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“A crystal requires particles to be arranged in a highly regular microscopic pattern.”
The conclusion
Crystals require long-range order in the microscopic arrangement of their constituent particles. “Highly regular” accurately conveys this defining feature, provided it is not interpreted as requiring perfect periodic repetition: quasicrystals are aperiodic but still highly ordered. Authoritative crystallography and chemistry definitions directly support the claim.
Caveats
- Low confidence conclusion.
- “Highly regular” means long-range order, not necessarily strict periodic repetition.
- Real crystals may contain defects; the arrangement need not be perfectly ordered everywhere.
- Several cited crystallography sources are related IUCr publications rather than fully independent confirmations.
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Crystals are fascinating structures of solid or liquid matter where atoms, molecules, and/or ions are, on average, arranged in a highly ordered lattice.Crystals are fascinating structures of solid or liquid matter where atoms, molecules, and/or ions are, on average, arranged in a highly ordered lattice. It is well-documented that some of the earliest objects collected by our hominin ancestors, without evident practical purpose, were small quartz and calcite crystals. These crystals, measuring a few centimeters, had no known utility as weapons, tools, or ornaments. However, hominins appear to have appreciated these stones, collecting and transporting them from their place of discovery to their shelters. …
Direct-space definition A solid is a crystal if its atoms, ions and/or molecules form, on average, a long-range ordered arrangement. … In most crystals the arrangement is a periodic array that is governed by the rules of translational symmetry.… Currently there are two alternative (but theoretically equivalent) definitions of a crystal; both are based on the central idea of spatial order. One focusses on direct (or real) space, the other on reciprocal (or diffraction) space. The latter is more compact and elegant; the former can be easier to visualize. Direct-space definition A solid is a crystal if its atoms, ions and/or molecules form, on average, a long-range ordered arrangement. In most crystals the arrangement is a periodic array that is governed by the rules of translational symmetry. In aperiodic crystals(incommensurate and quasicrystals) the arrangement is not periodic in three dimensions but is nevertheless still fully ordered, where the ordering follows particular mathematical rules. Reciprocal-space definition A material is a crystal if it has essentially a sharp diffraction pattern. A solid is a crystal if it has essentially a sharp diffraction pattern. …
The latest direct-space definition (Chapuis, 2024a) by the Commission on Crystallographic Nomenclature (CCN) says that ‘a solid is a crystal if its atoms, ions and/or molecules form, on average, a long-range ordered arrangement.… This paper does not reinvent the wheel but extends the discrete concepts to a new continuous domain in the language of present-day crystallography for present-day crystal lographers. The entry ‘A crystal’ appeared in the IUCr Online Dictionary of Crystallography (IUCr, 2021) in 1992 and has since been modified slightly. We propose updates to fill past gaps and meet present needs. The latest direct-space definition (Chapuis, 2024a) by the Commission on Crystallographic Nomenclature (CCN) says that ‘a solid is a crystal if its atoms, ions and/or molecules form, on average, a long-range ordered arrangement. In most crystals, the arrangement is a periodic array that is governed by the rules of translational symmetry.’ In this paper, a crystal is a periodic crystal, so we postpone similar developments for non-periodic materials including quasicrystals and amorphous solids to future work (see Senechal, 1996). The definition quoted above (Brock, 2021) for a periodic crystal means that the set of all atoms is preserved under all lattice translations. …
At the site that describes the latter applications [3] , we find the definition of a crystal as "any solid material with its atoms, or smallest units of matter, organized in a repeating pattern."… ('Essentially' is defined subsequently.) Approaching the nature of crystals from a slightly different direction, namely an on-line search engine, we might find subjective references to crystals in "stunning earrings and diamond rings," but we can also read about more functional crystal uses such as "solar-powered devices," "solving important biological puzzles," "monitors for computers," and even "tasty snacks." At the site that describes the latter applications [3] , we find the definition of a crystal as "any solid material with its atoms, or smallest units of matter, organized in a repeating pattern." The focus of that definition is on the crystal as a self-standing item, as opposed to the way it responds to a probe.
A solid is a crystal if its atoms, ions and/or molecules form, on average, a long-range**ordered**arrangement.… Currently there are two alternative (but theoretically equivalent) definitions of a crystal; both are based on the central idea of spatial order. One focusses on direct (or real) space, the other on reciprocal (or diffraction) space. The latter is more compact and elegant; the former can be easier to visualize. Direct-space definition A solid is a crystal if its atoms, ions and/or molecules form, on average, a long-range**ordered**arrangement. In most crystals the arrangement is a periodic array that is governed by the rules of translational symmetry. Inaperiodic crystals(incommensurate and quasicrystals) the arrangement is not periodic in three dimensions but is nevertheless still fully ordered, where the ordering follows particular mathematical rules. Reciprocal-space definition A material is a crystal if it has**essentially**a sharp diffraction pattern. A solid is a crystal if it has**essentially**a sharp diffraction pattern. …
we will use in the following the definition of a crystal given by the IUCr Commission on Aperiodic Crystals in their report for the year 1991 (International Union of Crystallography, 1992; see page 928): ‘by crystal we mean any solid having an essentially discrete diffraction diagram, and by aperiodic crystal we mean any crystal in which 3D periodicity can be considered to be absent’.… Wolff (Janssen & Tuinstra, 1998) and, most recently, Aloysio Janner (Janssen, 2016). This article reviews some of the major contributions Ted Janssen made to the field his scientific life was fully dedicated to: aperiodic crystals. Aperiodic crystals are long-range ordered structures which lack 3D periodicity. Although there are still on-going discussions and research on precisely how to define and characterize a long-range ordered structure, we will use in the following the definition of a crystal given by the IUCr Commission on Aperiodic Crystals in their report for the year 1991 (International Union of Crystallography, 1992; see page 928): ‘by crystal we mean any solid having an essentially discrete diffraction diagram, and by aperiodic crystal we mean any crystal in which 3D periodicity can be considered to be absent’. In other words, an aperiodic crystal is characterized by a diffraction pattern consisting mainly of sharp Bragg peaks and requiring more than three integer indices to be indexed properly. Aperiodic crystals are usually classified in three different categories: incommensurately modulated structures, incommensurate composite structures and quasicrystals (see Fig. 1 for an illustration). In an incommensurately modulated structure a periodic structure is subject to one or several …
the subsequent structure determinations, seem to have led to the acceptance of a definition of crystals based on the periodicity of their internal structure, and one which unnecessarily ruled out quasiperiodicity. … But by 1992 the IUCr Ad Interim Commission on Aperiodic Crystals wrote “by ‘crystal’ we mean any solid having an essentially discrete diffraction pattern, and by ‘aperiodic crystal’ we mean any crystal in which three-dimensional lattice periodicity can be considered to be absent”… Our solid was metallic and thus not a “clear transparent mineral.” It can be grown to form “convex solids enclosed by symmetrically arranged plane surfaces, intersecting at definite and characteristic angles.” According to the latter of these older definitions, quasicrystals are crystals. The discovery in 1912 that crystals could diffract x-rays discretely implied either their periodicity or quasiperiodicity. But as noted above, the subsequent structure determinations, seem to have led to the acceptance of a definition of crystals based on the periodicity of their internal structure, and one which unnecessarily ruled out quasiperiodicity. But by 1992 the IUCr Ad Interim Commission on Aperiodic Crystals wrote “by ‘crystal’ we mean any solid having an essentially discrete diffraction pattern, and by ‘aperiodic crystal’ we mean any crystal in which three-dimensional lattice periodicity can be considered to be absent” [9]. By this latest definition, our solid is a crystal, albeit an aperiodic one. It is a “quasiperiodic crystal” or quasicrystal for short, a word coined by Levine and Steinhardt [10]. Our surprising discovery created quite a stir and has influenced research in many fields, not just crystallography, but also materials science, physics, mathematics [11,12], biology [13,14], and even art. There have been about 10 000 papers in these fields and many conference proceedings [15]. …
The presence of three-dimensional order on the level of atomic dimensions.… G H I J K L M N O P Q R S T U V WXYZ Additional Indexes Physical ConstantsUnits of MeasurementPhysical QuantitiesSI PrefixesRing IndexGeneral FormulaeExact FormulaeSource DocumentsTerms by IUPAC DivisionTerms by Organization Version 5.0.0 (14588 Terms) `DOI: 10.1351/goldbook` Jan Kaiser - Content Editor (goldbook@iupac.org) Stuart J. Chalk - Technical Editor (goldbook@iupac.org) Joint Subcommittee on the IUPAC Gold Book ** ## crystallinity Copy https://doi.org/10.1351/goldbook.C01433 The presence of three-dimensional order on the level of atomic dimensions. Crystallinity may be detected by *diffraction* techniques, heat-of-fusion measurements, etc. The amount of disorder within the crystalline region is not incompatible with this concept. ***Source: *** Purple Book, 1st ed., p. 74 [Terms] [Book] **Citation:** 'crystallinity' in *IUPAC Compendium of Chemical Terminology*, 5th ed. International Union of Pure and Applied Chemistry; 2025. Online version 5.0.0, 2025. https://doi.org/10.1351/goldbook.C01433 RIS BibTex EndNote Div. IVPDFTextXMLJSON
A crystal is not a static arrangement of atoms or molecules. … There is no doubt that regular crystals possess translationally periodic structures on time and space average.… How does this compare with the information we have about periodic structures from small molecule crystals to virus crystals? Any real crystal, be it a periodic or an aperiodic one, is finite and has equilibrium and non-equilibrium defects such as thermal vacancies as well as dislocations and grain boundaries, respectively. If it only has equilibrium defects it is called a perfect crystal otherwise an imperfect crystal. Beside defects a crystal may also show inherent structural disorder. A crystal is not a static arrangement of atoms or molecules. The atoms vibrate around their equilibrium positions due to the superposition of all thermally excited lattice vibrations (phonons). Consequently, the ideal structure of a crystal is just a simplified model of the real structure. To fully describe the real structure of a crystal one needs a model for the ideal structure as well as one describing the deviations from it (dynamics, disorder and defects). A real crystal is rarely in thermodynamic equilibrium. If crystallized from the melt, the actual structure at ambient conditions always is a kind of quenched metastable state. Thermodynamic equilibrium cannot be reached due to sluggish kinetics at lower temperature. There is no doubt that regular crystals possess translationally periodic structures on time and space average. Nobody ever doubted that really and tried to prove this or even thought that it would make sense to prove it. In the case of QC the situation is different. At least on one single example it has to be demonstrated how an ideal QC structure looks like and what kind of disorder and defect structure is inherent or common. It is typical for X-ray diffraction patterns of QC that they show sharp Bragg reflections even if strong (phason) diffuse scattering is present. …
After Shechtman et al. (1984) published the paradigm-shattering 'Metallic Phase with Long-Range Orientational Order and No Translational Symmetry', it was evident (to all but quasicrystal-deniers) that the textbook answer to 'what is a crystal?' no longer sufficed. … In response, the IUCr charged its newly appointed Commission on Aperiodic Crystals with finding a sufficiently broad definition of 'crystal', one that went beyond three-dimensional periodicity to include quasicrystals and other unexpected structures that might be discovered.Abstract After Shechtman et al. (1984) published the paradigm-shattering 'Metallic Phase with Long-Range Orientational Order and No Translational Symmetry', it was evident (to all but quasicrystal-deniers) that the textbook answer to 'what is a crystal?' no longer sufficed. In response, the IUCr charged its newly appointed Commission on Aperiodic Crystals with finding a sufficiently broad definition of 'crystal', one that went beyond three-dimensional periodicity to include quasicrystals and other unexpected structures that might be discovered. No quasicrystal structure had yet been solved, but scientists had already broadened the crystal structure kingdom: de Wolff (1974) and Janner & Janssen (1977) had already shown that modulated crystals, with incommensurate periodicities, could be rationalized in a four-dimensional 'superspace'. …
Aquasicrystalis a solid or soft matter that exhibits diffraction symmetries that are not allowed for a periodic crystal. … The arrangement of atoms in aquasicrystaldoes not obey periodicity, but obeys a special rule,quasiperiodicity,over a long range.… doi:10.1107/S2052252516009842 MATERIALS|COMPUTATION OpenOpen Accessaccess Mysteries of icosahedral quasicrystals: how are the atoms arranged? CROSSMARK_Color_square_no_text.svg **Tsutomu Ishimasaa\*** **a**Division of Applied Physics, Graduate School of Engineering, Hokkaido University, Sapporo 060-8628, Japan \*Correspondence e-mail:ishimasa@eng.hokudai.ac.jp Keywords:quasicrystals;superspace crystallography;structure analysis;phasons;X-ray diffuse scattering. Similararticles Aquasicrystalis a solid or soft matter that exhibits diffraction symmetries that are not allowed for a periodic crystal. Quasicrystals are classified into several types (pentagonal, octagonal, decagonal, dodecagonal and icosahedral) according to their symmetry. The arrangement of atoms in aquasicrystaldoes not obey periodicity, but obeys a special rule,quasiperiodicity,over a long range. Thequasiperiodicitycan be related to a geometric progression, the common ratio of which is an irrational number, for example, the golden ratio. This property can be seen in Fig. 1[link], which shows the electron diffraction pattern of an icosahedral Sc–Zn–Mgquasicrystalobserved along the fivefold axis. Since the discovery of quasicrystals by Shechtman*et al.*(1984[Shechtman, D., Blech, I., Gratias, D. & Cahn, J. W. (1984). Phys. Rev. Lett. …
These principles were derived theoretically on the basis of the concept of periodicity; that is, it was assumed that the order of crystal structures is periodic in all three space dimensions.… In the eighteenth century, mineralogists already realised that the external polyhedral forms of minerals were constant and determined by an internal order of their constituting atoms or molecules [1,2]. Despite this remarkable finding, it took about a century to fully establish the crystallographic principles that govern such an order [3,4,5,6]. These principles were derived theoretically on the basis of the concept of periodicity; that is, it was assumed that the order of crystal structures is periodic in all three space dimensions. At the beginning of the twentieth century, internal periodicity of crystals was nicely demonstrated by X-ray diffraction experiments using minerals [7,8]. Notwithstanding this, diffraction studies soon showed that the structures of a number of minerals are occasionally not strictly periodic (e.g., calaverite, quartz, and feldspars). These anomalous structures usually resulted from phase transformations and were interpreted as being more or less complex modulations of average periodic lattices. …
A crystal of a given substance or material shows plane faces always at the same angles to each other and has its other orderly properties because it is made up of atoms, ions, or molecules arranged in a very orderly way.If your students have some conviction about such conclusions from their own observations, they will have a good foundation in the science of crystallography. A crystal of a given substance or material shows plane faces always at the same angles to each other and has its other orderly properties because it is made up of atoms, ions, or molecules arranged in a very orderly way. This orderliness of structure is found in almost all solid matter, though some substances have a more orderly arrangement than others. Even in wood the molecules are arranged in good order along the fibers, though there is not much orderliness from one fiber to the next. Is wood, then, a crystal? It doesn't show shiny faces. Some crystallographers (people who study crystals) would say its fibers are crystals; some would not.
In this space, the structures of finite real crystals are idealized as infinite perfect three-dimensional crystal structures (cf. Section 8.1.4). This implies that for crystal structures and their symmetries the surfaces of crystals as well as their defects and imperfections are neglected; for most applications, this is an excellent approximation.top · pdf Crystals are objects in the physical three-dimensional space in which we live. A model for the mathematical treatment of this space is the so-called point space, which in crystallography is known as direct or crystal space. In this space, the structures of finite real crystals are idealized as infinite perfect three-dimensional crystal structures (cf. Section 8.1.4). This implies that for crystal structures and their symmetries the surfaces of crystals as well as their defects and imperfections are neglected; for most applications, this is an excellent approximation. The description of crystal structures and their symmetries is not as simple as it appears at first sight. It is useful to consider not only the above-mentioned point space but also to introduce simultaneously a vector space which is closely connected with the point space. Crystallographers are used to working in both spaces: crystal structures are described in point space, whereas face normals, translation vectors, Patterson vectors and reciprocal-lattice vectors are elements of vector spaces.
Crystals, or ordered solids, were in fact defined as being periodic arrangements of atoms, with the allowance of certain modifications to the underlying periodicity as in the cases of incommensurately modulated crystals and incommensurate composite crystals. … Noting that the diffraction spectra of all experimentally observed crystals contain Bragg peaks, the International Union of Crystallography 8 has redefined a crystal to be “…any solid having an essentially discrete diffraction diagram.”7 long range order was thought to be synonymous with periodicity. Crystals, or ordered solids, were in fact defined as being periodic arrangements of atoms, with the allowance of certain modifications to the underlying periodicity as in the cases of incommensurately modulated crystals and incommensurate composite crystals. Nearly two decades later, it is now well established that Figure 1. Three different quasicrystals: (Left) A quasiperiodic tiling with 8-fold symmetry. (Center) A quasiperiodic tiling with 4-fold symmetry, created by distorting the 8-fold tiling. (Right) A quasiperiodic 4-fold tiling, created by a 90 degree superposition of two Fibonacci grids. periodicity is not necessary for producing long-range order, but it is still not quite clear how exactly one should characterize the existence of order. Noting that the diffraction spectra of all experimentally observed crystals contain Bragg peaks, the International Union of Crystallography 8 has redefined a crystal to be “…any solid having an essentially discrete diffraction diagram.” Crystals that are periodic on the atomic scale are explicitly called periodic crystals, all others are called aperiodic crystals. This definition is not merely an empirical one but is also motivated by the common practice of taking the set of density Fourier coefficients ρ(k) at non zero wave vectors k as the Landau order parameter, signaling a phase transition from a liquid state to an ordered solid state. …
crystal, any solid material in which the component atoms are arranged in a definite pattern and whose surface reShow more Show less crystal, any solid material in which the component atoms are arranged in a definite pattern and whose surface re
Packing of spheres is one of those subjects that we crystallographers are familiar with, since, to a reasonable approximation, we can usually treat atoms in a crystal structure as akin to spheres.… Anyway, what has resulted is what I sometimes say is the greatest book ever written! But then I am prejudiced, of course. Now, one of the odd leftovers is the question of the order in which the space group types are listed and numbered. This has been revisited in a recent publication written by Mois Aroyo and Carol Brock, which you can read about here. We also have the second article by Zbigniew Dauter and Mariusz Jaskólski, dealing with the packing of spheres in cubic space groups. Packing of spheres is one of those subjects that we crystallographers are familiar with, since, to a reasonable approximation, we can usually treat atoms in a crystal structure as akin to spheres. Another article that you may find interesting is on the development of Cryo-EM in Portugal by Célia V. Romão and Pedro M. Matias. Cryo EM is electron microscopy performed on flash frozen samples, allowing researchers to see proteins, viruses, and other macromolecules in a state very close to their natural environment, and was the subject of the Nobel Prize in Chemistry in 2017, awarded to Jacques Dubochet, Joachim Frank and Richard Henderson. …
In crystallography, crystal structure is a description of the ordered arrangement of atoms, ions, or molecules in a crystalline material. [1] Ordered structures occur from the intrinsic nature of constituent particles to form symmetric patterns that repeat along the principal directions of three-dimensional space in matter.Crystal structure of table salt (sodium in purple, chlorine in green) In crystallography, crystal structure is a description of the ordered arrangement of atoms, ions, or molecules in a crystalline material. [1] Ordered structures occur from the intrinsic nature of constituent particles to form symmetric patterns that repeat along the principal directions of three-dimensional space in matter. The smallest group of particles in a material that constitutes this repeating pattern is the unit cell of the structure. The unit cell completely reflects the symmetry and structure of the entire crystal, which is built up by repetitive translation of the unit cell along its principal axes. The translation vectors define the nodes of the Bravais lattice.
Generally speaking, crystals are solid state materials built from a long-range ordered, periodic, and symmetric arrangement of fundamental building units that are atoms, ions, or molecules.… [14, 15] These findings can be regarded as the cornerstones of modern crystallography. [13] [14] [15] These fundamental findings led to today's definition of crystals according to the International Union of Crystallography (IUCr): "A solid is a crystal if it has essentially a sharp diffraction pattern. The word essentially means that most of the intensity of the diffraction is concentrated in relatively sharp Bragg peaks, besides the always present diffuse scattering." [16] Generally speaking, crystals are solid state materials built from a long-range ordered, periodic, and symmetric arrangement of fundamental building units that are atoms, ions, or molecules. [4, 16] The properties of crystalline materials are subject to their chemical composition and their crystal structure, whereby the latter depends on the former. For the sam chemical composition, different crystal structures are often accessible depending on the crystallization conditions as defined by temperature, pressure, the solvent of crystallization etc. The according structure-property relationships are crucial for their sophisticated applications in modern technology. …
Amorphous solids such as glass, plastics and amorphous thin films are ubiquitous in our daily life and have broad applications ranging from telecommunications to electronics and solar cells1,2,3,4. However, owing to the lack of long-range order, the three-dimensional (3D) atomic structure of amorphous solids has so far eluded direct experimental determination5,6,7,8,9,10,11,12,13,14,15.View saved research * 46k Accesses * 449 Citations * 128 Altmetric * Metrics details Abstract Amorphous solids such as glass, plastics and amorphous thin films are ubiquitous in our daily life and have broad applications ranging from telecommunications to electronics and solar cells1,2,3,4. However, owing to the lack of long-range order, the three-dimensional (3D) atomic structure of amorphous solids has so far eluded direct experimental determination5,6,7,8,9,10,11,12,13,14,15. Here we develop an atomic electron tomography reconstruction method to experimentally determine the 3D atomic positions of an amorphous solid. Using a multi-component glass-forming alloy as proof of principle, we quantitatively characterize the short- and medium-range order of the 3D atomic arrangement. …
A crystal or crystalline solid is a solid material whose constituents (such as atoms, molecules, or ions) are arranged in a highly ordered microscopic structure, forming a crystal lattice that extends in all directions.Microscopically, a single crystal has atoms in a near-perfect periodic arrangement; a polycrystal is composed of many microscopic crystals (called " crystallites" or "grains"); and an amorphous solid (such as glass) has no periodic arrangement even microscopically. A crystal or crystalline solid is a solid material whose constituents (such as atoms, molecules, or ions) are arranged in a highly ordered microscopic structure, forming a crystal lattice that extends in all directions. [1] [2] In addition, macroscopic single crystals are usually identifiable by their geometrical shape, consisting of flat faces with specific, characteristic orientations. The scientific study of crystals and crystal formation is known as crystallography. The process of crystal formation via mechanisms of crystal growth is called crystallization or solidification.
When these ordered unit cells are repeated over long distances, that material is classified as crystalline.… These geometric arrangements of atoms are known as the atomic or crystal structure. Scientists and engineers have classified all of the possible atomic arrangements by geometric category, and the smallest possible group of atoms that maintain that shape are called unit cells. When these ordered unit cells are repeated over long distances, that material is classified as crystalline. When a material has no unit cell that can be repeated to describe its atomic ordering, it is classified as amorphous. Figure 1 shows representations of different geometric arrangements of common every day materials: table salt (sodium chloride), pencil “lead” (graphite), and window glass (silica). If you saw these materials at a scale 100,000 times smaller than the width of one human hair, this is what they would look like. …
When atoms or molecules are lined up in an orderly arrangement and connected by bonds, and these atoms or molecules have a repeating pattern, we can then say this material is a crystalline substance.II. Crystals and Crystal Systems A. Unit Cells When atoms or molecules are lined up in an orderly arrangement and connected by bonds, and these atoms or molecules have a repeating pattern, we can then say this material is a crystalline substance. The smallest subdivison of a crystal is a unit cell. It is a regular pattern of atoms held together by electrical forces or bonds. These unit cells are far too minute to be seen individual but can be combined together in incredibly large numbers to form visible shapes. As an example of the staggeringly large numbers of unit cells we are talking about we can take as an example sodium chloride, table salt. One typical salt grain has about 5.6x1018 unit cells. …
A crystal or crystalline solid is a solid material whose constituents (such as atoms, molecules, or ions) are arranged in a highly ordered microscopic structure, forming a crystal lattice that extends in all directions.Crystals of amethyst quartz Microscopically, a single crystal has atoms in a near-perfect periodic arrangement; a polycrystal is composed of many microscopic crystals (called " crystallites" or "grains"); and an amorphous solid (such as glass) has no periodic arrangement even microscopically. A crystal or crystalline solid is a solid material whose constituents (such as atoms, molecules, or ions) are arranged in a highly ordered microscopic structure, forming a crystal lattice that extends in all directions. In addition, macroscopic single crystals are usually identifiable by their geometrical shape, consisting of flat faces with specific, characteristic orientations. The scientific study of crystals and crystal formation is known as crystallography. The process of crystal formation via mechanisms of crystal growth is called crystallization or solidification.
A crystal (or crystalline solid) is a material whose constituent atoms, molecules, or ions are arranged in an orderly repeating pattern extending in all three spatial dimensions.Background Information A crystal (or crystalline solid) is a material whose constituent atoms, molecules, or ions are arranged in an orderly repeating pattern extending in all three spatial dimensions. The scientific study of crystals and crystal formation is known as crystallography. The process of crystal formation is called crystallization or solidification. The word crystal is derived from the ancient Greek word κρύσταλλος (krustallos), meaning both “ice” and “rock crystal”,[1] from κρύος (kruos), “icy cold, frost”.[2] [3] Examples of crystalline solids include water ice, minerals such as quartz and halite (rock salt), and many gem stones, such as rubies and diamonds. …
crystal exhibit a property called long-range order or translational periodicity; positions repeat in space in a regular array, as in Figure 2A.Learn about this topic in these articles: - amorphous solidDistinction between crystalline and amorphous solids…crystal exhibit a property called long-range order or translational periodicity; positions repeat in space in a regular array, as in Figure 2A. In an amorphous solid, translational periodicity is absent. As indicated in Figure 2B, there is no long-range order. The atoms are not randomly distributed in space, however, as… Read More…crystal exhibit a property called long-range order or translational periodicity; positions repeat in space in a regular array, as in Figure 2A. In an amorphous solid, translational periodicity is absent. As indicated in Figure 2B, there is no long-range order. The atoms are not randomly distri
In condensed matter physics and materials science, an amorphous solid (or non-crystalline solid) is a solid that lacks the long-range order that is a characteristic of a crystal. … Unlike in crystalline materials, however, no long-range regularity exists: amorphous materials cannot be described by the repetition of a finite unit cell.Amorphous solid In condensed matter physics and materials science, an amorphous solid (or non-crystalline solid) is a solid that lacks the long-range order that is a characteristic of a crystal. The terms " glass" and "glassy solid" are sometimes used synonymously with amorphous solid; however, these terms refer specifically to amorphous materials that undergo a glass transition. [1] Examples of amorphous solids include glasses, metallic glasses, and certain types of plastics and polymers. [2] [3] Etymology … Crystalline vs. amorphous solid Amorphous materials have an internal structure of molecular-scale structural blocks that can be similar to the basic structural units in the crystalline phase of the same compound. [4] Unlike in crystalline materials, however, no long-range regularity exists: amorphous materials cannot be described by the repetition of a finite unit cell. Statistical measures, such as the atomic density function and radial distribution function, are more useful in describing the structure of amorphous solids. [1] [3] Glass is a commonly encountered example of amorphous solids.
The 1992 revamped crystal definition reflects our current understanding that periodicity at the atomic scale is a sufficient but not necessary condition for crystallinity. Instead, the presence of a long-range atomic order rendering discrete diffraction patterns should be regarded as the essential attribute of crystalline matter rather than mere periodicity.… Carlos M. Pina and Victoria Sánchez-Acevedo who, after summarizing a number of studies of known minerals with aperiodic crystal structures, discuss current investigations aimed at the search for new possible quasicrystalline minerals in nature [13]. Quite interestingly, among the proposed potential candidates are skutterudite compounds, which have been intensively considered in the quest for novel thermoelectric materials during the past two decades [14]. The 1992 revamped crystal definition reflects our current understanding that periodicity at the atomic scale is a sufficient but not necessary condition for crystallinity. Instead, the presence of a long-range atomic order rendering discrete diffraction patterns should be regarded as the essential attribute of crystalline matter rather than mere periodicity. Two long standing open questions in the field concern what distributions of atoms in space are able to diffract and how to determine the exact positions of these atoms from the obtained diffraction patterns and electron microscope images. In their contribution, Ruitao Li, Zhong Li, Zhili Dong, and Khiam Aik Khor review recent progress in the structural study of QCs using transmission electron microscopy, the same tool originally used to …
The unit cell is the simplest repeating unit that comprises all crystalline solids. This basic pattern is repeated over and over to form a crystal lattice structure.In this lab, you will be investigating what a unit cell is and how it is used to visualize atoms and their interactions. This is the foundation of Materials Science and Engineering, but many other scientists must understand and utilize this information. The unit cell is the simplest repeating unit that comprises all crystalline solids. This basic pattern is repeated over and over to form a crystal lattice structure. There are 14 different unit cells and 7 lattice systems (see figure on back). All crystalline solids are based on these structures. Below are the models that you will be building from magnetic balls in activity #1. (From Lumen)
The constituents of a solid can be arranged in two general ways: they can form a regular repeating three-dimensional structure called a crystal lattice, thus producing a crystalline solid, or they can aggregate with no particular order, in which case they form an amorphous solidIntroduction With few exceptions, the particles that compose a solid material, whether ionic, molecular, covalent, or metallic, are held in place by strong attractive forces between them. When we discuss solids, therefore, we consider the positions of the atoms, molecules, or ions, which are essentially fixed in space, rather than their motions (which are more important in liquids and gases). The constituents of a solid can be arranged in two general ways: they can form a regular repeating three-dimensional structure called a crystal lattice, thus producing a crystalline solid, or they can aggregate with no particular order, in which case they form an amorphous solid (from the Greek ámorphos, meaning “shapeless”).
When most liquids are cooled, they eventually freeze and form crystalline solids, solids in which the atoms, ions, or molecules are arranged in a definite repeating pattern.- Define and describe the bonding and properties of ionic, molecular, metallic, and covalent network crystalline solids - Describe the main types of crystalline solids: ionic solids, metallic solids, covalent network solids, and molecular solids - Explain the ways in which crystal defects can occur in a solid When most liquids are cooled, they eventually freeze and form crystalline solids, solids in which the atoms, ions, or molecules are arranged in a definite repeating pattern. It is also possible for a liquid to freeze before its molecules become arranged in an orderly pattern. The resulting materials are called amorphous solids or noncrystalline solids (or, sometimes, glasses). The particles of such solids lack an ordered internal structure and are randomly arranged (Figure \(\PageIndex{1}\)). The crystalline arrangement shows many circles drawn in rows and stacked together tightly. …
Because a crystalline solid consists of repeating patterns of its components in three dimensions (a crystal lattice), we can represent the entire crystal by drawing the structure of the smallest identical units that, when stacked together, form the crystal.- To recognize the unit cell of a crystalline solid. - To calculate the density of a solid given its unit cell. Because a crystalline solid consists of repeating patterns of its components in three dimensions (a crystal lattice), we can represent the entire crystal by drawing the structure of the smallest identical units that, when stacked together, form the crystal. This basic repeating unit is called a unit cellThe smallest repeating unit of a crystal lattice.. For example, the unit cell of a sheet of identical postage stamps is a single stamp, and the unit cell of a stack of bricks is a single brick. In this section, we describe the arrangements of atoms in various unit cells. Unit cells are easiest to visualize in two dimensions. …
Many types of solid materials are what are known as crystals, which are made up of a regular, repeating pattern of atoms or molecules when viewed on the smallest scales.Develop models to describe the atomic composition of simple molecules and extended structures. Background Many types of solid materials are what are known as crystals, which are made up of a regular, repeating pattern of atoms or molecules when viewed on the smallest scales. Crystallography is the scientific study of crystals and their formation. Some common examples of crystals that we come into contact with in daily life are table salt, snowflakes, pencil lead (graphite), and metals, such as the zinc that pennies are made of or the gold and silver that is in jewelry. Gemstones like rubies, emeralds, and sapphires are also crystals. These examples demonstrate that crystals can come in many different forms and can exhibit a wide range of physical properties. …
An ideal single crystal has an atomic structure that repeats periodically across its whole volume. Even at infinite length scales, each atom is related to every other equivalent atom in the structure by translational symmetry.The fundamental difference between single crystal, polycrystalline and amorphous solids is the length scale over which the atoms are related to one another by translational symmetry ('periodicity' or 'long-range order'). Single crystals have infinite periodicity, polycrystals have local periodicity, and amorphous solids (and liquids) have no long-range order. - An ideal single crystal has an atomic structure that repeats periodically across its whole volume. Even at infinite length scales, each atom is related to every other equivalent atom in the structure by translational symmetry. - A polycrystalline solid or polycrystal is comprised of many individual grains or crystallites. Each grain can be thought of as a single crystal, within which the atomic structure has long-range order. In an isotropic polycrystalline solid, there is no relationship between neighbouring grains. Therefore, on a large enough length scale, there is no periodicity across a polycrystalline sample. …
The constituents of a solid can be arranged in two general ways: they can form a regular repeating three-dimensional structure called a crystal lattice, thus producing a crystalline solid, or they can aggregate with no particular order, in which case they form an amorphous solidIntroduction With few exceptions, the particles that compose a solid material, whether ionic, molecular, covalent, or metallic, are held in place by strong attractive forces between them. When we discuss solids, therefore, we consider the positions of the atoms, molecules, or ions, which are essentially fixed in space, rather than their motions (which are more important in liquids and gases). The constituents of a solid can be arranged in two general ways: they can form a regular repeating three-dimensional structure called a crystal lattice, thus producing a crystalline solid, or they can aggregate with no particular order, in which case they form an amorphous solid (from the Greek ámorphos, meaning “shapeless”).
Most solids form with a regular arrangement of their particles because the overall attractive interactions between particles are maximized, and the total intermolecular energy is minimized, when the particles pack in the most efficient manner.- Describe the arrangement of atoms and ions in crystalline structures - Compute ionic radii using unit cell dimensions - Explain the use of X-ray diffraction measurements in determining crystalline structures Over 90% of naturally occurring and man-made solids are crystalline. Most solids form with a regular arrangement of their particles because the overall attractive interactions between particles are maximized, and the total intermolecular energy is minimized, when the particles pack in the most efficient manner. The regular arrangement at an atomic level is often reflected at a macroscopic level. In this module, we will explore some of the details about the structures of metallic and ionic crystalline solids, and learn how these structures are determined experimentally. The Structures of Metals
In crystals the arrangement atoms and molecules is exactly repeated. … A crystal is a group of atoms, molecules, or ions arranged in ordered pattern in all three dimensions.Thinking about the Discovery Questions In this unit students investigate the structure and properties of crystals. Crystals are a common form of a solid. They are composed of repeated patterns of molecules held together by different kinds of bonds. In some solids the arrangement of atoms and molecules can be random or can vary in the material. In crystals the arrangement atoms and molecules is exactly repeated. Students will understand crystal forms by using models to investigate their structure at the atomic and molecular level. They will experiment with Molecular Workbench models to learn how temperature affects crystals and the phenomenon of melting. In the first activity "Introduction to Crystals" students will use a Molecular Workbench model. They will use this model to investigate the question, "What is a molecular crystal?". … ## Additional Background Crystals are an important part of the world we live in. A crystal is a group of atoms, molecules, or ions arranged in ordered pattern in all three dimensions. Crystals can be both organic or inorganic. Examples of organic crystals are foods like sugar, and the calcite crystals mollusks produce when forming their shells. Examples of inorganic crystals include quartz, sapphires, etc. Some crystals form perfect patterns of molecules. For example, a diamond that is pure carbon will be clear without color. Some crystals, however, may form with impurities or become flawed after formation. …
In contrast, crystalline solids have an extensively ordered structure with atoms arranged in periodic, three-dimensional patterns called crystal lattices.Crystalline Solids In contrast, crystalline solids have an extensively ordered structure with atoms arranged in periodic, three-dimensional patterns called crystal lattices. The highly organized patterns lead to areas of uniform alignment and symmetry. Examples include metals, minerals, ceramics, and semiconductors. Properties include: - Long-range order - Atoms repeat in geometric patterns over large atomic distances - Anisotropic - Properties depend on crystal direction - Definite melting point - Sharp transition from solid to liquid state
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Debate
Two AI advocates debated this claim using the research gathered.
Argument for
According to authoritative definitions from the International Union of Crystallography and IUPAC, a material is only classified as a crystal if its constituent particles form a long-range, highly ordered microscopic arrangement, which fundamentally distinguishes it from amorphous solids (Sources 2, 8, 27). While the discovery of aperiodic quasicrystals proved that this microscopic order does not strictly require traditional three-dimensional periodicity, all crystals still absolutely require a highly regular, mathematically governed spatial pattern to produce their defining sharp diffraction patterns (Sources 2, 6, 15).
The Proponent's rebuttal actually concedes the core point: by admitting that 'highly regular periodicity' is not strictly required and substituting a vaguer 'mathematically governed spatial pattern,' the Proponent quietly redefines 'highly regular' to mean whatever preserves the claim, which is a textbook No True Scotsman maneuver. Source 6's aperiodic crystals and Source 12's calaverite and feldspar structures are 'not strictly periodic' and only statistically ordered on average, so equating that with the atomic claim's plain-language demand for a 'highly regular microscopic pattern' stretches the IUCr's diffraction-based criterion (Sources 2, 5) far beyond what the original claim actually asserts.
Argument against
The claim collapses on inspection because the actual gold-standard IUCr definition (Sources 2, 3, 5) abandons strict 'regular pattern' requirements in favor of the reciprocal-space criterion—'essentially a sharp diffraction pattern'—precisely because quasicrystals like those in Source 7, 9, 11, and 15 lack the periodic, regularly repeating microscopic arrangement the claim demands, yet are indisputably classified as crystals. Even Source 9 admits quasicrystal atomic arrangements are 'not periodic' while still being crystalline, and Source 12 documents real minerals (calaverite, quartz, feldspars) with structures 'not strictly periodic,' proving that 'highly regular' periodicity is neither the technical nor the operative requirement for something to count as a crystal—making the claim an oversimplified popular misconception rather than the scientifically established definition.'
The Opponent commits a false equivalence by conflating a lack of strict three-dimensional periodicity with a lack of microscopic regularity, ignoring that the International Union of Crystallography explicitly defines even aperiodic quasicrystals as being 'fully ordered' according to 'particular mathematical rules' (Sources 2, 5). Furthermore, by cherry-picking the reciprocal-space definition, the Opponent fails to acknowledge that a sharp diffraction pattern is merely the physical manifestation of this underlying, highly regular atomic arrangement, which remains the fundamental prerequisite for crystallinity (Sources 6, 8).
Panel Review
3 reviewers assessed the evidence and the arguments.
Reviewer A · Claude
Multiple high-quality sources (2,3,5,21,24) define a crystal as having atoms/ions/molecules arranged in a highly ordered, long-range microscopic pattern, which matches the claim's wording of 'highly regular microscopic pattern' without requiring strict periodicity. The claim does not specify 'periodic,' so it accommodates aperiodic crystals/quasicrystals (Sources 6,7,9,11,15), which are still described as 'fully ordered' following 'particular mathematical rules,' consistent with 'highly regular.' The debate's disagreement centers on periodicity, but the claim as worded only requires regularity, which is satisfied by both periodic and aperiodic crystals per IUCr definitions. Thus the claim holds at its stated strength, though the precise scientific definition (reciprocal-space, diffraction-based) is more nuanced than 'regular pattern' alone.
Reviewer B · GPT
The International Union of Crystallography directly defines a crystal as a solid whose atoms, ions, or molecules form, on average, a long-range ordered arrangement, and states that even aperiodic crystals are fully ordered under particular mathematical rules [2]. IUPAC likewise identifies crystallinity with three-dimensional order at atomic dimensions [8]. These sources address the claim's microscopic-particle arrangement directly, and their definitions support “highly regular” as long-range spatial order rather than requiring strict periodic repetition. The claim is therefore true, although it should not be read as requiring a defect-free or conventionally periodic lattice.
Reviewer C · Gemini
The most reliable sources, including the International Union of Crystallography and IUPAC, define a crystal by the presence of a long-range, highly ordered microscopic arrangement of its constituent particles. While the discovery of quasicrystals expanded this definition to include aperiodic structures, these materials still require a fully ordered spatial arrangement governed by mathematical rules to produce their characteristic diffraction patterns. The claim accurately reflects this fundamental requirement of microscopic order, as 'highly regular' aligns with the scientific consensus of a 'fully ordered' structure.
Panel summary
Authoritative definitions from the International Union of Crystallography and IUPAC directly support the claim: crystals possess long-range order among atoms, ions, or molecules at microscopic scales. The only substantive qualification concerns the meaning of “highly regular.” Some simplified descriptions imply strict periodic repetition, but modern crystallography includes aperiodic crystals such as quasicrystals, whose particles remain highly ordered according to mathematical rules. Because the claim requires regular microscopic organization rather than periodicity or perfection, its wording accurately captures the defining structural feature of crystals. Several cited IUCr materials overlap institutionally, but the corroborating IUPAC definition supports the same conclusion.