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Benzenes lower chlorinated

HCB is an organochlorine product. It was first introduced in 1933 as a fungicide for seed treatment of onion, sorghum and crops, such as wheat, barley, oats and rye, and was used to make fireworks, ammunition and synthetic rubber (Barber et al., 2005 UNEP Chemicals, 2002). It is currently speculated that HCB originates in the environment as a by-product or is the result of impurity in the production of certain chlorinated pesticides, particularly lower chlorinated benzenes and industrial chemicals the manufacture and application of HCB-contaminated pesticides and the combustion of waste (Barber et al., 2005 UNEP, 2003 Voldner Smith, 1989). [Pg.378]

For the chlorinated benzenes, a very similar distribution within the sediment core is observed as for some PAHs, e.g. benzo[a]pyrene. An elevated large-scale industrial activity related to these compounds can be deduced for the time between 1947 and 1955. We attribute the decrease in contamination towards the top layers to a reduction of emissions as a result of more efficient sewage treatment plants (Fig. 1A,B) as well as a modified array of products. The concentration profile of HCB (Fig. 6C) and all lower chlorinated benzenes (Tab. 2) suggests the dominance of industrial sources responsible for the contamination as contrasted to agricultural emission derived from pesticide usage. It should be noted that the contamination level of 1,4-dichlorobenzene was elevated in the time period between 1975 and 1980, comparable with concentration levels determined in Rhine river sediments 1982/83. The extensive use of 1,4-dichlorobenzene as an odorous ingredient of toilet cleaners contributed additionally to the contamination via sewage effluents (LWA, 1987/1989). [Pg.369]

If the ratio of chlorine to benzene materially exceeds 1 1, inflammation may occur at the mixing point, but a cyclic operation with recycle of lower chlorinated benzenes allows easy chlorination to tri- and tetrachloroben-zenes. There is little change in the ratio of mono- to dichlorobenzenes at temperature increases above 400 C, but above 500 C pyrolysis and condensation reactions occur, with the formation of carbon, hexachloroben-zene, and chlorinated biphenyls. [Pg.237]

The results obtained for a (non-stratified) lake are also given in FIGURE 3. Because of the decreased volatilization of benzene and chlorinated benzene compounds the residence time has increased by two orders of magnitude over that of the river. The lower slope of the 1 m s line indicates that, in slow flowing surface water, the influence of chemical properties is more pronounced than in fast flowing rivers. [Pg.34]

Finally, halorespiration has been observed with highly chlorinated benzenes such as hexachlorobenzene, pentachlorobenzene, tetrachlorobenzene, and trichlorobenzene (Hol-liger et al, 1992 Ramanand et al, 1993 Suflita and Townsend, 1995). In anaerobic conditions, highly chlorinated benzenes can be easily reductively dechlorinated and product lower chlorinated benzenes. Bacteria from the genus Dehalococcoides are known for having the main role in this process. Conversely, lower chlorinated benzenes have a lower tendency for reductive dechlorination, and finally mono-chlorinated benzene is the most resistant in this anaerobic process (Field and Sierra-Alvarez, 2008). [Pg.880]

In spite of their comparatively high boiling points and water solubilities, the lower chlorinated benzenes are very volatile, so a large proportion of the losses will enter the atmosphere, either directly or indirectly. [Pg.98]

The lower chlorinated benzenes (di-, tri-, tetra- and penta-) have been found in sewage and effluents [15, 40, 60, 51, 120] in surface and ground waters in the Rhine Basin [10, 50, 56], and in some biological tissues [69, 134]. The high levels of p-dichlorobenzene shown in Tables 8 and 9 were recorded in Japan, where they are assumed to be caused by its considerable use as an odoriser. Monochlorobenzene is not normally detected in any samples. Both hexachlorobenzene and pen-tachloronitrobenzene are found in some foods, due to their use as fungicides, but not normally at levels above 0.05 mg/kg. [Pg.103]

The PMBs, when treated with electrophilic reagents, show much higher reaction rates than the five lower molecular weight homologues (benzene, toluene, (9-, m- and -xylene), because the benzene nucleus is highly activated by the attached methyl groups (Table 2). The PMBs have reaction rates for electrophilic substitution ranging from 7.6 times faster (sulfonylation of durene) to ca 607,000 times faster (nuclear chlorination of durene) than benzene. With rare exception, the PMBs react faster than toluene and the three isomeric dimethylbenzenes (xylenes). [Pg.504]

The reddish brown pentachloride, uranium pentachloride [13470-21 -8], UCl, has been prepared in a similar fashion to UCl [10026-10-5] by reduction—chlorination of UO [1344-58-7] under flowing CCl, but at a lower temperature. Another synthetic approach which has been used is the oxidation of UCl by CI2. The pentachloride has been stmcturaHy characterized and consists of an edge-sharing bioctahedral dimer, U2CI2Q. The pentachloride decomposes in H2O and acid, is soluble in anhydrous alcohols, and insoluble in benzene and ethers. [Pg.332]

Continuous chlorination processes permit the removal of mono-chlorohenzene as it is formed, resulting in lower yields of higher chlorinated benzene. [Pg.278]

Solvent — The transition energy responsible for the main absorption band is dependent on the refractive index of the solvent, the transition energy being lower as the refractive index of the solvent increases. In other words, the values are similar in petroleum ether, hexane, and diethyl ether and much higher in benzene, toluene, and chlorinated solvents. Therefore, for comparison of the UV-Vis spectrum features, the same solvent should be used to obtain all carotenoid data. In addition, because of this solvent effect, special care should be taken when information about a chromophore is taken from a UV-Vis spectrum measured online by a PDA detector during HPLC analysis. [Pg.467]

Aromatics, chlorinated hydrocarbons, lower alcohols, ketones, esters Alcohol, benzene, chlorinated hydrocarbons, esters, ether Alcohol, esters, ketones, dioxane... [Pg.147]

Nanocrystalline MgO and CaO also allow the destruction of chlorinated benzenes (mono-, di-, and trichlorobenzenes) at lower temperatures (700 to 900°C) than incineration.73 The presence of hydrogen as a carrier gas allows still lower temperatures to be used (e g., 500°C). MgO was found to be more reactive than CaO as the latter induces the formation of more carbon. [Pg.56]


See other pages where Benzenes lower chlorinated is mentioned: [Pg.141]    [Pg.263]    [Pg.398]    [Pg.399]    [Pg.569]    [Pg.1250]    [Pg.242]    [Pg.226]    [Pg.134]    [Pg.212]    [Pg.70]    [Pg.649]    [Pg.144]    [Pg.437]    [Pg.432]    [Pg.1233]    [Pg.829]    [Pg.830]    [Pg.468]    [Pg.398]    [Pg.399]    [Pg.89]    [Pg.535]    [Pg.230]    [Pg.907]    [Pg.166]    [Pg.167]    [Pg.170]    [Pg.254]    [Pg.535]    [Pg.565]    [Pg.387]    [Pg.7]    [Pg.158]    [Pg.415]    [Pg.175]    [Pg.214]   
See also in sourсe #XX -- [ Pg.103 ]




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Benzene chlorination

Benzene-chlorine

Chlorinated benzenes

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