Correção da atividade do dia 28/04/20 9º "A" e "B"
Escola Estadual Professor Marcilon Dorneles
Disciplina: Inglês
Professor: Vinícius
Data: 05/05/20
Série: 9º
Correção da atividade do dia 28/04/20
(encontrar e destacar as linking words presentes na matéria da revista
ScienceDaily). As linking words estão destacadas de amarelo.
New geochemical tool reveals
origin of Earth's nitrogen
Nitrogen is the most abundant gas in the atmosphere, and is the primary
component of the air we breathe. Nitrogen is also found in rocks, including those tucked deep
within the planet's interior. Until now, it was difficult to distinguish
between nitrogen sources coming from air and those coming from inside the Earth's mantle
when measuring gases from volcanoes.
"We found that air contamination was masking the pristine 'source
signature' of many volcanic gas samples," says WHOI geochemist Peter
Barry, a coauthor of the study.
Without that distinction, scientists weren't able to answer basic
questions like: Is nitrogen left over from Earth's formation or was it
delivered to the planet later on? How is nitrogen from the atmosphere related
to nitrogen coming out of volcanoes?
Barry and
lead author Jabrane Labidi of UCLA, now a researcher at Institut de Physique du
Globe de Paris, worked in partnership with international geochemists to analyze
volcanic gas samples from around the globe -- including gases from Iceland and Yellowstone National
Park -- using a new method of analyzing "clumped" nitrogen isotopes.
This method provided a unique way to identify molecules of nitrogen that come
from air, which allowed the researchers to see the true gas compositions deep
within Earth's mantle. This ultimately revealed evidence that nitrogen in the
mantle has most likely been there since our planet initially formed.
"Once air contamination is accounted for, we gained new and valuable insights
into the origin of nitrogen and
the evolution of our planet," Barry says.
While this new method helps scientists understand
the origins of volatile elements on Earth, it may prove useful as a way of
monitoring the activity of volcanoes, too. This is because the composition of gases bellowing from
volcanic centers change prior to eruptions. It could be that the mix of mantle
and air nitrogen could one day be used as a signal of eruptions.
This study was supported by the Deep Carbon Observatory and the Alfred
P. Sloan Foundation. The research team also included colleagues David Bekaert and Mark Kurz from WHOI,
scientists from several other U.S.-based universities, and from France, Canada, Italy, the United
Kingdom and
Iceland.
 
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