This thesis primarily investigates the effects of mechanical cyclic stretching, a 5 %
low oxygen atmosphere and the Rho - kinase inhibitor, Y - 27632, on protein responses in chondrocytic human chondrosarcoma (HCS - 2 / 8) cells.
Not exact matches
MAP modifies the internal
atmosphere of a package, usually
lowering the amount of
oxygen to slow the growth of organisms that would promote product oxidation and decay.
In principle, a controlled
atmosphere high in carbon dioxide and
low in
oxygen content slows down the rate of respiration, which may extend shelf life of any respiring fruit during storage.
Unlike commercial planes, which can use the
lower atmosphere's
oxygen to give their fuel systems a boost, suborbital rocket planes use liquid
oxygen tanks to compensate for the thin air and get the thrust they need.
While
lower - energy ultraviolet radiation breaks up water molecules — a process called photodissociation — ultraviolet rays with more energy (XUV radiation) and X-rays heat the upper
atmosphere of a planet, which allows the products of photodissociation, hydrogen and
oxygen, to escape.
LA's smog is caused by sunlight driving chemical reactions between
oxygen, nitrogen compounds and hydrocarbons in the
lower atmosphere.
The Rho - kinase inhibition stimuli under
low oxygen conditions (of 5 percent
oxygen atmosphere), which is a condition corresponding to conditions in the body's cartilage, produced a more effective increase in chondrocyte - specific gene expression and synthesis of extracellular matrix components by HCS - 2 / 8 cells.
This would include
low oxygen subsurface sites with environmental conditions predating the Great Oxidation Event that occurred about 2.3 billion years ago when the
atmosphere went from very
low to high
oxygen concentrations.
The green glow photographed by Kumar and Bondoux emanates from
oxygen atoms in the
atmosphere returning to their
lowest - energy state after being excited by charged solar particles.
Hope will probe the link between processes in the
lower atmosphere, which contains most of the martian
atmosphere's water vapor, and the escape of hydrogen and
oxygen from the upper
atmosphere.
«This period of extended
low oxygen spanning from roughly 2 to less than 1 billion years ago was a time of remarkable chemical stability in the ocean and
atmosphere,» Lyons said.
In Earth's geological record, the appearance of high concentrations of manganese oxide minerals is an important marker of a major shift in our
atmosphere's composition, from relatively
low oxygen abundances to the
oxygen - rich
atmosphere we see today.
By comparison, slightly younger deposits with
lower molybdenum and rhenium concentrations had osmium isotope evidence for less continental input, indicating the
oxygen in the
atmosphere had disappeared.
«Amber provides new insights into the evolution of Earth's
atmosphere:
Low oxygen levels for dinosaurs.»
Lower in the
atmosphere,
oxygen atoms and hydroxyl radicals (OH), which form when water molecules are broken apart by ultraviolet photons, oxidize methane.
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.
Build a new home for humanity on a world with a
low -
oxygen atmosphere, extreme electrical storms, shard storms, dust devils, deadly toxic gas eruptions from some of Aven Prime's many geothermal vents, and days so long they have their own seasons.
If the
atmosphere consisted of
Oxygen / Nitrogen only, its thermal conductivity would be very
low, solar heating would be much the same, and the insulation effect (and the gravitational lapse rate) would produce a substantial temperature differential from the surface to the top of the
atmosphere without any radiative absorption.
But the boiling point of heavy water, as well as heavy
oxygen water (H2O ^ 18 rather than H2O ^ 16) are higher than that of normal water, and are found in water vapor in the
atmosphere at
lower concentrations when the global temperature is
low.
The 2009 State of the Climate report gives these top indicators: humans emitted 30 billion tons of of CO2 into the
atmosphere each year from the burning of fossil fuels (oil, coal, and natural gas), less
oxygen in the air from the burning of fossil fuels, rising fossil fuel carbon in corals, nights warming faster than days, satellites show less of the earth's heat escaping into space, cooling of the stratosphere or upper
atmosphere, warming of the troposphere or
lower atmosphere, etc..
(Fingerprint studies draw conclusions about human causation that can be deduced from: (a) how the Earth warms in the upper and
lower atmosphere, (b) warming in the oceans, (c) night - time vs day - time temperature increases, (d) energy escaping from the upper
atmosphere versus energy trapped, (e) isotopes of CO2 in the
atmosphere and coral that distinguish fossil CO2 from non-fossil CO2, (f) the height of the boundary between the
lower and upper
atmosphere, and (g) atmospheric
oxygen levels decrease as CO2 levels increase.
Via the Water Cycle, it
lowers it 52 °C from the 67 °C the real greenhouse would be without it, this being the thermal blanket of the real gas fluid ocean
atmosphere of mainly nitrogen and
oxygen around our Earth:
«The results demonstrate how rapidly rising temperatures in the
atmosphere can affect ocean circulation, cutting off
oxygen to
lower depths and extinguishing most life,» says NCAR scientist Jeffrey Kiehl, the lead author.
In Paper 2, we suggest that the phase change we identified in Paper 1 involves the «multimerization» of
oxygen and / or nitrogen in the air above the «troposphere» (the
lower part of the
atmosphere).
Sulfur oxides are made of
oxygen and sulfur molecules and are normally found in the
lower atmosphere.
Without photosynthesizing organisms, the
atmosphere would contain extremely
low amounts of
oxygen.
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.
I've read that because CO2 has a
lower specific heat then other primary gases (Nitrogen /
Oxygen) in the
atmosphere when an additional amount CO2 is introduced to a volume of air inside say a greenhouse the temperature actually drops.
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.
Coupling of atmospheric regions: To study some of the mechanisms that provide coupling between the upper and
lower atmosphere, e.g., downward transport of NO with its effects on ozone photochemistry and the vertical exchange of minor species such as odd
oxygen, CO, and H2O.