scholarly journals K+[K(CO)8]-: an antipodal crystalline salt of alkalide [K(C222)]+K-

Author(s):  
xiaoyong yang
Keyword(s):  
2018 ◽  
Vol 131 ◽  
pp. 109-119 ◽  
Author(s):  
Mustafa Bookwala ◽  
Priyanka Thipsay ◽  
Samir Ross ◽  
Feng Zhang ◽  
Suresh Bandari ◽  
...  

1977 ◽  
Vol 30 (5) ◽  
pp. 957 ◽  
Author(s):  
SD Hamann ◽  
E Spinner

The infrared spectra of the solid metal formates HCO2Li, HCO2Li,H2O, HCO2Na, DCO2Na, H13CO2Na, HCO2K, DCO2K, HCO2Rb, DCO2Rb, HCO2Cs, DCO2Cs, (HCO2)2Ca, (HCO2)2Sr, (HCO2)2Ba and (HCO2)2Pb have been measured in the pressure range 0-42 kbar at 25�C. For the sodium salt two new modifications formed at high pressure have been observed, but the potassium, rubidium and caesium salts show only one phase transition. A phase change, though only at pressures far above 42 kbar, is indicated also for the calcium, the barium and probably the anhydrous lithium salt. The various spectral responses to changes in pressure strongly indicate that in the form prevailing at ordinary pressure and temperature, phase I, the formates of sodium and potassium have the same type of molecular packing in the crystal structure. Phases II of the sodium and potassium salt appear to belong to a new modification (?C?), whereas phase III of the sodium and phase II of the caesium salt belong to the modification ?B? previously observed in disc spectra. In a given phase, the effect of pressure on the formate vibration frequencies is sometimes quite different for the pure crystalline salt in bulk and for the same species when isolated by isotopic dilution. In these cases the main effect of pressure is that on the intermolecular coupling of vibrations. Several frequency changes accompanying phase transitions, by contrast, are essentially unchanged on isotopic dilution and arise mainly from changes in the effective intramolecular force constants.


Geophysics ◽  
1948 ◽  
Vol 13 (4) ◽  
pp. 584-594 ◽  
Author(s):  
Haakon M. Evjen

Based directly on Maxwell’s Field Equations, the extremely low end of the frequency spectrum may be reduced in first approximation to simple potential theory. The approximation theory is borne out by some field experiments, the results of which are presented. Agreement with the theory, however, requires that the ground have a very large effective dielectric constant. This conclusion is supported by previous observations by a number of independent observers. Thus, the relaxation time has been found to be extremely great, not only in observations directly on the ground, but also in small samples of mud, and the sign of an electric anomaly over a relative insulator, such as crystalline salt or gas and oil, invariably has been found to be negative. Both of these observations can be explained in terms of a very great dielectric constant. The value yielded by the present experimental work is of the order of [Formula: see text].


Soil Science ◽  
1970 ◽  
Vol 109 (3) ◽  
pp. 170-178 ◽  
Author(s):  
D. R. SCOTTER ◽  
P. A. C. RAATS
Keyword(s):  

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