A spectroscopic study of the reaction of gold atoms with CO in a rotating cryostat: formation of a variety of gold carbonyls

1989 ◽  
Vol 67 (4) ◽  
pp. 655-661 ◽  
Author(s):  
J. H. B. Chenier ◽  
J. A. Howard ◽  
H. A. Joly ◽  
B. Mile ◽  
M. Tomietto

Reaction of 197Au atoms with CO has been studied in inert hydrocarbon matrices in a rotating cryostat at 77 K by EPR, FTIR, and UV/visible spectroscopy. Au(CO)2 has been positively identified by FTIR spectroscopy and there is evidence for the formation of AuCO, a gold microcrystallite – CO complex and, upon annealing, Au2(CO)4. Electron paramagnetic resonance spectra are consistent with the formation of Au(CO) (OC) with the magnetic parameters: a13 = 325 MHz, a17 = 44 MHz, and g = 2.0014 and a gold microcrystallite – CO complex with g = 2.014. An intense broad absorption in the optical spectrum at 525 nm is assigned to Au(CO)2 and a less intense narrow band at 320 nm is assigned to AunCO. There is no spectroscopic evidence for the formation of Au(CO)3 in hydrocarbon matrices. Keywords: gold carbonyls, EPR, FTIR, UV/visible, matrix isolation.

2004 ◽  
Vol 15 (1) ◽  
pp. 10-15 ◽  
Author(s):  
Juciane B Luiz ◽  
Fabiano M. de Andrade ◽  
Eduardo L. de Sá ◽  
Geraldo R Friedermann ◽  
Antonio S Mangrich ◽  
...  

Clay Minerals ◽  
1999 ◽  
Vol 34 (3) ◽  
pp. 515-518 ◽  
Author(s):  
C. Ruby ◽  
Ph. Refait ◽  
J.-M. R. Génin ◽  
T. Delineau ◽  
J. Yvon

Ferric oxides or hydroxides are common minor components of kaolinites. If free, these minerals can be removed by Fe reduction and leaching (Mehra & Jackson, 1960), but Fe3+ions can substitute for Al3+ions in the octahedral sites of kaolinite (Weaveret al., 1967; Malden & Meads, 1967). Moreover, Fe2+ions can also substitute trioctahedrally in place of dioctahedral Al, leading to a local composition of Fe-antigorite (Cuttler, 1980).The Font-Bouillant quarry (Charentes, France) is the source of disordered kaolinite known as ‘FU7, U-7-10 or FBT’ (Caseset al., 1982, 1986). The samples used in this study were considered in an earlier genetic analysis of the deposit (Delineau, 1994; Delineauet al., 1994) and were analysed previously by X-ray diffraction (XRD), infrared (IR) spectroscopy, electron paramagnetic resonance (EPR) and UV-visible spectroscopy by Delineauet al. (1994) (Table 1).


2013 ◽  
Vol 17 (08n09) ◽  
pp. 778-784 ◽  
Author(s):  
Sabeeha Mughal ◽  
C. Grazia Bezzu ◽  
Emma Carter ◽  
Simon J.A. Pope ◽  
Neil B. McKeown

The spectroscopic behavior of octa-t-butyltetra-2,3-triptycenotetraazaporphyrin and some of its metal complexes ( Cu 2+, Zn 2+ and Co 2+) were examined. UV-visible and electron paramagnetic resonance spectroscopy indicate that these phthalocyanine derivatives form cofacial dimers in pentane solution. Modeling suggests that the lowest energy configuration of the dimer is a self-complementary embrace in which the two phthalocyanine cores are staggered at an angle of 45° relative to each other. This configuration results in a remarkably intense and sharp absorption band (~635 nm; ε = ~4.0 × 105 M-1.cm-1) arising from excitonic coupling within the dimer, a unique property for self-assembled dimers but analogous to the behavior of certain μ-oxo-dimers of silicon phthalocyanine. Introduction of methyl substituents into the bridgehead positions of the triptycene subunits prevents dimer formation.


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