This is the first
time hydrogen isotopes have been measured in eucrite meteorites.
Not exact matches
The composition of these ice cores, especially the presence of
hydrogen and oxygen
isotopes, provides a picture of the climate at the
time.
The particles carry up to 30
times as much of the
hydrogen isotope deuterium as typical terrestrial materials.
By looking at the chemistry of rocks deposited during that
time period, specifically coupled carbon and sulfur
isotope data, a research team led by University of California, Riverside biogeochemists reports that oxygen - free and
hydrogen sulfide - rich waters extended across roughly five percent of the global ocean during this major climatic perturbation — far more than the modern ocean's 0.1 percent but much less than previous estimates for this event.
They also used satellite precipitation data to «backsolve» the brine's origins using sodium concentrations, oxygen and
hydrogen isotopes, as the isotopic composition of water reflects the condensation temperature and precipitation rate over
time.
Chemically, muonium behaves like a
hydrogen isotope, but it's nine
times as light as
hydrogen.
They measure the
hydrogen and oxygen
isotopes to infer air temperatures at the
time the snow fell, and the dust particles give a nice indication of the dusty periods (much of the dust was kicked up far away, in the Gobi Desert, rather than from sources closer to Greenland).