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ISOSTRUCTURAL

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Exempel på hur man kan använda ISOSTRUCTURAL i en mening

  • Scolecite is isostructural (having the same structure) with the sodium-calcium zeolite mesolite and the sodium zeolite natrolite, but it does not form a continuous chemical series with either of them.
  • Olivenite is a copper arsenate that is isostructural with adamite and there is considerable substitution between zinc and copper resulting in an intermediate called cuproadamite.
  • It is an unusual ceramic, having relatively high thermal and electrical conductivities, properties it shares with isostructural titanium diboride and zirconium diboride.
  • Sodium cyanate is isostructural with sodium fulminate, confirming the linear structure of the cyanate ion.
  • The manganate(VI) ion is tetrahedral, similar to sulfate or chromate: indeed, manganates are often isostructural with sulfates and chromates, a fact first noted by Eilhard Mitscherlich in 1831.
  • However, with the help of cryptands and methylamine, pure sodium ozonide may be obtained as red crystals isostructural to.
  • It crystallizes in the Pnnm space group, which is an orthorhombically distorted variant of the rutile structure; making it isostructural to calcium chloride.
  • In addition to mixite, this mineral group contains the isostructural minerals agardite-(Y), agardite-(Ce), agardite-(Nd), agardite-(La), calciopetersite, goudeyite, petersite-(Ce), petersite-(Y), plumboagardite, and zálesíite.
  • It is isostructural with the vesuvianite group and is associated with wollastonite and olive-green grossulars (viluites) in a serpentinized skarn.
  • By contrast, the nearly isostructural tert-butyl nitrile does not readily isomerize to tert-butyl isocyanide.
  • A monoclinic mineral, julgoldite is isostructural to pumpellyite and epidote (Allman and Donnay, 1973).
  • It is an unusual ceramic, having relatively high thermal and electrical conductivities, properties it shares with isostructural titanium diboride and hafnium diboride.
  • Coloradoite, a member of the coordination subclass of tellurides, is a covalent compound that is isostructural with sphalerite (ZnS).
  • Minerals in this group are isostructural with each other and also with minerals in the crandallite and alunite groups.
  • Magnesium polonide is unusual as it is not isostructural with magnesium telluride: MgTe has a wurtzite structure, although a nickeline-type phase has also been reported.
  • "Isomorphous" when used in the relation to crystal structures is not synonymous: in addition to the same atomic connectivity that characterises isostructural compounds, isomorphous substances crystallise in the same space group and have the same unit cell dimensions.
  • The compound is isostructural with all other reported rare-earth hexaboride compounds including lanthanum hexaboride, samarium hexaboride, and cerium hexaboride.
  • Lead tetrafluoride is isostructural with tin(IV) fluoride and contains planar layers of octahedrally coordinated lead, where the octahedra share four corners and there are two terminal, unshared, fluorine atoms trans to one another.
  • Consistent with phyllosilicates, franklinphilite is composed of long flat sheets of linked silicon-oxygen and aluminium-oxygen tetrahedra bounded by an octahedral layer containing either potassium or manganese and is isostructural with lennilienapeite.
  • A miscibility gap between isostructural phases may be described as the solvus, a term also used to describe the boundary on a phase diagram between a miscibility gap and other phases.


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