Mg-rich silicates (chlorite, augite) were the main minerals affected by the experimental weathering design employed in this study, an observation that is consistent with field-based observations of mafic rocks in weathering environments. Weathering fluxes for chlorite and augite approximately double from sand-sized (∼250–500 m) to silt-sized (<45 m), and this has implications for forecasting potential for carbon dioxide reduction (CDR) by means of enhanced rock weathering (ERW) of basaltic powders applied to fields as a negative emission technology (NET). In particular, CDR rates vary by a factor of two, ranging from fine-medium sand of BR and PV basaltic powders (3–4 t/ha/yr), compared to a rate of 6–7 t/ha/yr for fine-medium silt."
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Small grain size is crucial for rapid dissolution, but there are tradeoffs as it is much more expensive to crush rocks to fine grain size!
Remineralize The Earth https://www.remineralize.org/ is the global NGO promoting use of rock powders, biochars, and sea salts as natural, slow-release, chemically balanced fertilizers that last decades, and is involved in developing applications for agriculture to promote rapid growth of healthy biomass, food, pastures, and forests around the world.
The carbon benefits naturally result, but a healthier, chemically-balanced, ecosystem with higher biomass, biodiversity, and ecosystem services is the goal, not simply dissolving chemicals where they serve no useful function, as seems to be the case with those only interested in peddling carbon credits to the fossil fuel producers who have driven coral reefs to imminent extinction. For this reason RTE promotes use of grain sizes that are not too small, as these clog the pores in soils and prevent water infiltration and CO2 and O2 exchange between soil air and the atmosphere.
Rock powders and biochar should always be used together because they synergistically increase each other’s fertilization and water storage effects see:
RTE and the Geological Survey of India have recently published a major paper on how the world’s largest country by population, India, can use its own geological resources to feed itself, with the carbon benefits being ancillary. Please see:
I A. Mir, T J F. Goreau, J. Campe, J. Jerden, 2024, India's biogeochemical capacity to attain food security and remediate climate: a review, Environmental Geochemistry and Health, 46:17, https://rdcu.be/duxoV
RTE works with many groups around the world to develop these applications, especially in Brazil, which is the world’s largest user of rock powders to replace expensive, unbalanced, short-lasting, imported chemical fertilizers. Brazilian researchers are world leaders in this field. RTE is working with Tanzania Engineers Without Borders to produce natural material fertilizers from volcanic rocks near Mount Kilimanjaro, local biochar, and compost, and to increase the water holding capacity and fertility of soils in the Panama Canal watershed, among other projects. These applications are covered in a 600 page book:
Geotherapy: Innovative Methods of Soil Fertility Restoration, Carbon Sequestration, and Reversing CO2 Increase
http://www.crcpress.com/product/isbn/9781466595392
Thomas J. F. Goreau, PhD
Scientific Advisor, Remineralize The Earth
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I don’t think the dissolution rate of minerals in the alkaline ocean is nearly as fast as these proponents assume and require, and the trays would vanish in the first storm.
I was a student of the geochemistry pioneers who measured the dissolution rates of all the major silicate minerals. They used finely ground powders in heated flasks constantly spinning with magnetic stirrers in order to jack up the dissolution rate to be able to measure the silica and metals released to solution. Many added acid to speed it up. Then they extrapolated their results back to rates at surface temperature and acidity. If they had just dumped a rock in a flask without grinding, heating, and stirring, they would have had to have their great grandchildren make the measurements, and would not have gotten tenure!
By far the best way to weather rock powders is not in the ocean but in soil penetrated by tree roots constantly releasing CO2 and organic acids and metal chelating agents at a far faster rate than the diffusion from the air that rock weathering proponents are counting on. In the 1970s I built soil probes to measure the vertical profile of CO2 and N2O in soil, and found it is much higher than in the atmosphere, sometimes thousands of ppm, depending on soil organic carbon content.
The best way to dissolve rock is growing plants in it! Dick Holland measured the rate of weathering of Iceland basalt, and found it weathered many times faster if the rock surface was vegetated. The Soil is not a sink of atmospheric CO2, it is a source, but largely recycled via fast root respiration, and slow decomposition.
The other reason dumping rock powder in the water won’t be very effective is that even if it all actually dissolves, ocean alkalinity has a 100,000 year residence time, so it takes impossible amounts of rock dissolution to make a significant difference, it’s pissing into the wind.
Thomas J. F. Goreau, PhD
President, Global Coral Reef Alliance
Chief Scientist, Blue Regeneration SL
President, Biorock Technology Inc.
Technical Advisor, Blue Guardians Programme, SIDS DOCK
37 Pleasant Street, Cambridge, MA 02139
gor...@globalcoral.org
www.globalcoral.org
Skype: tomgoreau
Tel: (1) 617-864-4226 (leave message)
Books:
Geotherapy: Innovative Methods of Soil Fertility Restoration, Carbon Sequestration, and Reversing CO2 Increase
http://www.crcpress.com/product/isbn/9781466595392
Innovative Methods of Marine Ecosystem Restoration
http://www.crcpress.com/product/isbn/9781466557734
Geotherapy: Regenerating ecosystem services to reverse climate change
No one can change the past, everybody can change the future
It’s much later than we think, especially if we don’t think
Those with their heads in the sand will see the light when global warming and sea level rise wash the beach away
“When you run to the rocks, the rocks will be melting, when you run to the sea, the sea will be boiling”, Peter Tosh, Jamaica’s greatest song writer
From:
ishfaq ahmad <geoi...@gmail.com>
Date: Sunday, March 10, 2024 at 1:57 AM
To: Tom Goreau <gor...@globalcoral.org>
Cc: Joanna Campe <joanna...@gmail.com>, jje...@metamorphic1.org <jje...@metamorphic1.org>, Thomas Vanacore <ston...@gmavt.net>
Subject: Re: FYI: [CDR] Optimal grain size of powdered basalt/olivine for enhanced weathering?
How beneficial it would be to utilise buoyant fabric trays with fine rock dust disseminated and kept floating in tropical oceans for the best results of reacting with ocean water without sinking for the best outcomes of weathering, carbon capturing, and moving down the ocean.
On Sun, Mar 10, 2024 at 2:54 AM Tom Goreau <gor...@globalcoral.org> wrote:
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Bear in mind that rock crushing plants produce gravel to mix into Portland cement or asphalt, and the fine powders we use as a natural, slow-release, long-lasting, nutrient balanced fertilizers are the waste products of crushing, what they bulldoze to the side, and is therefore free. It would not be economically worthwhile to ground basalt to agricultural size as a primary product without a much higher price.
Rock fragmentation speeds weathering up, but primary chemical weathering soils from even fairly small broken rocks typically takes thousands of years to form clay soils (such as rock scree fragments frost-cracked off mountain cliffs that fall into moraine lakes at their base).
The faster you can get life to grow on it the faster it will dissolve.
This takes a long time by itself, but can be kickstarted by adding biochar, compost and inoculation with beneficial bacterial and fungal cultures to the cracks in the basalt. Biogeochemically enhanced soil formation in years to decades will greatly accelerate carbon sequestration.
Under such conditions the best carbon farmers can draw down up to 40 TC/Ha/yr. Unfortunately the average global farming is not enriching their soil carbon but systematically depleting it and putting it into the atmosphere.
If all farmers followed best carbon farming practices there would be globally significant drawdown!
The CDR time scales to reduce CO2 to safe Preindustrial levels (280 ppm) for the spectrum of soil carbon increase rates and for the proportion of long lived soil carbon (biochar) are shown graphically in my poster at the UN Food and Agriculture Organization Conference on Soil Organic Carbon attached.
Thomas J. F. Goreau, PhD
President, Global Coral Reef Alliance
Chief Scientist, Blue Regeneration SL
President, Biorock Technology Inc.
Technical Advisor, Blue Guardians Programme, SIDS DOCK
37 Pleasant Street, Cambridge, MA 02139
gor...@globalcoral.org
www.globalcoral.org
Skype: tomgoreau
Tel: (1) 617-864-4226 (leave message)
Books:
Geotherapy: Innovative Methods of Soil Fertility Restoration, Carbon Sequestration, and Reversing CO2 Increase
http://www.crcpress.com/product/isbn/9781466595392
Innovative Methods of Marine Ecosystem Restoration
http://www.crcpress.com/product/isbn/9781466557734
Geotherapy: Regenerating ecosystem services to reverse climate change
No one can change the past, everybody can change the future
It’s much later than we think, especially if we don’t think
Those with their heads in the sand will see the light when global warming and sea level rise wash the beach away
“When you run to the rocks, the rocks will be melting, when you run to the sea, the sea will be boiling”, Peter Tosh, Jamaica’s greatest song writer
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Tom, what I'm wondering is what could be achieved with a brute-force method of applying rock crushing machinery to turn a cubic km of basalt rock into rock powder of a suitable average grain size (and I am wondering what that grain size would optimaly be: 0.1 mm? 0.3 mm? 0.5 mm?).
I have no idea how much CO2 could be soaked up and sequestered per ton of crushed basalt powder at a given grain size.
I've been trying to find out via Google scholar searches, and so far not having much luck.
Let me arbitrarily assume (pulling a number out of the ether) of 2 tons of crushed basalt powder of some grain size n, where n is perhaps more than 0.1 mm but less than 0.5 mm. I want those damn numbers, because I can then also find out what input of electricity will be necessary per ton of basalt and hence per ton of CO2, after combining the energy required to crush basalt down to the desired grain size, and also to mix the crushed basalt with biochar and transport it to suitable fields in EV trucks, and spread it on the land at suitable density.
I cannot work out these numbers on my own. I'll need input from people who have actual experience in doing this kind of thing in the field.There are regions of the world where there is plentiful stranded geothermal energy co-located with plentiful basalt. Some of that energy could be harvested to run rock crushers and biochar ovens and biochar/rock powder mixing facilities.
How big a mountain, in cubic km, would be required to draw down one trillion GtCO2?
How many TWh of electricity would be required?
And how much land would be required to draw down one trillion GtCO2 over (say) twenty years via basaltic rock powder EW?
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Cation release, like alkalinity, is a measure of CO2 consumption by weathering, but both are complicated by secondary reactions and formation of clay minerals.
Tom Vanacore knows much more about crushing costs and availability of fine rock powder “waste” material, and optimal sizes, which depend on the soil type and application.
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There’s no time frame on the graph?
Shouldn’t pH be going up if CO2 is being neutralized by weathering?
From:
Chris Harding <littl...@gmail.com>
Date: Monday, March 11, 2024 at 11:35
AM
To: Chris Van Arsdale <cvana...@google.com>
Cc: Jasper Sky <jasp...@gmail.com>, Tom Goreau <gor...@globalcoral.org>, Michael Hayes <electro...@gmail.com>, CarbonDiox...@googlegroups.com <carbondiox...@googlegroups.com>, ishfaq ahmad <geoi...@gmail.com>, Joanna Campe <joanna...@gmail.com>,
jje...@metamorphic1.org <jje...@metamorphic1.org>, Thomas Vanacore <ston...@gmavt.net>
Subject: Re: [CDR] Optimal grain size of powdered basalt/olivine for enhanced weathering?
Should be mol instead of "mil" in PARM(1).
On Mon, Mar 11, 2024 at 8:27 AM Chris Harding <littl...@gmail.com> wrote:
Hello,
I am currently learning PHREEQC, and one could use this software to find the optimal particle size in my opinion. For example,
PARM(1) = specific surface area (m^2/mil) #PARMS defined in KINETICS block.
PARM(20 = Lab to field adjusted rate.
SR = Saturation Ratio250 rate = rate_H + rate_H2O + rate_OH + rate_CO2
260 area = PARM(1) * M0 *(M/M0)^0.67
270 rate = PARM(2) * area * rate * (1-SR("K-feldspar"))
280 moles = rate*TIME
It is a steep learning curve, but not as steep as OpenFOAM. Great documentation and UsersGroup.
As an example, I believe I solved the challenge problem. The below graph shows the effect of water advection through a column of 10 cells. The time frame was near 520,000 years for kinetics these specific feldspars. Note, there is a typo in the legend, but it is obvious.
I find this software could be very useful for enhanced weathering and how the chemistry in the soil is affected. As you can see here, with the setup[see attached file for code.]. The potassium feldspar dissolves, and albite dissolves along the column of cells. Since Na CL are apart of the solution, the extra Na and Ionic Strength as well as pH could be affecting the albite precipitation. It is not a graded problem but a "Challenge Problem" so I am awaiting Dr. McNab's remarks on my script, results, and analysis. I share it here as an example of what can be done. Much more capable than this. A good book to read that uses PHREEQC samples is[1].
References:
[1] Appelo, C., Postma, D. (2004). Geochemistry, Groundwater and Pollution. Netherlands: CRC Press.
.
Tony Lasaga was a graduate student with me. His numbers come from many papers.
For the pH to fall like that implies that albite formation releases many more protons than orthoclase dissolution releases. In any event, it won’t be converted to albite at surface conditions but to clays.
Once again, the slowest way to dissolve minerals, regardless of grain size, is to dump them in the ocean! The second slowest is to expose them to rain on land! The fastest way is to grow tree roots in it!
From:
Chris Harding <littl...@gmail.com>
Date: Monday, March 11, 2024 at 12:12 PM
To: Tom Goreau <gor...@globalcoral.org>
Cc: Chris Van Arsdale <cvana...@google.com>, Jasper Sky <jasp...@gmail.com>, Michael Hayes <electro...@gmail.com>, CarbonDiox...@googlegroups.com <carbondiox...@googlegroups.com>, ishfaq ahmad <geoi...@gmail.com>, Joanna Campe
<joanna...@gmail.com>, jje...@metamorphic1.org <jje...@metamorphic1.org>, Thomas Vanacore <ston...@gmavt.net>
Subject: Re: [CDR] Optimal grain size of powdered basalt/olivine for enhanced weathering?
The text file shows the time in seconds. Sorry.
Follow the advice of: PHREEQC Users | Resource for geochemists | Forum (Topic: Computation time for advection with kinetics ) to find "age" of water.
I used:
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Nor does their bogus mathematics take into account the vastly larger increased soil and biomass carbon storage, which multiplies the weathering sink many, many times over!
As my FAO abstract shows, good farmers add up to 40m TC/Ha/yr.
Sorry, typo 40 TC/Ha/yr, no m for millions unfortunately.
But that’s good enough to make a huge difference if farmers regenerated their own soil carbon instead of degenerating it!
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I said, UP TO 40 TC/Ha/yr as a best case scenario, but many farmers who regenerate their soil health are getting over 10 TC/Ha/yr, see the graph. These are real results based on soil carbon measurements, not guess calculations made by people who don’t understand soil carbon.
Also this is up to 40 TC/Ha/yr measured soil carbon increases!
4 tons of basalt per hectare will not dissolve and provide four tons of carbon alkalinity in one year as your calculation assumes.
It will take decades, to centuries, to millenia, to millions of years, depending on the setting.
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Biochar is not spread as a pure black surface layer except by the laziest.
Only a few percent are normally added, and to get the best effects it is mixed down into the soil, so that the albedo effect is minor.
The whitest soils, like quartz clays and kaolinite are practically barren of nutrients and are the slowest minerals to weather, almost nothing grows on them, so very little CDR benefit.
Limestone soils can hurt your eyes with reflection, but are severely deficient in all nutrients except calcium, and sometimes magnesium (if on dolomite). They are especially poor in nitrogen, because ammonium oxidizing bacteria just love high pH, and the nitrate is flushed into the groundwater and out to sea. In Jamaica marine groundwater springs have a dissolved nitrogen to phosphorus molar ratio of up to 600! The phosphorus retained in the soil is useless, immobilized as insoluble surface phases by calcite and by iron and aluminium oxides in soils. That’s why we have so many nitrogen fixing trees in Jamaica.
Mirrors may be a better bet than white powders for albedo for cooling, but no CDR benefit.
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On Mar 11, 2024, at 1:07 PM, Tom Goreau <gor...@globalcoral.org> wrote:
<LIfetimeOfMinerals.Laboratory.png>
<Module 6.Rates.Kinestics.Advection.jpg>
.
Measured CARBON increase in soil. NOT CO2!
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This is why I'm desperate to learn whether there is some way we could suspend basalt rock dust in the upper ocean for long enough for it to fully weather. Maybe put floating burlap sacks full of basalt rock powder (tied to buoys), or something like that. This would overcome the problem of EW requiring implausible amounts of land to achieve multiple-Gt-scale CO2 sequestration.
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