This panorama was captured in 2005 as the Huygens probe plummeted through the thick
nitrogen atmosphere of Titan, Saturn's largest moon.
Not exact matches
And it has a very helpful
atmosphere which, in the case
of Mars, being primarily CO2 with some
nitrogen, and argon, and few other trace elements, means that we can grow plants on Mars just by compressing the
atmosphere.
It possesses a dense
nitrogen - rich
atmosphere with a surface pressure one and a half times that
of Earth's.
And what about the entire ecological system
of things, that works in harmony with us as humans for life to exist, from our
atmosphere at 78 %
nitrogen, 21 % oxygen down to the magnetosphere that comes from within the core
of the earth and protects us from the sun's damaging electrically charged particles?
Automobiles, power plants and industries release oxides
of nitrogen into the
atmosphere.
They now constitute quite a substantial proportion
of the
nitrogen that goes from the
atmosphere into the soils and waters
of the Earth.
Carbon - 13, one tracer used to probe a variety
of geochemical processes, is typically formed when high - energy cosmic rays enter the
atmosphere and strike the most abundant form
of nitrogen there —
nitrogen - 14 atoms.
When the Cornell researchers suggested the presence
of azotosomes on Titan, carbon, hydrogen and
nitrogen had already been detected in abundance in the moon's
atmosphere.
Saturn's moon Titan is the only moon in the solar system that has an
atmosphere as thick as Earth's, consisting
of more than 98 percent
nitrogen, roughly 1.4 percent
of methane, and smaller amounts
of other gases.
When burned, it produces nothing more than water vapour and
nitrogen, which makes up 78 per cent
of Earth's
atmosphere.
The
atmosphere consists primarily
of 78 percent
nitrogen, 21 percent oxygen, a highly variable smattering
of water vapor, and trace amounts
of argon, carbon dioxide, and other gases.
Previous modelling attempts to resolve the paradox by loading the early
atmosphere with greenhouse gases assumed that it has always had the same amount
of nitrogen.
«Titan's
atmosphere is made up mainly
of nitrogen and methane, with 50 % higher pressure at its surface than on Earth,» said Andrew Coates (UCL Mullard Space Science Laboratory), who led the study.
In a paper released for discussion in the journal Atmospheric Chemistry and Physics, Crutzen calculated that 3 to 5 percent
of the
nitrogen in the fertilizers used to raise crops for biofuels could end up in the
atmosphere as nitrous oxide, a potent, long - lived greenhouse gas.
The Methods: Photochemical modeling by a Caltech team indicates that ethane, a hydrocarbon detected on Titan by both
of the Voyager spacecraft and the European Infrared Space Observatory, is created when solar ultraviolet light breaks down methane, a minor component
of Titan's
nitrogen - rich
atmosphere, into a stew
of organic molecules that form a dense orange - brown smog.
Researchers believe that the cloud top reacts by driving swarms
of electrons into the upper
atmosphere; along the way, the electrons crash into
nitrogen molecules between 50 and 90 kilometers high and make them glow a fiery red.
We have no real idea what the
atmosphere of Proxima b is made
of, but for the sake
of argument the researchers tried out an
atmosphere like Earth's as well as a simpler one — mostly
nitrogen with a dash
of carbon dioxide.
They become caught in powerful magnetic fields and are channeled into the upper
atmosphere, where their interactions with gas particles, such as oxygen or
nitrogen, set off spectacular bursts
of light.
Eventually, they crash into the first wisps
of the
atmosphere, molecules
of nitrogen, oxygen, and other gases 100 to 300 kilometers high.
Titan, the largest
of Saturn's more than 60 moons, is the other body in our solar system with a
nitrogen - rich
atmosphere that resembles ours.
«It has been established that the nitrates, which is a form
of nitrogen, comes from fixation
of atmospheric diatomic
nitrogen in the
atmosphere during meteorite impacts, which is consistent with the data that we obtained through the SAM analyses, so this may be the main source
of fixed
nitrogen on Mars,» says Javier Martín - Torres.
A team
of scientists using a state -
of - the - art UCLA instrument reports the discovery
of a planetary - scale «tug -
of - war»
of life, deep Earth and the upper
atmosphere that is expressed in atmospheric
nitrogen.
Two
nitrogen atoms combine to form N2 molecules that stay in the
atmosphere for millions
of years.
Scientists now believe the primeval
atmosphere contained an inert mix
of carbon dioxide and
nitrogen — a change that made a world
of difference.
Scientists have discovered a planetary - scale tug -
of - war between life, deep Earth and the upper
atmosphere that is expressed in atmospheric
nitrogen.
The lack
of legions
of bacteria to recycle
nitrogen back into the Martian
atmosphere may explain why the red planet has no gaseous
nitrogen today, he says.
In parallel work, Mikhail Eremets
of the Max Planck Institute for Chemistry in Germany found a novel bond between atoms
of nitrogen, the most common element in Earth's
atmosphere.
Earth's
atmosphere differs from the
atmospheres of most other rocky planets and moons in our solar system in that it is rich in
nitrogen gas, or N2; Earth's
atmosphere is 78 percent
nitrogen gas.
On Titan the photochemistry starts at the top
of the
atmosphere, about 1000 kilometres up, where energetic ultraviolet photons from the sun and cosmic rays trigger reactions among methane and
nitrogen molecules.
However, the U.S. Environmental Protection Agency has increasingly recognized
nitrogen fertilizer use as a significant source
of NOx gases to the
atmosphere.
Its availability in the biosphere is limited by the fact that the global occurrence
of nitrogen is confined largely to the gas N2 in the
atmosphere.
«Those electrons are driven into the upper
atmosphere, collide with
nitrogen and oxygen atoms and molecules, and then create a spray
of secondary and tertiary radiation, likely in the form
of gamma rays,» Tobiska says.
Previous modelling efforts to resolve the paradox by loading the early
atmosphere with greenhouse gases assumed that it has always had the same concentration
of nitrogen.
Only a few bacteria and simple algae have the cellular equipment needed to «fix» the
nitrogen of the
atmosphere into ammonia.
The amount
of nitrous oxide in the
atmosphere has quickly increased as well, with about a third
of the total added by human activity — much
of that emitted by
nitrogen - based fertilizers, and half
of that from just three nations: China, the Soviet Union, and the United States.
The great benefit is that legumes contribute to cropping systems; they can help take
nitrogen out
of the
atmosphere and make it available in the soil.
The team thinks one reason their technique is so efficient is that a chemical reaction between the hydrogen plasma and air molecules in the chamber's
atmosphere generates cyano radicals — carbon -
nitrogen molecules that have been stripped
of their electrons.
By the way, this effect is most prevalent when the particles that do the scattering are smaller than the wavelength
of light, as is the case for the
nitrogen and oxygen molecules in the
atmosphere.
Carbon monoxide has a vapour pressure intermediate between that
of nitrogen and methane, so Owen and his colleagues believe that carbon monoxide is the second most abundant gas in Pluto's
atmosphere.
Even though
nitrogen gas makes up approximately 80 percent
of Earth's
atmosphere, the plant can only access it in a bound — or «fixed» — form.
To do this, the team first pumped all the oxygen out
of the chamber, and instead filled it with inert
nitrogen or carbon dioxide — the most common components
of the Martian
atmosphere.
Molecular
nitrogen (N2) dominates the
atmosphere (at altitudes
of less than 1800 kilometers or so), whereas methane (CH4), acetylene (C2H2), ethylene (C2H4), and ethane (C2H6) are abundant minor species and likely feed the production
of an extensive haze that encompasses Pluto.
Like Earth, Titan has an
atmosphere composed primarily
of molecular
nitrogen, and surface pressures are roughly comparable.
These, in turn, triggered reactions in the upper
atmosphere in which oxygen and
nitrogen molecules released photons
of light.
The haze results from chemical reactions in the upper
atmosphere, where ultraviolet radiation from the sun ionizes
nitrogen and methane, which react to form tiny hydrocarbon particles tens
of nanometers in diameter.
«We found that all
of these effects, which are the major ones from cratering, do not seem to supply enough
nitrogen to supply the escaping
atmosphere over time,» continued Singer.
Among biogenic volatile organic molecules is a class
of compounds called monoterpenes, which react with ozone, hydroxyl radicals,
nitrogen oxides, and other gases in the
atmosphere.
For example, they revealed that the west side
of Pluto's «heart» is rich in carbon - monoxide ice, unlike the rest
of the dwarf planet, and they announced that the probe had detected Pluto's thin,
nitrogen - dominated
atmosphere out to a distance
of 1,000 miles (1,600 km) from the surface.
«More
nitrogen has to come from somewhere to resupply both the
nitrogen ice that is moving around Pluto's surface in seasonal cycles, and the
nitrogen that is escaping off the top
of the
atmosphere as the result
of heating by ultraviolet light from the Sun,» said Singer.
Their analysis, which could discern human - derived
nitrogen from natural
nitrogen fixation, revealed that the oceanic nitrate concentration increased significantly over the last 30 years in surface waters
of the North Pacific due largely to the enhanced deposition
of nitrogen from the
atmosphere.