Dear Ron
  ----- Original Message ----- 
  From: Ronald Hongsermeier 
  To: Discussion of biomass cooking stoves 
  Sent: Thursday, August 08, 2013 10:22 AM
  Subject: Re: [Stoves] more on ocean acidification


  Dear Kevin,

  isn't a billion 10^9 ? and billion billion therefore 10^18?

  # You are correct. I was out by a factor of a million. I hate it when I make 
errors that big. :-( However, the good news there is 1,000,000 times as much 
water to absorb the Anthropogenic CO2, and it could take 1,000,000 times as 
long for the average Ocean pH to be changed, at the current rates of emission.

  the factors include water's ability to chemically shunt organic and inorganic 
contained and bottom materials within the pH system, which means we'd have to 
be able to at least model the composition of an average ocean bottom re. 
minerals, overall ocean avg. temp, surface to bottom migration, etc.

  # The issues are indeed complex.

  I am an ecologically sympathetic person, but see more danger presently from 
legal, semi-legal and illegal fishing practice to the overall health of the 
oceans.

  # In addition to these issues, there is also the issue of "micro plastics" 
dispersed through the water column. 

  I am also sympathetic with the concerns of Cecil Cook re. poisons, but think 
it somewhat confusing to put CO2 in the same class as CCl4. Depending on the 
amount of time between the cleaning process and the dipped sleeve there could 
well have been quite a significant amount of Carbon Tet in the water, 
especially in view of the proportions of scale-- I well remember being able to 
tell when I walked through the door of our house if my mother had brought 
things home from the cleaners and the odor was remarkable for some time after 
removing the plastic or paper wrappers of the day. And no, we don't know 
everything, which should make us more cautious not only in our actions, but 
also in concretizing our fears.

  # Agreed! The World Environment has a lot of real and imagined problems, and 
we need science, Truth, and Fact to determine which are the most serious 
problems, and which should be acted upon first. 
  Best wishes,

  Kevin


  regards,
  Ron von Bayernmittelwochenwochenende


  On 08.08.2013 13:41, Kevin wrote:

    Dear Paul

    Crispin indicates that the mass of the ocean is about 1.33 billion billion 
tons, i.e., 1.33 x 10^12 tons. That is a lot of water.

    The oceans are now alkaline. Some CO2 additions will lower the pH of the 
ocean, but the oceans will still be alkaline.

    How much CO2 would be required to actually make the oceans acidic? 

    At current rates of anthropogenic CO2 production, how long would it take 
for the Oceans to actually become acidic?

    Thanks!

    Kevin
      ----- Original Message ----- 
      From: Paul Olivier 
      To: Discussion of biomass cooking stoves 
      Sent: Thursday, August 08, 2013 7:08 AM
      Subject: Re: [Stoves] more on ocean acidification


      Crispin,


      The term that the scientific community uses is "ocean acidification," and 
this is a very real environmental problem that most people in the scientific 
community do not deny.


      Many thanks.

      Paul Olivier




      On Thu, Aug 8, 2013 at 12:27 PM, Crispin Pemberton-Pigott 
<[email protected]> wrote:

        Dear Friends



        I have been catching up on less important correspondence after being in 
Asia for a while. There is one thing that still needs to be put down like a 
broken-legged horse and that of course is the idea that CO2 ‘acidifies’ the 
ocean.



        Because this is a high school chemistry level topic and I know some of 
us took other things – or as the drummer in my brothers class said, “I don’t 
remember Chemistry, I was stoned that year.”



        So for those of you who were also stoned that year or can’t remember 
back that far, here is a simple review of pH with special reference to the 
oceans, CO2 and the false, badly mis-named idea that CO2 ‘increases the acidity 
of the oceans’.



        The term pH refers to one of three distinct chemical conditions which 
bear no relationship to each other. One is called acidity, another is called 
alkalinity and third is ‘neutral’. Acidity and alkalinity are so different that 
if equal in ‘strength’ they cancel each other completely leaving a neutral 
condition. Different pH numbers refer to different conditions.



        Acid solutions (it has to be a solution with water in it) have a 
chemistry that has Hydrogen atoms stripped of their single electron. They are 
thus positively changed and seeking an electron. This they will happily strip 
out of anything passing by if they can find it, tearing the molecules to bits 
in the process which is why acids ‘eat’ things.



        Alkaline solutions (again, involving water) have molecules that have an 
extra electron available (but not Hydrogen) and are thus negatively charged. 
They will give away an electron happily, often wrecking the object that 
receives it which is why they eat things too but by a completely different 
process.



        Both acidic and alkaline solutions can corrode things like metals and 
rocks. One takes electrons and one gives them. Quote opposite. The two 
conditions are so incompatible they cannot be present at the same time in a 
mixed solution. It is one, the other or ‘neutral’ if neither condition is 
present.



        If you have an alkaline solution like the ocean (pH 7.8 - 8.4 depending 
on where you are, the time of day and a host of other things) and you want to 
neutralise it so that all its spare electrons are taken up by various things, 
you would have to add something acidic. Adding CO2 by bubbling it through the 
seawater will convert some of the CO2 (about 1%) to carbonic acid which has a 
deficiency of electrons and that acid will merge with whichever passing 
opportunity presents itself. The corresponding alkaline molecule will be 
neutralised as its spare electron will be passed to the carbonic acid molecule 
(which has an H- in it) and afterwards neither will have any charge. Both will 
be neutralised if the charges are balanced.



        Because this happens very quickly, you cannot actually find any 
carbonic acid in the ocean. Nor any other acid. The oceans are not acidic at 
all.  Any ocean has quite a store of available electrons. Anything acidic you 
dump into the sea is quickly neutralised and the pH drops slightly because it 
is closer to a neutral condition. The oceanic capacity to hand over electrons 
to any passing electron gap is very, very large. There are several processes 
that would begin to offer electrons but do not because the ocean is too 
alkaline to allow them to get started. The ability to do this is called the 
‘buffering’ capacity. You may remember ‘Bufferin’ the pill that neutralises 
stomach acid. The pill is alkaline and has a large buffering capacity so it can 
hand a lot of electrons over to the acid in the stomach, thus neutralising it. 
If you took a whole bottle of Bufferin pills, your stomach would not become 
less and less and less acidic. It would be neutralised and then become alkaline 
and remains so until the spare electrons were taken up in a neutralising 
process. People are, in general, alkaline and should eat alkaline foods to 
remain healthy. Excess acid is a problem.



        By the same measure, reducing the availability of spare electrons in 
the ocean water does not at all make the water acidic because it still has many 
more available electrons. It is less alkaline, but it is not acidic at all – 
zero in the ‘acidic scale’ (there isn’t one). 



        In order to make a convenient metric for describing these two 
conditions (which can cancel each other out very predictably) the pH scale is 
used. Above 7.0 the solution has available electrons and is termed alkaline. 
Below 7.0 is has a deficiency of electrons and is called ‘acidic’. The reason 
for the use of two different terms is they are chemically dissimilar and cannot 
coexist.



        Acidity of a solution is often represented by the Hydrogen equivalent 
[H+]T which is the total number of Hydrogen electrons that would be needed to 
neutralise it.



        Alkalinity is often expressed in terms of its equivalence to Calcium 
Carbonate CACO3 in mg/Litre.



        Q.           Can CO2 ‘acidify’ water? 

        A.            Yes, if the water is neutral to begin with, or already 
acidic, like rain water. Because rain water is acidic, when it falls into the 
ocean it neutralises the drops of seawater where it touches, before becoming 
diluted again by the surrounding ocean. Rainwater does not impart to the ocean 
any microscopic ability to withdraw electrons. It is quickly neutralised by 
some seawater. When it is finished a few seconds later, the acid has been 
destroyed.



        Q.           If one bubbled CO2 through sea water, would it eventually 
become acidic?

        A.            Yes. If you were to first neutralise all the available 
electrons by mopping them up, after that it would start to become acidic. It 
would not considered be acidic at all until the whole body of the sample had 
first been neutralised. These two conditions cannot co-exist.



        Q.           What about ‘acid rain’. 

        A.            All rain is acidic. It is acidic because fresh water 
absorbs CO2 rapidly from the atmosphere, converting about 1% into carbonic 
acid. This falls into the oceans and reacts with the available alkaline 
molecules. It is easy to acidify rain. It is very difficult to neutralise the 
oceans because of the rocks upon which they sit which have a huge, massive 
buffering capacity. There are numerous life cycles of creatures that withdraw 
CO2, CO3-2 and HCO3- when it is available. Obviously CACO3 is high on the list 
for uptake by creatures that make shells.



        Q.           Which has a larger impact on ocean alkalinity: atmospheric 
CO2 or rain containing CO2?

        A.            Not clear. Rain has a big effect because oceans actually 
have difficulty picking up enough CO2 to drive the level much above 600 ppm 
because of the limited surface area compared with the volume and the huge 
buffering capacity.  Rain is much higher - about 1120 ppm CO2. Global rainfall 
totals about half a million cubic kilometers per year and contains about 600 
billion tons of CO2 which is about 20 times human output. 



        Q.           What is the mass of the oceans?

        A.            1.332 billion billion tons.



        Q.           Do reputable scientific organisations refer to 
‘acidifying’ the oceans even though that is not, chemically, what it happening?

        A.            Yes. NASA does. “As we burn fossil fuels and atmospheric 
carbon dioxide levels go up, the ocean absorbs more carbon dioxide to stay in 
balance. But this absorption has a price: these reactions lower the water’s pH, 
meaning it’s more acidic.”



        Q.           But it is less alkaline, not more acidic. Why do they 
write that when it is untrue, in fact it is unscientific?

        A.            I don’t think anyone knows.  Perhaps they too missed 
Chemistry in high school.



        +++++++

        Regards
        Crispin







        Sent: Friday, July 26, 2013 3:25 PM
        Subject: [Stoves] more on ocean acidification



        
http://www.scientificamerican.com/article.cfm?id=noaa-scientists-embark-voyage-asses-ocean-acidification

        -- 
        Paul A. Olivier PhD
        26/5 Phu Dong Thien Vuong
        Dalat
        Vietnam





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      -- 
      Paul A. Olivier PhD
      26/5 Phu Dong Thien Vuong
      Dalat
      Vietnam

      Louisiana telephone: 1-337-447-4124 (rings Vietnam)
      Mobile: 090-694-1573 (in Vietnam)
      Skype address: Xpolivier
      http://www.esrla.com/ 


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