Skip to main content
Log in

The polymorphism of copper-oxinate crystal

  • Originalarbeiten
  • Kolloide
  • Published:
Kolloid-Zeitschrift und Zeitschrift für Polymere Aims and scope Submit manuscript

Summary

a) Polymorphs

Copper-oxinate dihydrate has three different crystal forms, namely, α-, γ-, Β-form. The γ-form is an intermediate crystal form in the course of the α → Β transformation in aqueous suspension. They gave three anhydrous polymorphs respectively, that is, the α′-,γ′- and Β′-forms by the dehydration and they are all transformed into the most stable anhydride (Β∼-form). The Β′-form is also precipitated directly from the solution at about boiling temperature. The relationships among the various crystal forms are also discussed.

b) Crystal structure

The cell dimensions of the γ-form dihydrated crystal are assumed to be a=13.10 å. b=8.33 å, c=9.49 å and Β=106‡.

The Β′-form anhydride has the following lattice Constants a=12.25 å, b=3.78 å, c=14.95 å and Β=98.6‡ with the space group P2/c(C 42h ).

Zusammenfassung

a) Polymorphismus

Kupferoxynat-Dihydrat hat drei verschiedene Kristall-formen, nÄmlich die Alpha-, Gamma- und Beta-form. Die Gamma-Form ist eine intermediÄre Kristallform im Verlauf der Umwandlung von der Alpha- in die Beta-Form in wÄ\riger Suspension. Diese Umwandlungen ergeben 3 polymorphe Anhydrite, nÄmlich die Alpha-, Gamma- und Beta-Form durch Dehydrierung, und sie alle gehen über in die stabilste Anhydritdibeta-Form. Die Beta-Form fÄllt auch direkt aus der Lösung etwa bei der Siedetemperatur aus. Die Beziehung zwischen den verschiedenen Kristallformen wird ebenfalls diskutiert.

b) Kristallstrukturen

Die Parameter der Elementarzelle der Gamma-Form des dihydrierten Kristalls werden zu α=13,10 å, b=8,3 å, c=9,49 å und Β=106‡ festgestellt. Die Beta-Form des Anhydrits hat die folgenden Gitterkonstanten α=12,2 å, b=3,38 å, c=14,95 å und Β=98,6‡ und die Raumgruppe P2/c(C 7/42h ).

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  1. Suito, E. and E. Sekido, Proc. Japan Acad. 33, 196 (1957). Ishibashi, M., E. Suito and E. Sekido, J. Chem. Soc. Japan 77, 1836 (1956); 78, 1784 (1967), 80, 379 (1959).

    CAS  Google Scholar 

  2. Uyeda, N. and E. Suito, Colloid-Z. 193, 97 (1963).

    Google Scholar 

  3. Merrit, L. L., R. T. Cady and B. W. Mundy, Acta Cryst. 7, 473 (1954).

    Article  Google Scholar 

  4. Kruh, R. and C. W. Dwiggins, J. Amer. Chem. Soc. 77, 806 (1955).

    Article  CAS  Google Scholar 

  5. Palenik, G. J., Acta Cryst. 17, 687 (1964).

    Article  CAS  Google Scholar 

  6. Kanamaru, F., K. Ogawa and I. Nitta, Bull. Chem. Soc. Japan 36, 422 (1963).

    Article  CAS  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Suito, E., Arakawa, M. & Kobayashi, T. The polymorphism of copper-oxinate crystal. Kolloid-Z.u.Z.Polymere 212, 155–161 (1966). https://doi.org/10.1007/BF01553082

Download citation

  • Received:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF01553082

Keywords

Navigation