Based on measurements of Jupiter and the solar wind, which are thought to preserve
the hydrogen isotopic ratio of the protosolar nebula, scientists think nebular water had an extremely light hydrogen isotopic signature — much closer to what the Baffin Island lavas suggest about the deep mantle's water.
Not exact matches
The discovery's telltale sign is found in the
ratio of an
isotopic form of
hydrogen, called deuterium, to standard
hydrogen.
Because the
isotopic ratios of carbon and
hydrogen display geographic variation, the composition of a feather can reveal where the bird was when the feather grew.
Within these archives, scientists can measure the
isotopic ratios of oxygen and
hydrogen to deduce changes over time in the
isotopic composition of environmental waters, such as precipitation, seawater, and groundwater.