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Books on the topic 'Formation polluant'

Author: Grafiati
Published: 4 June 2021
Last updated: 3 February 2022

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1

Lemieux, Paul M. Pulverized coal combustion: Pollutant formation and control, 1970-1980. Research Triangle Park, NC: U.S. Environmental Protection Agency, Air and Energy Engineering Research Laboratory, 1990.

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2

Warnatz, Jürgen. Combustion: Physical and Chemical Fundamentals, Modeling and Simulation, Experiments, Pollutant Formation. 3rd ed. Berlin, Heidelberg: Springer Berlin Heidelberg, 2001.

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3

1959-, Maas U., and Dibble Robert W, eds. Combustion: Physical and chemical fundamentals, modelling and simulation, experiments, pollutant formation. Berlin: Springer, 1996.

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4

Warnatz, Jürgen. Combustion: Physical and Chemical Fundamentals, Modeling and Simulation, Experiments, Pollutant Formation. Berlin, Heidelberg: Springer Berlin Heidelberg, 1999.

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1959-, Maas U., and Dibble Robert W, eds. Combustion: Physical and chemical fundamentals, modeling and simulation, experiments, pollutant formation. 2nd ed. Berlin: Springer, 1999.

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6

Gillani, Noor V. Ozone formation in pollutant plumes: A reactive plume model with arbitrary crosswind resolution. Research Triangle Park, NC: U.S. Environmental Protection Agency, Atmospheric Sciences Research Laboratory, 1987.

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7

Montoya, Barry L. Factors affecting total organic carbon and trihalomethane formation potential in exports from the South Sacramento-San Joaquin Delta and down the California Aqueduct. Sacramento, Calif.]: State of Calif., The Resouces Agency, Dept. of Water Resources, Division of Operations and Maintenance, Environmental Assessment Branch, 2005.

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8

Leenheer, J. A. Effects of organic wastes on water quality from processing of oil shale from the Green River Formation, Colorado, Utah, and Wyoming. Washington, D.C: U.S. G.P.O., 1986.

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9

K, Baumann, ed. Air quality control: Formation and sources, dispersion, characteristics and impact of air pollutants : measuring methods, techniques for reduction of emissions and regulations for air quality control. New York: Springer-Verlag, 1996.

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10

Baumbach, Günter. Air quality control: Formation and sources, dispersion, characteristics and impact of air pollutants--measuring methods, techniques for reduction of emissions and regulations for air quality control. Berlin: Springer, 1996.

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11

Christian, Vovelle, ed. Pollutants from combustion: Formation and impact on atmospheric chemistry. Dordrecht: Kluwer Academic Publishers, 2000.

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12

Vovelle, Christian. Pollutants from Combustion Formation and Impact on Atmospheric Chemistry. Springer, 2000.

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13

Schwarz, Christian, Gunnar Stiesch, Günter P. Merker, and Frank Otto. Simulating Combustion: Simulation of combustion and pollutant formation for engine-development. Springer, 2005.

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14

Vallero, Daniel A. Air Pollution Calculations: Quantifying Pollutant Formation, Transport, Transformation, Fate and Risks. Elsevier, 2019.

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15

Combustion: Physical and Chemical Fundamentals, Modeling and Simulation, Experiments, Pollutant Formation. 4th ed. Springer, 2006.

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16

Vallero, Daniel A. Air Pollution Calculations: Quantifying Pollutant Formation, Transport, Transformation, Fate and Risks. Elsevier, 2019.

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17

Combustion: Physical and Chemical Fundamentals, Modeling and Simulation, Experiments, Pollutant Formation. 3rd ed. Springer, 2001.

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18

Eran, Sher, ed. Handbook of air pollution from internal combustion engines: Pollutant formation and control. Boston: Academic Press, 1998.

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19

Succi, Sauro. Lattice Boltzmann for reactive flows. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780199592357.003.0026.

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The dynamics of reactive flows lies at the heart of several important applications, such as combustion, heterogeneous catalysis, pollutant conversion, pattern formation in biology and many others. In general, LB is well suited to describe reaction-diffusion applications with flowing species. This chapter provides the basic guidelines to include reactive phenomena within the LBE formalism. Reactive flows obey the usual fluid equations, augmented with a reactive source term, accounting for species transformations due to chemical reactions. Such term comes typically in the form of a polynomial product of the mass densities of the reacting species.
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20

Unintentional formation and emission of the persistent organic pollutants HCB and PCBs in the Nordic countries. Nordic Council of Ministers, 2009. http://dx.doi.org/10.6027/tn2009-518.

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21

Formation, distribution and chemical transformation of air pollutants: Papers of the workshop held in Frankfurt am Main, 5 to 6 February 1986. Weinheim: VCH, 1987.

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22

R, Zellner, ed. Formation, distribution, and chemical transformation of air pollutants: Papers of the workshop held at Frankfurt am Main, 5 to 6 February 1986. Weinheim: VCH, 1986.

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23

Baumbach, Günter, and Masamichi Kobayashi. Air Quality Control: Formation and Sources, Dispersion, Characteristics and Impact of Air Pollutants - Measuring Methods, Techniques for Reduction of ... Brand: Springer, 2011.

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24

Toxicological and Immunological Aspects of Drug Metabolism and Environmental Chemicals: Symposium Hotel Schloss Fuschl, Austria 1St-4Th, Nov 1987. John Wiley & Sons Inc, 1988.

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25

W, Estabrook Ronald, ed. Toxicological and immunological aspects of drug metabolism and environmental chemicals: Symposium, Hotel Schloss Fuschl, Austria, 1st-4th November 1987. Stuttgart ; New York: Schattauer Verlag, 1988.

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26

Tibaldi, Stefano, and Franco Molteni. Atmospheric Blocking in Observation and Models. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.611.

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The atmospheric circulation in the mid-latitudes of both hemispheres is usually dominated by westerly winds and by planetary-scale and shorter-scale synoptic waves, moving mostly from west to east. A remarkable and frequent exception to this “usual” behavior is atmospheric blocking. Blocking occurs when the usual zonal flow is hindered by the establishment of a large-amplitude, quasi-stationary, high-pressure meridional circulation structure which “blocks” the flow of the westerlies and the progression of the atmospheric waves and disturbances embedded in them. Such blocking structures can have lifetimes varying from a few days to several weeks in the most extreme cases. Their presence can strongly affect the weather of large portions of the mid-latitudes, leading to the establishment of anomalous meteorological conditions. These can take the form of strong precipitation episodes or persistent anticyclonic regimes, leading in turn to floods, extreme cold spells, heat waves, or short-lived droughts. Even air quality can be strongly influenced by the establishment of atmospheric blocking, with episodes of high concentrations of low-level ozone in summer and of particulate matter and other air pollutants in winter, particularly in highly populated urban areas.Atmospheric blocking has the tendency to occur more often in winter and in certain longitudinal quadrants, notably the Euro-Atlantic and the Pacific sectors of the Northern Hemisphere. In the Southern Hemisphere, blocking episodes are generally less frequent, and the longitudinal localization is less pronounced than in the Northern Hemisphere.Blocking has aroused the interest of atmospheric scientists since the middle of the last century, with the pioneering observational works of Berggren, Bolin, Rossby, and Rex, and has become the subject of innumerable observational and theoretical studies. The purpose of such studies was originally to find a commonly accepted structural and phenomenological definition of atmospheric blocking. The investigations went on to study blocking climatology in terms of the geographical distribution of its frequency of occurrence and the associated seasonal and inter-annual variability. Well into the second half of the 20th century, a large number of theoretical dynamic works on blocking formation and maintenance started appearing in the literature. Such theoretical studies explored a wide range of possible dynamic mechanisms, including large-amplitude planetary-scale wave dynamics, including Rossby wave breaking, multiple equilibria circulation regimes, large-scale forcing of anticyclones by synoptic-scale eddies, finite-amplitude non-linear instability theory, and influence of sea surface temperature anomalies, to name but a few. However, to date no unique theoretical model of atmospheric blocking has been formulated that can account for all of its observational characteristics.When numerical, global short- and medium-range weather predictions started being produced operationally, and with the establishment, in the late 1970s and early 1980s, of the European Centre for Medium-Range Weather Forecasts, it quickly became of relevance to assess the capability of numerical models to predict blocking with the correct space-time characteristics (e.g., location, time of onset, life span, and decay). Early studies showed that models had difficulties in correctly representing blocking as well as in connection with their large systematic (mean) errors.Despite enormous improvements in the ability of numerical models to represent atmospheric dynamics, blocking remains a challenge for global weather prediction and climate simulation models. Such modeling deficiencies have negative consequences not only for our ability to represent the observed climate but also for the possibility of producing high-quality seasonal-to-decadal predictions. For such predictions, representing the correct space-time statistics of blocking occurrence is, especially for certain geographical areas, extremely important.
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