Standard

The possibilities and limitations of electrostatic approximation in determining the orientation of OH-bonds in layered silicates. / Bukin, A. S.; Drits, V. A.; Rozhdestvenskaya, I. V.; Semenova, T. F.; Tsipursky, S. I.

в: Mineralogicheskii Zhurnal, Том 4, № 3, 01.01.1982, стр. 29-34.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Bukin, AS, Drits, VA, Rozhdestvenskaya, IV, Semenova, TF & Tsipursky, SI 1982, 'The possibilities and limitations of electrostatic approximation in determining the orientation of OH-bonds in layered silicates.', Mineralogicheskii Zhurnal, Том. 4, № 3, стр. 29-34.

APA

Bukin, A. S., Drits, V. A., Rozhdestvenskaya, I. V., Semenova, T. F., & Tsipursky, S. I. (1982). The possibilities and limitations of electrostatic approximation in determining the orientation of OH-bonds in layered silicates. Mineralogicheskii Zhurnal, 4(3), 29-34.

Vancouver

Bukin AS, Drits VA, Rozhdestvenskaya IV, Semenova TF, Tsipursky SI. The possibilities and limitations of electrostatic approximation in determining the orientation of OH-bonds in layered silicates. Mineralogicheskii Zhurnal. 1982 Янв. 1;4(3):29-34.

Author

Bukin, A. S. ; Drits, V. A. ; Rozhdestvenskaya, I. V. ; Semenova, T. F. ; Tsipursky, S. I. / The possibilities and limitations of electrostatic approximation in determining the orientation of OH-bonds in layered silicates. в: Mineralogicheskii Zhurnal. 1982 ; Том 4, № 3. стр. 29-34.

BibTeX

@article{d9b3119d09304546bfcf7c5b465d2528,
title = "The possibilities and limitations of electrostatic approximation in determining the orientation of OH-bonds in layered silicates.",
abstract = "Orientations of the OH-vectors of the structural OH-groups of layered silicates have been determined from diffraction data and from calculations of electrostatic energy. A comparison of the results from both methods has shown that in the hydroxyls of the 2:1 layers of micas and chlorites, the position of the hydroxyl proton is mainly determined by electrostatics. In the case of the internal hydroxyls of dickite and those of the brucite lattice of the chlorites, the results derived from these two methods differ constantly, indicating a change in the nature of the bond in these hydroxyl groups. -D.A.B.",
author = "Bukin, {A. S.} and Drits, {V. A.} and Rozhdestvenskaya, {I. V.} and Semenova, {T. F.} and Tsipursky, {S. I.}",
year = "1982",
month = jan,
day = "1",
language = "русский",
volume = "4",
pages = "29--34",
journal = "МИНЕРАЛОГИЧЕСКИЙ ЖУРНАЛ",
issn = "0204-3548",
publisher = "Институт геохимии, минералогии и рудообразования НАН Украины",
number = "3",

}

RIS

TY - JOUR

T1 - The possibilities and limitations of electrostatic approximation in determining the orientation of OH-bonds in layered silicates.

AU - Bukin, A. S.

AU - Drits, V. A.

AU - Rozhdestvenskaya, I. V.

AU - Semenova, T. F.

AU - Tsipursky, S. I.

PY - 1982/1/1

Y1 - 1982/1/1

N2 - Orientations of the OH-vectors of the structural OH-groups of layered silicates have been determined from diffraction data and from calculations of electrostatic energy. A comparison of the results from both methods has shown that in the hydroxyls of the 2:1 layers of micas and chlorites, the position of the hydroxyl proton is mainly determined by electrostatics. In the case of the internal hydroxyls of dickite and those of the brucite lattice of the chlorites, the results derived from these two methods differ constantly, indicating a change in the nature of the bond in these hydroxyl groups. -D.A.B.

AB - Orientations of the OH-vectors of the structural OH-groups of layered silicates have been determined from diffraction data and from calculations of electrostatic energy. A comparison of the results from both methods has shown that in the hydroxyls of the 2:1 layers of micas and chlorites, the position of the hydroxyl proton is mainly determined by electrostatics. In the case of the internal hydroxyls of dickite and those of the brucite lattice of the chlorites, the results derived from these two methods differ constantly, indicating a change in the nature of the bond in these hydroxyl groups. -D.A.B.

UR - http://www.scopus.com/inward/record.url?scp=0019912005&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0019912005

VL - 4

SP - 29

EP - 34

JO - МИНЕРАЛОГИЧЕСКИЙ ЖУРНАЛ

JF - МИНЕРАЛОГИЧЕСКИЙ ЖУРНАЛ

SN - 0204-3548

IS - 3

ER -

ID: 50027533