Standard

Comparison of orientations of OH-bonds in layer silicates by diffraction methods and electrostatic calculations. / Bookin, A. S.; Drits, V. A.; Rozdestvenskaya, I. V.; Semenova, T. F.; Tsipursky, S. I.

в: Clays & Clay Minerals, Том 30, № 6, 01.01.1982, стр. 409-414.

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

Harvard

Bookin, AS, Drits, VA, Rozdestvenskaya, IV, Semenova, TF & Tsipursky, SI 1982, 'Comparison of orientations of OH-bonds in layer silicates by diffraction methods and electrostatic calculations.', Clays & Clay Minerals, Том. 30, № 6, стр. 409-414. https://doi.org/10.1346/CCMN.1982.0300602

APA

Bookin, A. S., Drits, V. A., Rozdestvenskaya, I. V., Semenova, T. F., & Tsipursky, S. I. (1982). Comparison of orientations of OH-bonds in layer silicates by diffraction methods and electrostatic calculations. Clays & Clay Minerals, 30(6), 409-414. https://doi.org/10.1346/CCMN.1982.0300602

Vancouver

Author

Bookin, A. S. ; Drits, V. A. ; Rozdestvenskaya, I. V. ; Semenova, T. F. ; Tsipursky, S. I. / Comparison of orientations of OH-bonds in layer silicates by diffraction methods and electrostatic calculations. в: Clays & Clay Minerals. 1982 ; Том 30, № 6. стр. 409-414.

BibTeX

@article{9a9e628553db4d2aa7634ff34d0c7705,
title = "Comparison of orientations of OH-bonds in layer silicates by diffraction methods and electrostatic calculations.",
abstract = "The positions of hydroxyl protons in 2:1 layers of chlorites and micas are mainly determined by electrostatics. For the hydroxyls of dickite, amesite and the brucite sheets of chlorite, systematically different results are given by the two methods. Causes and implications of these results are discussed.-D.F.B.",
author = "Bookin, {A. S.} and Drits, {V. A.} and Rozdestvenskaya, {I. V.} and Semenova, {T. F.} and Tsipursky, {S. I.}",
year = "1982",
month = jan,
day = "1",
doi = "10.1346/CCMN.1982.0300602",
language = "English",
volume = "30",
pages = "409--414",
journal = "Clays and Clay Minerals",
issn = "0009-8604",
publisher = "Clay Minerals Society",
number = "6",

}

RIS

TY - JOUR

T1 - Comparison of orientations of OH-bonds in layer silicates by diffraction methods and electrostatic calculations.

AU - Bookin, A. S.

AU - Drits, V. A.

AU - Rozdestvenskaya, I. V.

AU - Semenova, T. F.

AU - Tsipursky, S. I.

PY - 1982/1/1

Y1 - 1982/1/1

N2 - The positions of hydroxyl protons in 2:1 layers of chlorites and micas are mainly determined by electrostatics. For the hydroxyls of dickite, amesite and the brucite sheets of chlorite, systematically different results are given by the two methods. Causes and implications of these results are discussed.-D.F.B.

AB - The positions of hydroxyl protons in 2:1 layers of chlorites and micas are mainly determined by electrostatics. For the hydroxyls of dickite, amesite and the brucite sheets of chlorite, systematically different results are given by the two methods. Causes and implications of these results are discussed.-D.F.B.

UR - http://www.scopus.com/inward/record.url?scp=0020331182&partnerID=8YFLogxK

U2 - 10.1346/CCMN.1982.0300602

DO - 10.1346/CCMN.1982.0300602

M3 - Article

AN - SCOPUS:0020331182

VL - 30

SP - 409

EP - 414

JO - Clays and Clay Minerals

JF - Clays and Clay Minerals

SN - 0009-8604

IS - 6

ER -

ID: 50027343