Abstract
Nowadays, it is possible to calculate, at the ab initio level, large classes of properties of condensed matter, from the crystal structure and mechanical properties, to the thermodynamics, and therefore the stability in a given environment and in a range of temperature and pressure conditions. Predictions from calculations of this type can be used to estimate geophysical properties such as densities of mantle rocks as they change along geotherms, the geotherms themselves, phase transitions and their features, seismic velocity profiles to be compared with models derived from other paradigms and techniques. Moreover, known facts and observations concerning structure, behaviour, properties of materials and properties of whole complex systems of materials can be explained or at least rationalized within a common and very general frame that is at the basis of all the currently known physics and chemistry. However, the development of ideas, paradigms and related techniques did not come out all of a sudden, but steadily proceeded from the early days till now, without a real solution of continuity. During the time, quantum mechanics heavily contributed to create a language, a set of basic ideas and a frame of mind that is extensively used by chemists and crystallographers to interpret the relevant facts. What we know today, and how we currently apply quantum mechanics to systems of our interest, is largely dependent upon the path followed during the years to implement the theory in practical and efficient algorithms to make calculations for real systems. This paper will present a brief review of the paths followed, along with their motivations, since those early and heroic days of physics at the beginning of the last past century. The aim is to provide the reader with a general view of the subject that could possibly drive her/him toward the choice of more specific papers from the huge literature, concerning more restricted and specialized topics.
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Notes
However, it seems that Einstein was not aware of the Michelson and Morley findings when he wrote his paper in 1905 (Einstein 1905).
Consider two electrons: each has always the same spin; however, their spin vectors may differ in the orientation; the latter one is specified by the three components of the vector along the axes of a Cartesian frame. Due to the commutation rules of the angular momentum operators, only one component of the spin vector can be precisely assigned and, by convention, this is the z component. The variable s given in the text is exactly such component, and it can assume only two possible values: 1/2 or \(-1/2\) in units of \(\hbar \). In the jargon, when it is said that two electrons have the same spin (spin parallel electrons), the z component of it is meant; the same is true for spin paired electrons: they have different (opposite) values of the z component.
In systems having no spin unpaired electrons, in a non-relativistic approximation, an orbital (\(\zeta \)) gives rise to two spin orbitals (\(\eta _1\) and \(\eta _2\)) having the same orbital part (\(\zeta )\) and two different spin functions (\(\sigma _1\) and \(\sigma _2\)): \(\eta _i(x)=\zeta (r)\cdot \sigma _i(s)\).
Although all pointwise correlation effects are short ranged if compared to mean field effects described at the Hartree–Fock level, they can be classified in two categories: short-range and long-range effects, where the adjectives short and long have here a relative meaning inside this further classification. Dispersion forces are ascribed to such long-range correlation effects, and are generally not properly accounted for by DFT functionals; DFT correlation functionals are instead effective in dealing with the short-range effects.
This is at the core of the Born–Oppenheimer approximation that separates the nuclear motion from the electron motion, justified by the large difference of mass of the two types of particles.
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Acknowledgements
The Accademia dei Lincei must be acknowledged for offering me the opportunity to write this review. Gerald Gibbs must also be gratefully acknowledged for reviewing the manuscript, and for being one of the most important inspiring sources in my scientific career.
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The author Mauro Prencipe has been awarded with the 2018 Lincei Prize on Geosciences.
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Prencipe, M. Quantum mechanics in Earth sciences: a one-century-old story. Rend. Fis. Acc. Lincei 30, 239–259 (2019). https://doi.org/10.1007/s12210-018-0744-1
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DOI: https://doi.org/10.1007/s12210-018-0744-1