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Plume

Morsing. 1996. Jet drop models for control of cold air trajectories m ventilated buildings. In Roomvent 96 Proceedings of the. Sth International Conference on Air Distribution in Rooms, vol. 1, July. Yokohama, Japan. [Pg.517]

Zhivov, A. M. 1992. Selection of general ventilation method for industrial spaces. Presented at 1992 annual ASHRAE meeting ( Supply air systems for industrial facilities seminar). [Pg.517]

Zhivov, A., J.B. Priest, and L.L.. Christianson. 1996. Air distribution design for realistic rooms, in R.oomvent 96 Proceedings of the Sth International Conference on Air Distrihutinn m Rooms, vol. l,July. Yokohama, Japan, [Pg.517]

Zhivov, A. M. 1994. Air supply with directing jets. In Ventilation 94 Proceedings of the fourth International Symposium on Ventilation for Contaminant Control. Stockholm, Sweden. [Pg.517]

Theory and Practice of ait distribution with inclined jets. ASFIR.AE Transactions, vol. 9, no, 1. Stockholm,. Sweden. [Pg.517]


The nature of these paraffins and their concentration in diesel fuel affect the three temperatures that characterize the cold behavior. The cloud point is the temperature at which crystals of paraffins appear when the temperature is lowered. The cold filter pluming point is defined as the temperature under which a suspension no ionger flows through a standard filter. Finally, the pour point is the temperature below which the diesel fuel no longer flows by simple gravity in a standard tube. These three temperatures are defined by regulations and the refiner has three types of additives to improve the quality of the diesel fuel of winter. [Pg.353]

Gaussian mode Gaussian plume model Gauss-Seidel Gauzes Gaylusite... [Pg.436]

Plictran Plioflex Plot plan PLP-DPG-PLP Plug valves Plumbic acetate Plumbing applications PlumbopaHadimte Plumbostanmte Plumbous acetate Plume containment Plummer s disease Plums... [Pg.772]

Atmospheric stabUity can be examined utilising the Gaussian Plume model which ignores possible transformations ... [Pg.367]

If condensation requires gas stream cooling of more than 40—50°C, the rate of heat transfer may appreciably exceed the rate of mass transfer and a condensate fog may form. Fog seldom occurs in direct-contact condensers because of the close proximity of the bulk of the gas to the cold-Hquid droplets. When fog formation is unavoidable, it may be removed with a high efficiency mist collector designed for 0.5—5-p.m droplets. Collectors using Brownian diffusion are usually quite economical. If atmospheric condensation and a visible plume are to be avoided, the condenser must cool the gas sufftciendy to preclude further condensation in the atmosphere. [Pg.389]

Direct water spray cooling must be carried out with care. The spray chamber must be designed to ensure complete evaporation of all Hquid droplets before the gas enters the baghouse. Spray impinging on the chamber walls can result ia a dust mud iaside the chamber and any increase ia gas dewpoint may result in baghouse problems or atmospheric plume condensation. Spray nozzle wear can result in coarse or distorted spray and wetted bags, and water pressure failure can cause high temperature bag deterioration. [Pg.406]

G. A. Briggs, "Plume Rise," USAEC Critical Review Series TID-25075, NTIS, Springfield, Va., 1969. [Pg.414]

Effective Stack Height Plume Rise, US EPA Air Pollution Training Institute Pub. SP.406, with Chapts. D, E, and G by G. A. Briggs and Chapt. H by D. [Pg.414]

G. A. Briggs, Plume Rise Predictions, Eectures on Air Pollution andEnvironmental Impact Analyses, American Meteorological Society, Boston, Mass., 1975. [Pg.414]

N. E. Bowne, R. J. Londergan, R. J. Minott, D. R. Murray, "Preliminary Results from the EPRI Plume Model VaUdafion Project— Plains Site,"... [Pg.414]

Fig. 8. Characteristic plume patterns where (--) represents dry-adiabatic lapse rate and (—), air (a) fanning (b) fumigation (c) lofting and (d) looping. Fig. 8. Characteristic plume patterns where (--) represents dry-adiabatic lapse rate and (—), air (a) fanning (b) fumigation (c) lofting and (d) looping.
Fig. 3. (a) General locations of hydrothemial power plants in the continental United States (6). Power is produced directiy from hydrothermal steam indicated by the steam plume at The Geysers in northern California. At all other locations, hot water resources are utilized for power production. In 1993, a hydrothermal power plant also came on line on the island of Hawaii, (b) Location of The Geysers steam-dominated hydrothermal field (D) in Lake and Sonoma counties, within the boundaries of the Cleadake—Geysers thermal anomaly (B). [Pg.264]

Groundwater monitoring is a necessary component in any investigation of subsurface contamination. A wide variety of information can be gleaned from the data including groundwater velocity and direction, and contaminant identification and concentration. These data can be combined with other observations to infer various characteristics of the contamination. Examples are source and timing of the release, and future location of the contaminant plume. [Pg.401]

The dispersion model is typically used to determine the downwind concentrations of released materials and the total area affected. Two models are available the plume and the puff. The plume describes continuous releases the puff describes instantaneous releases. [Pg.475]

The environmental appHcations of infrared spectrometry are many and varied. Many appHcations at industrial sites are analogous to those for on-line process analysis waste streams and recycling processes can be monitored in the same way. Commercial infrared stack-gas monitors are based on either an extractive probe attached to a long-path gas ceU or an open-path (across stack) configuration (69). Stack plume and flare monitoring can be done externally... [Pg.201]

Some results of the constant-value pricing system are as foUow generation in a central unit at relatively low pressure, <4.24 MPa (600 psig) tremendous economic pressure to use turbines rather than motors for drives lack of incentive for high efficiency turbines excessively high temperature differentials in steam users tremendous incentive to recover waste heat as low pressure steam and a large plume of excess low pressure steam vented to the atmosphere. [Pg.92]

Cooling-Tower Plumes. An important consideration in the acceptabiHty of either a mechanical-draft or a natural-draft tower cooling system is the effect on the environment. The plume emitted by a cooling tower is seen by the surrounding community and can lead to trouble if it is a source of severe ground fog under some atmospheric conditions. The natural-draft tower is much less likely to produce fogging than is the mechanical-draft tower. Nonetheless, it is desirable to devise techniques for predicting plume trajectory and attenuation. [Pg.105]

Not only may the cooling-tower plume be a source of fog, which in some weather conditions can ice roadways, but the plume also carries salts from the cooling water itself. These salts may come from salinity in the water, or may be added by the cooling-tower operator to prevent corrosion and biological attack in the column. [Pg.105]


See other pages where Plume is mentioned: [Pg.301]    [Pg.1331]    [Pg.185]    [Pg.30]    [Pg.34]    [Pg.39]    [Pg.367]    [Pg.368]    [Pg.376]    [Pg.377]    [Pg.377]    [Pg.407]    [Pg.34]    [Pg.41]    [Pg.256]    [Pg.93]    [Pg.93]    [Pg.94]    [Pg.489]    [Pg.200]    [Pg.12]    [Pg.327]    [Pg.79]    [Pg.395]    [Pg.395]    [Pg.5]    [Pg.94]    [Pg.348]    [Pg.351]    [Pg.327]    [Pg.105]    [Pg.105]    [Pg.106]   
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See also in sourсe #XX -- [ Pg.133 ]

See also in sourсe #XX -- [ Pg.253 ]




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13.1 Plume Hypothesis

Age Dating of NAPL Pools and Dissolved Hydrocarbon Plumes

Air plume modeling

Air plume models

Analytical Properties of the Gaussian Plume Equation

Atmospheric dispersal, plume elevation

Biogeochemical interactions in plumes

Biomass plumes

Bubbles plume

Buoyant plume

Chemical plumes

Chlorinated solvent plume

Chlorinated solvent plumes - case studies of natural attenuation

Combusting Plumes

Concentration fields, plumes

Concentration gradient, plumes

Conservation equations plumes

Containment plume

Containment plume pumping well method

Contaminant plume

Contaminant plumes, determination

Contamination/plumes

Cooling towers plume abatement

Dense plumes

Discharge plume

Dispersion Gaussian plume model

Dispersion parameters mean plume concentrations

Dissolved plume

Dissolved plume portion

Droplet plume technique

Dynamic plume model

East African plume

Edge of the plume

Electrospray ionization spray plume

Event plumes

Explosive plume

Filament, plume

Fire plumes

Fire plumes described

Fire plumes entrainment rate

Fire plumes with combustion

Fogging and Plume Abatement

Following plumes

Formation of the Electrospray Plume

Gasoline plume

Gaussian plume

Gaussian plume computations

Gaussian plume equation

Gaussian plume equation analytical properties

Gaussian plume equation derivation

Gaussian plume equation dispersion parameters

Gaussian plume formula

General features of hydrothermal plumes

Groundwater, contaminant plume

He plumes in the ocean

Heat Transfer above the Plume

Heat flow mantle plumes

Holland plume rise

Holland plume rise equation

Hydrothermal fluids plumes

Hydrothermal plumes

Hydrothermal plumes sulphidic

Information for Tracking Chemical Odor Plumes

Laser ablation plumes used in thin film

Laser plume

Laser vaporization/ablation plumes

Mantle plumes

Mantle plumes origin

Matrix plume, MALDI ionization

Melting plume

Mercury vapor plumes

Metadynamics Input Files with PLUMED

Methane plumes

Micro-plume injection mixer

Micro-plume injection mixing

Microbial ecology of hydrothermal plumes

Microbial productivity and organic carbon in plumes

Migration of an Acid Plume at a Uranium Mill Tailings Site

Model plume search

Modeling chlorinated solvent plumes

Models Gaussian plume

Models plume rise

Models tilted plume model

Moth, plume

Odor plumes

Odour plumes

Optimal plume control

PLUMED

PLUMED

Pheromone plume

Plane Plume

Plume Gaussian profiles

Plume Interaction

Plume Subject

Plume abatement

Plume aerosol dispersion

Plume airflow turbulence

Plume analysis

Plume attenuation

Plume behavior

Plume boundaries

Plume characteristic scales

Plume characteristics

Plume classification schemes

Plume collisions

Plume control

Plume databases

Plume defined

Plume dilution

Plume elevation

Plume elevation products

Plume expansion

Plume head flow

Plume heights

Plume injection

Plume laser ablation

Plume mapping

Plume material

Plume material spreading

Plume material thickness

Plume migration

Plume model

Plume model dispersion

Plume model pollution concentration

Plume model sedimentation

Plume model, described

Plume model, fluctuating

Plume models, multiple source

Plume orientation

Plume photographs

Plume physics

Plume physics dispersion

Plume property

Plume releases

Plume rise

Plume spreading

Plume stability

Plume standard deviations

Plume structure

Plume suppressant

Plume tails

Plume temperature

Plume tracing

Plume transport models

Plume velocity

Plume-lithosphere interactions

Plume-related Hypotheses

Plumes 196 INDEX

Plumes Focus Area

Plumes dimensions

Plumes in Confined Spaces

Plumes length

Plumes types

Plumes used in thin film deposition

Plumes, particulate stack

Pollutant plume

Ponding, plume material

Radioactive plume

Rapid plume tracking

Remediation strategies, for dissolved contaminant plumes

River plume

Rocket plume

STRUCTURE OF TURBULENT CHEMICAL PLUMES

Sea plumes

Semi-plumes

Slender-plume approximation

Sources Producing Plumes

Spray Pattern and Plume Geometry of Nasal Products

Stack-plume observations

Starting plume

Steam vent plumes

Temporal Evolution of a Laser Desorption Plume

The Plume Hypothesis

Thermal plume

Thermal plume rise

Tower Plumes

Transient Aspects of Fire Plumes

Turbulent chemical plume

Turbulent plume

Turbulent plume zone

Turbulent stack plumes

Underwater chemical plumes

Underwater plumes

Urban plume

Vapor plume

Variation of the Plume Structure

Volcanic helium plumes

Volcanic plume

Western Trace plume

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