December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion1 Unrestrained Expansion a Source of Entropy by Louis M. Michaud Vortex Engine.

Slides:



Advertisements
Similar presentations
THE SIMPLEST EXPLANATION CAME FIRST
Advertisements

Chapter 2 Introduction to Heat Transfer
Advanced Thermodynamics Note 4 The Second Law of Thermodynamics
Section 16.3 Using Heat.
Exergy: A Measure of Work Potential Study Guide in PowerPoint
Convection in Air Investigation 5, Part 3
ENERGY FROM THE SUN Chapter 14.3 Pages Energy in the Atmosphere The sun is the source of ALL energy in our atmosphere. Three things that can.
Energy in Earth’s Atmosphere
AVEtec Energy Corporation We produce perfectly green electrical energy from low temperature heat. For more information visit: Contact:
Heat Engines, Entropy and the Second Law of Thermodynamics
Atmospheric Heat Convection, The Sun & Wind
Thermodynamics, Buoyancy, and Vertical Motion Temperature, Pressure, and Density Buoyancy and Static Stability Adiabatic “Lapse Rates” Convective Motions.
Thermal Energy and Heat
Chapter 15: Thermodynamics
Heating of the Atmosphere
Chapter 24 Thermodynamics
Important Terms & Notes Conceptual Physics Mar. 13, 2014.
Heat Transfer and Solar Radiation
UNIT THREE: Matter, Energy, and Earth  Chapter 8 Matter and Temperature  Chapter 9 Heat  Chapter 10 Properties of Matter  Chapter 11 Earth’s Atmosphere.
Precipitation Hydrology (Spring 2013) Illinois State University Instructor: Eric Peterson.
The Atmosphere and is its importance to the Earth.
Unit 3 Lesson 3 Energy Transfer
Unit 10 Lesson 3 Energy Transfer
Chapter Eleven: Heat 11.1 Heat 11.2 Heat Transfer.
Conduction, Convection, Radiation, oh my!!. Conduction –Involves objects in direct contact –2 objects in contact are at unequal temperature –Example:
Investigation 9B  Key Question: How is convection responsible for the movement of air through the atmosphere?? Convection in Earth’s Atmosphere.
Weather Review. Air Masses Air Mass – A large body of air through which temperature and moisture are the same. Types 1. Continental – formed over land.
Gas Turbines for Aircraft Propulsion. AIR CRAFT ENGINE The turbojet engine consists of three main sections: the diffuser, the gas generator, and the nozzle.
Heat Transfer What do you know about heat transfer?
Heat Transfer in the Atmosphere Essential Question: How is heat transferred in the atmosphere?
Background and Purpose of Study Definition of Desertification Mechanism of Desertification Summary Air Environment Engineering 2.
Weather & Water Investigation 8
HEAT 11.2.
Characteristics of the Atmosphere. The Composition of the Atmosphere The atmosphere is made of 78% Nitrogen gas and about 21% oxygen. The atmosphere also.
The Atmosphere Preview Section 2 Atmospheric Heating Concept Mapping.
1 16 Heat Transfer how does heat move? Conduction through matter Convection of matter By emitting/absorbing Radiation Homework: RQ: 3, 6, 11, 20, 21, 25.
What processes heat the atmosphere?
NOVEMBER 12, 2015 RIGHT NOW: GET 6.2 NOTES AGENDA: 6.2 NOTES SKILLS SHEET/HOMEWORK OBJECTIVE: DETERMINE HOW THE SUN DRIVES ATMOSPHERIC CONVECTION.
MME 2009 Metallurgical Thermodynamics
Heat Transfer Conduction, Convection, Radiation. Three Main Processes of Heat Transfer  Conduction  Convection  Radiation.
Bell work How is food heated in an oven? How is food heated on a range top?
Wind. Review  What is a convection cell?  An area where high and low energy molecules move in a circular pattern rising when they gain energy and falling.
2 pt 3 pt 4 pt 5pt 1 pt 2 pt 3 pt 4 pt 5 pt 1 pt 2pt 3 pt 4pt 5 pt 1pt 2pt 3 pt 4 pt 5 pt 1 pt 2 pt 3 pt 4pt 5 pt 1pt Hot, hot, hot Baby, it’s cold outside.
Weather and Climate Unit Investigative Science. * All materials are made of particles (atoms and molecules), which are constantly moving in random directions.
1.3 notes  There are 3 types of heat transfer: radiation, conduction, and convection.  The transfer of energy through space is radiation. Sunlight.
Heat Engines A gasoline engine is a form of a heat engine, e.g. a 4-stroke engine INTAKE stroke: the piston descends from the top to the bottom of the.
Atmospheric Heating Radiation Conduction Convection.
1 3E-03 Fire Syringe RAPID COMPRESSION IS ADIABATIC GIVING RAPID RISE OF AIR TEMPERATURE IN THE CHAMBER WHICH EXCEEDS THE IGNITION TEMPERATURE OF THE FLAMMABLE.
Atmosphere. Earth’s Radiation Budget Earth maintains an energy balance and a temperature balance by radiating as much energy into space as it absorbs.
 ADIABATIC HEATING/COOLING A. Adiabatic temperature changes occur when 1. Air is compressed as pressure increases a. Motion of air molecules increases.
Atmospheric Heating.
Unit 3 Lesson 2 Energy Transfer
What do you mean with Earth’s Energy Budget?
Solar collectors for water heating
Hello, my name is Louis Michaud.
Land Breezes and Sea Breezes Sea Breeze
Unit 3 Lesson 2 Energy Transfer
Atmospheric Heating Chapter 15 section 2
Section 2 Atmospheric Heating.
Thermal Energy from the Sun
AVE stands for Atmospheric Vortex Engine.
Convection in Air Investigation 5, Part 3
Weather dynamics Day 2 – Heat Science 10.
As an engineer I was aware that more work is produced by the expansion of a warm gas than is required to compress the same gas after it has been cooled.
Thermal Energy from the Sun
Convection in Air Investigation 5, Part 3
Unit 3 Lesson 2 Energy Transfer
Begin working on the winds worksheet from the quiz day.
What happens to solar energy as it enters the atmosphere?
The Sun is the source of energy for the Earth.
Presentation transcript:

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion1 Unrestrained Expansion a Source of Entropy by Louis M. Michaud Vortex Engine

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion2 Earth Overall Entropy Budget Balancing the earth’s entropy budget requires that entropy be produced internally within the earth system. Entropy produced: 892 mW K -1 m -2 –Absorbtion in Upper atmosphere: 255 mW K -1 m -2 –Absorbtion at Surface: 580 mW K -1 m -2 –Atmospheric Convection: 77 mW K -1 m -2 Entropy received: 41 mW K -1 m -2 Entropy given up: 933 mW K -1 m -2

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion3 Fig. 1

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion4 Entropy budget of the Atmosphere Entropy production when solar radiation is absorbed by the upper atmosphere or by the earth’s surface results from thermal unequilibrium. Entropy production is immediate and occurs when the radiation is absorbed. – Fig 1 Entropy production when heat is transported upward by convection in the atmospheres results from mechanical unequilibrium. Entropy production is delayed and occurs when the heat is transported upward. - Fig. 2 Entropy production during upward heat transported could be avoided if the heat were transported by a Carnot engine. Dissipating the energy produced by the Carnot engine would restore entropy production. – Fig 3

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion5 Fig. 2

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion6 Fig. 3

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion7 Gravity Power Cycle The differential pressure across the turbine results from the difference in density between the warmed rising air and the cooled descending air. – Fig. 4 Very high vertical conduits are required to achieve significant efficiency. There must be a turbine or expander to capture the work. - without the expander the work reverts to heat. The gravity cycle is equivalent to the ideal gas turbine power cycle. There is no entropy production in an ideal gas- turbine cycle. The efficiency of the gravity cycle is the same as that of a Carnot engine with the same average effective hot and cold source temperatures.

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion8 Fig. 4

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion9 Entropy Production In ideal cycles entropy production is eliminated by: 1.Keeping temperature differences small to eliminate thermal unequilibrium 2.Keeping velocites low to eliminate friction losses 3.Eliminating mixing by postulating that the water does not separate from the air 4.Restraining the expansion in an expander - either a turbine or piston expander Entropy production during upward heat convection can be due to: 1.Temperature differences (thermal unequilibrium) 2.Friction (mechanical unequilibrium) 3.Mixing of fluid of different temperature or composition (non-mechanical unequilibrium) 4.Unrestrained expansion. (mechanical unequilibrium)

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion10 Unrestrained Expansion Van Ness Expander The Automat of the Van Ness expander illustrates the fact the work reverts to heat unless there is a force to restrain the expansion. – Fig. 5 Releasing the latch only produces useful work when the Automat restrains the piston. Unrestrained expansion in an ascending air parcel reduces net work to zero while producing the 77 mW K -1 m -2 of entropy necessary to balance the atmospheric entropy budget. Unrestrained expansion, which is usually ignored, is responsible for the largest part of the entropy produced during atmospheric upward heat convection.

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion11 Fig. 5

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion12 Atmospheric Engine Since atmospheric entropy production is mainly the result of unrestrained expansion, it might be possible to capture the work that would be produced if the heat were transported with a Carnot engine by simply providing an expander. There have been two proposals for capturing the energy produced during atmospheric upward heat convection: 1. The Solar Chimney – Fig. 6 2.The Atmospheric Vortex Engine – Fig. 7 - where the physical tube is replaced by centripetal force See web site: for additional information including text of the AGU presentation.

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion13 Fig. 6 Manzanares solar chimney 200 m high, 10 m diameter, 50 kW

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion14 Fig. 7 Vortex Solar chimney 100 m high, 200 m diameter, 200 MW

December 2005 / L. MichaudAGU NG23A-0090 Unrestrained Expansion15 Unrestrained Expansion – A Source of Entropy Louis Michaud, Vortex Engine AGU Poster Session paper: NG23A-0090 Paper sponsored and posted by: Dr. Ralph Lorenz Author Louis Michaud is unable to attend the AGU Fall 2005 Meeting. He can be reached by at: or by phone at: (519) Additional information including the text of this presentation is available at website: Summar y