Sentences with phrase «oxygen gas molecules»

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 nitroMolecules with three or more atoms, like CO2 and other greenhouse gases, do this much better than molecules with just two, like oxygen (O2) and nitromolecules 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.
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