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Water escape, velocity

Figure 11.2 V is the velocity of the water escaping from the hole. Figure 11.2 V is the velocity of the water escaping from the hole.
Figure 9.10. Shock pressure versus particle velocity for water ice, and snow with different densities. Curves for serpentine with the impact velocity of Earth s escape velocity and ice with Ganymede s escape velocity are plotted for the estimation of shock pressure by means of impedance matching method. Escape velocities for satellites are indicated on the particle velocity axis. (Figure from /Vhrens and O Keefe [31].)... Figure 9.10. Shock pressure versus particle velocity for water ice, and snow with different densities. Curves for serpentine with the impact velocity of Earth s escape velocity and ice with Ganymede s escape velocity are plotted for the estimation of shock pressure by means of impedance matching method. Escape velocities for satellites are indicated on the particle velocity axis. (Figure from /Vhrens and O Keefe [31].)...
The undissolved gas, which contains a small amount of ozone, accumulates under pressure at the top of the ozonation chamber. This gas is exhausted through a pipe which leads to the channel where the raw water enters. The residual ozone is thus recovered for the purpose of preozonating the water. In a permanent installation the outflow of the gas under pressure from the ozonation chamber is regulated by a control activated by the level of the water in this chamber. The undissolved gas finally escapes at the top of the water entrance channel, the bubbles of gas moving counter-current to the flow of water. The velocity of the water in the preozonation channel is not sufficient to carry the bubbles of gas towards the ozonation chamber. [Pg.457]

Water was surely abundant in early atmospheres and throughout Earth s history with a cooled lithosphere. If there were water. Earth had an oxidizing atmosphere, while hydrogen liberated from water escaped from Earth s atmosphere just as it continues to do today. Both hydrogen gas and helium, when released into Earth s atmosphere, escape from Earth never to return, because the thermal velocity of these gases is above the escape velocity of a mass of their size. They are two of a very few substances that are not automatically recycled. We have no other choice than to recycle unless garbage is to be disposed of in outer space, a highly unlikely event. [Pg.36]

A distributor is frequently installed at the top of the column for use during backwash. It collects water evenly and prevents resin from escaping the column should unexpected surges develop in the water flow during backwash. Columns lacking an upper distributor or screen to prevent loss of resin should have an external system to prevent resin from being lost to the drain. It is referred to as a resin trap and may consist of a porous bag that fits over the outlet pipe or a tank designed to lower the linear velocity. Resin drops to the bottom of the tank and is returned to the column when convenient. [Pg.381]

Gas flow in these rotary dryers may be cocurrent or countercurrent. Cocurrent operation is preferred for heat-sensitive materials because gas and product leave at the same temperature. Countercurrent operation allows a product temperature higher than the exit gas temperature and dryer efficiency may be as high as 70%. Some dryers have enlarged cylinder sections at the material exit end to increase material holdup, reduce gas velocity, and minimize dusting. Indirectly heated tubes are installed in some dryers for additional heating capacity. To prevent dust and vapor escape at the cylinder seals, most rotary dryers operate at a negative internal pressure of 50—100 Pa (0.5—1.0 cm of water). [Pg.249]

Design faults in two-pass condensers and heat exchangers that can cause corrosion include poor division plate seals allowing the escape of water at high velocity between the passes, and flow patterns that produce stagnant zones. [Pg.76]

The discussion in the previous section suggests that the track of a heavy ion becomes more like that of a fast electron with increasing velocity. Therefore one expects that in the high velocity limit the yields of water products with heavy ions are the same as with fast electrons or y-rays. The yields for the major products of water radiolysis in fast electron or y-radiolysis are given in Table 1. These values were taken from a number of different sources in conjunction with the results predicted by model calculations [73,116,119-123]. Material balance shows that almost four molecules of water are decomposed for every 100 eV of energy absorbed by fast electrons or y-rays. Because only about six water molecules are initially decomposed, most of the water products escape intraspur reactions in fast electron or y-radiolysis. [Pg.418]

Let s take a close look at the use of the term AH. Figure 11.2 shows a bucket with a hole punched in its side. The velocity of the water, as it escapes from the hole is V in the preceding equation. The height of water in the bucket, above the center of the hole, is AH. If we replaced the water in the bucket with gasoline, which has a lower density, the same hole velocity would occur with the same height of fluid. [Pg.126]

The pressure drop of the fluid escaping from the bucket is called nozzle exit loss. Actually, nothing is lost the potential energy, or pressure head of the water in the bucket, is just converted into velocity, or kinetic energy. [Pg.126]

The velocity of water flowing from the tub through the drain is 20 ft/s. The pressure drop, in psi, of the water as it escapes from the tub, is... [Pg.129]

In contrast, Zahnle et al. [116] argued tliat the present atmosphere of Titan was delivered by comets of low velocity at late accretion, ai d Uiat Titan has suffered less atmospheric erosion and has retained a higher fraction of incoming atmophiles. For a more-or-less solar composition comet, the most important C-and N-bearing products are likely CO and N2, witli small additional amounts of CO2, CH4, C2H2, and HCN. Most of the comet s N2 entered the atmosphere on Titan, where CO has been consumed by reaction with water to form CO2, CH4, and H2, the latter readily escaping into space. This alternative model for the formation of the present day atmosphere on Titan does not require conversion of N2 from NH3. [Pg.53]

Example 9.11. Retention of Hydrophobic Organic Pollutants in Ground-water Aquifer Because of a leak in a waste container, traces of tetrachlor-ethylene and 1,2,4,5-tetrachlorobenzene escape in a groundwater. Provide an estimate of how long it takes to find these pollutants at a distance (direction of flow) of 25 m. The flow velocity of the groundwater is 2 m day . The following characteristics of the aquifer are available ... [Pg.597]

The fastest water molecules are escaping from the water on his skin. The average velocity, and thus the temperature, of the remaining water molecules is lower. [Pg.536]

Air flow across the dried wood surface is essential to remove the escaping water vapor, a factor that was emphasized by Mery man (58), who was able with his equipment to achieve sublimation drying for his standard specimen in 8 h, as opposed to 6 h in an eflSciently designed vacuum apparatus. The Davis Base wind is predominantly from an easterly sector, with little seasonal variation, and has a mean velocity of 5 4.4 m s" ... [Pg.256]


See other pages where Water escape, velocity is mentioned: [Pg.118]    [Pg.119]    [Pg.129]    [Pg.218]    [Pg.220]    [Pg.367]    [Pg.184]    [Pg.372]    [Pg.156]    [Pg.476]    [Pg.249]    [Pg.18]    [Pg.1652]    [Pg.1698]    [Pg.476]    [Pg.840]    [Pg.941]    [Pg.200]    [Pg.459]    [Pg.236]    [Pg.48]    [Pg.1372]    [Pg.780]    [Pg.840]    [Pg.304]    [Pg.662]    [Pg.304]    [Pg.47]    [Pg.569]    [Pg.48]    [Pg.28]    [Pg.207]    [Pg.723]   
See also in sourсe #XX -- [ Pg.184 ]




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