<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Cheng, L.</style></author><author><style face="normal" font="default" size="100%">Peake, E.</style></author><author><style face="normal" font="default" size="100%">Rogers, D.</style></author><author><style face="normal" font="default" size="100%">Davis, A.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Oxidation of nitric oxide controlled by turbulent mixing in plumes from oil sands extraction plants</style></title></titles><keywords><keyword><style  face="normal" font="default" size="100%">air emissions</style></keyword><keyword><style  face="normal" font="default" size="100%">Alberta Innovates</style></keyword><keyword><style  face="normal" font="default" size="100%">AOSTRA</style></keyword><keyword><style  face="normal" font="default" size="100%">ARC</style></keyword><keyword><style  face="normal" font="default" size="100%">plume measurement and movement</style></keyword><keyword><style  face="normal" font="default" size="100%">UofC</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">1986</style></year></dates><publisher><style face="normal" font="default" size="100%">Atmospheric Environment </style></publisher><volume><style face="normal" font="default" size="100%">20 </style></volume><pages><style face="normal" font="default" size="100%">6 pages </style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Results are presented of airborne measurements taken in oil sands extraction plant plumes in Fort McMurray, Alberta, Canada. Measurements with fast response monitors at a high sampling rate illustrate the narrow reaction zone in the plume caused by a turbulent diffusion reaction of NO to NO2 as suggested by theoretical and laboratory studies. The measured conversion rates of NO to NO2 varied considerably from day to day, from 0.2 to 21.4% min−. Analysis of the oxidation rate of NO to NO2 and of the atmospheric turbulence parameter reveals that, over the distances and time scales within which the plumes are distinguishable from the background, the nitrogen oxides chemistry in the plumes is controlled by the rates at which the plumes mix with the ambient air (containing ozone), rather than by chemical kinetics.</style></abstract><issue><style face="normal" font="default" size="100%">9</style></issue><custom2><style face="normal" font="default" size="100%">Fort McMurray </style></custom2><custom3><style face="normal" font="default" size="100%">http://www.worldcat.org/oclc/4923193298</style></custom3><custom4><style face="normal" font="default" size="100%">OSEMB</style></custom4></record></records></xml>