Olaf,

 

You’ve likely explained this, but what grain size distribution does $2/ton 
provide?  Maybe you already have a trade-off table listing $__/ton for various 
grain sizes.

 

With such a table, you could make optimization analysis on ways to make the 
reaction faster.  For example (hypothetical numbers needing research): Maybe 
the $2/ton size takes 1,000 years to react with the atmosphere if stored in a 
desert.  Maybe the $2/ton size takes 10 years to react on average when placed 
less than 1 meter thick on a salt water beach with __ average wave size.  Maybe 
the $2/ton size takes a day to react in a fluidized bed reactor inside a 
geosynthetic membrane with seawater containing 50,000 ppm CO2 at 500 meters 
depth. 

 

Mark

 

From: [email protected] [mailto:[email protected]] 
On Behalf Of Schuiling, R.D. (Olaf)
Sent: Thursday, August 24, 2017 6:23 AM
To: '[email protected]' <[email protected]>; geoengineering 
<[email protected]>
Cc: Arnold van Ittersum ([email protected]) <[email protected]>
Subject: RE: [geo] Slicing the pie: how big could carbon dioxide removal be? - 
Psarras - 2017 - Wiley Interdisciplinary Reviews: Energy and Environment - 
Wiley Online Library

 

What an utter nonsense to think that CO2 capture and removal by mining, milling 
and spreading olivine would cost  in the order of 100 US$ per ton. If you don’t 
know anything of mining and mining cost, don’t come up with confusing and 
ridiculous guesswork. There are many olivine massifs on every continent and in 
many countries. Mining is from open pits (at a cost of 4 US$ per ton), and 
milling adds another 2 US$. These numbers are from reliable mining engineers. 
Every ton of olivine removes somewhat more than 1 ton of CO2 from the 
atmosphere. And, because there are hundreds of times more tons of olivine are 
available, in principle can the spreading of milled olivine solve the whole CO2 
problem, as it is scalable to any desired scale, and usually has additional 
advantages as well, Olaf Schuiling

 

From: [email protected] <mailto:[email protected]>  
[mailto:[email protected]] On Behalf Of Andrew Lockley
Sent: donderdag 24 augustus 2017 11:27
To: geoengineering
Subject: [geo] Slicing the pie: how big could carbon dioxide removal be? - 
Psarras - 2017 - Wiley Interdisciplinary Reviews: Energy and Environment - 
Wiley Online Library

 

http://onlinelibrary.wiley.com/doi/10.1002/wene.253/full

 



Slicing the pie: how big could carbon dioxide removal be?


Authors


*         Peter Psarras,


1.        


*         Holly Krutka,


*         Mathilde Fajardy,


1.        


*         Zhiqu Zhang,


1.        


*         Simona Liguori,


1.        


*         Niall Mac Dowell,


1.        


*         Jennifer Wilcox


o     

2.        

o     

*         First published:28 July 2017 
<http://onlinelibrary.wiley.com/doi/10.1002/wene.253/full#publication-history> 
Full publication history

*         DOI:10.1002/wene.253   
<http://onlinelibrary.wiley.com/enhanced/exportCitation/doi/10.1002/wene.253> 
View/save citation

*         Cited by (CrossRef):0 articles 
<http://onlinelibrary.wiley.com/enhanced/refreshCitedBy?doi=10.1002/wene.253&refreshCitedByCounter=true>
 Check for updates

Citation tools

*          

*         Conflict of interest: The authors have declared no conflicts of 
interest for this article.


Abstract


The current global dependence on fossil fuels to meet energy needs continues to 
increase. If a 2°C warming by 2100 is to be prevented, it will become important 
to adopt strategies that not only avoid CO2 emissions but also allow for the 
direct removal of CO2 from the atmosphere, enabling the intervention of climate 
change. The primary direct removal methods discussed in this review include 
land management and mineral carbonation in addition to bioenergy and direct air 
capture with carbon capture and reliable storage. These methods are discussed 
in detail, and their potential for CO2 removal is assessed. The global upper 
bound for annual CO2removal was estimated to be 12, 10, 6, and 5 GtCO2/year for 
bioenergy with carbon capture and reliable storage (BECCS), direct air capture 
with reliable storage (DACS), land management, and mineral carbonation, 
respectively—giving a cumulative value of ~35 GtCO2/year. However, in the case 
of DACS, global data on the overlap of low-emission energy sources and reliable 
CO2storage opportunities—set as a qualification for DAC viability—were 
unavailable, and the potential upper bound estimate is thus considered 
conservative. The upper bounds on the costs associated with the direct 
CO2removal methods varied from approximately $100/tCO2 (land management, BECCS, 
and mineral carbonation) to $1000/tCO2 for DACS (again, these are the upper 
bounds for costs). In this review, these direct CO2 removal technologies are 
found to be technically viable and are potentially important options in 
preventing 2°C warming by 2100. WIREs Energy Environ 2017, 6:e253. doi: 
10.1002/wene.253

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