ChemInform ◽  
1989 ◽  
Vol 20 (33) ◽  
Author(s):  
J. LORBERTH ◽  
S.-H. SHIN ◽  
S. WOCADLO ◽  
W. MASSA
Keyword(s):  

Author(s):  
F. A. Bannister

In a brief account of the Johnston-Lavis collection of Vesuvian minerals, now preserved in University College, London, Dr. K. W. Earle mentions ‘a large number of specimens of “Thermokalite”, a new member of the Haloid group, which has, apparently, so far escaped description.’ This previously unpublished name was copied from Dr. Johnston-Lavis's manuscript labels. The late Dr. H. J. Johnston-Lavis (1856-1914) possibly considered that this mineral was the potassium compound corresponding to thermonatrite [Na2CO3.H2O]. A provisional name for an undetermined mineral having, in this way, unfortunately been published, it seemed desirable to clear up the matter. For this purpose Dr. Earle very kindly supplied two good specimens of the mineral for investigation. Access was also given to the note-books kept by Dr. Johnston-Lavis. He had made a separate entry for each specimen and the carbon copies were placed with the specimens. The entry for ‘thermokalite’ reads in every case : ‘Thermokalite (n. sp.) by Tunnel nr. Stufe di Nerone, Baja.’ This locality is situated about nine miles west of Naples in the Phlegrean Fields (Campi Phlegraei).


2013 ◽  
Vol 25 (14) ◽  
pp. 8217-8218
Author(s):  
Hai-Xing Liu ◽  
Qing Liu ◽  
Lin-Tong Wang ◽  
Huan-Mei Guo ◽  
Kai-Qi Ye ◽  
...  

1961 ◽  
Vol 39 (4) ◽  
pp. 799-807 ◽  
Author(s):  
G. W. H. Scherf ◽  
R. K. Brown

Equimolar quantities of 9-fluorenyl-potassium, -sodium, or -lithium and alkyl or aralkyl halides at room temperature in ether solvents yielded a mixture of unchanged fluorene, C9-monosubstituted fluorene, and C9-disubstituted fluorene. The amount of disubstitution never exceeded that of unchanged fluorene, and was found to be maximum (∼35%) for the potassium compound in 1,2-dimethoxyethane, somewhat less for the sodium analogue, and small (∼5%) for the lithium compound. In hydrocarbon solvents such as hexane, 9-fluorenylpotassium gave only 7% of C9-disubstituted fluorene. The lithium compound, upon reaction with methyl iodide or ethyl iodide gave, along with unreacted fluorene, only C9-monosubstituted fluorene. But reaction of 9-fluorenyllithium with benzyl chloride in hexane gave a small quantity (∼5%) of disubstituted fluorene as well as the monosubstituted product.The results are explained in terms of (a) the solubilities of the organometallic compounds in ether and hydrocarbon solvents, (b) the polarity of the metal carbon bond, and (c) the acidity of the hydrogen on C9 of fluorene.


ChemInform ◽  
2014 ◽  
Vol 45 (31) ◽  
pp. no-no
Author(s):  
Bao-Xia Dong ◽  
Liang Song ◽  
Jun Ge ◽  
Yun-Lei Teng ◽  
Shi-Yang Zhang

1994 ◽  
Vol 49 (10) ◽  
pp. 1368-1372 ◽  
Author(s):  
Yue Qing Zheng ◽  
Arnold Adam

Abstract The new complex carbonate Rb2[Mg(CO3)2(H2O))4] crystallizes in the Baylissite-type structure with a = 1130,4(3), b = 641,9(1), c = 703,3(2) pm, β = 99,62(1)°, VEZ = 503,2(2), space group P21/n (No. 14) and Z = 2. In comparison with the isostructural potassium compound the cell dimensions increase in b- and c- and decrease in a-direction. This effect depends on the greater coordination number of Rb+ and the rigidity of strong hydrogen bonds. The carbonate anion exhibits significant deviations from D3h-symmetry (C -O: 127,1(5)-130,2(5) pm, ∠ O - C - O: 117,9(4)-121,1(3)°).


Crystals ◽  
2020 ◽  
Vol 10 (11) ◽  
pp. 1052
Author(s):  
Martha Falk ◽  
Marco Wendorff ◽  
Caroline Röhr

The Ga-rich gallides of the alkali metals present an interesting, yet still scarcely investigated case of polyanionic cluster compounds with subtle variations in the character of their chemical bonding. In the present work, the Ga richest phases K3Ga13, RbGa7, and CsGa7, which are formally electron-precise Zintl/Wade cluster compounds, are systematically studied with respect to a partial substitution of Ga by In and Hg. The pure hepta-gallides AGa7 (A = Rb/Cs; R3¯m), which were formerly obtained from Ga-rich melts in powder form only, were crystallized from Hg-rich melts. Herein, up to 9.9/13.6% (Rb/Cs) of Ga could be substituted by In, which partly takes the four-bonded [M2] dumbbells connecting layers of Ga-icosahedra. Even though the structures are electron precise, the pseudo band gap does not coincide with the Fermi level. In the most Ga-rich potassium compound K3Ga13 (Cmcm) only 1.2% of In and 2.7% of Hg could be incorporated. Although Rb3Ga13 remains unknown, ternary variants containing 5.2 to 8.2% In could be obtained; this structure is also stabilized by a small Hg-proportion. The likewise closed-shell 3D polyanion consists of all-exo-bonded Ga-icosahedra and closo [Ga11] clusters, which are connected by two tetrahedrally four-bonded Ga− and a trigonal-planar three-bonded Ga0. The aspects of the electronic structures and the site-specific Ga↦Hg/In substitution in the polyanion (“coloring”) are discussed for the title compounds and other mixed Ga/In trielides.


1995 ◽  
Vol 50 (8) ◽  
pp. 1185-1194 ◽  
Author(s):  
Yue Qing Zheng ◽  
Arnold Adam

The new alkalimetal-hydrogenbis(carbonato)-bis(carbonato)complexes with penta-coordinated zinc atoms, NaA2{Zn2[H(CO3)2](CO3)2(H2O)2} with A = Kor Rb, crystallize in the monoclinic system, P21/n (no. 14), Z = 2 with a = 1057,9(1), b = 1102,2(1), c = 514,9(1) pm, β = 92,94(1)°, VEZ = 599,6(2) · 106 pm3, R = 0,052, Rw = 0,029 for the potassium compound and with a = 1068,2(2), b = 1131,6(4), c = 518,6(1) pm, β = 92,07(1)°, VEZ = 626,4(4)·106 pm3, R = 0,050, Rw = 0,028 for the rubidium compound. These compounds are the first to be structurally characterized with a simultaneous presence of discrete [H(CO3)2]3-and CO32- anions. The crystal structure of the isostructural compounds contains two-dimensional infinite {Zn2[H(CO3)2](CO3)2(H2O)2} layers parallel [1 0 1] with zinc coordinated in a slightly distorted trigonal-bipyramidal geometry. The layers are held together by hydrogen bonds from water molecules to oxygen atoms of the carbonato groups in adjacent layers. Potassium or rubidium atoms are located between the layers, and sodium atoms in smaller vacancies within the layers. The hydrogen bond of the [H(CO3)2]3- anion is very short, O···O: 247,4(2) pm (K) and 246,9(5) pm (Rb). The carbonate groups in both compounds exhibit significant deviations from D3h symmetry in accordance with the vibrational modes observed in the IR spectra. The thermal behaviour of the potassium compound is also reported.


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