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Methane concentrations ambient

The large number of individual hydrocarbons in the atmosphere and the many different hydrocarbon classes make ambient air monitoring a very difficult task. The ambient atmosphere contains an ubiquitous concentration of methane (CH4) at approximately 1.6 ppm worldwide (9). The concentration of all other hydrocarbons in ambient air can range from 100 times less to 10 times greater than the methane concentration for a rural versus an urban location. The terminology of the concentration of hydrocarbon compounds is potentially confusing. Hydrocarbon concentrations are referred to by two units—parts per million by volume (ppmV) and parts per million by carbon (ppmC). Thus, 1 fx of gas in 1 liter of air is 1 ppmV, so the following is true ... [Pg.201]

Since the critical temperature of methane is 190.6 K, methane-containing mixtures at ambient temperatures always have some range of methane concentrations at which the retrograde condensation occurs. This condensation complicates gas field operation, since it results in partial condensation of natural gas near a well bottom. It lowers a well yield and decreases the amount of recoverable hydrocarbons. [Pg.138]

The Kr/Xe concentration in the sump of the enrichment column is controlled by the amount of withdrawn sump product (d). The smaller the flow, the higher will be the concentration. Thus the Kr/Xe-concentration could be theoretically increased up to the solubility limit of krypton (30%) and xenon (2%). The maximal admissible concentration is however determined by the solubility and the explosion limit of the hydrocarbon components, which accumulate in the sump product as well. The most prominent component is CH4, which is contained in ambient air with up to 5 ppm. Owing to its low volatility (Table 3.2), CH4 accumulates together with Kr/Xe in the liquid bath. The methane concentration in the Kr/Xe pre-product must remain well below its lower explosion limit of about 4.4%. [Pg.114]

The alcohol (11.9 mmol) was added with stirring to a solution of chromium trioxide (69.4 mmol) and pyridine (133 mmol) in dichloro-methane (150ml) at ambient temperature. After a further 15 min, the solution was filtered, washed with saturated sodium hydrogen carbonate solution, dilute HC] and brine, and dried. Concentration and distillation gave the y -ketosilane (7.4mmol, 62%), b.p. 120°C/0.5mmHg. [Pg.134]

Fig. 12. Profile of the concentration of methane in the ambient air showing 1-h averages for an 8-day period. Determined with correlation (multiplex) chromatography utilizing catalytical oxidation as a modulation. Fig. 12. Profile of the concentration of methane in the ambient air showing 1-h averages for an 8-day period. Determined with correlation (multiplex) chromatography utilizing catalytical oxidation as a modulation.
Sodium methane sulfinate (3.0 g) and sulfur (1.41 g) were mixed in 180 ml of methanol and then refluxed under argon for 45 minutes. The mixture was then cooled to ambient temperature, filtered, the filtrate concentrated, and 3.2 g product isolated. [Pg.464]

Since the concentration of C02 in water is rather low, increasing pressure may enhance the performance of photoreduction. Studies using Ti02 in water showed that hydrocarbons such as methane and ethylene, which were not produced at ambient pressure, were obtained under high pressure.161 166 Methane was formed as the main reduction product when the reduction was performed in isopropyl alcohol, a positive hole scavenger.167... [Pg.98]

CCL + HCI + excess CH4. The reaclion is carried out in the liquid phase al about 35 C. Ultraviolet light is used as a catalyst. The same reaclion can be carried oul al 475"C without catalyst. The unreacted methane and partially chlorinated products are recycled to control the yield of CCL. Toxicity. The experimental exposure of laboratory animals to the vapors or CCL has shown it to be very toxic by inhalation at concentrations easily obtainable at ambient temperatures, An overexposure to carbon tetrachloride has been known to cause acute but temporary loss of renal function. [Pg.294]

Rhodium complexes with l,3-bis(di-fert-butylphosphino)methane (dtbpm), [(dtbpm) RhCl]2/PPh3 (89), (dtbpm)RhS i(OEt)3 (PMe3) (90) and (dtbpm)RhMe(PMe3) (91) are found to be effective catalysts for the hydrosilylation of an internal alkyne, 2-butyne, with HSi(OEt)3 at ambient temperature without solvent to yield (E)-2-triethoxysilyl-2-butene with complete stereoselectivity in quantitative yield using a proper concentration of the catalysts, i.e. >0.05 mol% for 89, >0.4 mol% for 90 and 91114. When the reaction is carried out at lower catalyst concentrations, i.e. 0.1 mol% for 90 or 91, (Z)-product is formed via frans-addition in 7-13% yield. [Pg.1720]

The fate of the peroxy radical depends on the ambient concentration of nitric oxide. In the presence of sufficient NO the CH30) radical is converted to methanal ... [Pg.135]

The simplest monocyclic thiophene cation-radicals which are persistent at ambient temperature and for which ESR spectra have been recorded and assigned are a series of 2,5-bis(alkylthio)thiophene cation-radicals. These radicals exhibit conformational isomerism. Thus, 2,5-bis(metliyltliio)-tliiophene cation-radicals exists as a mixture of 75% of the symmetrical S-cis-cis isomer (93A) and 25% of the unsymmetrical S-cis-trans isomer (93B) with no detectable concentration of the symmetrical S-trans-trans isomer. The radicals were formed by treatment of the parent heterocycles in nitro-methane with AICI3 the assignments were made on the basis of both S- and C-alkyl substitution experiments and supported by MO calculations (hyper-fine splittings given for 93A and B are in gauss). [Pg.70]

A customized Cu(I)Y zeolite is employed as a sorbent to actively collect CO in air samples to measure the concentration of CO in ambient air.The interaction is selective to CO only, but not to N2, O2, and CO2. The sorption process is facilitated by formation of Cu(l)-CO complexes, while CO can be desorbed at 300°C under helium flow for 2 min. Before the gas chromatographic analysis, a methanizer is used to reduce CO to CH4, which can then be quantified by FID. Detection limit of methane by this method is approximately 0.2 ppm. The laboratory data shows the capacity of the Cu(I)Y zeolite sorbent as 2.74 mg CO/g of sorbent. For a typical sorbent tube containing 0.5 g of treated zeolite sampling at the PEF of 50 ppm with a nominal flow rate of 100 ml/min, sampling can last as long as approximately 4 h before a breakthrough point is reached. Furthermore,... [Pg.248]

An example of an automatic analyser for the determination of organic pollutants is the Meloy HC 500-2C from Columbia Scientific Industries. It is a self-contained system for monitoring ambient concentrations of non-methane hydrocarbons (NMHC), methane and total hydrocarbons. Sample air Is first introduced directly into the flame ionization detector to yield a total hydrocarbon reading which Is stored In an electrical circuit. The pneumatic system Is automatically switched so that the sample air passes through a catalytic converter before It Is Introduced Into the detector, which converts ail the NMHC Into a non-detectable species. Hence, only the methane in the sample Is... [Pg.508]


See other pages where Methane concentrations ambient is mentioned: [Pg.2000]    [Pg.3891]    [Pg.603]    [Pg.184]    [Pg.252]    [Pg.281]    [Pg.16]    [Pg.46]    [Pg.335]    [Pg.37]    [Pg.88]    [Pg.339]    [Pg.59]    [Pg.8]    [Pg.512]    [Pg.214]    [Pg.198]    [Pg.286]    [Pg.91]    [Pg.140]    [Pg.53]    [Pg.406]    [Pg.337]    [Pg.343]    [Pg.433]    [Pg.2696]    [Pg.20]    [Pg.22]    [Pg.2593]    [Pg.12]    [Pg.52]    [Pg.90]    [Pg.2573]    [Pg.607]    [Pg.169]   
See also in sourсe #XX -- [ Pg.43 ]




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Methane concentration

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