[permaculture] Soil Carbon Sequestration

Charles de Matas cdematas at hotmail.com
Tue Jul 10 12:26:53 EDT 2007


[Sending this again, sorry for any duplication.  Charles]

Yoeman seems to think nuclear is necessary also, which I don't agree with.
  I agree with Paul's statement: "I would suggest that the alt. ag. methods 
resulted in a recovery of soil organic matter, but that regeneration to 
forest would have provided a greater rate."
  To sequester enough CO2 in the soil we would have to completely reverse 
deforestation worldwide.  Wetlands and tropical forests that have high 
rainfall would have to be completely protected for human activity.  I don't 
see any signs of this happening soon.
   Anyway here is the passage for Dr Young’s book.



<<<<<<<<<<<<<<<<<<<<<<<<<<<<<<<<
                Agroforestry and the greenhouse effect
It has been suggested that the wider adoption of agroforestry could help to 
reduce the build-up of atmospheric carbon dioxide and other ‘greenhouse 
gases’ (Dixon et al. 1994; Schroeder, 1994; Dixon, 1995, 1996). Possible 
means by which such a reduction could come about are:
-	taking up carbon into trees on farms;
-	increasing soil carbon;
-	indirectly, by reducing pressure for forest clearance.
Widespread adoption of the growing of more trees on farms would lead to a 
temporary increase in carbon storage, followed by its maintenance at the 
higher level. The same changes would follow increases in soil organic matter 
brought about by the adoption of agroforestry. Potential changes of this 
kind are, however, small in relative magnitude.  Soils are the largest pool 
of terrestrial carbon, estimated at 2200 Bt (billion tonnes=10^9 tonnes) in 
the top 100cm.  Of this total, 1500 Bt is organic carbon and 700 Bt is in 
the form of carbonates; about one-third is in the tropics.  An estimated 900 
Bt is in topsoils, 0-30 cm (Batjes, 1996). Let it be supposed that a very 
widespread adoption of agroforestry and other methods of improved soil 
management in the tropics led to a relative increase in topsoil carbon of 
10%.  Since tropical soils contain only 280/2200 or 13% of world soil 
carbon, this relative change would amount to a relative increase in soil 
carbon storage of about 1%.  The contribution from the temperate zone would, 
on a realistic assessment of current potential for adoption, be very much 
smaller.  The effect of agroforestry in raising soil organic-matter levels 
is therefore in the right direction in this respect, but small in relative 
magnitude.
	The indirect effects through the other environmental means noted above can 
be very much greater.  In particular, through reducing land pressure and 
thus forest clearance, it can help to reduce a major source of carbon 
dioxide emissions. Taking the same assumptions on agroforestry and forest 
clearance as made above, the potential for a reduction of forest clearance 
by 5 Mha/year would lead to a lowering of carbon emissions from forest 
burning from 1.6 to 1.1 Bt/year (Dixon, 1995).  The assumptions on which 
this estimate is made are very optimistic, but sufficient to show that a 
contribution of significance is possible.
>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>
Batjes, N.H. (1996) Total carbon and nitrogen in the soils of the world. 
European Journal of Soil Science 47, 151-163.
Dixon, R.K. (1995) Agroforestry systems: sources or sinks of greenhouse 
gases? Agroforestry systems 31, 99-116
Dixon, R.K. (1996) Agroforestry systems and greenhouse gases.  Agroforestry 
Today 8(1), 11-14.
Dixon, R.K., Winjum, J.K., Andrasco, K.J. et al. (1995) Integrated land use 
systems… Climatic Change 30, 1-23.
Schroeder, P. (1994) Carbon storage benefits of agroforestry systems. 
Agroforestry Systems 27, 89-97.

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