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Isotopic composition of Antarctic Dry Valley nitrate: Implications for NO y sources and cycling in Antarctica
Ist Teil von
Geophysical research letters, 2005-07, Vol.32 (13)
Erscheinungsjahr
2005
Quelle
Wiley Online Library Journals Frontfile Complete
Beschreibungen/Notizen
Nitrates minerals from the Dry Valleys of Antarctica have been analyzed for their oxygen and nitrogen isotopic compositions. The
15
N was depleted with δ
15
N values ranging from −9.5 to −26.2‰, whereas the
17
O and
18
O isotopes were highly enriched (with excess
17
O) with δ
18
O values spanning 62–76‰ and Δ
17
O values from 28.9 to 32.7‰. These are the largest
17
O enrichments observed in any known mineral. The oxygen isotopes indicate that nitrate is from a combination of tropospheric transport of photochemically produced HNO
3
and HNO
3
formed in the stratosphere.