CrusaderFrank
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- May 20, 2009
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A liter of water has a pH of 8.25. In order to drop the pH to 8.15, how much CO2 must you add to it ?
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Can someone with a scientific background (that leaves Old Rocks and Abe out in the cold) please weigh in here?
honey hush i can tell you how pure you coke is....but this is beyond me.....i would just add vingear
honey hush i can tell you how pure you coke is....but this is beyond me.....i would just add vingear
It's a high school chemistry question, well at least when I went to high school.
No one responds, especially the AGWCult, because the answer requires an amount of CO2 several orders of magnitude above what's currently produced
"The hydration equilibrium constant at 25°C is called Kh, which in the case of carbonic acid is [H2CO3]/[CO2] ≈ 1.7×10−3 in pure water[3] and ≈ 1.2×10−3 in seawater.[4] Hence, the majority of the carbon dioxide is not converted into carbonic acid, remaining as CO2 molecules."
Carbonic acid - Wikipedia, the free encyclopedia
See, there's just no conceivable way that manmade CO2 is turning the oceans acidic as alleged by the AGWCult. It baffles me that the Warmers haven't been kicked to the curb by real scientists that work alongside them.
I'm not a scientist. I'm a real estate analyst and none of the "theories" put forth by the AGWCult ever make the least bit of sense.
So, again, how does CO2 turn the oceans acidic?
honey hush i can tell you how pure you coke is....but this is beyond me.....i would just add vingear
What is ocean acidification?
FAQ on ocean acidification
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The other CO2 problem animation
The consequences of man's use of fossil fuels (coal, oil and natural gas) in terms of global warming has not escaped anyones attention. Ocean acidification is another, and much less known, result of the approximately 79 million tons of carbon dioxide (CO2) released into the atmosphere every day, not only as a result of fossilfuel burning but also of deforestation and production of cement (7). Since the beginning of the industrial revolution, about one third ofthe CO2 released in the atmosphere by anthropogenic (human-caused) activities has been absorbed by the worldÂ’s oceans,which play a key role in moderating climate change (5). Without this capacity of the oceans, the CO2 content in the atmosphere would have been much higher and global warming and its consequences more dramatic. The impacts of ocean acidification on marine ecosystems are still poorly known but one of the most likely consequences is the slower growth of organisms forming calcareous skeletons or shells, suchas corals and mollusks.
The carbon cycle
Inorder to understand ocean acidification and its possible impacts, one needs to understand the behaviour of carbon in nature. Carbon, as other elements, is circulating in different chemical forms and between different parts of the Earth system (atmosphere, biosphere and the oceans). These fluxes of carbon in inorganic (e.g. CO2) and organic forms (sugar and more complex carbohydrates in the biosphere) constitute the carbon cycle. In a very short time span, human activities use an old reservoir of carbon (fossil fuels) which took millions of years to accumulate, thus creating a new and massive flux of CO2 into the atmosphere. The oceans can mitigate this additional carbon dioxide flux and thus help moderate global warming but this is not without consequences.
The world's oceans play a fundamental role in the exchange of CO2 with the atmosphere and constitute an important sink for atmospheric CO2. Once dissolved in sea water, carbon dioxide is subject to two possible fates. It can either be used by photosynthesis or other physiological processes, or remain free in its differentdissolved forms in the water. The latter leads to ocean acidification.
The chemical process of ocean acidification
There is a constant exchange between the upper layers of the oceans and the atmosphere. Nature strives towards equilibrium, and thus for the ocean and the atmosphere to contain equal concentrations of CO2. Carbon dioxide in the atmosphere therefore dissolves in the surfacewaters of the oceans in order to establish a concentration inequilibrium with that of the atmosphere. As CO2 dissolves in the ocean it generates dramatic changes in sea water chemistry. CO2 reacts with water molecules (H2O) and forms the weak acid H2CO3 (carbonic acid). Most of this acid dissociates into hydrogen ions (H+) and bicarbonate ions (HCO3-). The increase in H+ ions reduces pH (measure of acidity) and the oceans acidify, that is they become more acidic or rather less alkaline since although the ocean is acidifying, its pH is still greater than 7 (that of water with a neutral pH). The average pH of today's surface waters is 8.1, which is approximately 0.1 pH units less than the estimated pre-industrial value 200 years ago (2,3).
Projections of future changes
Modeling demonstrates that if CO2 continues to be released on current trends, ocean average pH will reach 7.8 by the end of this century, corresponding to 0.5 units below the pre-industrial level, a pH level that has not been experienced for several millions of years (1). A change of 0.5 units might not sound as a very big change, but the pH scale is logaritmic meaning that such achange is equivalent to a three fold increase in H+ concentration. All this is happening at a speed 100 times greater than has ever been observed during the geological past. Several marine species, communities and ecosystems might not have the time to acclimate or adapt to these fast changes in ocean chemistry
Can someone with a scientific background (that leaves Old Rocks and Abe out in the cold) please weigh in here?
****://en.wikipedia.org/wiki/Carbonic_acid#pH_and_composition_of_carbonic_acid_solutions
Can someone with a scientific background (that leaves Old Rocks and Abe out in the cold) please weigh in here?
Well...............that's tricky
I think you might have already asked Dr. Google and found out that this would get nasty.
1. If you have a pH of 8.25 in the original water, that means that there is some basic solution in it. Whatever, maybe Ca and Mg Carbonates. This makes it even more complicated, because there exists an equilibrium between H2CO3 and the Carbonates which varies over the respective concentrations.
2. The acid constant of H2CO3 changes with the concentration
3. the dissociation factor of H2CO3 varies with the temperature, additionally you have always just dissolved CO2 in the water that is not reacting to H2CO3.
A little introduction: ****=http
HTML:****://en.wikipedia.org/wiki/Carbonic_acid#pH_and_composition_of_carbonic_acid_solutions