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Q: Science key stage 3 ( Answered 1 out of 5 stars,   0 Comments )
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Subject: Science key stage 3
Category: Reference, Education and News > Education
Asked by: bulabear-ga
List Price: $20.00
Posted: 30 Oct 2002 11:04 PST
Expires: 29 Nov 2002 11:04 PST
Question ID: 93331
How is air seperated and why?
Answer  
Subject: Re: Science key stage 3
Answered By: tox-ga on 08 Nov 2002 20:58 PST
Rated:1 out of 5 stars
 
bulabear-ga,
    Assuming that you mean what the composition of air is and why it
is composed that way, then...http://mistupid.com/chemistry/aircomp.htm
will give you the average percentage compositions of various gases in
the air.
    To explain the current composition of air, one must travel back to
the time of the formation of earth.  Five billion years ago, the Earth
was probably too hot to retain any of its original atmosphere.  The
atmosphere at that time is speculated to have consisted of helium,
hydrogen, ammonia and methane.  At that time, because of volcanic
activity large amounts of water vapor, carbon dioxide, and nitrogen
were expelled from the interior of the earth in a process called
outgassing (assuming that what they expel today is what they expelled
5 billion years ago).  The huge amount of water vapour in the air
caused rain, which eventually pooled to form large bodies of water. 
These bodies of water absorbed CO2 from the atmosphere.
    Nitrogen however, which is quite inert, remained and accumulated
in the atmosphere.  Oxygen appeared much later, when the first
unicellular organisms appeared on Earth, they were most likely
autotrophs, specifically, phototrophs.  They used the light energy
from the sun to drive chemical processes (calvin cycle, electron
transport chain) to produce glucose from carbon dioxide.  In the
process, oxygen is created. This is where the 21% oxygen in the
atmosphere comes in.
    After a few million years, the relative ratios of gases in the
atmosphere has reached an equilibrium and has remained that way until
now.

If that is not what you mean, then assuming you meant what the
composition of the atmosphere is and why:
The ATMOSPHERE is a protective cover of air blanketing our Earth. It
has five layers:
The atmosphere is divided into several distinct spherical layers, or
strata, separated by narrow transition zones.  The study of these
layers is called aeronomy.  The temperature structure of the
atmosphere of the planet behaves in a manner dependent upon the
balance between heating from the sun's incoming radiation, heating
from the surface below, and properties inherent to the gases of the
atmosphere itself.  Each atmospheric layer is characterized by
differences in chemical composition that produce variations in
temperature.  The upper boundary at which gases disperse into space
extends to several hundred kilometers above sea level.  Being
compressible, the air is more dense near the surface of the earth than
at higher altitudes.
  The troposphere is the atmospheric layer closest to the planet and
contains the largest percentage of mass of the total atmosphere.  It
is characterized by the density of its air and an average vertical
temperature change of approximately  6 degrees Celsius per kilometer. 
In this layer temperature and water vapor composition decrease rapidly
with altitude.  Water vapor is important in regulating air temperature
because it absorbs solar energy and thermal radiation from the
planet's surface.  The troposphere contains 99% of the water vapor in
the Earth's atmosphere.  Water vapor concentrations vary with
latitudinal position.  The concentrations are greatest above the
tropics and decrease toward the polar regions.  The upper boundary of
the troposphere ranges in height from 8 km in high latitudes, to 18 km
above the equator.  Its height also varies with seasonal changes; it
is highest in the summer and lowest in the winter.  A narrow zone
called the tropopause separates the troposphere from the next highest
layer called the stratosphere.  Air temperature within the tropopause
remains constant with increasing altitude.
    In general, weather is a tropospheric phenomenon. Troposphere
means "region of mixing" and is named because of vigorous convective
air currents within the layer.  Clouds frequently are found up to
elevations of 9 km, and rarely reach 13 km. The exception is
thunderstorms, where they  may get beyond 25 km. The study of
meteorology is therefore restricted mainly to a study of a thin
boundary layer of the atmosphere about 24 km in thickness.
    The stratosphere is the second major layer of air in the
atmosphere.  It resides between 10 and 50 km above the planet's
surface.  The air temperature in the stratosphere remains constant up
to an altitude of 25 km.  It then increases gradually to 200-220
degrees Kelvin at the lower boundary of the stratopause, which is
marked by a decrease in temperature.  Air temperatures increase with
altitude in the stratosphere, which has a stabilizing effect on
atmospheric conditions.  Ozone plays the major role in regulating
temperature.  Temperatures increase as the ozone concentration
increases.  Solar energy is converted to kinetic energy when ozone
molecules absorb ultraviolet radiation in heating the stratosphere.
    The mesosphere extends from approximately 50 km to 80 km. It is
characterized by decreasing temperatures, which register at about
190-180 K and at an altitude of 80 km.  Because there are decreased
concentrations of ozone and water vapor, the temperature is lower than
in the troposphere or stratosphere.
   The thermosphere is located right above the mesosphere, separated
by the mesopause.  The temperature in the thermosphere increases with
altitudes up to 1000-1500 K.  The increase in temperature is due to
the absorption of intense solar radiation by the remaining molecules
of oxygen.
   The exosphere is the most distant atmospheric layer.  It extends to
about 960-1000 km.  It is a transitional zone between earth's
atmosphere and interplanetary space.
Reason:
Atmospheric layers are characterized by differences in the chemical
composition that produce variations in temperature.  Each layer has a
different set of chemical compounds which in turn creates a boundary
that seperates these layers.

Hope that helps.

-Tox-ga

Request for Answer Clarification by bulabear-ga on 25 Nov 2002 14:47 PST
Sorry But I did actually mean 'How is Air Seperated and why?' For
example oxygen for medical purposes or diving, Nitrogen for chrisp
packets and hot air ballons, neon for signs. How and Why do we
seperate air? NOT what is air made up of now and in history. I gave
you the question you changed the question completely and just gave me
any answer. Are you a politician?

Clarification of Answer by tox-ga on 06 Dec 2002 11:15 PST
bulabear-ga,
  Sorry for the misinterpretation of your question, I'll attempt to
clarify now.
  The process of seperating air into its component elements has been
around for quite some time.  Since 1895 actually, when it was
discovered by Dr. Carl von Linde.
  Oxygen was first extracted from the atmosphere by a chemical
process. This was superseded over 80 years ago by the cryogenic (low
temperature) process involving the liquefaction and distillation of
air.
  The cryogenic air separation process is still by far the most widely
used. However, non-cryogenic techniques first developed during the
1970s -- pressure swing adsorption (PSA), and membrane diffusion --
are becoming increasingly significant for smaller or less demanding
on-site applications.
  There are several factors influencing the choice of separation
technology. The best supply option for each customer depends upon the
following:

Volume required - Cryogenic separation is economical for large tonnage
users.
Low temperature applications - Only cryogenic systems provide the
liquefied gases essential for low temperature applications such as
food freezing.

Purity required - Non-cryogenic systems are generally unable to
achieve high purities economically, but less pure products may be
adequate for some applications.

Continuity of supply - Fluctuating demand is best satisfied from
liquid storage tanks filled by road tanker or an on-site plant. If a
gas supply is an essential process requirement, perhaps for safety
reasons, a non-cryogenic system would usually need to be backed up
with liquid storage for emergency use.

Customer location - Some places are too remote for economical delivery
of liquid supplies by road tanker or may be out of reach altogether,
such as on board a ship.

   The purpose of air seperation is to obtain the many gases required
to drive processes in industry, as well as for recreational purposes. 
It is the most cost-effective and efficient way to produce many of the
common gases.  For example, although oxygen COULD be produced through
the electrolysis of water, such a process would requre massive amounts
of energy. Extracting it from the air where it is very abundant is a
much more viable process.  Some of the noble gases can actually only
be obtained in large quantities from the air.  Although the represent
only a minute fraction of the composition of air as indicated by our
previous answer, the absolultely massive amounts of air available more
than makes up for this deficiency. For example the Hitachi plant
produces argon, oxygen and nitrogen in a very high purity form
(http://www.pi.hitachi.co.jp/sanpu/lowtemp/to-apn-e.html)

    The air in the earth's atmosphere contains gasses that have many
industrial and scientific uses once they are separated to highly pure
substances.  The air in the earth's atmosphere is composed of nitrogen
(78.08%), oxygen, carbon dioxide and trace amounts of noble gases.

Separation 
    Gases are separated using a variety of methods.  The separation
method used is determined by a variety of factors, which include the
volume required, low temperature applications, customer location,
continuity of supply, and purity level.   The separation processes are
broken down into two categories: cryogenic separation processes and
non cryogenic processes. Cryogenic is the keystone of cryogenic
processing since it is the source of many cryogenics fluids for use in
science and technology.  In volume of production the separation of air
into its components at low temperatures is by far the most important
of the separation processes.(Sittig 1963)   Non cryogenic processes
are methods used to separate air at ambient, or room temperature.  Non
cryogenic methods include pressure swing absorption, membrane
diffusion, and vacuum swing absorbent.
(http://www.boc.com/gases/air/noncryo/noncryo.htm)

Noncryogenic Methods:
> Pressure swing absorption
  Pressure swing absorption (PSA) is a non cryogenic method of
separating gases.  PSA works because the molecules of each gas are
different sized.  The air is gathered by a compressor and placed into
a tank, which contains molecular sieves containing various absorbents,
depending on which gas is being produced.  Pressure pushes the air up
against the sieves, and the smallest molecules pass through, therefore
separating the desired gas.  Pressure is released and the process
occurs over again in the second tank in order to increase the purity
level. Nitrogen produced by PSA are very similar to those produced by
membrane diffusion.  They are low cost, many units are on site, and
they have a low purity level.
(http://www.boc.com/gases/air/noncryo/psa.htmEquipmentused)

> Vacuum swing absorption
  Vacuum swing absorption (VSA) is a non cryogenic air separation
method.  In VSA compressed air is placed into a tank that contains
molecular sieves. Molecular sieve are little balls that look like
ferterlizer. The sieves contain absorbents to gather the gasses that
are unwanted.  Once the sieves are saturated with the unwanted gasses,
a vacuum pump turns on and sucks the sieves clear of the unwanted
gasses, allowing the sieve to be reused.  There are two tanks used in
this process.  One is being used while the other is regenerating so
that the product is continuously available.  VSA has the ability to be
used on site, but it also produces a low purity gas.
(http://www.boc.com/gases/air/noncryo/vsa.htm)
                             
> Membrane diffusion
  Membrane diffusion is the simplest method by which gasses are
separated from another.  The process works by pushing compressed air
into one end of a membrane, which contains many hollow fibers through
which the air flows.  The fibers absorb the fast gasses of oxygen,
carbon dioxide and water vapor, allowing the slow gas  of nitrogen to
separate.  Membrane systems are often smaller onset systems, which are
more convenient for customer control.  Membrane diffusion gasses are
significantly less expensive than gasses from other separation
processes because the purity is low  level of about 95%.  They are
also less expensive because there is not the need for monitoring,
ordering and storing.
(http://www.boc.com/gases/air/noncryo/membrane.htm )

BOC Membrane Systems onset Nitrogen Supply 
 "While "fast gases" such as oxygen, carbon dioxide, and water vapor
quickly permeate the membrane, most of the nitrogen flows along the
membrane fiber as a separate product stream."
(http://www.boc.com/gases/air/noncryo/memscheme2.htm)

Cryogenic Method:
  "Is the study and use of materials at very low temperatures. The
upper limit of cryogenic temperatures has not been agreed on, but the 
National Bureau Of Standards has suggested that the term cryogenics be
applied to all temperatures below -150° C (-238° F or 123° above
absolute  zero on the Kelvin scale). Some scientists regard the normal
Boiling Point of oxygen (-183° C or -297° F), as the upper limit (see
Absolute Zero).  Cryogenic temperatures are achieved either by the
rapid evaporation of volatile liquids or by the expansion of gases
confined initially at pressures of  150 to 200 atm. The expansion may
be simple, that is, through a valve to a region of lower pressure, or
it may occur in the cylinder of a reciprocating  engine, with the gas
driving the piston of the engine. The second method is more efficient
but is also more difficult to apply."
(http://www.fwkc.com/encyclopedia/low/articles/c/c005002389f.html)

  Cryogenic air separation uses pressure and temperature control in
order to separate gasses.  The cryogenic air separation process uses
the boiling points of gasses as the main principle.  When a gas
reaches its boiling point, it turns into a liquid state.  The
difference in boiling points causes gasses to separate because each
gas will turn to a liquid at a different point.  The temperatures at
which gasses turn to a liquid are very low.  Nitrogen liquefies at
-320.4 F, argon at -302.6 F, and oxygen -297.3 F.  Once each gas
reaches its boiling point, it begins to condense and separate.
Cryogenic separation is used mainly for medium to large scaled
production of nitrogen, oxygen, and argon.  Cryogenics is normally
used to produce gasses in liquefied form for storage or
transportation, and a gaseous form for pipeline transportation to
large industrial users.
(http://www.praxair.com/Praxair.nsf/1b1a158c246dbf3e8525654300683b77/45da5d07b15e43c385256569005b7db9?OpenDocument)

Industrial Uses
  "Among the many important industrial applications of cryogenics are
the large-scale production of oxygen and nitrogen from air.   The
oxygen can be used in a variety of ways, for example, in rocket
engines, for cutting and welding torches, for supporting life in space
and deeps vehicles, and for blast furnace operations. The nitrogen
goes into the making of ammonia for fertilizers, and it is used to
prepare frozen foods by cooling them rapidly enough to prevent
destruction of cell tissues. It can also serve as a
refrigerant and for transporting frozen foods. 
    Cryogenics has also made possible the commercial transportation of
liquefied natural gas.  Without cryogenics, nuclear research would
lack liquid hydrogen and helium for use in particle detectors and for
the powerful electromagnets needed in large particle accelerators.
Such magnets are also being used in nuclear fusion research. Infrared
devices, masers, and lasers can employ cryogenic temperatures as well.
    Cryogenic surgery, or cryosurgery, is being used for the treatment
of Parkinson's disease, the technique being based on the selective
destruction of tissue by freezing it with a small cryogenic probe. A
similar technique has also been employed to destroy brain
tumors and to arrest cervical cancer.
(http://encarta.msn.com/index/conciseindex/30/0300C000.htm?z=1&pg=2&br=1#s5)

Delivery
  Cryogenics can be delivered by semitankers, pipelines and or
containors.

Environment
        The process of separating air has little effect on the natural
environment.  The pollutants that are in the air when it goes through
the process are released back into the environment which they came. 
The manufactures of this process are very concusses about the
environment. Cryogenics plants such as "Praxair products and
technologies are used by many industries to benefit the environment.
In the face of increasingly stringent regulations, our global
customers rely on our expertise to help them cut emissions and energy
consumption, while improving productivity.
(http://www.praxair.com/Praxair.nsf/X1/envi?OpenDocument)

Hazards
    "The primary hazards of dealing with cryogenics are those
associated with the human body and the surroundings.  The firsts
includes frostbite, respiratory, ailments, and chemical burns; the
second, phases changes and low temperature effects; and the third,
ignition and combustion reactions".

I hope that helps.  Ask for clarification if it is still required.

-Tox-ga
bulabear-ga rated this answer:1 out of 5 stars
Only got one star because I couldn't give none. How is air seperated
and why? eg for medical gases, nitrogen for hot air ballons, neon for
signs. How do we seperate air into its different parts how do we
seperate air? I never asked what is air made up of. If I had wanted to
know that I would have asked 'What is Air made up of?' wouldn't I?

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