Mass-Independent Fractionation of Oxygen Isotopes in the Atmosphere

2021 ◽  
Vol 86 (1) ◽  
pp. 197-216
Author(s):  
Marah Brinjikji ◽  
James R. Lyons
Keyword(s):  
Oxygen Isotopes ◽  
Mass Independent Fractionation

scholarly journals Mass-independent fractionation of oxygen isotopes during thermal decomposition of carbonates

2002 ◽  
Vol 99 (17) ◽  
pp. 10988-10993 ◽  
Author(s):  
M. F. Miller ◽  
I. A. Franchi ◽  
M. H. Thiemens ◽  
T. L. Jackson ◽  
A. Brack ◽  
...  
Keyword(s):  
Thermal Decomposition ◽  
Oxygen Isotopes ◽  
Mass Independent Fractionation

Mass-independent fractionation of oxygen isotopes during H2O2 formation by gas-phase discharge from water vapour

2016 ◽  
Vol 193 ◽  
pp. 54-65 ◽  
Author(s):  
Tatiana A. Velivetskaya ◽  
Alexander V. Ignatiev ◽  
Sergey Y. Budnitskiy ◽  
Victoria V. Yakovenko ◽  
Sergey V. Vysotskiy
Keyword(s):  
Gas Phase ◽  
Water Vapour ◽  
Oxygen Isotopes ◽  
Mass Independent Fractionation ◽  
H2o2 Formation

Changes of Ionic and Oxygen Isotopic Composition of the Snowpack at the Glacier Austre Okstindbreen, Norway, 1995

1998 ◽  
Vol 29 (1) ◽  
pp. 1-20 ◽  
Author(s):  
Peter Raben ◽  
Wilfred H. Theakstone
Keyword(s):  
Isotopic Composition ◽  
Sea Level ◽  
Oxygen Isotopes ◽  
Oxygen Isotopic Composition ◽  
Isotopic Ratios ◽  
Vertical Variations ◽  
Oxygen Isotopic ◽  
The Difference ◽  
Liquid Precipitation ◽  
Different Altitudes

Marked vertical variations of ions and oxygen isotopes were present in the snowpack at the glacier Austre Okstindbreen during the pre-melting phase in 1995 at sites between 825 m and 1,470 m above sea level. As the first meltwater percolated from the top of the pack, ions were moved to a greater depth, but the isotopic composition remained relatively unchanged. Ions continued to move downwards through the pack during the melting phase, even when there was little surface melting and no addition of liquid precipitation. The at-a-depth correlation between ionic concentrations and isotopic ratios, strong in the pre-melting phase, weakened during melting. In August, concentrations of Na+ and Mg2+ ions in the residual pack were low and vertical variations were slight; 18O enrichment had occurred. The difference of the time at which melting of the snowpack starts at different altitudes influences the input of ions and isotopes to the underlying glacier.

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