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Carbon dioxide molecular formula

Hexamefoylenediamine (MM = 116.2 g/mol), a compound made up of carbon, hydrogen, and nitrogen atoms, is used in the production of nylon. When 6.315 g of hexamefoylenediamine is burned in oxygen, 14.36 g of carbon dioxide and 7.832 g of water are obtained. What are foe simplest and molecular formulas of this compound ... [Pg.70]

Carbon dioxide has the formula COj. Remembering that the prefix di means two, and tri means three, write the molecular formula for each of the following substances carbon disulfide, sulfur dioxide, sulfur trioxide. (If you don t know the symbol for an element, use the table inside the back cover of the book.)... [Pg.32]

The molecular formula for the substance formaldehyde is HsCO. Formaldehyde burns to form carbon dioxide and water. What equation represents this reaction ... [Pg.43]

A paraffin candle bums in air to form water and carbon dioxide. Paraffin is made up of molecules of several sizes. We shall use the molecular formula Cj Hm as representative of the molecules present. One mole of candle contains the Avo-gadro number of these molecules. [Pg.43]

M.9 The stimulant in coffee and tea is caffeine, a substance of molar mass 194 g-mol When 0.376 g of caffeine was burned, 0.682 g of carbon dioxide, 0.174 g of water, and 0.1 10 g of nitrogen were formed. Determine the empirical and molecular formulas of caffeine, and write the equation for its combustion. [Pg.123]

M.10 Nicotine, the stimulant in tobacco, causes a very complex set of physiological effects in the body. It is known to have a molar mass of 162 g-mol. When a sample of mass 0.385 g was burned, 1.072 g of carbon dioxide, 0.307 g of water, and 0.068 g of nitrogen were produced. What are the empirical and molecular formulas of nicotine Write the equation for its combustion. [Pg.123]

C03-0089. Combustion analysis of 0.60 g of an unknown organic compound that contained only C, H, and O gave 1.466 g of carbon dioxide and 0.60 g of water in a combustion analysis. Mass spectral analysis showed that the compound had a molar mass around 220 g/mol. Determine the empirical formula and molecular formula. [Pg.190]

As an example that uses structural formulas and Equation, consider the energy change that takes place during the combustion reaction of propane (C3 Hg). Recall from Chapter 3 that combustion is a reaction with molecular oxygen. The products of propane combustion are carbon dioxide and water ... [Pg.383]

For example, Dalton designed a system of symbols to show how atoms combine to form other substances. Figure 3.2 on the next page shows several of these symbols. As you will no doubt notice, Dalton correctly predicted the formulas for carbon dioxide and sulfur trioxide, but ran into serious trouble with water, ammonia, and methane. Dalton s attempt at molecular modelling highlights a crucial limitation with his atomic model. Chemists could not use it to explain why atoms of elements combine in the ratios in which they do. This inability did not prevent chemists from pursuing their studies. It did, however, suggest the need for a more comprehensive atomic model. [Pg.119]

CASRN 2032-59-9 molecular formula C11H16N2O2 FW 208.26 Plant/Surface Water. Several transformation products reported by Day (1991) include 4-amino-/n-tolyl-7V-methylcarbamate (AA), 4-amino-3-methylphenol (AC), 4-formamido-/n-tolyl-TV-methylcarbamate (FA), 7V-(4-hydroxy-2-methylphenyl)-yV-methylformamide (FC), 4-methyl-formamido-/n-tolyl-7V-methylcarbamate (MFA), 4-methylamino-/n-tolyl-Wmethylcarbamate (MAA), 3-methyl-4-(methylamino)phenyl-Wmethylcarbamate (MAC), phenol, methylamine, and carbon dioxide. MAA was not detected in natural water but was detected in fish tissues following exposure to aminocarb-treated water in the laboratory. The metabolites FA, AC, and MAC were detected in Canadian forests treated with aminocarb but the metabolites AA, MAA, and FC were not detected (Day, 1991). [Pg.1547]

CASRN 17804-35-2 molecular formula C14H18N4O3 FW 290.62 Biological. Mixed cultures can grow on benomyl as the sole carbon source. It was proposed that benomyl degraded to butylamine and methyl 2-benzimidazolecarbamate, the latter undergoing further degradation to 2-aminobenzimidazole then to carbon dioxide and other products (Fuchs and deVries, 1978). [Pg.1555]

CASRN 314-40-9 molecular formula C9Hi3BrN202 FW 261.12 Soil Metabolites tentatively identified in soil were 5-bromo-3-(3-hydroxy-l-methylpropyl)-6-methyluracil, 5-bromo-3-5ec-butyl-6-hydroxymethyluracil, 5-bromo-3-(2-hydroxy-l-methylprop-yl)-6-methyluracil, and carbon dioxide. The presence of uracil products suggests that bromacil was degraded via hydroxylation of the side chain alkyl groups. In the laboratory, 25.3% of C-bromacil degraded in soil to carbon dioxide after 9 wk but mineralization in the field was not observed. The half-life of bromacil in a silt loam was 5-6 months (Gardiner et al, 1969). [Pg.1557]

CASRN 133-90-4 molecular formula C7H5CI2NO2 FW 206.02 Soil. In soils, chloramben was degraded by microorganisms but no products were identified (Humburg et al, 1991). The main degradative pathway of chloramben in soil is decarboxylation and subsequent mineralization to carbon dioxide. The calculated half-lives in Ella loamy sand, Kewaunee clay, and Poygan silty clay were 120-201, 182-286, and 176-314 d, respectively (Wildung et al, 1968). Persistence in soil is 6-8 wk (Hartley and Kidd, 1987). [Pg.1561]

CASRN 535-80-8 molecular formula C7H5CIO2 FW 156.57 Biological. Suflita et al. (1983) reported an enriched bacterial consortium degraded 3-chlorobenzoic acid via delhalogenation yielding the intermediate benzoic acid before mineralizing to methane and carbon dioxide. [Pg.1562]

CASRN 510-15-6 molecular formula C16H14CI2O3 FW 325.21 Biological. Rhodotomla gracilis, a yeast isolated from an insecticide-treated soil, degraded chlorobenzilate in a basal medium supplemented by sucrose. Metabolites identified by this decarboxylation process were 4,4 -dichlorobenzilic acid, 4,4 -dichlorobenzophenone, and carbon dioxide (Miyazaki et al., 1969, 1970). [Pg.1562]

CASRN 88-73-3 molecular formula C6H4CINO2 FW 157.55 Photolytic. An aqueous solution containing o-chloronitrobenzene and a titanium dioxide (catalyst) suspension was irradiated with UV light (X >290 nm). Chloronitrophenols formed as the intermediate product. Continued irradiation caused further degradation yielding carbon dioxide, water, hydrochloric and nitric acids (Hustert et ah, 1987). [Pg.1563]

CASRN 108-43-0 molecular formula CeHsClO FW 128.56 Photolytic. Irradiation of an aqueous solution containing 3-chlorophenol and titanium dioxide with UV light (X >340 nm) resulted in the formation of chlorohydroquinone then to hydroxyhydroquinone. Identification of compounds from the oxidation of hydroxyhydroquinone to carbon dioxide were not identified because of the low concentrations (D Oliveira et al, 1990). [Pg.1563]

CASRN 127-20-8 molecular formula C3H3Cl2Na02 FW 164.95 Soil. Undergoes dechlorination and the liberation of carbon dioxide in soil. The residual activity is limited to approximately 3-4 months (Hartley and Kidd, 1987). The average half-life for dalapon-sodium in soil incubated in the laboratory under aerobic conditions was 15 d (Namdeo, 1972). [Pg.1567]

CASRN 4147-51-7 molecular formula CnH2iN5S FW 255.40 Soil. Degradation of dipropetryn includes dealkylation of the side chain(s), ring opening, and the evolution of carbon dioxide (Hartley and Kidd, 1987). The reported half-life in soil is approximately 100 d (Worthing and Hance, 1991). [Pg.1578]

CASRN 2164-17-2 molecular formula CioHnF3N20 FW 232.21 Soil. In soils, fluometuron rapidly degrades (half-life approximately 30 d) to carbon dioxide, polar, and nonextractable compounds (Hartley and Kidd, 1987 Humburg et al., 1989). [Pg.1584]

CASRN 35065-27-1 molecular formula C12H4CI6 FW 360.88 Biological. Nitrogen-deficient cultures of the white rot fungus Phanerochaete chrysosporium degraded 2,2, 4,4, 5,5 -hexachlorobiphenyl to carbon dioxide (Bumpus et al., 1985). [Pg.1586]

CASRN 51235-04-2 molecular formula C12H20N4O2 FW 252.30 Soil/Plant. Degrades in soil and natural waters releasing carbon dioxide. The reported half-life in soil is 1 to 6 months (Hartley and Kidd, 1987). Rhodes (1980) found that the persistence of hexazinone varied from 4 wk in a Delaware sandy loam to 24 wk in a Mississippi silt loam. [Pg.1586]

CASRN 36734-19-7 molecular formula C13H13CI2N3O3 FW 330.17 Soil. Readily degrades in soil (half-life 20-160 d) releasing carbon dioxide and dichloroaniline (Hartley and Kidd, 1987 Walker, 1987). The rate of degradation increases with repeated applications of this fungicide. In a clay loam, the half-life was 1 wk. After the second and third applications, the half-lives were 5 and 2 d, respectively (Walker et al., 1986). [Pg.1588]

CASRN 25311-71-1 molecular formula C15H24NO4PS FW 345.40 Soil. Rapidly degraded by microbes via oxidative desulfuration in soils forming isofenphos oxon (Abou-Assaf et al, 1986 Abou-Assaf and Coats, 1987 Somasundaram et al., 1989), isopropyl salicylate, and carbon dioxide (Somasundaram et al., 1989). The formation of isofenphos oxon is largely dependent upon the pH, moisture, and temperature of the soil. The degradation rate of isofenphos decreased with a decrease in temperature (35 °C >25 °C >15 °C), moisture content (22.5% >30% >15%), and in acidic and alkaline soils (pH 6 and 8). After isofenphos was applied to soil at a rate of 1.12 kg ai/ha, concentrations of 8.3, 7.2, 5.1, and 1.0 ppm were found after 5, 21, 43, and 69 d, respectively. Following a second application, 4.9, 1.55, 0.25, and 0.10 ppm of isofenphos were found after 5, 21, 43, and 69 d, respectively (Abou-Assaf and Coats, 1987). [Pg.1588]


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