The atmosphere is heated from
the bottom by solar radiation and cooled from the top by infrared
radiation to space. Mechanical energy is produced when heat is
carried upward by convection. The Atmospheric Vortex Engine (AVE)
is a process for capturing the energy produced when heat is
carried upward by convection in the atmosphere.
The AVE uses a tornado-like vortex to concentrate the
mechanical energy produced during upward heat convection where it
can be captured. A vortex engine consists of a cylindrical wall
open at the top and with tangential air entries or deflectors
around its base. Heating the air within the wall using a temporary
heat source such as steam starts the vortex. The heat required to
sustain the vortex once established can be the natural heat
content of the warm humid air or can be provided in cooling towers
located outside of the cylindrical wall and upstream of the
deflectors. The continuous heat source for the peripheral heat
exchangers can be waste industrial heat or warm seawater. The
intensity of the vortex is regulated by restricting the flow of
air with dampers located upstream of the deflectors. The vortex
can be stopped by restricting the airflow to deflectors with
direct orientation and if necessary opening the airflow to
deflectors with reverse orientation.
The electrical energy is produced in turbo-expanders located
upstream of the tangential entries. The pressure at the base of
the vortex is less than ambient pressure because the density of
the rising air is less than the density of the ambient air at the
same level. The outlet pressure of the turbo-expanders is
sub-atmospheric because they exhaust in the vortex.
The cylindrical wall could have a diameter of 200 m and a
height of 100 m; the vortex could be 50 m in diameter at its base
and extend up to the tropopause. An AVE could generate 50 to 500
MW of electrical power.
Thermodynamic Basis
The Atmospheric Vortex Engine has the same thermodynamic basis
as the solar chimney. The physical tube of the solar chimney is
replaced by centrifugal force in the vortex and the atmospheric
boundary layer acts as the solar collector. The AVE needs neither
the collector nor the high chimney. The efficiency of the solar
chimney is proportional to its height which is limited by
practical considerations, but a vortex can extend much higher than
a physical chimney.
The average upward convective heat flux at the bottom
atmosphere is 150 W/m2, one sixth of this heat could be converted
to work while it is carried upward by convection. The heat to work
conversion efficiency of the atmosphere is approximately 15%
because the heat is received at an average temperature of 15 °C
and given up at an average temperature of minus 15 °C. The average
work produced in the atmosphere is therefore 25 W/m2. The total
mechanical energy produced in the atmosphere is 12000 TW (25 W/m2
x 510 x 10E12 m2) whereas the total work produced by humans is 2
TW. The mechanical energy produced in a single large hurricane can
exceed all the energy produced by humans in a whole year.
The thermodynamic basis of the AVE is consistent with currently
accepted understanding of how energy is produced in the
atmosphere. Atmospheric scientists call the mechanical energy
produced when a unit mass of air is raised reversibly from the
bottom to the top of the troposphere Convective Available
Potential Energy (CAPE). CAPE during periods of insolation or
active convection is typically 1500 J/kg which is equal to the
mechanical energy produced by lowering a kilogram of water 150 m.
The vortex would transfer the mechanical energy down to the
Earth's surface where it would be captured.
The existence of tornadoes proves that low intensity solar
radiation can produce concentrated mechanical energy. It should be
possible to control a naturally occurring process. Controlling
where mechanical energy is produced in the atmosphere offers the
possibility of harnessing solar energy without having to use solar
collectors.
Process Potential
The process could provide large quantity of renewable energy,
could alleviate global warming, and could contribute to meeting
the requirements of the Kyoto protocol. The AVE has the potential
of providing precipitation as well as energy. There is reluctance
to attempt to reproduce a phenomenon as destructive as a tornado,
but controlled tornadoes could reduce hazards by relieving
instability rather than create hazards. A small tornado firmly
anchored over a strongly built station need not be a hazard.
The AVE could increase the power output of a thermal power
plant by 30% by converting 20% of its waste heat to work. The
power increase results from reducing the temperature of the cold
sink from the temperature at the bottom of the atmosphere (15 °C)
to the temperature at which the atmosphere radiates heat to space
(-15 °C).
The process could be adapted for use with all existing thermal
power plants, whether they are coal fired, natural gas or nuclear.
The main requirement for the AVE is a steady supply of low-grade
heat. The temperature of the saturated air coming out of power
plant cooling towers is higher than that of the warm humid air
responsible for the energy of tornadoes and hurricanes.
The process could be developed with relatively little
engineering effort. The technology is similar to that of cooling
towers and turbine-generators. The upward heat convection process
responsible for producing energy in the AVE is the process
responsible for producing the circulation in natural draft cooling
towers and in natural circulation boilers. Engineers with
experience in the power industry would be good candidate for
developing the process.
Electrical utilities are invited to consider participating in
the development and commercialization of the AVE. The unit cost of
electrical energy produced with an AVE could be less than half the
cost of the next most economical alternative. Additional
electrical energy would be produced without additional fuel. The
process is protected by patent applications and could become an
important source of electrical energy.
Initial development work would concentrate on producing stable
vortices. Under favorable conditions, it should produce a steam
assisted vortex with a station 10 m in diameter and a
self-sustaining vortex with a station 30 m in diameter. Learning
to control large vortices under all conditions will be an
engineering challenge. Developing the process will require
determination, engineering resources and cooperation between
engineers and atmospheric scientists. There will be difficulties
to overcome, but they should be no greater than in other large
technical enterprises.
Additional Information
In December 2004, a detailed description of the AVE including
drawings and thermodynamic calculations was published as a White
Paper in Energy Central's
Knowledge Center.
On September 29 2005 the Economist had an article on the AVE
which resulted in a lot of media attention:
http://www.economist.com/science/displayStory.cfm?story_id=4455446
There is much more information including: drawings,
presentations, and technical publications on the AVE web site:
http://vortexengine.ca
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