The production of methane is accelerated because stationary pools of water contain
much less oxygen than a flowing river interacting with the atmosphere and microbes thrive in low - oxygen environments.
For teams coming from low - lying areas, it can be quite an ordeal playing a full 90 minutes when there is
much less oxygen available than they are used to.
Not exact matches
No
oxygen is needed for this conversion, but the downside is that it produces
much less energy.
The mid-stage population that began appearing after day 7 featured
oxygen - intolerant bacterial species often seen in American individuals but
much less frequently in developing nations.
By looking at the chemistry of rocks deposited during that time period, specifically coupled carbon and sulfur isotope data, a research team led by University of California, Riverside biogeochemists reports that
oxygen - free and hydrogen sulfide - rich waters extended across roughly five percent of the global ocean during this major climatic perturbation — far more than the modern ocean's 0.1 percent but
much less than previous estimates for this event.
When an
oxygen molecule comes in and wants to react with that surface,
much less energy is needed to break the
oxygen -
oxygen bond in the
oxygen molecule.
Similar islands of material in the early universe could have held as
much water vapor as we find in our galaxy today, despite containing a thousand times
less oxygen.
With an atmosphere of
much less than one percent
oxygen, scientists have presumed that there were things living in deep water in the mud that didn't need sunlight or
oxygen, but Czaja says experts didn't have any direct evidence for them until now.
On Titan, where solar ultraviolet radiation is
much weaker and
oxygen - bearing molecules are substantially
less abundant, methane can last 10 million to 100 million years (which is still a short time in geologic terms).
Eventually, Stars Aa and Ab will lose
much of their current mass, from intensified stellar winds that eventually puff out their outer gas envelopes of hydrogen and helium (and
lesser amounts of higher elements such as carbon and
oxygen) into interstellar space as planetary nebulae.
Although LGM
oxygen isotope changes can not be used to independently assess cooling, they provide a useful additional constraint that is difficult to reconcile with a cooling
much less than 3 deg.
Oxygen provides
much less fuel (2 energy molecules) for cancer cells compared to sugar (2 energy molecules).
So if
oxygen replaces the sulfur it would «result in a
much less hydrophobic amino acid.»
Again, glycine molecules are larger than
oxygen, so there's
less magnesium by weight, but the gut is
much more able to absorb it.
With
less blood flow, your skin doesn't get as
much oxygen and important nutrients, such as vitamin A.
Space Engineers is
much less forgiving in that aspect, as starting off on a planet with little to no
oxygen will most likely result in you running out of your supply before you can even start constructing an
oxygen tank, let alone shelter.
Although LGM
oxygen isotope changes can not be used to independently assess cooling, they provide a useful additional constraint that is difficult to reconcile with a cooling
much less than 3 deg.
A future hydrogen economy could use the gas as an energy carrier As this method doesn't produce
oxygen which needs to be kept separate from hydrogen, safety from explosion of the two gases is
much less of a problem with electricity in the national grids carried by ageing cables, it would be useful to replace them by passing the hydrogen along gas pipes used currently for natural methane gas.
It is an allotrope of
oxygen that is
much less stable than the diatomic allotrope O 2, breaking down in the lower atmosphere to normal dioxygen.