[geo] Geoengineering Lecture | HUCE

2013-02-07 Thread Andrew Lockley
http://environment.harvard.edu/events/2013-02-12/geoengineering-lecture

Geoengineering Lecture

Tuesday, February 12, 2013 - 5:00pm

Contact Name:  Lisa Matthews
matt...@fas.harvard.edu
Haller Hall, Geo Museum 102, 24 Oxford Street, Cambridge

Smoke and Mirrors:  Is Geoengineering a Solution to Global Warming?

with Alan Robock, Department of Environmental Sciences, Rutgers University

ABSTRACT: In response to the global warming problem, there has been a
recent renewed interest in geoengineering “solutions” involving “solar
radiation management” by injecting particles into the stratosphere,
brightening clouds, or blocking sunlight with satellites between the Sun
and Earth.  While volcanic eruptions have been suggested as innocuous
examples of stratospheric aerosols cooling the planet, the volcano analog
actually argues against geoengineering because of ozone depletion and
regional hydrologic responses.  In this talk, I describe different proposed
geoengineering designs, and then show climate model calculations that
evaluate both their efficacy and their possible adverse consequences.  No
such systems to conduct geoengineering now exist, but a comparison of
different proposed stratospheric injection schemes, using airplanes,
balloons, and artillery, shows that using airplanes to put sulfur gases
into the stratosphere would not be expensive.  Nevertheless, it would be
very difficult to create stratospheric sulfate particles with a desirable
size distribution.  Our GeoMIP project, conducting climate model
experiments with standard stratospheric aerosol injection scenarios, is
ongoing, but has already shown that temperature and precipitation responses
would be uneven globally.  If there were a way to continuously inject SO2
into the lower stratosphere, it would produce global cooling, stopping
melting of the ice caps, and increasing the uptake of CO2 by plants.  But
there are at least 26 reasons why geoengineering may be a bad idea.  These
include disruption of the Asian and African summer monsoons, reducing
precipitation to the food supply for billions of people; ozone depletion;
no more blue skies; reduction of solar power; and rapid global warming if
it stops.  Furthermore, the prospect of geoengineering working may reduce
the current drive toward reducing greenhouse gas emissions, there are
concerns about commercial or military control, and it may seriously degrade
terrestrial astronomy and satellite remote sensing.  Global efforts to
reduce anthropogenic emissions and to adapt to climate change are a much
better way to channel our resources to address anthropogenic global warming.

ABOUT THE LECTURE SERIES:

Solar geoengineering is the concept of deliberately cooling the Earth by
reflecting a small amount of inbound sunlight back into space. It is the
only currently known method for reducing temperatures in the short term
(years to decades), and therefore has the potential to reduce many of the
worst impacts of global warming. But what would be the side effects, both
physical and socio-political? How would it work and who gets to decide if
it is deployed?  Does humanity have the wisdom and the institutions to
govern the development of such a powerful technology in this messy,
multi-polar world? This seminar series, held jointly by the Harvard
University Center for the Environment (HUCE) and MIT’s Joint Program on the
Science and Policy of Global Change, will explore the science, technology,
governance and ethics of solar geoengineering. In bringing together
international experts, participants will learn some of the greatest
challenges and hear opinions on how this technology could and should be
managed.

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[geo] Re: Nickel nanoparticles catalyse reversible hydration of carbon dioxide for mineralization carbon capture and storage - Catalysis Science Technology (RSC Publishing)

2013-02-07 Thread lidijasiller

 With presence of Ni we have increases at the same time trapping of CO2 and 
increased the rates of conversion to carbonic acid on room temperature and 
on the atmospheric pressure.
We still working to find the best mineralisation pathway - we will use 
silicates (magnesium calcium silicates) as a source of Ca2+ or Mg2+.
 
While nickel nanoparticles are toxic as already mentioned in the paper we 
do not propose to spread this around in the enviroment but to have local 
disposal next to power plant or industrial plant.
We made brief cost - 8$ per ton of CO2 if we can recover Ni 99% yield based 
on current price of nickel.
 
 
 

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Re: [geo] Re: Nickel nanoparticles catalyse reversible hydration of carbon dioxide for mineralization carbon capture and storage - Catalysis Science Technology (RSC Publishing)

2013-02-07 Thread Rau, Greg
Thanks for responding.  I really don't follow this. If I have a beaker of water 
fully equilibrated with air (CO2) and add your Ni particles, you are saying 
that more HCO3- and ultimately CO3s will spontaneously be produced. This won't 
happen unless thermodynamically favored, and if that water if fully 
equilibrated with air CO2 there is no thermodynamic condition that will force a 
change in the C chemistry.  If your Ni particles are somehow consuming H+ or 
producing OH- then you've got a driving force, but you still need a source 
cations to make CaCO3s (am very interested to learn how you cheaply extract 
cations from silicates.)  Otherwise, adding a catalyst to a system at 
thermodynamic equilibrium does nothing.  On the other hand, adding something to 
seawater that overcomes the natural, chemical inhibition of abiotic CaCO3s 
precipitation could really cause some serious precipitation and CO2 injection 
into the atmosphere. No?
-Greg

From: lidijasil...@gmail.commailto:lidijasil...@gmail.com 
lidijasil...@gmail.commailto:lidijasil...@gmail.com
Reply-To: lidijasil...@gmail.commailto:lidijasil...@gmail.com 
lidijasil...@gmail.commailto:lidijasil...@gmail.com
Date: Thursday, February 7, 2013 8:32 AM
To: geoengineering 
geoengineering@googlegroups.commailto:geoengineering@googlegroups.com
Subject: [geo] Re: Nickel nanoparticles catalyse reversible hydration of carbon 
dioxide for mineralization carbon capture and storage - Catalysis Science  
Technology (RSC Publishing)


With presence of Ni we have increases at the same time trapping of CO2 and 
increased the rates of conversion to carbonic acid on room temperature and on 
the atmospheric pressure.
We still working to find the best mineralisation pathway - we will use 
silicates (magnesium calcium silicates) as a source of Ca2+ or Mg2+.

While nickel nanoparticles are toxic as already mentioned in the paper we do 
not propose to spread this around in the enviroment but to have local disposal 
next to power plant or industrial plant.
We made brief cost - 8$ per ton of CO2 if we can recover Ni 99% yield based on 
current price of nickel.




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Re: [geo] Re: Nickel nanoparticles catalyse reversible hydration of carbon dioxide for mineralization carbon capture and storage - Catalysis Science Technology (RSC Publishing)

2013-02-07 Thread lidijasiller
 
Yes there is a driving force - we see OH and HCO3 on surface of nickel 
particles . Due to large surface area of particles the Ni-HCO3 plays large 
part how much of CO2 in total can be stored in this system.
If you need a paper I can send you via my university account- 
lidia.sil...@ncl.ac.uk.
Regarding the mineralisation part we are working on this.

   o


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Re: [geo] Re: Nickel nanoparticles catalyse reversible hydration of carbon dioxide for mineralization carbon capture and storage - Catalysis Science Technology (RSC Publishing)

2013-02-07 Thread gaurav bhaduri
Dear Dr Rau,

Thank you for your response towards our research, I appreciate your 
comments on our work. To explain about the saturation experiments; we tried 
to saturate the CO2 within water and with and without the nanoparticles 
present in the system and found that there was more CO2 in the nanoparticle 
solution in that of pure water.We do not claim in the paper that we are 
getting CO3-- in our system at all. We have observed that the concentration 
of the acid in the nanoparticle solution is higher than that of pure water. 
We observed that here was HCO3- species on our nanoparticle surface and the 
possible explanation (for this increase) we suggested was that there might 
me adsorption of HCO3- ions (from the acid) on the nanoparticle surface. As 
all this is happening at a pH in the acidic range (5) thus according to 
chemistry of CO2 in water at this pH range there is acid system and none of 
the basic system of bicarbonates or carbonates exist.

As mentioned by Dr Siller, previously we are yet experimenting on the 
method of carbonate mineral formation with; possibly silicate sources. 

We do not tend to use sea water or oceanic system in our work at all. The 
idea to use Nickel for this reaction was taken from the sea urchin studies 
conducted by Dr Siller and other my other colleagues. We do not dump 
anything into the sea or use the oceanic system into the process. We 
suggest using a mineral source (terrestrial) for the metal ion (Ca2+ or 
Mg2+) to form corresponding mineral carbonate. The concept is to use it as 
a satellite unit for point source emission (power plants for example) 
trapping. 

On Thursday, 7 February 2013 18:49:41 UTC, Greg Rau wrote:

  Thanks for responding.  I really don't follow this. If I have a beaker 
 of water fully equilibrated with air (CO2) and add your Ni particles, you 
 are saying that more HCO3- and ultimately CO3s will spontaneously be 
 produced. This won't happen unless thermodynamically favored, and if that 
 water if fully equilibrated with air CO2 there is no thermodynamic 
 condition that will force a change in the C chemistry.  If your Ni 
 particles are somehow consuming H+ or producing OH- then you've got a 
 driving force, but you still need a source cations to make CaCO3s (am 
 very interested to learn how you cheaply extract cations from silicates.) 
  Otherwise, adding a catalyst to a system at thermodynamic equilibrium does 
 nothing.  On the other hand, adding something to seawater that overcomes 
 the natural, chemical inhibition of abiotic CaCO3s precipitation could 
 really cause some serious precipitation and CO2 injection into the 
 atmosphere. No?
 -Greg
  
   From: lidija...@gmail.com javascript: lidija...@gmail.comjavascript:
 
 Reply-To: lidija...@gmail.com javascript: 
 lidija...@gmail.comjavascript:
 
 Date: Thursday, February 7, 2013 8:32 AM
 To: geoengineering geoengi...@googlegroups.com javascript:
 Subject: [geo] Re: Nickel nanoparticles catalyse reversible hydration of 
 carbon dioxide for mineralization carbon capture and storage - Catalysis 
 Science  Technology (RSC Publishing)
  
  
  With presence of Ni we have increases at the same time trapping of CO2 
 and increased the rates of conversion to carbonic acid on room temperature 
 and on the atmospheric pressure.
  We still working to find the best mineralisation pathway - we will use 
 silicates (magnesium calcium silicates) as a source of Ca2+ or Mg2+.
  
 While nickel nanoparticles are toxic as already mentioned in the paper we 
 do not propose to spread this around in the enviroment but to have local 
 disposal next to power plant or industrial plant.
 We made brief cost - 8$ per ton of CO2 if we can recover Ni 99% yield 
 based on current price of nickel.
  
  
  

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[geo] Sooty ships may be geoengineering by accident - 06 February 2013 - New Scientist

2013-02-07 Thread Andrew Lockley
Posters note : Ships apparently 'geoengineering' with iron as well as
sulfur. Where would we be without them?

http://www.newscientist.com/article/mg21729035.100-sooty-ships-may-be-geoengineering-by-accident.html
?

Sooty ships may be geoengineering by accident

06 February 2013 by Jeff Hecht

Magazine issue 2903.

GEOENGINEERING is being tested - albeit inadvertently - in the north
Pacific. Soot from oil-burning ships is dumping about 1000 tonnes of
soluble iron per year across 6 million square kilometres of ocean, new
research has revealed.Fertilising the world's oceans with iron has been
controversially proposed as a way of sucking carbon dioxide out of the
atmosphere to curb global warming. Some geoengineers claim releasing iron
into the sea will stimulate plankton blooms, which absorb carbon, but ocean
processes are complex and difficult to monitor in tests.Experiments
suggest you change the population of algae, causing a shift from
fish-dominated to jellyfish-dominated ecosystems, says Alex Baker of the
University of East Anglia, UK. Such concerns led the UN Convention on
Biological Diversity (CBD) to impose a moratorium on geoengineering
experiments in 2010.The annual ship deposition is much larger, if less
concentrated, than the iron released in field tests carried out before the
moratorium was in place. Yet because ship emissions are not intended to
alter ocean chemistry, they do not violate the moratorium, says Jim Thomas
of the ETC Group, a think tank that consults for the CBD. If you
intentionally drove oil-burning ships back and forth as a geoengineering
experiment, that would contravene it.The new study, by Akinori Ito of
the Japan Agency for Marine-Earth Science and Technology, is the first to
quantify how shipping deposits iron in parts of the ocean normally
deficient in it. Earlier models had assumed that only 1 to 2 per cent of
the iron contained in aerosols, including shipping emissions, is soluble in
seawater, so the remaining 98 to 99 percent would sink to the bottom
without affecting ocean life. But Ito found that up to 80 per cent of the
iron in shipping soot is soluble (Global Biogeochemical Cycles, doi.org/kdj).
As this soot rapidly falls to the sea surface, it is likely to be
fertilising the oceans.In the high-latitude north Pacific - a region that
is naturally iron-poor and therefore likely to be most affected by human
deposits - ship emissions now account for 70 per cent of soluble iron from
human activity, with the burning of biomass and coal accounting for the
rest. Shipping's share will rise as traffic continues to grow and
regulations restrict coal and biomass emissions.Can we learn anything from
this unintentional experiment? Baker thinks not. The process isn't
scientifically useful, he says, because the uncontrolled nature of the
iron makes it difficult to draw meaningful comparisons.The depositions are
unlikely to be harmful at current levels, he says, but given the
uncertainties, I just don't know how much these iron emissions would have
to increase before there was demonstrable harm to an ecosystem, or benefit
in terms of carbon uptake, for that matter.

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Re: [geo] Re: Nickel nanoparticles catalyse reversible hydration of carbon dioxide for mineralization carbon capture and storage - Catalysis Science Technology (RSC Publishing)

2013-02-07 Thread gaurav bhaduri
Dear all

Thank you for your interest in our work and your comments. To clarify some 
of the misunderstanding in the process conditions that I'd like to clarify. 
When we bubble CO2 in water with and without the nanoparticles, we observed 
that there is more CO2 in the nanoparticle system than in pure water. We 
also observed that there was HCO3- ions on the surface of the Ni 
nanoparticles surface, we thus explained that this enhancement could be due 
to adsorption of the HCO3- (from the acid) onto the Ni surface. We in no 
place claim the formation of CO3-- ions, to be clear on this point the 
system we are addressing in this article is at a acidic pH (5). Thus there 
is only carbonic acid species present no bicarbonate or carbonate system as 
they exist at higher pH values.

Now coming to the point of mineralization. We are currently working on this 
(as explained by Dr Siller, previously) and would like to use silicates as 
our metal source (Ca2+ or Mg2+).

Regarding the confusion of sea or oceanic system. We do not tend to imply 
the use of Ni nanoparticles in the ocean or any thing around it. The 
relation with sea urchin (or the marine environment) is just that, the use 
of Ni to study the hydration reaction we triggered by the studies done on 
the sea urchin by Dr Siller and my other colleagues. 

Our major application is to use this system as a satellite unit (plant) to 
an operational point source emitter (for example a power plant). The 
carbonate mineral thus produced would be used as landfill or in any other 
useful application. As mentioned above, we are working on the use of 
silicate sources (terrestrial) for the source of the alkali earth metals 
(Ca2+ or Mg2+), thus ruling out acidification of the ocean or any relation 
to the ocean. 

Hope I was able to explain the application of our technology. If you still 
have any doubts, please feel free to ask. We will try our level best to 
clarify any confusion.

Thanks to all 

Kind regards
Gaurav

On Thursday, 7 February 2013 18:49:41 UTC, Greg Rau wrote:

  Thanks for responding.  I really don't follow this. If I have a beaker 
 of water fully equilibrated with air (CO2) and add your Ni particles, you 
 are saying that more HCO3- and ultimately CO3s will spontaneously be 
 produced. This won't happen unless thermodynamically favored, and if that 
 water if fully equilibrated with air CO2 there is no thermodynamic 
 condition that will force a change in the C chemistry.  If your Ni 
 particles are somehow consuming H+ or producing OH- then you've got a 
 driving force, but you still need a source cations to make CaCO3s (am 
 very interested to learn how you cheaply extract cations from silicates.) 
  Otherwise, adding a catalyst to a system at thermodynamic equilibrium does 
 nothing.  On the other hand, adding something to seawater that overcomes 
 the natural, chemical inhibition of abiotic CaCO3s precipitation could 
 really cause some serious precipitation and CO2 injection into the 
 atmosphere. No?
 -Greg
  
   From: lidija...@gmail.com javascript: lidija...@gmail.comjavascript:
 
 Reply-To: lidija...@gmail.com javascript: 
 lidija...@gmail.comjavascript:
 
 Date: Thursday, February 7, 2013 8:32 AM
 To: geoengineering geoengi...@googlegroups.com javascript:
 Subject: [geo] Re: Nickel nanoparticles catalyse reversible hydration of 
 carbon dioxide for mineralization carbon capture and storage - Catalysis 
 Science  Technology (RSC Publishing)
  
  
  With presence of Ni we have increases at the same time trapping of CO2 
 and increased the rates of conversion to carbonic acid on room temperature 
 and on the atmospheric pressure.
  We still working to find the best mineralisation pathway - we will use 
 silicates (magnesium calcium silicates) as a source of Ca2+ or Mg2+.
  
 While nickel nanoparticles are toxic as already mentioned in the paper we 
 do not propose to spread this around in the enviroment but to have local 
 disposal next to power plant or industrial plant.
 We made brief cost - 8$ per ton of CO2 if we can recover Ni 99% yield 
 based on current price of nickel.
  
  
  

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