Abstract
Yet in 1960s Del Re with coworkers considered the electronic structure of organic molecules using hybrid orbitals. They studied the simplest molecules: CH4, NH3, H2O, and more complex ones: cyclopropane, cyclobutane, cubane, using either the optimal overlap or maximal localization principles to determine the hybrids. Later Malrieu with coworkers used hybrid orbitals in the PCILO method. Later, we determined either the form and orientation of the hybrid orbitals or two-electron functions of the two-center bonds constructed on the basis of these hybrids from the minimum condition for total electronic energy as implemented in the SLG method. This gave us significant improvement in the efficiency: the dependence of the required computational resources on the molecule size reduces down to O(N). The paradigm based on the usage of the variation principle for determination of either the hybrid orbitals or the elements of the reduced density matrices in their basis allows one to formulate and prove exact statements about electronic structure. We start from establishing the energy expression for highly symmetric non-molecular ice X and prove mathematically the stability of this polymorph above a critical pressure. Below it, we derive the pressure dependence of the interaction energy of the effective dipoles emerging in the system when the symmetric layout of the hydrogen atoms, specific for ice X, breaks down. This reproduces semiquantitatively the characteristic and unusual (as compared to the others—practically vertical) form of the boundary between the areas of the ordered and disordered ice VIII and VII. We also discuss the possibility of describing the differences between the ice phases existing at lower pressures (down to normal) by including the long-range electrostatic contributions: charge-charge and dipole-dipole in the crystal energy.
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Notes
We subtract twice the products of the 1-RDM’s \(2P_{h}P_{l}\) and \(2P_{h}P_{s}\) form Eq. (15) and include them into classical two-center Coulomb interactions of charge distributions residing on the corresponding atoms.
This applies to the crystals where R is the only independent geometry variable. For more complex situations see below.
Actually, it goes about the existence of a minimum of a function being a sum of a component monotonously decreasing which diverges in the coordinate origin, and thus, its first derivative as a function of R takes once all values in the interval \(\left( -\infty ,0\right)\) and of a monotonously increasing non-divergent component whose first derivative takes values in the interval \(\left( 0,A\right) ,A>0\). Thus, there is a point R where the derivatives have opposite values and the derivative of the sum vanishes and the function itself has an extremum.
This is easy to understand: ice Ic and ice X are formed by the same H bond networks; however, in ice X there are two such networks interpenetrating each other without being chemically bound (that is atoms of one network are located in the voids of another and vice versa) [1].
One cannot expect that such a simple model yields numerically correct estimates of the transition pressures. However, we stress that the obtained orders of magnitude of several hundredths of GPa are correct ones.
Two Greek words are oxygonōn (Gen. Plur. of oxygono—Greek for oxygen) and oxymoron both derived from \({\mathrm{o}}{\upxi }{\acute{\upupsilon }}{\varsigma}\): sharp, acidic.
Mathematical truths established about its sharp concepts are believed to be immutable again as a counterposition to those of chemistry.
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Acknowledgements
This work is supported in the frame of joint trilateral German–Russian–Ukrainian projects by the Volkswagenstiftung Grant No. 151110. Valuable discussions with Prof. G.G. Malenkov (Moscow), Prof. I.V. Abarenkov (St. Petersburg), and Prof. M.V. Kirov (Tyumen) are gratefully acknowledged. The author is thankful to the Referees for their benevolent comments and to Dr. Peter Reinhardt of Université Paris-Sorbonne (Jussieu) for his friendly help during the XLIII Congrès des Chimistes Théoriciens d’Expression Latine in Paris, in July 2017. Mr M. Rudenko is acknowledged for drawing author's attention to the quotation Ref. [48].
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Published as part of the special collection of articles “CHITEL 2017—Paris—France”.
Appendix: Parameterization
Appendix: Parameterization
The most ridiculous part of this story is the parameterization. It used to be a common place to complain about numerous parameters characteristic for semiempirical theories. Our days it is considered to be acceptable to upload a ca. 500 kB file of parameters not having whatever physical sense per atom within a PAW/DFT procedure and to call this ab initio.
Nevertheless, we find even the number of parameters required by the standard CNDO setting to be excessive for analytical treatment. Thus, we extended the procedure Ref. [39] and express required parameters through the Slater orbital exponents characteristic for atoms O and H: \(\zeta _{\mathrm{H}}=1;\,\zeta _{\mathrm{O}}=2.275\) [13]. For the atomic parameters, the following exact expressions are used
which produce the “theoretical” values given in Table 2. Corresponding “experimental” values are extracted from different parameterization schemes previously developed for the CNDO approximation [50,51,52,53,54,55,56,57,58] to comply with experiment. In case of W, some scaling is obviously necessary (factor of ca. 0.3), but it is understandable due to the absence of the radial node in the 2s-Slater AO. The overestimate of U with respect to “ experimental” values is compensated by the respective overestimate of G and h which non-trivially enter only together.
One-electron resonance integrals \(t_{\sigma \sigma },t_{\zeta \sigma }\) are expressed as \(t_{\mu \nu }=\beta S_{\mu \nu }\), where \(S_{\mu \nu }\) is the corresponding overlap integral between the relevant Slater AOs.
For the two-center Coulomb repulsion integrals \(\gamma _{\mathrm {AB}}\) the exact formulae [59] are employed which guarantees the “Yukawa-like” exponential decay of the core-core repulsion \(Y_{\mathrm {AB}}\).
Finally, the value of G is scaled by the factor of 0.9151 to get the critical pressure exactly at 61 GPa. This, of course, does not affect the qualitative picture.
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Tchougréeff, A.L. De glaciēbus or deductive molecular mechanics of ice polymorphs. Theor Chem Acc 137, 138 (2018). https://doi.org/10.1007/s00214-018-2322-0
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DOI: https://doi.org/10.1007/s00214-018-2322-0