Abstract
Tropospheric ozone is formed in the atmosphere by a series of reactions that involve volatile organic compounds (VOCs) and nitrogen oxides (NOx). NOx emissions are composed primarily of NO and NO2, but hundreds of VOCs are being emitted. Generally, VOCs promote ozone formation; however, the rate and extent of ozone produced by VOCs vary considerably.
| Original language | American English |
|---|---|
| Publisher | National Laboratory of the Rockies (NLR) |
| Number of pages | 164 |
| DOIs | |
| State | Published - 1996 |
Bibliographical note
Work performed by Carnegie Mellon University, Pittsburgh, Pennsylvania; University of Connecticut, Storrs, Connecticut; University of Colorado, Boulder, Colorado; and Fraunhofer Institute for Atmospheric Environmental Research, Garmish-Partenkirchen, GermanyNLR Publication Number
- NREL/TP-425-7636
Keywords
- nitrogen oxides
- tropospheric ozone
- volatile organic compounds
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