Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

TYPES OF ATMOSPHERES

In order to use, compare and extrapolate results obtained from outdoor corrosion testing stations, corrosion specialists have defined a typology of atmospheres in which the test (or the use) takes place. This typology is based on the general climate of the zone and the presence of possible pollutants. Quantitative data have been collected, while the measurement methods and the equipment available have continued to progress. [Pg.261]


Atmospheric information, including local climate (precipitation, temperature, wind speed and direction, presence of inversion layers), weather extremes (storms, floods, winds), release characteristics (direction and speed of plume movement, rate, amount, and temperature of release, relative densities), and types of atmospheric hazards and hazards assessment... [Pg.601]

Other types of atmospheric pressure ionisation detectors are available including APPI (photon ionisation) and MALDI (matrix-assisted laser desorption ionisation). More conventional detection systems for LC include UV absorption, fluorescence and evaporative light scattering. Developments in column packings,... [Pg.570]

An increase in temperature tends to widen the flammable range, reducing the LFL. For example, the LFL for methane in air is commonly quoted as 5%. As the temperature of methane increases to autoignition temperature, the LFL falls to around 3%. Stronger ignition sources can ignite leaner mixtures. Flammability limits also depend on the type of atmosphere. Flammability limits are much wider in oxygen, chlorine, and other oxidizers than in air (NFPA, 1997). [Pg.400]

Figure 3. Changes in average, average maximum and minimum, maximum and minimum air temperature depending on exposure condition and type of atmosphere for test stations located in the western side of the Cuban Isle. Figure 3. Changes in average, average maximum and minimum, maximum and minimum air temperature depending on exposure condition and type of atmosphere for test stations located in the western side of the Cuban Isle.
Figure 5. Time of wetness at different exposure conditions and types of atmospheres calculated according to ISO 9223 for test stations of the western side of the Cuban Isle. Figure 5. Time of wetness at different exposure conditions and types of atmospheres calculated according to ISO 9223 for test stations of the western side of the Cuban Isle.
Changes in steel corrosion rate for different exposure conditions and types of atmosphere are better explained based on average deposition rate of Chlorides, as can be observed on figure 5. It can be note that Chloride deposition is higher in coastal stations, as it should be expected, and it is in agreement with a higher weight lost for these stations. [Pg.79]

Figure 7. Annual average Chloride deposition rate for test station located at the western side of the Cuban Isle depending on exposure conditions and type of atmosphere. Figure 7. Annual average Chloride deposition rate for test station located at the western side of the Cuban Isle depending on exposure conditions and type of atmosphere.
On figure 7 there is represented Average Chloride Deposition rate determined in Cuba for different types of atmosphere and exposure conditions. The results are very similar to those presented on figure 6, particularly respecting outdoor and ventilated shed conditions. Chloride deposition is determined under shelter, that is why it is assumed the same value for ourdoor and sheltered conditions however, it is very well known, the significant influence of precipitations upon outdoor corrosion and its negligible effect under sheltered conditions. In... [Pg.79]

The superficial characteristics of atmospheric corrosion products of steel depend on the type of atmosphere where the sample has been exposed. The way of adsorption of the corrosion products obtained in the coastal atmosphere is polymolecular due to a higher content of salts. This makes easier the presence of water in the metal-corrosion products interface and determines a high corrosion rate. The adsorption of water of a corrosion product formed in a rural zone obeys a Langmuir isotherm, i.e. a monomolecular adsorption takes place. It causes a lower corrosion rate. [Pg.88]

Because of its fundamental characteristics, nitric oxide is an important species in three types of atmospheric concerns ballistic-missile reentry, polluted air, and the upper atmosphere. Understanding its reactions, therefore, is of consequence in the development of an effective military defense, the solution of urban air-pollution problems, and the exploration of space. The concern of Government, as well as private industry, in these areas is obvious and has led to the appropriation of considerable funds for studies of nitric oxide and its related species. Consequently, a large number of publications has appeared in recent years (more than half our references are 1960 or later). [Pg.159]

The hydrostatic state of equilibrium of the atmosphere varies with the type of atmosphere that is under consideration. [Pg.158]

At the same time, this method has a series of disadvantages. Among them, we note the possibiity of contamination of the final product not only by the excess of one of the reactants [2], but also by complexes of the components of the ligand system. So, to carry out strictly template synthesis experiments, it is necessary to take into account a comparative stability of coordination compounds, obtained on the basis of initial components-precursors and the ligand itself. Not only the thermodynamic characteristics of complex-formation processes should be taken into consideration [326,327], but also the influence of solvolysis processes (especially hydrolysis) and the type of atmosphere (air oxygen). [Pg.215]

A miniature cylindrical ion trap mass spectrometer with APCI and ESI capabilities was developed [22], The system includes a three-stage, differentially pumped vacuum system and can be interfaced to many types of atmospheric pressure ionization sources. [Pg.57]

Typical values of scavenging ratio lie within the range 300-2000. Scavenging ratios are rather variable, dependent upon the ehemieal nature of the trace substance (particle or gas, soluble or insoluble, etc) and the type of atmospheric precipitation. Incorporation of gases and particles into rain can occur both by in-cloud scavenging (also termed rainout) and below-cloud scavenging (termed washout). [Pg.329]

Present knowledge of the atmospheric aerosol and the limits of this review do not permit a detailed comparative analysis of the available variety and types of atmospheric particles, whose mechanisms of generation are both natural and anthropogenic. Therefore, proceeding from comparative data on the power of the sources of different kinds of aerosols... [Pg.283]

Modem mass spectrometers within the pharmaceutical industry are more usually fitted with atmospheric pressure ionisation sources that are ideally suited to be connected to HPLC equipment. They are very robust which enables them to be used unattended for many weeks without the need for source cleaning or routine maintenance. There are two types of atmospheric ionisation sources, namely Electrospray Ionisation (ESP) or Atmospheric Pressure Chemical Ionisation (APCl) [15]. Both ionisation modes provide soft ionisation which favours quasi-molecular ion production with little or no fragmentation. Most typically MH ions are observed but MNa, MNHj and MK may also be produced. [Pg.341]

Considerable attention has been given to nitrogen oxides (and sulfur oxides) in the atmosphere because of their contributions to acid rain. Several studies suggest that different isotopic techniques can be used to differentiate among different types of atmospherically derived nitrate and ammonium. For example, Heaton (1990) found that derived from vehicle exhaust... [Pg.2599]

An inductively-coupled plasma (ICP) is an effective spectroscopic excitation source, which in combination with atomic emission spectrometry (AES) is important in inorganic elemental analysis. ICP was also considered as an ion source for MS. An ICP-MS system is a special type of atmospheric-pressure ion source, where the liquid is nebulized into an atmospheric-pressure spray chamber. The larger droplets are separated from the smaller droplets and drained to waste. The aerosol of small droplets is transported by means of argon to the torch, where the ICP is generated and sustained. The analytes are atomized, and ionization of the elements takes place. Ions are sampled through an orifice into an atmospheric-pressure-vacuum interface, similar to an atmospheric-pressure ionization system for LC-MS. LC-ICP-MS is extensively reviewed, e.g., [12]. [Pg.8]

Methods using some type of atmospheric or reduced pressure steam distillation have been historically the most commonly used, and essential oils were (11) and are still frequently isolated this way on a commercial scale. The SDE or Likens Nickerson extraction method (12,13) was an extension of the Essential Oil industry s technique of cohobation where Ae condensed steam is separated fiom the volatile oil using a simple trap and returned to the still in order to minimize loss of water soluble volatiles. SDE had actually been described earlier in practical organic chemistry textbooks (14,15). The Likens Nickerson head though was simpler and easier to construct and control than the earlier organic chemist s version. Other versions of the head have been designed and used (2). [Pg.242]

Perhaps the most widely studied instrument variable has been the effect of furnace atmosphere on the TG curve of a sample. The effect of the atmosphere on the mass-change curve depends upon (I) the type of reaction, (2) the nature of the decomposition products, and (3) the type of atmosphere employed. For (1), three types of reactions may be studied, either reversible... [Pg.12]

Morita (144) also studied the DTA of several a- and jS-Iinked polygluco-sans, as well as rice starch. An interesting feature of this investigation was the study of the effect of moisture on the DTA curves obtained. This was illustrated by the study of rice starch stored in various types of atmospheres such as vacuum, 100% relative humidity water vapor, and so on. The presence of moisture altered the endothermic peak with a A7 in of 130°C, but not the 275 or 310°C peaks. The results suggest that the original 130°C peak is not entirely due to the loss of residual moisture and that the dehydration process is not completely reversible. [Pg.365]


See other pages where TYPES OF ATMOSPHERES is mentioned: [Pg.491]    [Pg.165]    [Pg.577]    [Pg.293]    [Pg.346]    [Pg.494]    [Pg.498]    [Pg.543]    [Pg.493]    [Pg.327]    [Pg.215]    [Pg.747]    [Pg.374]    [Pg.915]    [Pg.491]    [Pg.227]    [Pg.246]    [Pg.269]    [Pg.297]    [Pg.840]    [Pg.184]    [Pg.258]    [Pg.123]    [Pg.360]    [Pg.82]    [Pg.295]    [Pg.85]   


SEARCH



Atmosphere types

© 2024 chempedia.info