Greg and ccs: 

This is partly to support your concern about Direct Air Capture (DAC), since we 
are hearing only part of the O&M portion of costs. We need to hear more, but I 
believe the $100/ton CO2 number (likely equivalent to about $300/ton of 
charcoal) is encouragingly lower than what we have heard before - and we should 
be pleased to hear of cost reductions, even though this is still a large 
number. 

But I am mostly asking how you calculate the "...in gross some 700+ GT of air 
CO2 capture/yr naturally going on..." . If I divide by 3.67 for molecular 
weight differences, you are talking about 190 Gt C/yr. I often see a number 
around 60 Gt C/yr for both land-based and ocean based photosynthetic removal 
(of course mostly balanced by an annual return of about the same amount). But 
this presumably leaves (190-2*60=) 70 Gt C for some two-way annual ocean 
process? 

I'd like to hear your thoughts on the realistic net (not gross) removals that 
society might be able to achieve in say 2050 and 2100. 

I personally am hoping for new massive forest tree-planting to get us from 60 
Gt C/yr up to 70. Then perhaps 5 of this added annual 10 can be harvested, 
leaving 5 for new added global standing biomass stock. The new annual 
harvestable 5 can be added to another 5 from today's already dying 60 (5/60=8% 
= new added human appropriation of the existing 60 Gt C/yr). Of this new 
available 5+5 =10, about half could be assigned to carbon-negative Biochar and 
half to carbon-neutral biofuels/biopower (2.5 Gt C/yr each). This would mean 
than about 1/6 of the total of 15 is being used primarily as backup for other 
(PV wind) sources of thermal and electric energy. This leaves considerable need 
for other forms of energy storage. Having only 2.5 Gt C/yr for biofuels, will 
greatly drop today's liquid/transportation portion of the total global energy 
budget - but 25% of annual biomass supply is all we can spare if we are serious 
about carbon negativity. 

In the above, I am imagining a scenario where there are no fossil fuels and the 
non-biomass RE sources are contributing about 10 Gt C/yr of fossil-replacement 
value. In other words- a total global energy equivalent of about 15 Gt C/yr - 
about twice today's fossil input, but now fossil-fuel-free.. I recognize this 
is aggressive and probably impossible. But I am projecting at only about 7 % 
(=15/190) of your 190 Gt C/yr "naturally going on". If we can achieve this new 
added harvest of 10 GtC/yr at a rate of 10 tonnes per hectare-yr (same as 1 
kg/sqm-yr), then we need about 1 Gha - or 10 percent of the available arable 
land (including some off-shore resource - as is included in the computations at 
the Global Footprint Network (GFN). 

What alternative scenario would you propose to best exploit your 190 Gt C/y - 
to get CO2 down to 350 ppm soon? 

Thanks for giving the opportunity to be more scenario-oriented on this list. 

Ron 
----- Original Message -----
From: "Greg Rau" <[email protected]> 
To: "andrew lockley" <[email protected]>, "geoengineering" 
<[email protected]> 
Sent: Thursday, July 26, 2012 3:17:59 PM 
Subject: RE: [geo] Air capture: Modification of the Mg/DOBDC MOF with Amines to 
Enhance CO2 Adsorption from Ultradilute Gases 

Thanks, Andrew, for the recent updates on DAC. I remain puzzled, however, by 
the continuing interest in artificial air CO2 capture when we've got in gross 
some 700+ GT of air CO2 capture/yr naturally going on, in net consuming 55-60% 
of our CO2 emissions. Contrary to one of the articles*, air capture is not a 
"concept", it's what is currently saving our bacon right now. Wouldn't it make 
a lot more sense (and save a lot of cents) figuring out how to enhance/exploit 
these natural CO2 absorption and conversion processes (e.g, BECCS, CROPS, ocean 
alkalization, enhance mineral weathering, etc.) rather than trying to reinvent 
the wheel from the ground up, competing on a cost basis with what nature 
already does for free? How about investing in improving on the global scale 
"engineering" that's already in place? 
Regards, 
Greg 

*http://pubs.acs.org/doi/abs/10.1021/ie300691c?prevSearch=air%2Bcapture&searchHistoryKey=
 
________________________________________ 
From: [email protected] [[email protected]] On 
Behalf Of Andrew Lockley [[email protected]] 
Sent: Wednesday, July 25, 2012 11:59 AM 
To: geoengineering 
Subject: [geo] Air capture: Modification of the Mg/DOBDC MOF with Amines to 
Enhance CO2 Adsorption from Ultradilute Gases 

http://pubs.acs.org/doi/abs/10.1021/jz300328j 

Modification of the Mg/DOBDC MOF with Amines to Enhance CO 2 Adsorption from 
Ultradilute Gases 

Sunho Choi, Taku Watanabe, Tae-Hyun Bae, David S. Sholl, Christopher W. Jones 

J. Phys. Chem. Lett., 2012, 3 (9), pp 1136–1141 DOI: 10.1021/jz300328j 

The MOF Mg/DOBDC has one of the highest known CO 2 adsorption capacities at the 
low to moderate CO 2 partial pressures relevant for CO 2 capture from flue gas 
but is difficult to regenerate for use in cyclic operation. In this work, 
Mg/DOBDC is modified by functionalization of its open metal coordination sites 
with ethylene diamine (ED) to introduce pendent amines into the MOF micropores. 
DFT calculations and experimental nitrogen physisorption and thermogravimetric 
analysis suggest that 1 ED molecule is added to each unit cell, on average. 
This modification both increases the material’s CO 2 adsorption capacity at 
ultradilute CO 2 partial pressures and increases the regenerability of the 
material, allowing for cyclic adsorption–desorption cycles with identical 
adsorption capacities. This is one of the first MOF materials demonstrated to 
yield significant adsorption capacities from simulated ambient air (400 ppm CO 
2 ), and its capacity is competitive with the best-known adsorbents based on 
amine–oxide composites. 

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