Molecular hydrogen (H-2), its isotopic signature (deuterium/hydrogen, delta D), carbon monoxide (CO), and other compounds were studied in the exhaust of a passenger car engine fuelled with gasoline or methane and run under variable air-fuel ratios and operating modes. H-2 and CO concentrations were largely reduced downstream of the three-way catalytic converter (TWC) compared to levels upstream, and showed a strong dependence on the air-fuel ratio ( expressed as lambda, lambda). The isotopic composition of H-2 ranged from delta D=-140 parts per thousand to delta D =-195 parts per thousand upstream of the TWC but these values decreased to -270% to -370 parts per thousand after passing through the TWC. Post-TWC delta D values for the fuel-rich range showed a strong dependence on TWC temperature with more negative delta D for lower temperatures. These effects are attributed to a rapid temperature-dependent H-D isotope equilibration between H-2 and water (H2O). In addition, post TWC delta D in H-2 showed a strong dependence on the fraction of removed H-2, suggesting isotopic enrichment during catalytic removal of H-2 with enrichment factors (epsilon) ranging from -39.8 parts per thousand to -15.5 parts per thousand depending on the operating mode. Our results imply that there may be considerable variability in real-world delta D emissions from vehicle exhaust, which may mainly depend on TWC technology and exhaust temperature regime. This variability is suggestive of a delta D from traffic that varies over time, by season, and by geographical location. An earlier-derived integrated pure (end-member) delta D from anthropogenic activities of -270% (Rahn et al., 2002) can be explained as a mixture of mainly vehicle emissions from cold starts and fully functional TWCs, but enhanced delta D values by >50 parts per thousand are likely for regions where TWC technology is not fully implemented. Our results also suggest that a full hydrogen isotope analysis on fuel and exhaust gas may greatly aid at understanding process-level reactions in the exhaust gas, in particular in the TWC.
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School of Science, Beijing University of Civil Engineering and ArchitectureSchool of Science, Beijing University of Civil Engineering and Architecture
Dong Gao
Hui Ma
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Department of Mathematical Sciences, Tsinghua UniversitySchool of Science, Beijing University of Civil Engineering and Architecture
Hui Ma
Zeke Yao
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Department of Mathematical Sciences, Tsinghua UniversitySchool of Science, Beijing University of Civil Engineering and Architecture
机构:
Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
NOAA, Global Monitoring Lab, Boulder, CO USANOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA
Petron, Gabrielle
Crotwell, Andrew M.
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Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
NOAA, Global Monitoring Lab, Boulder, CO USANOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA
Crotwell, Andrew M.
Bertagni, Matteo B.
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Princeton Univ, High Meadow Environm Inst, Princeton, NJ USA
Princeton Univ, Dept Civil & Environm Engn, Princeton, NJ USANOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA
机构:
Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USAUniv Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA
Patterson, John D.
Aydin, Murat
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Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USAUniv Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA
Aydin, Murat
Crotwell, Andrew M.
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NOAA, Global Monitoring Lab, Boulder, CO 80305 USA
Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USAUniv Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA
Crotwell, Andrew M.
Petron, Gabrielle
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NOAA, Global Monitoring Lab, Boulder, CO 80305 USA
Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USAUniv Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA
Petron, Gabrielle
Severinghaus, Jeffrey P.
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Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92037 USAUniv Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA