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| title | chunk | source | category | tags | date_saved | instance |
|---|---|---|---|---|---|---|
| Chemical crystallography before X-rays | 2/6 | https://en.wikipedia.org/wiki/Chemical_crystallography_before_X-rays | reference | science, encyclopedia | 2026-05-05T16:17:25.610345+00:00 | kb-cron |
In 1723 Moritz Anton Cappeller published Prodromus Crystallographiae, the first treatise on crystal shapes. The introduction of the term crystallography is attributed to Cappeller. In 1735 Carl Linnaeus, who is known for his system of classification of biological species in his Systema Naturae, also classified minerals and stated that "their transparency is derived from their atomical construction". In 1745 Guillaume-François Rouelle carried out a microscopic analysis of sea salt and proposed that the crystals were composed of cubic particles. In 1758 Roger Joseph Boscovich published his atomic theory which stated that particles of matter were linked by attractive and repulsive forces and that the solid so formed was compressible rather than rigid; this would become relevant in the 19th century when Haüy theorised that crystals were constructed from identical units stacked up without spaces. The idea of a polyhedral molecular unit of crystal structure was promoted by Pierre-Joseph Macquer in his handbook Dictionnaire de chymie of 1766. In 1767 Christian Friedrich Gotthard Westfeld wrote that calcite crystals could be built from rhombohedra. In 1773 Torbern Bergman, a leader in the field of chemical analysis, described the crystal forms of calcite and stated that all the forms could be built up from the cleavage rhombohedron. Bergman developed a classification of minerals based on chemical characteristics (extending the work of Linnaeus), with subclasses organized by their external shapes, and defined seven primary crystal forms. With Jean-Baptiste L. Romé de l'Isle's Essai de cristallographie published in 1772 and Cristallographie published in 1783 the scientific approach to crystal structure began. Romé de l'Isle described over 500 crystal forms and accurately measured the interfacial angles of a great variety of crystals, using the goniometer designed by his student Arnould Carangeot. Romé de l'Isle noted that the angles are characteristic of a substance, thus generalizing the law of constancy of angles postulated by Steno. Romé de l'Isle considered that the shape of a crystal is a consequence of the packing of elemental particles, and defined six primitive forms. In 1781 René Just Haüy (often termed the "Father of Modern Crystallography") discovered that crystals always cleave along crystallographic planes. Based on this observation, and the fact that the inter-facial angles in each crystal species always have the same value, Haüy concluded that crystals must be periodic and composed of regularly arranged layers of tiny polyhedra (molécules intégrantes). This theory explained why all crystal planes are related by small rational numbers (the law of rational indices). In 1784 René-Just Haüy published Essai d'une théorie sur la structure des cristaux, appliquée à plusieurs genres de substances cristallisées in which he stated his law of decrements: a crystal is composed of molecules arranged periodically in three dimensions without leaving any gaps. Haüy's molecular crystal structure theory assumed that molécules intégrantes were specific in shape and composition for every compound. Haüy developed a mathematical theory of crystal structure that turned out to be remarkably accurate and gave crystallography a legitimate place among the sciences.
== Early 19th century ==