Kourosh Kalantar - Zadeh, an engineer at the Royal Melbourne Institute of Technology in Australia, and his colleagues built plastic capsules about 2.5 centimeters long — about as long as a Jolly Rancher hard candy — that sniff out carbon dioxide, hydrogen and
oxygen gas molecules in the gut.
Not exact matches
Really easy actually, in an infinate universe, the speed of
gases, for example hydrogen and
oxygen molecules, continues to build there is no «matter» to slow them down.
Like hydrogen,
oxygen, and iodine, nitrogen normally exists as two - atom
molecules in the form of a
gas at room temperature.
Eventually, they crash into the first wisps of the atmosphere,
molecules of nitrogen,
oxygen, and other
gases 100 to 300 kilometers high.
Solar particles (the electric current) stream down Earth's magnetic field lines (the tube) and collide with
molecules of nitrogen and
oxygen (the
gas), exciting them until they glow in various colors.
They are not like the
oxygen molecules or the nitrogen
molecules in the atmosphere, which do not absorb infrared, but the greenhouse
gases do.
By separating out the starlight from the planet light, we can identify
molecules in the planet's atmosphere and look for
gases produced by life, like
oxygen, ozone and ammonia.
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.
The
gas is produced by splitting up
oxygen molecules with an electric discharge.
Ideally, you'd also measure other
gases like carbon dioxide and carbon monoxide [a
molecule with one carbon atom and one
oxygen atom].
The answer is that before the sunlight reaches Earth, it first has to travel through our atmosphere, which is a layer of
gas made up of tiny
molecules of mostly nitrogen and
oxygen that surrounds our planet.
With too much UV light, no water could persist on the surface because its
molecules would break down into hydrogen and
oxygen gas and escape through the atmosphere.
The reaction combines the hydroxyl
molecule (OH, produced by reaction of
oxygen and water) and carbon monoxide (CO, a byproduct of incomplete fossil fuel combustion) to form hydrogen (H) and carbon dioxide (CO2, a «greenhouse
gas» contributing to global warming), as well as heat.
At the photoanode side, water
molecules are split into
oxygen gas (O2), electrons and hydrogen protons through oxidation in the presence of sunlight and the thin film coating the team recently developed.
Presumably, the strong stellar wind emitted by giant stars eventually blows the titanium oxide out of the star's outer regions (along with hydrogen and helium
gases and dust made of elements and
molecules like carbon) into interstellar space, until vigorous convection brings out more titanium and
oxygen that are created from nuclear processes deeper in the star.
Earth's much thicker layer of low - level ozone, however, has a much larger contribution from the build - up of molecular
oxygen beginning some 2.4 billion years ago from photosynthetic microbes excreting
oxygen as a waste
gas, which now along with plant life is constantly replenishing Earth's two - atom as well as three - stom ozone
oxygen molecules.
The results quantify the nature of
gas molecules containing carbon, hydrogen, and sulfur in the earliest atmosphere, but they shed no light on the much later rise of free
oxygen in the air.
Composed of carbon, hydrogen, nitrogen and
oxygen atoms (forming the CH3NCO
molecule) a tragic methyl isocyanate
gas leak caused thousands of deaths and injuries during what is considered to be the deadliest industrial accident in history — the Indian 1984 Bhopal disaster.
Molecules with three or more atoms, like CO2 and other greenhouse gases, do this much better than molecules with just two, like oxygen (O2) and nitro
Molecules with three or more atoms, like CO2 and other greenhouse
gases, do this much better than
molecules with just two, like oxygen (O2) and nitro
molecules with just two, like
oxygen (O2) and nitrogen (N2).
carbon monoxide A toxic
gas whose
molecules include one carbon atom and one
oxygen atom.
He suggests that the flakes could also be added as a filler into plastic drinks bottles — where their added strength reduces the amount of plastic needed, and their ability to block the passage of
gas molecules such as
oxygen and carbon dioxide maintains the drink's shelf life.
This really is more appropriate in the chemistry community, but just a really short answer, the spark causes the
gas molecules to react with
oxygen thus releasing the chemical energy stored in the
gas molecule.
Which references... «Absolute Intensities of the Discrete and Continuous Absorption Bands of
Oxygen Gas at 1.26 and 1.065 Micron» (1965, Badger et al.) https://authors.library.caltech.edu/10448/1/BADjcp65.pdf «Molecular oxygen (O2) has absorption bands throughout the spectrum from the infrared (IR) to the ultraviolet... The oxygen absorptions at 1.06 and 1.27 um may be attributed to two types of absorption (1) from individual O2 molecules and (2) from O2 molecules that are involved in some interaction through collisions or transient pairings with other molecules (in this case either O2 or N2).&
Oxygen Gas at 1.26 and 1.065 Micron» (1965, Badger et al.) https://authors.library.caltech.edu/10448/1/BADjcp65.pdf «Molecular
oxygen (O2) has absorption bands throughout the spectrum from the infrared (IR) to the ultraviolet... The oxygen absorptions at 1.06 and 1.27 um may be attributed to two types of absorption (1) from individual O2 molecules and (2) from O2 molecules that are involved in some interaction through collisions or transient pairings with other molecules (in this case either O2 or N2).&
oxygen (O2) has absorption bands throughout the spectrum from the infrared (IR) to the ultraviolet... The
oxygen absorptions at 1.06 and 1.27 um may be attributed to two types of absorption (1) from individual O2 molecules and (2) from O2 molecules that are involved in some interaction through collisions or transient pairings with other molecules (in this case either O2 or N2).&
oxygen absorptions at 1.06 and 1.27 um may be attributed to two types of absorption (1) from individual O2
molecules and (2) from O2
molecules that are involved in some interaction through collisions or transient pairings with other
molecules (in this case either O2 or N2).»
But greenhouse
gases like CO2 then emit a photon, that can bump into neighbouring
oxygen molecules.
Any individual hydrocarbon
molecule in your gasoline might contain six, or seven, or eight, or etc. atoms of Carbon, and each ONE of those Carbon atoms can create a
molecule of CO2, when combined with
Oxygen gas.
Only greenhouse
gases like CO2 absorb IR, and they collide with other
molecules like
oxygen, and so everything heats up.
Almost immediately (nanoseconds) they relax from their excited state by either 1) emitting that energy as a new photon, some of which will continue up towards space, some of which will go back downward to be reabsorbed, thus keeping the energy in the atmosphere longer, or 2) by colliding with another
gas molecule, most likely an O2 (
oxygen) or N2 (nitrogen)
molecule since they make up over 98 % of the atmosphere, thereby converting the extra vibrational energy into kinetic energy by transferring it to the other
gas molecule, which will then collide with other
molecules, and so on, making the air warmer.
He found that
gases and vapors whose
molecules had three or more atoms, such as water vapor and CO2, absorbed much more of the thermal radiation passing through the tube than did two - atom
molecules such as
oxygen and nitrogen.
For every million
molecules of other
gases in the atmosphere (such as nitrogen,
oxygen, and hydrogen), there are only 385
molecules of CO2.
Compare with electronic transition absorption of visible light by the electrons of the
molecules of nitrogen and
oxygen in the atmosphere, the real
gas Air, which is what gives us our blue sky, reflection / scattering.
Often the CO2 will strike one of the
oxygen or nitrogen
molecules which make up the great majority of atmospheric
gases, setting them in motion, too — warming them.
The example I've given is of visible light in the atmosphere being bounced around the sky, actually reflected / scattered, by the electrons of the
molecules of nitrogen and
oxygen which comprise c98 % of our fluid
gas atmosphere.
Most of the
gas molecules in our atmosphere are nitrogen (N2) and
oxygen (O2).
Because the
molecules in a
gas are constantly moving about and colliding with each other, it is very likely that some nearby nitrogen or
oxygen molecule will collide with our excited infrared - active
gas molecule before it has a chance to emit its light.
Since the infrared - inactive
gases don't emit infrared light, if enough absorbed energy is transferred to the nitrogen and
oxygen molecules through collisions, that could theoretically increase the average energy of the air
molecules, i.e., it could «heat up» the air.
When water
molecules rise high in an atmosphere, ultraviolet radiation split the water
molecules into its component
gases,
oxygen and hydrogen, and the lighter hydrogen
molecules escape into space.
Sulfur dioxide
gas (SO2) is not itself reflective, but up there it reacts with water, picking up
oxygen molecules to become sulfate aerosol (SO4)-- now that's reflective.
For
oxygen gas at STP, the
molecules have a separation on the order of 3 nm and DeBroglie wavelengths on the order of 0.03 nm, a factor of a thousand smaller.
Global warming is implicated in the loss of Arctic ozone because greenhouse
gases trap energy lower down, heating up the atmosphere nearer the ground but cooling the stratosphere, creating conditions conducive to the formation of the reactive chemicals that break apart the three -
oxygen molecules of ozone.
The best way to do this, in my opinion, is using a fuel cell — a device that can electrochemically convert natural
gas into a useable fuel by stripping off the hydrogen portion of the methane
molecule and combining it with
oxygen to generate clean electricity and some waste heat.
This is not the first catalyst with a metal core that can pull CO2 from a
gas stream, but it is the first that when faced with air, prefers to couple with
oxygen molecules.
And as for greenhouse
gases, we all of course know that plants turn various carbon
molecules (and in some cases even methane and other greenhouse
gases) back into other useful compounds and
gases such as
oxygen and carbohydrates.
Oxygen (O2) has only two atoms per
molecule, whereas carbon dioxide (CO2) and other greenhouse
gases have three atoms or more.
Of course Carbon Dioxide is a heavy
gas, as its volume proves against the lighter predominant
molecules of Nitrogen and
Oxygen, which also means that Carbon Dioxide is a COOLING
molecule in Earth's atmosphere due to the smaller volume of heat it can maintain against the larger volumes for Nitrogen and
Oxygen...
However,
gases are different: An individual
molecule of nitrogen or
oxygen is non-polar and even its modes of oscillation are non-polar.
Their AirFlex plastics are made by extracting carbon and
oxygen molecules out of air and greenhouse
gases (including CO2 and methane) which could be fed from sources such as landfills, wastewater treatment plants, or energy plants.