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Real  climate mitigation  – facts and fears
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Content
Numbers and figures ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
More numbers and figures ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object]
Emission reductions only  – is futile ! It is like cutting the branch – but slowering the rate !
Assume a 20% emission reduction  in  ten  years For the entire world! Reduced emissions Gt Carbon 7,68 7,53 7,38 7,23 7,09 6,95 6,81 6,67 6,54 6,41 7,84 8,00 390 ppm 0 10 20 30 40 2009 2010 2011 2012 2013 2014 2015 2016 2017 2016 2017 2019 Current CO 2  concentration
Accumulation Emissions Gigatonnes Carbon But, carbon dioxide  accumulate  in the   air 7,68 7,53 7,38 7,23 7,09 6,95 6,81 6,67 6,54 6,41 7,84 16 24 31 38 46 53 60 67 73 80 86 8,00 0 10 20 30 40 50 60 70 80 90 100 2009 2010 2011 2012 2013 2014 2015 2016 2017 2016 2017 2019
Accumulated Atmospheric CO 2  concentration, ppm Emissions Gigatonnes Carbon Thus, even a bold emisson reduction  will lead to a disastous  increase in concentration 413ppm   7,68 7,53 7,38 7,23 7,09 6,95 6,81 6,67 6,54 6,41 7,84 16 24 31 38 46 53 60 67 73 80 86 8,00 389ppm 0 10 20 30 40 50 60 70 80 90 100 370 375 380 385 390 395 400 405 410 415 2009 2010 2011 2012 2013 2014 2015 2016 2017 2016 2017 2019
[object Object],[object Object],[object Object]
Antarctic ozone    Arctic summer sea-ice  Arctic permafrost ( going on ) Atlantic thermohaline circulation (NADW) El Niño–Southern Oscillation (ENSO) Indian summer monsoon Sahara/Sahel and West African monsoon Amazon rainforest Boreal forest Antarctic Bottom Water Arctic ozone Tipping   points = the Humpty Dumpty effect Tipping points: Non-linear changes  – a fast change, followed by a  very  long recovery time Systems prone to tipping: FG FG FG The tipping level The tipping level
The CO 2   accumulates  in the atmosphere
280 300 350 400 387 Risk for tipping increase considerably over 350 ppm ppm CO 2
Tipping points of the global system, example: Arctic sea ice ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Tipping level No return FG FG FG FG FG
FG
[object Object],[object Object],[object Object],[object Object]
Gt/yr Assume, a  radical  emission reduction This will not solve the problems ppm 1 2 3 4 5 6 7 8 9 0 90%
[object Object],[object Object],[object Object],[object Object],[object Object]
By that,  carbon dioxide  is  removed  from the atmosphere. The process is called  photosynthesis /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n When plants add  solar energy   to the carbon dioxide molecules,  carbon dioxide is converted into biomass Carbon sequestration FG
However… /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n After a century, or less, the biomass decomposes and releases the carbon dioxide again It is like putting dirt under the carpet.  It will reveal… Carbon sequestration FG
Gt/yr A  radical  emission reduction  can  solve the problems! At this time, the CO2 level stops rising ! ppm if it is combined with carbon sequestration  ! 1 2 3 4 5 6 7 8 9 0 1 Gt net   seque-  stration Emission reduction Carbon sequestration Atmospheric carbon
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],However, this effort would dwarf the Chinese wall,  the pyramides and the  first and second world war – together
If you convert biomass into charcoal /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n FG
/C(H 2 O)/ n ..and bury it into the soil.. Carbon sequestration FG
Then, you have created a pathway for carbon dioxide into a semi-permanent storage Carbon sequestration FG
32 000 years old char !
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Anila Biomass Gasifier Stove Designed and built by Professor U.N. Ravikumar (Eng) Mysore University, India Biochar production FG
Raw Material Pyrolysis Charcoal 4 kg dry waste biomass 1 kg dry hard wood Wood burns from the top down When the waste biomass reaches 360 deg C it begin to release gases and turn into charcoal The Pyrolysis gases burn hot and last for more than 1 hour At the end of the process , the biomass has changed into about 1 kg charcoal FG FG FG AIR
Simple char making at home Fill the bucket with biomass  Put the bucket  upside down  in the barrel A barrel  And a bucket  Make a fire outside the bucket  The char is ready! The pyrolysis gasses takes fire More heat! Biochar production FG
The savonius pyrolyser FG FG FG FG FG FG
Lambiotte continouos charcoal production Kiln
1000-Hour Demonstration of Hydrogen by Biomass Catalytic Steam Reforming and co-products (Completed May 17 th  2007 )  2007 Bio-refinery Conversion Project at University of Georgia Danny Day, Eprida
Commercial Facilty in Blakely, Georgia Biomass Conversion to Activated Carbon and Electricity Danny Day, Eprida
Is there enough biomass for 2Gt? ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Total: 2.2 Gt char
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Charcoal works as an adsorption lattice for micro-organsism and nutrient particles Biochar soils FG
1 gramme of well-made charcoal will have an inner area of about 400 sq. meters Biochar soils FG
Which means that one bag of barbeque char  … will have an inner area of  1 sq. km! Biochar soils FG FG
The plants seek contact with microorganisms Richard Haard, February 12, 2007   Charcoal after one year of application Biochar soils FG
Charcoal is sought out by soil micro-organism Charcoal addition to the soil provides nutrient and water storage for  mycorrhizal fungi Their hyphae invade charcoal pores and support spore  reproduction Ogawa  Kansai Environmental Fungi on New Char Fungi on 100 Yr Old Char Biochar soils FG
Effects of biochar ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],FG
Why? ,[object Object],[object Object],[object Object],[object Object],FG
Humic acids  (there are plenty!) FG
Complex of humic acids FG
Char structure FG
Oxisol (normal rain- forest soil) Terra Preta ( anthrosol :  charcoal enriched  oxisol, made by human activities) FG FG
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
If you want to  emit  net carbon dioxide: Situation of today :
And  you must buy an emission permit You have to pay a tax FG
Tax and permit fund $ P ayment P ermission E mission The PPE Model (currently used) The economist solution: Climate problems from approved  carbon dioxide! FG
The arguments for biochar ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],FG
Is that enough? FG
Probably not The arguments don’t speak to our immediate self-interest FG
To  really  get people’s attention ,  you have to talk money FG
What about a  fair  carbon tax? FG
/C(H 2 O)/ n Carbon sequestration fund $ S equestration V alidation P ayment The SVP model Another solution: Climate problems reduced by payment for sequestration ! ,[object Object],[object Object],[object Object],[object Object],[object Object],FG
An example ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],FG
Thank you!

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Co2 ecounit

  • 1. Real climate mitigation – facts and fears
  • 2.
  • 3.
  • 4.
  • 5.
  • 6. Emission reductions only – is futile ! It is like cutting the branch – but slowering the rate !
  • 7. Assume a 20% emission reduction in ten years For the entire world! Reduced emissions Gt Carbon 7,68 7,53 7,38 7,23 7,09 6,95 6,81 6,67 6,54 6,41 7,84 8,00 390 ppm 0 10 20 30 40 2009 2010 2011 2012 2013 2014 2015 2016 2017 2016 2017 2019 Current CO 2 concentration
  • 8. Accumulation Emissions Gigatonnes Carbon But, carbon dioxide accumulate in the air 7,68 7,53 7,38 7,23 7,09 6,95 6,81 6,67 6,54 6,41 7,84 16 24 31 38 46 53 60 67 73 80 86 8,00 0 10 20 30 40 50 60 70 80 90 100 2009 2010 2011 2012 2013 2014 2015 2016 2017 2016 2017 2019
  • 9. Accumulated Atmospheric CO 2 concentration, ppm Emissions Gigatonnes Carbon Thus, even a bold emisson reduction will lead to a disastous increase in concentration 413ppm 7,68 7,53 7,38 7,23 7,09 6,95 6,81 6,67 6,54 6,41 7,84 16 24 31 38 46 53 60 67 73 80 86 8,00 389ppm 0 10 20 30 40 50 60 70 80 90 100 370 375 380 385 390 395 400 405 410 415 2009 2010 2011 2012 2013 2014 2015 2016 2017 2016 2017 2019
  • 10.
  • 11. Antarctic ozone  Arctic summer sea-ice  Arctic permafrost ( going on ) Atlantic thermohaline circulation (NADW) El Niño–Southern Oscillation (ENSO) Indian summer monsoon Sahara/Sahel and West African monsoon Amazon rainforest Boreal forest Antarctic Bottom Water Arctic ozone Tipping points = the Humpty Dumpty effect Tipping points: Non-linear changes – a fast change, followed by a very long recovery time Systems prone to tipping: FG FG FG The tipping level The tipping level
  • 12. The CO 2 accumulates in the atmosphere
  • 13. 280 300 350 400 387 Risk for tipping increase considerably over 350 ppm ppm CO 2
  • 14.
  • 15. FG
  • 16.
  • 17. Gt/yr Assume, a radical emission reduction This will not solve the problems ppm 1 2 3 4 5 6 7 8 9 0 90%
  • 18.
  • 19. By that, carbon dioxide is removed from the atmosphere. The process is called photosynthesis /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n When plants add solar energy to the carbon dioxide molecules, carbon dioxide is converted into biomass Carbon sequestration FG
  • 20. However… /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n After a century, or less, the biomass decomposes and releases the carbon dioxide again It is like putting dirt under the carpet. It will reveal… Carbon sequestration FG
  • 21. Gt/yr A radical emission reduction can solve the problems! At this time, the CO2 level stops rising ! ppm if it is combined with carbon sequestration ! 1 2 3 4 5 6 7 8 9 0 1 Gt net seque- stration Emission reduction Carbon sequestration Atmospheric carbon
  • 22.
  • 23. If you convert biomass into charcoal /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n /C(H 2 O)/ n FG
  • 24. /C(H 2 O)/ n ..and bury it into the soil.. Carbon sequestration FG
  • 25. Then, you have created a pathway for carbon dioxide into a semi-permanent storage Carbon sequestration FG
  • 26. 32 000 years old char !
  • 27.
  • 28. Anila Biomass Gasifier Stove Designed and built by Professor U.N. Ravikumar (Eng) Mysore University, India Biochar production FG
  • 29. Raw Material Pyrolysis Charcoal 4 kg dry waste biomass 1 kg dry hard wood Wood burns from the top down When the waste biomass reaches 360 deg C it begin to release gases and turn into charcoal The Pyrolysis gases burn hot and last for more than 1 hour At the end of the process , the biomass has changed into about 1 kg charcoal FG FG FG AIR
  • 30. Simple char making at home Fill the bucket with biomass Put the bucket upside down in the barrel A barrel And a bucket Make a fire outside the bucket The char is ready! The pyrolysis gasses takes fire More heat! Biochar production FG
  • 31. The savonius pyrolyser FG FG FG FG FG FG
  • 32. Lambiotte continouos charcoal production Kiln
  • 33. 1000-Hour Demonstration of Hydrogen by Biomass Catalytic Steam Reforming and co-products (Completed May 17 th 2007 ) 2007 Bio-refinery Conversion Project at University of Georgia Danny Day, Eprida
  • 34. Commercial Facilty in Blakely, Georgia Biomass Conversion to Activated Carbon and Electricity Danny Day, Eprida
  • 35.
  • 36.
  • 37. Charcoal works as an adsorption lattice for micro-organsism and nutrient particles Biochar soils FG
  • 38. 1 gramme of well-made charcoal will have an inner area of about 400 sq. meters Biochar soils FG
  • 39. Which means that one bag of barbeque char … will have an inner area of 1 sq. km! Biochar soils FG FG
  • 40. The plants seek contact with microorganisms Richard Haard, February 12, 2007 Charcoal after one year of application Biochar soils FG
  • 41. Charcoal is sought out by soil micro-organism Charcoal addition to the soil provides nutrient and water storage for mycorrhizal fungi Their hyphae invade charcoal pores and support spore reproduction Ogawa Kansai Environmental Fungi on New Char Fungi on 100 Yr Old Char Biochar soils FG
  • 42.
  • 43.
  • 44. Humic acids (there are plenty!) FG
  • 45. Complex of humic acids FG
  • 47. Oxisol (normal rain- forest soil) Terra Preta ( anthrosol : charcoal enriched oxisol, made by human activities) FG FG
  • 48.
  • 49. If you want to emit net carbon dioxide: Situation of today :
  • 50. And you must buy an emission permit You have to pay a tax FG
  • 51. Tax and permit fund $ P ayment P ermission E mission The PPE Model (currently used) The economist solution: Climate problems from approved carbon dioxide! FG
  • 52.
  • 54. Probably not The arguments don’t speak to our immediate self-interest FG
  • 55. To really get people’s attention , you have to talk money FG
  • 56. What about a fair carbon tax? FG
  • 57.
  • 58.

Editor's Notes

  1. We are now implementing a 1000 hour demonstration at the University of Georgia’s Bioconversion Research facility. In addition to producing hydrogen rich syn-gas, we will also be producing about 5 tons of a special type of charcoal.
  2. We are now implementing a 1000 hour demonstration at the University of Georgia’s Bioconversion Research facility. In addition to producing hydrogen rich syn-gas, we will also be producing about 5 tons of a special type of charcoal.
  3. Charcoal has been shown to provide nutrients to fungi.