Isotopic composition of Antarctic Dry Valley nitrate: Implications for NOy sources and cycling in Antarctica

Biology

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

10

Biogeosciences: Biosphere/Atmosphere Interactions (0315), Biogeosciences: Evolutionary Geobiology, Biogeosciences: Nitrogen Cycling, Biogeosciences: Soils/Pedology (1865), Cryosphere: Biogeochemistry (0412, 0414, 1615, 4805, 4912)

Scientific paper

Nitrates minerals from the Dry Valleys of Antarctica have been analyzed for their oxygen and nitrogen isotopic compositions. The 15N was depleted with δ15N values ranging from -9.5 to -26.2‰, whereas the 17O and 18O isotopes were highly enriched (with excess 17O) with δ18O values spanning 62-76‰ and Δ17O values from 28.9 to 32.7‰. These are the largest 17O enrichments observed in any known mineral. The oxygen isotopes indicate that nitrate is from a combination of tropospheric transport of photochemically produced HNO3 and HNO3 formed in the stratosphere.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Isotopic composition of Antarctic Dry Valley nitrate: Implications for NOy sources and cycling in Antarctica does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Isotopic composition of Antarctic Dry Valley nitrate: Implications for NOy sources and cycling in Antarctica, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Isotopic composition of Antarctic Dry Valley nitrate: Implications for NOy sources and cycling in Antarctica will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1249632

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.