the ions and electrons is broken down and the matter could best be resolved for a system consisting of densely packed ions and condensed electrons. Under high pressure, the inner shell electrons of atoms become quite reactive and may interact strongly with condensed valence electrons. From X-ray diffraction study [23] with Cs it is inferred that the atomic radius decreases dramatically which suggests a discontinuous s-d electronic transition. 170

IV. CONCLUSION Empirical relations developed in terms of Grüneisen parameter and bulk modulus are used to obtain the melting curves of Li, K, Rb and Cs as a function of pressure. Both linear and non-linear dependence of ξ and B on pressure are considered and analytical relations for T m P variation are derived. The melting temperature of Li, K, Rb and Cs exhibits maximum with concave curve facing downward. The maxima in T m for Li, K, and Rb varies between 7 and 10.5 GPa. The computed value of maximum of T m Cs is found to be at comparatively low pressure of 2.2 GPa. REFERENCES [1] E. Gregoryanz, O. egtyareva, M. Somayazulu, R.J. Hemley, H.K. Mao, Phys. Rev. Lett. 94 (2005) 185502. [2] A.M.J. Schaeffer, W.B. Talmadge, S.R. Temple, S. eemyad, High pressure melting of Lithium, PRL. 109 (2012) 185702. [3] R. Jeanloz, Ann. Rev. Phys. Chem. 40 (1989) 237. [4] R.M. Martin, Nature. (1999) 117. [5] J.B. Neaton, N.W. Ashcroft, Nature. (1999) 141. [6] M.S. Anderson, C.A. Swenson, Phys Rev. 31 (1985) 668. [7] K. Takemura, K. Syassen, Phys. Rev. B. 28 (1983) 1193. [8] H. Olijnyk, W.B. Holzapfel, Phys. Lett. A 99 (1983) 381. [9] P.W. Bridgeman, Proc. R. Soc (London), A203 (1950) 1 [10] S. Arafin, R.N. Singh, A.K. George, Int J Thermophys 33 (2012) 1013. [11] S. Arafin, R.N. Singh, A.K. George, Physica B, 419 (2013) 40. [12] S. Arafin, R.N. Singh, A.K. George, Int. J. Thermophys, 34 (2013) 395. [13] H.. Leudemann, G.C. Kennedy, J. Geophys. Res. 73 (1968) 2795. [14] F.A. Lindemann, Phys. Z. 11, (1910) 609. [15] N.F. Mott, H. Jones, The Theory of the Properties of Metals and Alloys, 2nd edn. Oxford University Press, Oxford, 1936. [16] L. Vocadlo, J.P. Porier, G.. Price, American Mineralogist, 85 (2000) 390. [17] S. Arafin, Ram N. Singh, Appl. Phys. A, OI 10.1007/s00339-014- 8540-y (2014). [18] T.E. Faber, Theory of Liquid Metals (Cambridge Monographs on Physics, Cambridge University Press, Cambridge, 1972. [19] M. Shimoji, Liquid Metals: An Introduction to Physics and Chemistry of Metals in the Liquid State, Academic Press, London, 1977. [20] M. Hanfland, K Syassen, N.E. Christensen,.L. Novikov, Nature 408 (2000) 174. [21] C.L. Guillaume, E. Gregoryanz, O. egtyareva, M.I. McMoMahon, M.Hanfland, S. Evans, M. Guthrie, S.V. Sinogeikin, H.K. Mao, Nature Phys. 7 (2011) 211. [22] R. Boehler, Phys. Rev. B27 (1983) 6754. [23] K. Takemura, S. Minomura, O. Shimimura, Phys. Rev. Lett. 51 (1983) 1603. 171