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Normal atmospheric pressures

Ad ceds are bipolar operating at normal, atmospheric pressure unless otherwise noted. Monopolar ceds are used. [Pg.425]

The activation parameters for an initiator can be deterrnined at normal atmospheric pressure by plotting In vs 1/T using initiator decomposition rates obtained in dilute solution (0.2 M or lower) at several temperatures. Rate data from dilute solutions are requited in order to avoid higher order reactions such as induced decompositions. The intercept for the resulting straight line is In and the slope of the line is —E jR therefore both and E can be calculated. [Pg.221]

Mercury vapor discharge from vents of reactors or storage tanks at normal atmospheric pressure is controlled readily by means of activated carbon. Standard units (208-L (55-gal) dmms) of activated carbon equipped with proper inlet and outlet nozzles can be attached to each vent. To minimize the load on the carbon-absorbing device, a small water-cooled condenser is placed between the vent and the absorber. [Pg.116]

Fig. 2. Vapor pressure and temperature (4), where the bold and dashed horizontal lines represent normal atmospheric pressure at sea level and at 609.6 m... Fig. 2. Vapor pressure and temperature (4), where the bold and dashed horizontal lines represent normal atmospheric pressure at sea level and at 609.6 m...
Combustion. The primary reaction carried out in the gas turbine combustion chamber is oxidation of a fuel to release its heat content at constant pressure. Atomized fuel mixed with enough air to form a close-to-stoichiometric mixture is continuously fed into a primary zone. There its heat of formation is released at flame temperatures deterruined by the pressure. The heat content of the fuel is therefore a primary measure of the attainable efficiency of the overall system in terms of fuel consumed per unit of work output. Table 6 fists the net heat content of a number of typical gas turbine fuels. Net rather than gross heat content is a more significant measure because heat of vaporization of the water formed in combustion cannot be recovered in aircraft exhaust. The most desirable gas turbine fuels for use in aircraft, after hydrogen, are hydrocarbons. Fuels that are liquid at normal atmospheric pressure and temperature are the most practical and widely used aircraft fuels kerosene, with a distillation range from 150 to 300 °C, is the best compromise to combine maximum mass —heat content with other desirable properties. For ground turbines, a wide variety of gaseous and heavy fuels are acceptable. [Pg.412]

Water at 4 C and normal atmospheric pressure taken as unity. For more detailed data on any material, see die section dealing widi die properties of that material. [Pg.163]

At sea level, water normally boils at 212°F. If the pressure should increase above 14.7 psia, as in a boiler or pressure vessel, then the boiling point of the water also inereases. If the pressure decreases, then the water s boiling point also decreases. For example in the Andes Mountains at 15,000 ft (4,600 meters) above sea level, normal atmospheric pressure is about 8.3 psia instead of 14.7 psia water would boil at 184°F. [Pg.24]

The overhead products from light ends fractionators are frequently gases, or a mixture of gas and liquid, at normal atmospheric pressure and 100°F. (an average temperamre for products condensed by cooling water). To avoid the... [Pg.81]

The temperature of the water in the heating panel is limited by the boiling of the water. The boiling temperature of water increases with increasing pressure. If the pressure of the water is about normal atmospheric pressure, then the temperature of the water can be 90-95 °C. If we w ant to raise the temperature of water to 120 C, the absolute pressure of water must be above 2 bar. [Pg.667]

The product is hydrogenated in 4,000 cc of ethanol at room temperature and under normal atmospheric pressure with a catalyst prepared In the usual manner from 400 g of Raney nickel alloy. The calculated amount of hydrogen is taken up in approximately 75 hours. After filtration and evaporation to a small volume, the residue Is distributed between 1,000 cc of chloroform and water each. The chloroform solution is then dried over sodium sulfate and evaporated to a small volume. Precipitation of the hydrogenation product with petroleum ether yields an amorphous white powder which Is filtered by suction, washed with petroleum ether and dried at 50°C In a high vacuum. 1. athyl-2-podophyllinic acid hydrazide is obtained in a practically quantitative yield. [Pg.1034]

Because of the importance of mass airflow rate in establishing engine output power, power available is sensitive to ambient conditions. Full-throttle engine power varies approximately inversely with inlet-air absolute temperature, but more significantly, approximately directly with ambient pressure. Mountain passes exist on public roads in the United States that have altitudes of over 12,000 ft. The normal atmospheric pressure at such altitudes results in a one-third loss in power capability in the typical passenger-car engine. [Pg.102]

Propane is a nontoxic, colorless, odorless hydrocarbon chat occurs naturally in natural gas streams and crude oil. At normal atmospheric pressure and temperature, it is a gas under moderate pressure propane becomes liquid. The ratio ofhquid to gas is 270—one unit of liquid expands to 270 units of vapor. [Pg.720]

This chart is applicable only to flammable liquids or gases in equilibrium In a closed container. Mixtures of vapor and air will be too lean to burn at temperatures below and at pressures above the values shown by the line on the chart for any substance. Conditions represented by points to the left of and above the respective lines are accordingly nonflammable. Points where the diagonal lines cross the zero gauge pressure line (760 mm of mercury absolute pressure) indicate flash point temperatures at normal atmospheric pressure. [Pg.492]

The datum point, when considering the steam/water substance, is usually taken as water at the temperature of melting ice, at normal atmospheric pressure and so at a temperature of 0°C. Adding heat energy raises its temperature some 419.04kJ will raise 1 kg to 100°C, when any further addition of heat evaporates some of the water. If 2257 kJ are added to each kg of water, then all the water becomes the dry gas, steam. Equally, if only part of this extra energy is added - say, 90 per cent - then 90 per cent of the water evaporates and the other 10 per cent... [Pg.311]

Although the SI unit of pressure is the pascal (Pa), there are several other units in common use. Normal atmospheric pressure is close to 100 kPa, and it is useful to... [Pg.265]

Fig. 20 Schematic representation of an eiectric spark discharge chamber for the activation of gases at normal atmospheric pressure for the production of fluorescence in substances separated by thin-layer chromatography [2],... Fig. 20 Schematic representation of an eiectric spark discharge chamber for the activation of gases at normal atmospheric pressure for the production of fluorescence in substances separated by thin-layer chromatography [2],...
With his team organized, Haber began looking at the problem in its simplest form—at normal atmospheric pressure. After publishing some preliminary results, Haber met Walther Nernst at a scientific conference in Hamburg. Nernst, who was only four years older than Haber, had a pugnacious personality that made him quarrel with almost everyone in academia. Worried that Haber s work cast doubt on the validity of his new law of thermodynamics, Nernst publicly ridiculed Haber s highly erroneous data and told him scornfully to do his homework. ... [Pg.65]

Column inlet pressures in hplc can be as much as 200 times atmospheric pressure, and hplc columns are packed using much larger pressures (up to 700 times atmospheric). The SI unit of pressure is the Pascal (1 Pa = 1 Nm-2) normal atmospheric pressure is about 105 Pa. Because it is convenient to express pressure using reasonably small numbers, experimental workers and instrument manufacturers report pressures in bar, or pounds per square inch (psi), or sometimes in kg cm-2. The bar is defined by 1 bar = 105 Pa, so that 1 bar corresponds roughly to normal atmospheric pressure. You will need to be able to convert between these units. [Pg.254]

Result The recovery of different fractions of petroleum distillate under atmospheric pressure was more than under reduced pressure because at lower pressure the vapour pressure of lighter molecule of crude oil increased so that they were siphoned out from the system without being condensed. Whereas a combination of distillation of lighter fraction under normal atmospheric pressure followed by the distillation of heavier contents under reduced pressure showed an improvement in the recovery of petroleum products. Recovery of distillates was still more when crude oil was first sonicated and then distilled under normal and reduced pressures. The viscosity of distillate increased with sonication whereas there was a decrease in value of density. [Pg.390]

The conditions that apply for the saturated liquid-vapor states can be illustrated with a typical p-v, or (1 /p), diagram for the liquid-vapor phase of a pure substance, as shown in Figure 6.5. The saturated liquid states and vapor states are given by the locus of the f and g curves respectively, with the critical point at the peak. A line of constant temperature T is sketched, and shows that the saturation temperature is a function of pressure only, Tsm (p) or psat(T). In the vapor regime, at near normal atmospheric pressures the perfect gas laws can be used as an acceptable approximation, pv = (R/M)T, where R/M is the specific gas constant for the gas of molecular weight M. Furthermore, for a mixture of perfect gases in equilibrium with the liquid fuel, the following holds for the partial pressure of the fuel vapor in the mixture ... [Pg.139]

A common consideration is the presence of water vapor, H20(g). Water generates a vapor pressure, which varies with the temperature. Daltons law is used in these cases to adjust the pressure of a gas sample for the presence of water vapor. The total pressure (normally atmospheric pressure) is the pressure of the gas or gases being collected and the water vapor. When the pressure of an individual gas is needed, the vapor pressure of water is subtracted from the total pressure. Finding the vapor pressure of water requires measuring the temperature and using a table showing vapor pressure of water versus temperature. [Pg.112]

Litre—is defined as the volume occupied hy one kilogram of water at its temperature of maximum density (4°C) and subjected to normal atmospheric pressure . The litre is considered as the standard unit of volume for all volumetric measurements. [Pg.49]


See other pages where Normal atmospheric pressures is mentioned: [Pg.16]    [Pg.127]    [Pg.98]    [Pg.291]    [Pg.294]    [Pg.38]    [Pg.81]    [Pg.479]    [Pg.6]    [Pg.156]    [Pg.8]    [Pg.253]    [Pg.2]    [Pg.29]    [Pg.68]    [Pg.270]    [Pg.71]    [Pg.97]    [Pg.64]    [Pg.252]    [Pg.135]    [Pg.17]    [Pg.222]    [Pg.40]    [Pg.397]    [Pg.26]   
See also in sourсe #XX -- [ Pg.248 ]




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