1 / 15

What we learned about isotopes

What we learned about isotopes. Elizabeth Sulzman. Problem 1: Sources of nitrate in ground water. The ground water in your area exceeds the EPA standard of 10 ppm of nitrate. What nitrate sources are responsible?. 3 possible sources 2 isotopic signatures measured in sources and groundwater.

gil
Download Presentation

What we learned about isotopes

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. What we learned about isotopes Elizabeth Sulzman

  2. Problem 1: Sources of nitrate in ground water The ground water in your area exceeds the EPA standard of 10 ppm of nitrate. What nitrate sources are responsible? 3 possible sources 2 isotopic signatures measured in sources and groundwater

  3. Problem 1: Sources of nitrate in ground water

  4. Problem 1: Sources of nitrate in ground water

  5. Problem 1: Sources of nitrate in ground water

  6. Problem 2 What is the isotopic composition of soil respiration from a 40-yr-old stand dominated by Douglas-fir in the Cascade mountains of central Oregon.

  7. Problem 2 What is the isotopic composition of soil respiration from a 40-yr-old stand dominated by Douglas-fir in the Cascade mountains of central Oregon. • Differences north / south slopes? • Spatial aggregation to watershed level • Small scale Keeling plots • Soils & Foliage • North & South facing slopes • At different elevations • Watershed level Keeling plot

  8. Keeling plots Keeling (1958) Cmix= Cbg+ Csource dmixCmix= dbgCbg+ dsourceCsource dmixCmix = dbgCbg + dsource (Cmix – Cbg) dmixCmix = (dbg- dsource)Cbg + dsourceCmix dmix = (dbg- dsource)Cbg / Cmix+ dsource dmix= (slope)*(1/Cmix)+ dsource

  9. Keeling plot: dmix = (slope)*(1/Cmix) + dsource Hypothesis: North facing slope has a more negative (lighter) isotopic signature due to: Lower water stress Lower temperature

  10. Isotopic signature soil respiration

  11. Isotopic signature soil respiration Difference in isotopic signatures between north and south facing slope not large enough ?

  12. Problem 3: Contributions of C3 and C4 to ecosystem respiration Miranda et al. 1997

  13. Problem 3: Contributions of C3 and C4 to ecosystem respiration Miranda et al. 1997

  14. Problem 3: Contributions of C3 and C4 to ecosystem respiration Miranda et al. 1997 Two source mixing model: 54 +/- 7 % of ecosystem respiration stems from C3 sources.

  15. On to radioactive isotopes …

More Related