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Temperature differential surveying

Design temperatures, operator guesses, and actual operating temperature differentials almost never correspond. Representatives should always carry a pocket thermometer with them (accurate to 0.2°F/0.rC) and carry out an actual measurement during the survey. A difference of 1.0°C between actual and estimated temperatures can eventually produce a considerable difference in estimated annual chemical costs. Again, it is necessary to qualify the temperature differentials for seasonal variations. [Pg.274]

The coliform group of organisms does not come from only the intestinal tract of man but also from the outside surroundings. There are situations, as in pollution surveys of a water supply with a raw water source, that the fecal variety needs to be differentiated from the nonfecal ones. For this and similar situations, the procedure is modified by raising the incubation temperature to 44.5 + 0.2°C. The broth used is the EC medium which stiU contains lactose. The high incubation temperature... [Pg.170]

Tables XIII I76-I79), XIV (I80-I83), and XV present a survey of micro-calorimetric studies performed for silica, alumina, and silica-alumina, respectively. Silica displays relatively low heats of adsorption for both basic probe molecules (e.g., ammonia, triethylamine, n-butylamine, pyridine, and trimethylamine) and acidic probe molecules (e.g., hexafluoroisopropanol), indicating that the surface sites on silica are both weakly acidic and basic. Most of the adsorption over silica is considered mainly to be due to hydrogen bonding and van der Waals interaction. Infrared and gravimetric adsorption measurements of pyridine adsorbed on SiO at 423 K have shown that more than 98% of the pyridine adsorbed was hydrogen bonded (62). The differential heats of ammonia 18, 74, 85, 105, 140, 147) and triethylamine (18, 71, 94. 105, 176) on silica show a considerable decrease as the adsorption temperature is increased. Tables XIII I76-I79), XIV (I80-I83), and XV present a survey of micro-calorimetric studies performed for silica, alumina, and silica-alumina, respectively. Silica displays relatively low heats of adsorption for both basic probe molecules (e.g., ammonia, triethylamine, n-butylamine, pyridine, and trimethylamine) and acidic probe molecules (e.g., hexafluoroisopropanol), indicating that the surface sites on silica are both weakly acidic and basic. Most of the adsorption over silica is considered mainly to be due to hydrogen bonding and van der Waals interaction. Infrared and gravimetric adsorption measurements of pyridine adsorbed on SiO at 423 K have shown that more than 98% of the pyridine adsorbed was hydrogen bonded (62). The differential heats of ammonia 18, 74, 85, 105, 140, 147) and triethylamine (18, 71, 94. 105, 176) on silica show a considerable decrease as the adsorption temperature is increased.
Microwave processing of zeolites and their application in the catalysis of synthetic organic reactions has recently been excellently reviewed by Cundy [25] and other authors [26], The microwave synthesis of zeolites and mesoporous materials was surveyed, with emphasis on those aspects which differ from conventional thermal methods. The observed rate enhancement of microwave-mediated organic synthesis achieved by use of these catalysts was caused by a variety of thermal effects, including very high rates of temperature increase, bulk superheating, and differential heating. Examples of microwave activation of chemical reactions catalyzed by zeolites will be presented in Section 13.3. [Pg.620]

Analytical methods describing the thermal behavior of substances during programmed temperature changes, like thermogravimetry, differential thermoanalysis, or differential scanning calorimetry are old methods, which were applied at first to problems of inorganic chemistry, mainly to minerals. The analysis of petroleum and petroleum products has been mentioned relatively late. In the literature survey by Weselowski [1-1] the first citation dates from 1958. Also, the oldest citation in the research report by Kettrup and Ohrbach [1-2] dates from 1965. [Pg.2]


See other pages where Temperature differential surveying is mentioned: [Pg.134]    [Pg.454]    [Pg.40]    [Pg.420]    [Pg.316]    [Pg.111]    [Pg.219]    [Pg.2]    [Pg.388]    [Pg.603]    [Pg.231]    [Pg.148]    [Pg.149]    [Pg.444]    [Pg.289]    [Pg.309]    [Pg.275]    [Pg.530]   
See also in sourсe #XX -- [ Pg.274 ]




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