A Difference Band of a Fundamental and a Lattice Mode in the Infra-red Spectra of Lead and Other Carbonates-Reference-Cited by-同舟云学术

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A Difference Band of a Fundamental and a Lattice Mode in the Infra-red Spectra of Lead and Other Carbonates

Published:1961-10 Issue:4800 Volume:192 Page:351-352
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

SCHUTTE C. J. H.,BUIJS K.

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/192351a0.pdf

Reference2 articles.

1. Landolt-Börnstein, Zahlenwerte und Funktionen, 4 (Springer Verlag, 1955).

2. Haas, C., thesis, Amsterdam (1956). Shultin, A. A., Dokl. Akad. Nauk S.S.S.R., 125, 767 (1959) assigns the bans in NaNO3 to a component of Davydov splitting of the ν2 mode. This assignment is not in agreement with the temperature-dependence of the intensity which he finds.

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1. Single crystal raman spectroscopy of cerussite;American Mineralogist;2004-02

2. Crystal structure and infrared spectrum of anhydrous guanidinium copper(II) carbonate;Journal of the Chemical Society, Dalton Transactions;1981

3. The Characterization of Soil Minerals by Infrared Spectroscopy;Soil Components;1975

4. Infrared Determination of Alkali Carbonates by the Pellet Technique Using a Dry Box;Applied Spectroscopy;1974-03

5. Factors affecting the infrared spectra of planar anions with D3h, symmetry—V;Spectrochimica Acta Part A: Molecular Spectroscopy;1971-07

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