Big Chemical Encyclopedia

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

Articles Figures Tables About

Water helium

The extrapolation of Battino s recommended equations above about 350 K is not recommended. However, for several of the systems, especially helium + water and krypton + water, the extrapolated equation represents the higher temperature data surprisingly well. The extrapolation of Battino s equation for the neon +... [Pg.520]

Helium + water. Battino selected solubility data from nine papers for the 273-348 K region (1). We have added values calculated from the data of Potter and Clynne ( ) and from Wiebe and Gaddy (7). The solubility value which was calculated from the data of Wiebe and Gaddy at 590 K, was not used in the linear regression. The data and curve are shown in Figure 2. Only one curve is shown. Battino s recommended equation for the solubility data below 348 K and the equation for the entire data set differ by only a fraction of a percent. The curve for the four constant equation is not shown. [Pg.521]

Figure 2. Helium + water—mole fraction solubility at 1 atm helium partial pressure vs. temperature. At temperatures above 353 K (O) (6) ( , ) (1). The 590 K value of Wiebe and Gaddy was not included in the linear regression. Figure 2. Helium + water—mole fraction solubility at 1 atm helium partial pressure vs. temperature. At temperatures above 353 K (O) (6) ( , ) (1). The 590 K value of Wiebe and Gaddy was not included in the linear regression.
Based on 220 experiments with helium-water, nitrogen-water, nitrogen-ethanol and nitrogen-aqueous 40 % ethyleneglycol within the ranges ... [Pg.284]

The diameter and volume of the micropores were also determined by the measurement of the density using as displacement molecules with different sizes, e g., helium, water, benzene, decaline. It was found that in the case of CMS-Kl and CMS-K2 sieves, the micropores with the pore size within the range 0.255-0.528 are dominated and that the used measurements enable characterisation of the structure of carbon molecular sieves. For equilibrium sieve the analysis of the micropores volume with the use of the pycnometric technique does not give proper results. [Pg.225]

Today, basin-scale mass transfer of some materials (e.g., helium, water, and petroleum) is unquestioned (e.g.. Hunt, 1996). OAer materials (e.g., titanium and the REEs) are sufficiently mobile to appear within authigenic precipitates, but are likely to be immobile on the scale of a hand specimen. Mobilities of the major elements that make up sandstones and shales (silicon, aluminum, calcium, sodium, potassium) remain controversial. Conflicting notions about processes in rock suites across the wide range of burial conditions and alteration show that fundamental questions remain unanswered about the nature of the volumetrically significant processes within a major segment of the rock cycle. It is very likely that something is wrong, or at least inadequate. [Pg.3624]

The steam experiments were carried out by flowing helium through a water bubbler maintained at constant temperature in a water bath. The water flow rate was controlled by manipulating the helium flow rate and the temperature of the bath. The tube carrying the helium-water mixture was heated to 353 K to prevent any further condensation before the reaction zone. The water was trapped in a water condenser after the reactor. [Pg.386]

Since carbon molecular sieves are amorphous materials, the dimensions of their pore structures must be measured phenomenologically by the adsorption of small probe molecules with different critical dimensions. There is insufficient long range order to utilize standard x-Ray diffraction methods for characterization. The earliest reports of molecular sieving carbons dealt primarily with coals and charcoals. Sorption of helium, water, methanol, n-hexane, and benzene was measured and related to the porosity of the carbon. Pore-sizes were estimated to be two to six angstroms (3-6). In a classic paper P.H. Emmett described methods for tailoring the adsorptive properties and pore size distributions of carbon Whetlerites. [Pg.336]

Penetrant carbon dioxide nitrogen oxygen helium water vapor... [Pg.410]

A phase diagram is a map that indicates the areas of stability of the various phases as a function of external conditions (temperature and pressure). Pure materials, such as mercury, helium, water, and methyl alcohol are considered one-component systems and they have unary phase diagrams. The equilibrium phases in two-component systems are presented in binary phase diagrams. Because many important materials consist of three, four, and more components, many attempts have been made to deduce their multicomponent phase diagrams. However, the vast majority of systems with three or more components are very complex, and no overall maps of the phase relationships have been worked out. [Pg.2150]

A helium/water cooler was provided in order to ensure the desired temperature equilibrium between added and removed heat as well as to supply cooling gas and sealing gas. [Pg.192]

A distinction might be made, in fact, when the MR is used to carry out a catalytic reaction, considering whether the membrane itself has a catalytic function or not. In the case of MRs for H2 production, most of the membranes used are permselective, which allows the selective removal of H2 from the reaction volume under the effect of a driving force. This is a function of the species partial pressures on both the membrane sides and can be created by means of an inert sweep gas in the permeate compartment (nitrogen, helium, water, etc.), or with the application of a pressure difference between the retentate and permeate sides. [Pg.90]

Holt et al. [16] measured water and gas flow through the pores of double-walled carbon nanotubes. These tubes had inner diameters less than 2 nm with nearly defect-free graphitic walls. Five hydrocarbon and eight non-hydrocarbon gases were tested to determine flow rates and to demonstrate molecular weight selectivity compared with helium. Water flow was pressure driven at 0.82 atm and measured by following the level of the meniscus in a feed tube. The results for both gas and liquid show dramatic enhancements over flux rates predicted with continuum flow models. Gas flow rates were between 16 and 120 times than expected according to the Knudsen diffusion model in which fluid molecule-wall collisions dominate the flow. [Pg.2369]

Figure 11. Radial distribution functions for the water-water (ideal solution), helium-water, and neon-water interactions at infinite dilution at =1.0 and p, = 1.5. Figure 11. Radial distribution functions for the water-water (ideal solution), helium-water, and neon-water interactions at infinite dilution at =1.0 and p, = 1.5.
In this section, reference is made to discrete approaches for the modeling of gas/condensate flow through mesoporous structures. Capillary network models are presented along with typical predictions and sensitivity studies. Comparison is made with results from the literature. Finally, experimental results obtained in our laboratory are presented for the system helium-water vapor on two mesoporous membranes, made by compaction of alumina microspheres, with porosities 0.41 and 0.48, respectively. [Pg.700]

The first division in the classification of matter is between a pure substance and a mixture. A pure substance is made up of only one component and its composition is invariant (it does not vary from one sample to another). The components of a pure substance can be individual atoms or groups of atoms joined together. For example, helium, water, and table salt (sodium chloride) are all pure substances. Each of these substances is made up of only one component helium is made up of helium atoms, water is made up of water molecules, and sodium chloride is made up of sodium chloride units. The composition of a pure sample of any one of these is always exactly the same (because you can t vary the composition of a substance made np of only one component). [Pg.7]

Compatible coolant(s) Water Helium, water (in metal clad)... [Pg.60]

Figure 15 Radial distribution functions, g (r), for water-water (ideai soiution), helium-water, and neon-water at infinite dilution at Pr = i. 5 and T, = 1.0... Figure 15 Radial distribution functions, g (r), for water-water (ideai soiution), helium-water, and neon-water at infinite dilution at Pr = i. 5 and T, = 1.0...
J. A. Luker and Thomas Gniewek, Saturation Composition of Steam— Helium—Water Mixtures PVT Data and Heat Capacity of Superheated Steam— Helium Mixtures, USAEC Report AECU-3299, Syracuse University Research Institute, July 29, 1955. [Pg.126]


See other pages where Water helium is mentioned: [Pg.1415]    [Pg.520]    [Pg.47]    [Pg.249]    [Pg.1865]    [Pg.582]    [Pg.249]    [Pg.40]    [Pg.173]    [Pg.464]    [Pg.317]    [Pg.419]    [Pg.1417]    [Pg.431]    [Pg.431]    [Pg.392]    [Pg.351]    [Pg.76]   
See also in sourсe #XX -- [ Pg.521 , Pg.522 ]




SEARCH



Helium in water

Helium solubility in water

© 2024 chempedia.info