It doesn’t need to be one-time, if you add fine olivine grains to the soil. 
Helps to give poor acid soils a healthy pH, and provides magnesium at the same 
time (most important metal in chlorophyll), Olaf Schuiling

From: [email protected]<mailto:[email protected]> 
[mailto:[email protected]] On Behalf Of David desJardins
Sent: donderdag 12 februari 2015 17:25
To: Fred Zimmerman; [email protected]<mailto:[email protected]>
Cc: [email protected]<mailto:[email protected]>; 
[email protected]<mailto:[email protected]>; 
[email protected]<mailto:[email protected]>; geoengineering
Subject: Re: [geo] A closer look at the flawed studies behind policies used to 
promote 'low-carbon' biofuels | University of Michigan News

Certainly there's no question that we could have a big one-time (but large even 
though it's one-time) removal of carbon from the atmosphere if we convert large 
land areas from agriculture to be optimized carbon sinks.

But if you want to use currently-agricultural land to remove carbon from the 
atmosphere, then it's probably even better to grow trees and cut those trees 
down and bury them and do that over and over again every 10-20 years, than to 
convert the land to a carbon-dense biome?  That gives you ongoing carbon 
removal, not just a one-time effect.

On Thu Feb 12 2015 at 8:16:40 AM Fred Zimmerman 
<[email protected]<mailto:[email protected]>> wrote:
A couple of weeks ago Greg Rau shared a Jan. 30 article from Science that 
discussed the difficulty of accurately characterizing biomes (land use/land 
cover maps are not perfect) and the pitfalls in targeting particular biomes for 
interventions.
[Image removed by sender.]ᐧ

On Thu, Feb 12, 2015 at 10:56 AM, Aines, Roger D. 
<[email protected]<mailto:[email protected]>> wrote:
That seems like the important argument, John. Are there any simple metrics
we can use to think about the best way to optimize soil carbon in a
particular biome?  And, are there realistic totals that we could say those
optimized situations represent in the US, or even the world?


--
Roger D. Aines

Fuel Cycle Innovations Program Leader

E Programs, Global Security

Lawrence Livermore National Laboratory

Mail Stop L-090  Livermore, CA 94551

925 423-7184<tel:925%20423-7184>
925 998-2915<tel:925%20998-2915> cell



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Michelle Herawi [email protected]<mailto:[email protected]>

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On 2/12/15 7:49 AM, "John Harte" 
<[email protected]<mailto:[email protected]>> wrote:

>Remember: forests = trees + soil + microbes +Š  Much of the carbon is in
>the soil and converting meadow/grasslands/prairie to some kinds of forest
>or woody shrubland can result in net carbon loss even as the woody plants
>grow.  World wide 4 or 5 times as much carbon in soil as in all living
>biomass.
>
>
>John Harte
>Professor of Ecosystem Sciences
>ERG/ESPM
>310 Barrows Hall
>University of California
>Berkeley, CA 94720  USA
>[email protected]<mailto:[email protected]>
>
>
>
>On Feb 12, 2015, at 6:37 AM, "Robert H. Socolow" 
><[email protected]<mailto:[email protected]>>
>wrote:
>
>> Many second-growth forests are still increasing their carbon stocks. I
>>think that's the argument being made.
>>
>> Sent from my iPhone
>>
>>> On Feb 11, 2015, at 7:38 PM, David desJardins 
>>> <[email protected]<mailto:[email protected]>>
>>>wrote:
>>>
>>> forest has to be carbon-balanced, it isn't removing net carbon from
>>>the atmosphere but essentially all of the carbon taken up by plants
>>>eventually gets returned to the atmosphere when those
>>
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