1 / 26

Anthropogenic C Emissions: Fossil Fuel

1850. 1870. 1890. 1910. 1930. 1950. 1970. 1990. 2010. Anthropogenic C Emissions: Fossil Fuel. 2006 Fossil Fuel: 8.4 Pg C. [2006-Total Anthrop. Emissions:8.4+1.5 = 9.9 Pg]. 1990 - 1999: 1.3% y -1 2000 - 2006: 3.3% y -1. Raupach et al. 2007, PNAS; Canadell et al 2007, PNAS.

yuri
Download Presentation

Anthropogenic C Emissions: Fossil Fuel

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. 1850 1870 1890 1910 1930 1950 1970 1990 2010 Anthropogenic C Emissions: Fossil Fuel 2006 Fossil Fuel: 8.4 Pg C [2006-Total Anthrop. Emissions:8.4+1.5 = 9.9 Pg] • 1990 - 1999: 1.3% y-1 • 2000 - 2006: 3.3% y-1 Raupach et al. 2007, PNAS; Canadell et al 2007, PNAS

  2. Friedlingstein et al. 2010

  3. Nitrogen Cycle Units=teragrams yr-1

  4. Nitrogen Cycle Largest pool of nitrogen=atmospheric N2 vegetation = 4,000 Tg soils = 100,000 Tg atmosphere = 3,900,000,000 Tg Biological N fixation has historically been the major input of N into ecosystems Oceans = 100 Tg/yr Land = 140 Tg/yr Denitrification is major output of N back to the atmosphere Oceans = 110 Tg/yr Land = 200 Tg/yr Balance?

  5. Nitrogen Cycle N is most commonly limiting element in terrestrial ecosystems, and in some aquatic ecosystems (estuaries, coastal seas) Amount that cycles within terrestrial ecosystems is 9 times the land N fixation rate Amount that cycles within ocean ecosystems is 80 times the ocean N fixation rate

  6. Changing Nitrogen Cycle Humans have doubled the N fixation rates over natural levels Haber-Bosch 3CH4 + 6H2O --> 3CO2 + 12H2 4N2+12H2 --> 8NH3 (high T,pressure, Fe) Bread AND Bombs

  7. Changing Nitrogen Cycle About half of human additions come from fertilizer production About a quarter from increasing amount of biological N fixation The other quarter inadvertently from fossil fuel combustion

  8. Changing Nitrogen Cycle Increased fertilizer inputs can: volatilize from fields, pastures (NH3) increase nitrification (NO, N2O,NO3- leaching) increased denitrification (NO, N2O, N2)

  9. Townsend et al. 2003

  10. Other Changes in the Nitrogen Cycle • Mobilization of N from long term storage • incomplete fossil fuel combustion releases NOx • biomass burning releases NH3, NOx • land clearing, conversion, drainage, or permafrost thaw can increase leaks in the N cycle

  11. GWP=200 Changing N Cycle: Effects on Atmosphere N2O (nitrous oxide) N2O (Nitrous oxide) Reacts with excited O in stratosphere to form NO and catalyze destruction of O3 IPCC 2007

  12. Changing N Cycle: Effects on Atmosphere NOx (Nitric oxides) high concentrations contribute to O3 formation in troposphere stratospheric ozone = good (but, ozone hole = bad) tropospheric ozone = bad (smog, greenhouse gas)

  13. Trophospheric ozone formation and destruction Net reaction at high [NOx]: CO + 2O2 + hv --> CO2 + O3 Net reaction at low [NOx]: CO + O3 + hv --> CO2 + O2

  14. Trophospheric ozone OH + CO + O2 --> CO2 + HO2 HO2 + NO --> NO2 + OH NO2 + hv --> NO+ O O2 + O + M --> O3 + M net: CO + 2O2 + hv --> CO2 + O3

  15. Changing N Cycle: Effects on Atmosphere NOx contributes to nitric acid formation in troposphere HO2 + NO --> NO2 + OH NO2 + H2O --> H+ + HNO3- N transfer to “downwind” terrestrial and aquatic ecosystems

  16. Acid deposition and atmosphere pH • Wetfall: deposition of nutrients by precipitation (easy to • measure with exception of fog) • Acid rain = pH  5.6, bad for ecosystems! • NO3-  HNO3 • SO42-  H2SO4 • NH3 and Ca2+ important for neutralizing atm.’s acidity • Globally, 22% of acidity is neutralized by NH3 • Regionally: • Southern hemisphere: NH3 most important • NE US and Europe: SO42- drives acidity • Western US: acid ions interact with CaCO3

  17. Dry deposition • Dryfall: gravitational sedimentation of particles without rain • NH4+, NO3- • Dust • NO2 and NH3 gases • Acid vapors • Controlled by wind and canopy structure • Hard to measure and poorly constrained

  18. Effects of N Transfers on Ecosystems Nitrogen deposition downwind from NH3 and NOx sources unpolluted areas = 1 kg N/ha/yr Northeastern US = 10-20 kg N/ha/yr some parts of Europe = 50-100 kg N/ha/yr How much N is this?

  19. National Atmospheric Deposition Program

  20. NADP animations • http://nadp.sws.uiuc.edu/data/animaps.aspx

  21. (1 g N m-2 yr-1 = 10 kg ha-1 yr-1) Galloway et al. 2008

  22. Next Monday: Ecosystem-level effects of N deposition Fertilization Saturation Biogeochemical feedbacks

  23. Fig. 1. N contained in internationally traded (A) fertilizer (31 Tg N), (B) grain (12 Tg N), and (C) meat (0.8 Tg N). J N Galloway et al. Science 2008;320:889-892 Published by AAAS

  24. Fig. 3. Conceptual model of where interventions in the N cycle can be used to decrease the amount of Nr created or the amount of Nr lost to the environment. J N Galloway et al. Science 2008;320:889-892 Published by AAAS

More Related