Not exact matches
Heaven is that planet 35000 light - years from earth, ten times
as big made of hydrogen and
oxygen for water, gold
as atmosphere (yes we're taking the gold) But to desist
as soul when given the chance in hell if you truly believe seems impassible for me to fathom.
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?
That means that
oxygen is produced at about the same rate
as it is removed from the
atmosphere and all is well.
In order to keep our Inglewood Organic Chicken products
as fresh
as possible, we opt to remove the
oxygen from the packaging and thereby change the «air» or «
atmosphere» surrounding the meat; without the use harmful additives.
Eventually, the
atmosphere contained enough
oxygen and high - altitude ozone to sustain air - breathing life
as we now know it.
If the process is done in a vacuum, the carbon forms on the surface
as graphene; if it is done in
oxygen, it forms GO; and if done in a humid
atmosphere followed by a vacuum, it forms
as rGO.
The moon has an
oxygen atmosphere and scientists suspect that sulfur is present,
as well.
We can thank them for
oxygen in the
atmosphere, oil in the lithosphere
as well
as dead zones in the oceans and now even a dead horse in France.
The presence of multiple chemicals such
as methane and
oxygen in an exoplanet's
atmosphere is considered an example of a biosignature, or evidence of past or present life.
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.
To identify a truly Earthlike exoplanet with the potential for life, astronomers need to confirm three essential attributes: an
atmosphere that contains life - supporting molecules such
as oxygen and water, plus a size and mass similar to Earth's.
If Proxima b proves to have an
atmosphere, Loeb and Kreidberg have also proposed using Webb to probe for the infrared signature of ozone in Proxima Centauri's glare
as a possible sign that the planet's air is filled with
oxygen — something that, on Earth, is mostly produced by life.
But if pushed to the limit, it just might be able to provide the first indication of life — a telltale molecule, such
as oxygen, in the planet's
atmosphere — on a super-Earth circling another star.
«
As in our own
atmosphere, where ultraviolet sunlight breaks molecules apart, ultraviolet starlight can break water vapour in the
atmospheres of exoplanets into hydrogen and
oxygen.»
For this reason methanol fuel cells will be used, where the combination of methanol and
oxygen produces water and carbon dioxide
as a waste product (note that the carbon footprint in this case is neutral in that the methanol will be produced by photosynthesis, removing CO2 from the
atmosphere).
The heat absorbed by water vapor and carbon dioxide is shared with all the nitrogen,
oxygen and argon, because the latter molecules are always bumping into water vapor and carbon dioxide
as they mix in the
atmosphere.
Any massive, long - term changes in their numbers could alter fish migration patterns, growth rates, and mortality,
as well
as change the amount of
oxygen and carbon dioxide in the
atmosphere.
Such one - step
oxygen formation could be happening now
as carbon dioxide increases in the region of the upper
atmosphere, where high energy vacuum ultraviolet light from the Sun hits Earth or other planets.
It is 10 times
as far from the sun
as Earth is, its thick
atmosphere is tinged with methane (the air would burst into flame if
oxygen were present), and it has about a seventh of Earth's surface gravity.
Yet until 600 million years ago, the
atmosphere contained
as little
as one - tenth the amount of
oxygen it does today.
In observations obtained at the William Herschel Telescope in the Canary Islands, the University of Warwick astronomers detected a large quantity of hydrogen and
oxygen in the
atmosphere of a white dwarf (known
as SDSS J1242 +5226).
The
oxygen levels also varied in step with water levels
as Rosetta flew around the comet, suggesting that ice and
oxygen in 67P's
atmosphere are coming from the same places in its nucleus.
As plants spread over the planet, they absorbed CO2 from the
atmosphere and released
oxygen (PDF).
It was the proliferation of such
oxygen - producing species throughout Earth's evolutionary trajectory that changed the composition of our
atmosphere — adding much more O2 — which was
as important for the development of ancient multi-cellular life
as it is for us today.
At 5260 meters, close to the level of the Mount Everest Base Camp in Nepal, the
atmosphere holds 53 %
as much
oxygen as the air at sea level, making it harder to breathe — and to exercise.
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.
If there were too much UV light, no water could survive on the surface because the water molecules would break up and escape through the top of the
atmosphere as hydrogen and
oxygen gas.
As oxygen increased in Earth's
atmosphere and organisms became more complex, different forms of metabolism evolved, from plants» photosynthesis to the lesser - known chemolithotrophy.
In fact, the completely unplanned «experiment» had left the crew gasping for breath
as the
oxygen concentration gradually fell from 21 per cent to less than 15 per cent, making the
atmosphere as thin
as at an altitude of 4000 metres.
When these worms began to mix up the ocean floor's sediments (a process known
as bioturbation), their activity came to significantly influence the ocean's phosphorus cycle and
as a result, the amount of
oxygen in Earth's
atmosphere.
«It looks
as if there's a significant time interval between the appearance of
oxygen - producing organisms and the actual oxygenation of the
atmosphere.»
«The resulting six-fold increase in
oxygen would have significantly influenced biogeochemical cycling of [oxidation] sensitive elements such
as [iron] and [sulfur] and ultimately increased the
oxygen concentration of the
atmosphere,» the team writes in a paper published online today by the journal Science.
What makes the WEAV potentially appealing
as a way to power spacecraft is that it relies on electricity (from a battery or some other power source) rather than combustion — a process that requires
oxygen, which is in short supply outside Earth's
atmosphere, Colozza says.
If there are a lot of gases that consume
oxygen, such
as methane or hydrogen, then any
oxygen or ozone produced will be destroyed in the
atmosphere.
In an
oxygen - free
atmosphere,
as prevailed on early Earth, uranium stayed immobile in rocks
as tetravalent uranium (IV).
The dense carbon dioxide
atmosphere often invoked to explain the warm era should have left its mark on the planet's geology,
as carbon and
oxygen sequestered in carbonate minerals.
The osmium isotope evidence found in black shales correlates with higher continental weathering
as a result of
oxygen in the
atmosphere.
These whiffs of
oxygen likely happened in the following 100 million years, changing the levels of
oxygen in Earth's
atmosphere until enough accumulated to create a permanently oxygenated
atmosphere around 2.4 billion years ago — a transition widely known
as the Great Oxidation Event.
As the particles journeyed around Earth, the lighter hydrogen particles were lost in collisions with the
atmosphere, leaving an
oxygen - rich plasma.
Its combination with
oxygen in the
atmosphere produces energy and water
as its sole by - product, making it one of the main candidates to substitute fossil fuels
as a source of energy for the transport sector.
The hydroxyl radical consisting of one hydrogen and one
oxygen atom, is one of the most common free radicals in the air and is therefore often referred
as the detergent of the
atmosphere.
MAVEN focuses on hydrogen and
oxygen as ways to trace water and carbon dioxide, and neutral argon
as a way to measure the sheer volume of
atmosphere loss.
Consequently, massive amounts of reactive gases such
as oxygen, hydrogen, and methane are continually being added to Earth's now «anomalous»
atmosphere faster than they would otherwise be removed by inorganic chemical processes.
Although the evidence was subsequently contested, some single - celled microbial life lacking a nucleus that segregates their internal DNA or RNA («prokaryotes») from the surrounding cytoplasm may have flourished in darkness within cracks in Earth's seafloor crust and around deep, warm or boiling hot ocean springs (hydrothermal or volcanic vents, such
as at Lost City or at black smokers) without a need for light or free
oxygen in the oceans or
atmosphere.
© Wim van Egmond (Photo from Ciliates, used with permission)
As the level of oxygen in the atmosphere rose, however, most surface lifeforms on Earth became oxygen breathing, such as these two single - celled protoctists (Euplotes, left, and Stylonychia) which move with hairlike cili
As the level of
oxygen in the
atmosphere rose, however, most surface lifeforms on Earth became
oxygen breathing, such
as these two single - celled protoctists (Euplotes, left, and Stylonychia) which move with hairlike cili
as these two single - celled protoctists (Euplotes, left, and Stylonychia) which move with hairlike cilia.
«When ozone reacts with carbon dioxide in the
atmosphere, it transfers its isotopic weirdness to the new molecule,» said Shaheen, who investigated this process of
oxygen isotope exchange
as a graduate student at the University of Heidelberg in Germany.
As less methane was available to to remove
oxygen from the
atmosphere, however, the result was a build up of
oxygen over time during the subsequent «Great Oxygenation Event» (or «Great Oxidation Event») between Years 2.2 and 2.3 billion (Devin Powell, New Scientist, January 12, 2009; 2007 NASA press release; and Anbar el al, 2007).
With little
oxygen available to convert that hydrogen into water, hydrogen gas probably accumulated in the
atmosphere and oceans in concentrations
as high
as hundreds to thousands of parts per million.
Today, a UCLA - led team of scientists reports that it has discovered the existence of a white dwarf star whose
atmosphere is rich in carbon and nitrogen,
as well
as in
oxygen and hydrogen, the components of water.
I've also been wondering, and will now do a little investigating of the issue, whether or not the Level of
Oxygen in our
Atmosphere has been declining measurably;
as it seems to me to be of an issue of Great Concern, now that we've cut down so much our Rainforests and are in danger of destroying the ability of Chloroplankton to form the Carbonate shells necessary to their existence, through Oceanic Acidulation.