Hubbry Logo
DisphenoidDisphenoidMain
Open search
Disphenoid
Community hub
Disphenoid
logo
8 pages, 0 posts
0 subscribers
Be the first to start a discussion here.
Be the first to start a discussion here.
Disphenoid
Disphenoid
from Wikipedia

The tetragonal and digonal disphenoids can be positioned inside a cuboid bisecting two opposite faces. Both have four equal edges going around the sides. The digonal has two pairs of congruent isosceles triangle faces, while the tetragonal has four congruent isosceles triangle faces.
A rhombic disphenoid has congruent scalene triangle faces, and can fit diagonally inside of a cuboid. It has three sets of edge lengths, existing as opposite pairs.

In geometry, a disphenoid (from Greek sphenoeides 'wedgelike') is a tetrahedron whose four faces are congruent acute-angled triangles.[1] It can also be described as a tetrahedron in which every two edges that are opposite each other have equal lengths. Other names for the same shape are isotetrahedron,[2] sphenoid,[3] bisphenoid,[3] isosceles tetrahedron,[4] equifacial tetrahedron,[5] almost regular tetrahedron,[6] and tetramonohedron.[7]

All the solid angles and vertex figures of a disphenoid are the same, and the sum of the face angles at each vertex is equal to two right angles. However, a disphenoid is not a regular polyhedron, because, in general, its faces are not regular polygons, and its edges have three different lengths.

Special cases and generalizations

[edit]

If the faces of a disphenoid are equilateral triangles, it is a regular tetrahedron with Td tetrahedral symmetry, although this is not normally called a disphenoid. When the faces of a disphenoid are isosceles triangles, it is called a tetragonal disphenoid. In this case it has D2d dihedral symmetry. A sphenoid with scalene triangles as its faces is called a rhombic disphenoid and it has D2 dihedral symmetry. Unlike the tetragonal disphenoid, the rhombic disphenoid has no reflection symmetry, so it is chiral.[8] Both tetragonal disphenoids and rhombic disphenoids are isohedra: as well as being congruent to each other, all of their faces are symmetric to each other.

It is not possible to construct a disphenoid with right triangle or obtuse triangle faces.[4] When right triangles are glued together in the pattern of a disphenoid, they form a flat figure (a doubly-covered rectangle) that does not enclose any volume.[8] When obtuse triangles are glued in this way, the resulting surface can be folded to form a disphenoid (by Alexandrov's uniqueness theorem) but one with acute triangle faces and with edges that in general do not lie along the edges of the given obtuse triangles.

Two more types of tetrahedron generalize the disphenoid and have similar names. The digonal disphenoid has faces with two different shapes, both isosceles triangles, with two faces of each shape. The phyllic disphenoid similarly has faces with two shapes of scalene triangles.

Disphenoids can also be seen as digonal antiprisms or as alternated quadrilateral prisms.

Characterizations

[edit]

A tetrahedron is a disphenoid if and only if its circumscribed parallelepiped is right-angled.[9]

We also have that a tetrahedron is a disphenoid if and only if the center in the circumscribed sphere and the inscribed sphere coincide.[10]

Another characterization states that if d1, d2 and d3 are the common perpendiculars of AB and CD; AC and BD; and AD and BC respectively in a tetrahedron ABCD, then the tetrahedron is a disphenoid if and only if d1, d2 and d3 are pairwise perpendicular.[9]

The disphenoids are the only polyhedra having infinitely many non-self-intersecting closed geodesics. On a disphenoid, all closed geodesics are non-self-intersecting.[11]

The disphenoids are the tetrahedra in which all four faces have the same perimeter,[10] the tetrahedra in which all four faces have the same area,[10][12] and the tetrahedra in which the angular defects of all four vertices equal π. They are the polyhedra having a net in the shape of an acute triangle, divided into four similar triangles by segments connecting the edge midpoints.[6]

Metric formulas

[edit]

The volume of a disphenoid with opposite edges of length l, m and n is given by[13]

The circumscribed sphere has radius[13] (the circumradius)

and the inscribed sphere has radius[13]

where V is the volume of the disphenoid and T is the area of any face, which is given by Heron's formula. There is also the following interesting relation connecting the volume and the circumradius:[13]

The squares of the lengths of the bimedians are[13]

Other properties

[edit]

If the four faces of a tetrahedron have the same perimeter, then the tetrahedron is a disphenoid.[10]

If the four faces of a tetrahedron have the same area, then it is a disphenoid.[9][10]

The centers in the circumscribed and inscribed spheres coincide with the centroid of the disphenoid.[13]

The bimedians are perpendicular to the edges they connect and to each other.[13]

Honeycombs and crystals

[edit]
A space-filling tetrahedral disphenoid inside a cube. Two edges have dihedral angles of 90°, and four edges have dihedral angles of 60°.

Some tetragonal disphenoids will form honeycombs. The disphenoid whose four vertices are (−1, 0, 0), (1, 0, 0), (0, 1, 1), and (0, 1, −1) is such a disphenoid.[14][15] Each of its four faces is an isosceles triangle with edges of lengths 3, 3, and 2. It can tessellate space to form the disphenoid tetrahedral honeycomb. As Gibb (1990) describes, it can be folded without cutting or overlaps from a single sheet of a4 paper.[16]

"Disphenoid" is also used to describe two forms of crystal:

  • A wedge-shaped crystal form of the tetragonal or orthorhombic system. It has four triangular faces that are alike and that correspond in position to alternate faces of the tetragonal or orthorhombic dipyramid. It is symmetrical about each of three mutually perpendicular diad axes of symmetry in all classes except the tetragonal-disphenoidal, in which the form is generated by an inverse tetrad axis of symmetry.
  • A crystal form bounded by eight scalene triangles arranged in pairs, constituting a tetragonal scalenohedron.

Other uses

[edit]

Six tetragonal disphenoids attached end-to-end in a ring construct a kaleidocycle, a paper toy that can rotate on 4 sets of faces in a hexagon. The rotation of the six disphenoids with opposite edges of length l, m and n (without loss of generality nl, nm) is physically realizable if and only if[17]

See also

[edit]

References

[edit]
[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
In geometry, a disphenoid (from Greek sphenoeides, meaning "wedge-like"), also known as an isosceles tetrahedron, is a tetrahedron whose four faces are congruent acute-angled triangles. This polyhedron is defined by three pairs of opposite edges of equal lengths aa, bb, and cc. It exhibits central symmetry about its centroid, through which the lines connecting the midpoints of each pair of opposite edges pass; disphenoids are the only irregular tetrahedra with this property. The faces satisfy the triangle inequality to ensure the tetrahedron is non-degenerate and convex. Disphenoids are notable in the study of Heronian tetrahedra, which have integer edge lengths and rational volume, and admit a volume formula analogous to : V2=1288(a2+b2c2)(a2b2+c2)(b2+c2a2)V^2 = \frac{1}{288} (a^2 + b^2 - c^2)(a^2 - b^2 + c^2)(b^2 + c^2 - a^2). Special cases include the tetragonal disphenoid with isosceles triangular faces and the regular when a=b=ca = b = c. They appear in as wedge-shaped forms in tetragonal or orthorhombic systems.

Definition and History

Definition

A disphenoid is a special type of in which all four faces are congruent acute-angled triangles. This distinguishes it from more general tetrahedra, as the congruence of faces imposes a specific on the structure. The disphenoid is isohedral, meaning it is face-transitive with all faces identical, though it is not necessarily regular unless all edges are equal. It features exactly three pairs of opposite edges, each pair equal in length and denoted by parameters aa, bb, and cc, where opposite edges share no common vertex. This edge-pairing configuration ensures the triangular faces are scalene or isosceles but always congruent to one another. One standard geometric construction positions the vertices at (±x,0,0)(\pm x, 0, 0), (0,±y,0)(0, \pm y, 0), and (0,0,±z)(0, 0, \pm z) in a Cartesian coordinate system, with x,y,z>0x, y, z > 0. The values of xx, yy, and zz must be selected to guarantee that all angles in each triangular face are acute, preventing any obtuse or right angles.

History and Etymology

The term disphenoid derives from sphenoeidēs, meaning "wedge-shaped" or "wedgelike," a descriptor that captures the polyhedron's characteristic form resembling a double wedge or paired triangular prisms. The related term sphenoid has been used in since the to describe wedge-like structures observed in minerals. The prefix di- emphasizes the form's composition from two such sphenoids alternating in orientation, a rooted in crystallographic morphology. Unlike the regular tetrahedron, which was known to ancient Greek mathematicians such as Euclid as one of the Platonic solids, the disphenoid—a non-regular variant—lacks references in classical antiquity and emerged later as an extension of Euclidean geometry into irregular polyhedra. Systematic descriptions of similar wedge-shaped forms appeared in 19th-century crystallographic studies, analyzing tetrahedral crystals in minerals like chalcopyrite and noting their congruent triangular faces without using the precise term disphenoid. The English term disphenoid first appeared in print in 1895, coined by British mineralogist Nevil Story-Maskelyne in his treatise on crystal morphology, marking its entry into scientific literature as a specific geometric and mineralogical concept. In the , the disphenoid gained prominence in polyhedral geometry, often termed an isosceles tetrahedron or isotetrahedron to highlight its property of pairwise equal opposite edges. Mathematician H.S.M. Coxeter contributed to its standardization in works like Regular Polytopes (3rd edition, 1973), where he classified it among irregular tetrahedra with congruent faces, distinguishing tetragonal (isosceles-faced) and rhombic (scalene-faced) subtypes and integrating it into broader discussions of symmetry and polytopes.

Geometric Characterizations

Structural Characterizations

A disphenoid can be characterized as a that admits a circumscribed possessing right angles, where the centers of each pair of opposite edges of the tetrahedron lie at the centers of the corresponding faces of this parallelepiped. This rectangular parallelepiped is formed by completing the tetrahedron such that its edges become the face diagonals of the parallelepiped, and the right angles ensure the structural congruence of the disphenoid's faces. Another equivalent structural condition is that the centers of the and the coincide at the of the . This concentricity of the insphere and circumsphere distinguishes the disphenoid among tetrahedra, as the and circumcenter align due to the balanced edge pairings. The disphenoid is also defined by the property that the common between each pair of opposite edges is to both edges and passes through their midpoints, with these three common perpendiculars being mutually and concurrent at the . These common perpendiculars reflect the orthogonal inherent in the edge pairings, ensuring the tetrahedron's isohedral nature without relying on facial congruence alone. Finally, a qualifies as a disphenoid all four faces have equal perimeters, which implies that opposite edges are equal in length. This perimeter equality enforces the congruence of the triangular faces, providing a metric-free structural invariant that uniquely identifies the form.

Symmetry Properties

A disphenoid, as a with four congruent triangular faces and three pairs of equal opposite edges, possesses properties that are subgroups of the full tetrahedral TdT_d. This reduction occurs because the three pairs of edges have distinct lengths, preserving only specific rotations while eliminating higher symmetries like 3-fold axes. The exact symmetry group varies with the face type. Tetragonal disphenoids, featuring isosceles triangular faces, belong to the point group D2dD_{2d} (Hermann-Mauguin notation 4ˉ2m\bar{4}2m), which includes a principal 4-fold rotoinversion axis (S4S_4) along the elongation direction, two perpendicular 2-fold rotation axes (C2C_2), and two dihedral mirror planes (σd\sigma_d). This symmetry arises from viewing the shape as a regular elongated along a C2C_2 axis, maintaining reflection symmetries. In contrast, rhombic disphenoids with scalene triangular faces exhibit the lower symmetry of the point group D2D_2 (Hermann-Mauguin notation ), comprising three mutually perpendicular 2-fold rotation axes passing through the midpoints of opposite edges, but lacking any mirror planes, inversion centers, or rotoinversions. The absence of improper rotations in D2D_2 renders rhombic disphenoids chiral, meaning they occur in enantiomorphic pairs that are non-superimposable mirror images. All disphenoids are isohedral, with the symmetry operations transitively mapping any face to any other, ensuring equivalence among the four congruent triangles. This isohedral property underscores their classification as face-transitive tetrahedra, distinct from general tetrahedra lacking such uniformity.

Metric Properties

Formulas for Dimensions

A disphenoid with opposite edge lengths aa, bb, and cc can be coordinatized by placing its vertices at (u,v,w)(u, v, w), (u,v,w)(u, -v, -w), (u,v,w)(-u, v, -w), and (u,v,w)(-u, -v, w), where u,v,w>0u, v, w > 0. The corresponding edge lengths are then a=2u2+v2,b=2u2+w2,c=2v2+w2.a = 2\sqrt{u^2 + v^2}, \quad b = 2\sqrt{u^2 + w^2}, \quad c = 2\sqrt{v^2 + w^2}.
Add your contribution
Related Hubs
User Avatar
No comments yet.