Carbon-coated annular denuders and ion chromatographic measurements for the determination of nitrogen-containing species (NO2 and NOy) in remote atmospheres

1999 ◽  
Vol 846 (1-2) ◽  
pp. 265-268 ◽  
Author(s):  
I. Allegrini ◽  
A. Ianniello ◽  
M. Montagnoli ◽  
R. Sparapani ◽  
C. Mazziotti Gomez de Teran
Keyword(s):  
2006 ◽  
Vol 46 ◽  
pp. 180-187 ◽  
Author(s):  
Masahiro Toyoda ◽  
Beata Tryba ◽  
Fumi Koujin ◽  
Tomoki Tsumura ◽  
Michio Inagaki

Carbon-coated TiO2 photocatalysts were prepared by a simple heat treatment of the powder mixtures of anatase-type TiO2 with PVA at a temperature of 700 and 900 oC in a N2 atomosphere. Diffuse optical reflectance spectra for carbon-coated TiO2 showed the absorption edge for anatase structure clearly, overlapping with absorption due to coated carbon over whole range of wavelegth. These carbon-coated TiO2 photocatalysts had relatively high apparent BET surface area, from 50 to 170 m2/g, which suggested the formation of porous carbon layers, and showed relatively high adsorption of various pollutants, methylene blue (MB), reactive black (RB-5), phenol (Ph) and iminoctadine triacetate (IT), in water. Photocatalytic activity of carbon-coated TiO2 thus prepared was evaluated through the determination of the rate constant for the decomposition of different pollutants in water. Rate constant values were strongly depend on the pollutants, but their dependence on the crystallinity of TiO2 phase. The relations between adsorptivity and rate constant for four pollutants looked similar with each other, and the pollutants adsorbed in the larger amount was decomposed with the higher rate. Adsorptivity of carbon-coated TiO2 photocatlysts was determined and discussed on the relations to BET surface area, amount of carbon coated and also rate constant k for the decomposition of MB, RB5, Ph and IT. Adsorptivity of carbon-coated catalysts depends strongly on the adsorbate (pollutant) but also on the surface nature of carbon layer on TiO2 particles. The relations between adsorptivity and rate constant k for four pollutants looked similar, suggesting that the pollutant adsorbed in the larger amount being decomposed with the higher rate.


Carbon ◽  
2011 ◽  
Vol 49 (13) ◽  
pp. 4191-4196 ◽  
Author(s):  
Kazuhisa Inaba ◽  
Kouji Saida ◽  
Pradip Ghosh ◽  
Ken Matsubara ◽  
Munisamy Subramanian ◽  
...  

1998 ◽  
Vol 16 (6) ◽  
pp. 453-463 ◽  
Author(s):  
R.N. Nickolov ◽  
D.R. Mehandjiev

A carbon-coated support has been prepared by the impregnation of commercial alumina with an ammoniacal solution of amphiphilic carbonaceous material. It was established that the method used for the deposition of the carbon coating on the support allowed control of both the layer thickness and the degree of filling of the surface in the low carbon content region. Equations proposed for the approximate determination of the thickness of the deposited carbon layer and of the surface occupied by this layer enabled a tentative prediction to be made of the most desirable parameters for such a system.


Author(s):  
L. Rice ◽  
J. Dash

Mount St. Helens ash is a pumaceous, pyroclastic material which has been dispersed in varying amounts over most of the Pacific Northwest on a number of occasions during 1980, including the catastrophic eruption of May 18 1980. Samples have been collected and examined from several sites between the crater itself and northwestern Oregon from March 20, 1980 through October 17, 1980. Ejected material consists of both older mountain and new particles. Tephra composition varies in proportions of glass and glass-coated minerals with length of plume travel time. Portland area fallout has ranged from coarse, steel gray, low in glass on June 12, 1980 (travel time two hours) to fine, talcy, brownish gray, high in glass on May 25, 1980 (travel time six to eight hours).Crystalline, sub-micron sized particles of the ash are being studied by the selected-area electron diffraction technique with the TEM in an effort to determine the nature of the mineral content of the ash. The particles are deposited on carbon-coated grids containing small pieces of evaporated gold film for determination of accurate camera constants. Several plagioclase feldspar minerals (70-75% of the mineral fraction for Cascade volcanoes) have been identified from random samples of the atmospheric fallout.


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