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.. water is one of the few substances that is slightly denser as a liquid than as a solid. This is why ice cubes float in water. .. Most icebergs actually contain a lot of air. Far from being the solid blocks of ice many people imagine, icebergs are riddled with billions of tiny, trapped air bubbles, giving the huge bergs their white appearance. .. icebergs are made from fresh water. Because of the dissolved salts in ocean water, it is denser than freshwater, adding bouyancy to the icebergs
You ask “ .. how can you even know the starting point of a molecule? I sounds like a lot of guess work to me .. ” and I can’t argue with that. The experts call it probabilities.
Hi Wiybit, regarding your Quote 15/04/2011 16:21:39 .. I think you mean it's a multi-layered process. I see the size-dependent fractionation and close-off processes as being “multi-layered” in space and time.
15/04/2011 16:21:39 .. I think you mean it's a multi-layered process.
Your Quote … Ice is a solid isn't it, I kinda think it's like as ice forms and compacts the gases are squezzed out, and if as you are suggesting gases can move through smaller, gaps then I suppose more would be squezzed out. is getting there. Put simply, snow is also ice but, as I said before, has a density of as low as 0.2 that of water. As it is compacted it approaches a density of about 0.9 that of water. The remaining 0.1 is air, hence 10% of an ice berg is above water.
… Ice is a solid isn't it, I kinda think it's like as ice forms and compacts the gases are squezzed out, and if as you are suggesting gases can move through smaller, gaps then I suppose more would be squezzed out.
Regarding kinetic diameter you asked Quote .. but why do they ignore it? They either are ignorant of it or some some reason feel it has no bearing, or plays to insignifcant a role to be accounted for. I assume, but it sounds a bit strage for scientists to just ignore, a kinetic factor for no reason. What is the justifaction for ignoring it? . You are repeating the question that I have been putting to the paleoclimatologists for more than a year now and The Naked Scientists three days ago in my first post above. None have answered it yet. It is worth noting that experts in the field of gas purification, such as in the energy and pollutant extraction industries use kinetic, not collision, diameter. I have made this point on numerous occasions to the “experts” and none have explained why they choose to ignore the smaller kinetic diameter of CO2 compared with N2, O2 CH4 and Ar. That’s odd, don’t you think?
.. but why do they ignore it? They either are ignorant of it or some some reason feel it has no bearing, or plays to insignifcant a role to be accounted for. I assume, but it sounds a bit strage for scientists to just ignore, a kinetic factor for no reason. What is the justifaction for ignoring it?
Quote .. what is it about Co2 that makes it so different? Personally I think much of the man made co2 we have in the atmospere is comming from CO cabon monoxide, which when realesed from burning fuels etc grabs an oxygen and so forms Co2 .. . I’m would expect that this “ .. media-savvy group of physicians and researchers from Cambridge University .. ” (http://www.thenakedscientists.com/HTML/about-us/) called The Naked Scientists should be able to offer a valid answer to that question. I think that you may be way off-beam with your hypothesis about CO, considering that when hydro-carbon fossil fuels are burnt the main products are H2O and CO2, with CO being comparatively minor.
.. what is it about Co2 that makes it so different? Personally I think much of the man made co2 we have in the atmospere is comming from CO cabon monoxide, which when realesed from burning fuels etc grabs an oxygen and so forms Co2 ..
Quote .. Implies Co2 is a smaller molecule, yet surely it's bigger then 02? What missing? .. . In this context we are talking about size in terms of volume not weight (think of a balloon).Quote .. could it not also be the case that the cores have trapped Co2 from the ice below them? Can we trust the findings at all really? .. . My hyp[othesis says “Yes” to part 1 and “No” to part 2.Regarding the difference in collision and kinetic diamter Quote .. Note the difference for CO2. It's .6 compared to 0, 0.2 or 0.1 with the others, why does it have such variation? .. , again, there should be at least one of The Naked Scientists who can answer that question.You seem to have completely missed the point of my mention of the He balloon by saying Quote .. Strange he is lighter than Co2, so Co2 moves more in because it's smaller fairly clear .. . I was hoping that you’d realise that the reason the He-filled balloon collapses relatively quickly is because the balloon is a bit like those air pockets in firn – it has lots of tiny pores that are so small that He (0.26nm kinetic diameter) can escape more readily that the larger N2, O2 and Co2 molecules of the expelled air we puff into a balloon.
.. Implies Co2 is a smaller molecule, yet surely it's bigger then 02? What missing? ..
.. could it not also be the case that the cores have trapped Co2 from the ice below them? Can we trust the findings at all really? ..
.. Note the difference for CO2. It's .6 compared to 0, 0.2 or 0.1 with the others, why does it have such variation? ..
.. Strange he is lighter than Co2, so Co2 moves more in because it's smaller fairly clear ..
In saying of the scientists that I mentioned Quote .. Maybe it's too complicated, and add too many varibles .. you are effectively agreeing with Professor Jaworowski, who, as I’ve already told you, said “This is a highly specialized field of science. My impression is that it is a terra incognita for glaciologists”.Finally you said of that CO2 that escapes from the air pockets and heads down the pressure gradient towards the surface Quote .. Yes, I meant escaped into the atmosphere. From what you have said I'm not sure if you could really say either way .. [/quote. I ’m inclined to agree with that.(I know, I still haven’t responded on Fickian diffusion. I need more time for that one, after all, I’m only a retired engineer).May I just say how enjoyable it is exchanging opinions with you in the spirit of improving understanding rather than scoring points or pushing a particular doctrine. It’s a great shame that on most blogs that I get involved with it ends up simply being a battle by both sides to win an argument.Best regards, Pete Ridley
.. Maybe it's too complicated, and add too many varibles ..
.. Yes, I meant escaped into the atmosphere. From what you have said I'm not sure if you could really say either way .. [/quote. I ’m inclined to agree with that.(I know, I still haven’t responded on Fickian diffusion. I need more time for that one, after all, I’m only a retired engineer).May I just say how enjoyable it is exchanging opinions with you in the spirit of improving understanding rather than scoring points or pushing a particular doctrine. It’s a great shame that on most blogs that I get involved with it ends up simply being a battle by both sides to win an argument.Best regards, Pete Ridley
Do you think a lump of ice composed of 10 % air bubbles by volume would be strong enough to withstand being pulled out of the ground with an ice-core drill? Seems rather unlikely to me. Ice is brittle stuff
.. Using the PICO (Polar Ice Coring Office) lightweight auger, a 31 m long firn core was drilled adjacent to the cane farm at GD03. The GD03 core represents 55 years of annual snow-accumulation increments which were interpreted from the combined stratigraphic analyses of density, oxygen-isotope and visible layering. A vertical profile of density .. shown in Figure 2 ..
.. fickian law .. looks to relate more to solids then gases ..
Fick's Law: The net diffusion rate of a gas across a fluid membrane is proportional to the difference in partial pressure, proportional to the area of the membrane and inversely proportional to the thickness of the membrane. Combined with the diffusion rate determined from Graham's law, this law provides the means for calculating exchange rates of gases across membranes
.. I find it interesting that anyone who is unaware of why ice cubes float in water might think they are qualified to call into question the scientific credentials of anyone else ..
Hi Wiybit, I was disappointed that none of this “ .. media-savvy group of physicians and researchers from Cambridge University .. ” have tried to help you out on your Quote .. fickian law .. looks to relate more to solids then gases .. .
I’d love some help on the relevant laws of diffusion too and since none of The Naked Scientists seems to be able to help I took the opportunity of chatting about that (and my question about “Another Hockey Stick Illusion?”) with Professor Andrew White who was visiting us this weekend.Andrew is Professor and Director, Center for High Energy Physics Research and Technology, Department of Physics, The University of Texas at Arlington and has been a Professor of Physics there for 20 years (http://www.uta.edu/physics/main/faculty/). During that time he has been involved in research at CERN so I thought that he could perhaps save me some time digging up an answer for you. As Bored chemist might say “Nope”.
His response was “I’m not up on diffusion” so I had to try elsewhere. Does this help Quote Fick's Law: The net diffusion rate of a gas across a fluid membrane is proportional to the difference in partial pressure, proportional to the area of the membrane and inversely proportional to the thickness of the membrane. Combined with the diffusion rate determined from Graham's law, this law provides the means for calculating exchange rates of gases across membranes (http://hyperphysics.phy-astr.gsu.edu/hbase/kinetic/henry.html)?
suggests that you haven't spent much time researching ice cores or much time trying to understand my question about “Another Hockey Stick Illusion?”.
Now, if anyone is actually interested (and I acknowledge this isn't rocket science...), the densities of water at different temperatures are given here:http://www.sfu.ca/physics/ugrad/courses/teaching_resources/demoindex/fluids/fl2b/density.htmlThe density of pure water is, at least, 0.998 (density at 0 oC, density at 4 oC is a little higher. If the ice (at 0.92) were floating entirely on its own (pure) melt-water, it would float with 8.5 % of its volume above the water. But the water is not pure, it is mixing all the time with salt sea-water, so it might be fractionally less dense than the average surface water density (1.02-1.03), but the absolute lower limit is that 8.5 % will float above the surface, in reality it will be more, and that's entirely without considering the effects of air bubbles.
Rosy, doesn't water compact as it frezzes? shouldn't the density be highier at 0, as the atoms are more compacted than at density at 4 oC?
.. Seriuosly you shouldn't encourage them(if you get me) ..
.. BC can be slightly funny at times, but generally he's ok, when not .. trying to catch you out(so he can laugh at you) ..
.. you still haven't said what it is about Co2 that causes it to act so differently to the other elements, surely HE should move more, in ice if it's smaller and lighter? ..
Abstract .. For smaller gas species (mainly He and Ne) the fractionation factors are linearly correlated to the molecule size, whereas for diameters greater than about 3.6 Å the fractionation seems to be significantly smaller or even negligible ..
.. Close-off fractionation factors for different gases depend strongly on the diameter. The mass of the molecule is less important, since the effect on isotope ratios is very low. The critical size of about 3.6 Å seems to be an upper limit up to which molecules fractionate during the close-off process in the firn. A possible explanation for this could be the diffusion of molecules through channels in the ice lattice. From our findings we believe that the effect of close-off fractionation is nonexistent or at least very small for isotope ratios and for large molecules, like Xe, Kr, N2, CO2, CH4, and N2O. This is an important confirmation for the integrity of polar ice cores as a climate archive of the ancient atmospheric composition of these gases ..
.. Firn density at surface [g/cm3] 0.40 0.32 .. Firn density at close off [g/cm3] 0.838 0.811 ..
On a more hands-on level, consider an ice cube made in your freezer to cool a drink. Not being made from snow, it doesn't contain (a significant number of) bubbles, and yet it floats. If you think about it, I'm pretty sure this is something you know and understand! The density of ice is, inherently, less than that of water at the same temperature. Equally, if you close up a bottle full to the top with water at room temperature (using a plastic bottle is important for safetly..), and freezing the water, the bottle will split as the water expands on forming ice... which shows you that the same mass of water takes up more space (is less dense) when frozen than as a liquid.
QuoteRosy, doesn't water compact as it frezzes? shouldn't the density be highier at 0, as the atoms are more compacted than at density at 4 oC? No. Water doesn't compact as it freezes, and the maximum density of water occurs at 4 oC. Water's funny stuff. I'm not going to try to explain in any detail here, because it needs diagrams, but there's lots of information on the internet about this. For example this page: http://kentsimmons.uwinnipeg.ca/cm1504/water.htmOn a more hands-on level, consider an ice cube made in your freezer to cool a drink. Not being made from snow, it doesn't contain (a significant number of) bubbles, and yet it floats. If you think about it, I'm pretty sure this is something you know and understand! The density of ice is, inherently, less than that of water at the same temperature. Equally, if you close up a bottle full to the top with water at room temperature (using a plastic bottle is important for safetly..), and freezing the water, the bottle will split as the water expands on forming ice... which shows you that the same mass of water takes up more space (is less dense) when frozen than as a liquid. Incidentally, if ice didn't float, and if the coldest water didn't float on top of water at 4 oC, then the coldest water would sink to the bottom of lakes and rivers, and they'd freeze from the bottom up. That would mean that instead of a layer of ice over liquid water the whole of the lake would freeze, which would kill the fish and other animals living in the water whereas in reality they can hide in the relatively warm water at the bottom until spring.
Hi Wiybit, sorry that I didn’t have time to respond straight away to the points you raised on 16/04/2011 @ 20:48:50 and today @ 13:40:20. I don’t want to get distracted from the focus of my question about “Another Hockey Stick Illusion?”, i.e. why the “experts” ignore kinetic in favour of collision diameter. If it’s OK with you I’ll leave it to the Naked Scientists to respond to any that I see as a side-issue. You may have to raise such questions separately in order to attract their attention.Quote .. Seriuosly you shouldn't encourage them(if you get me) .. is not the reason that I joined this blog. I will do my utmost to encourage The Naked Scientists to offer their expertise where it relates to my question. I’m very disappointed that I’ve had nothing from them yet and the appropriate laws of molecular dynamics covering the movement of atmospheric gases in firn are certainly relevant.
Quote .. BC can be slightly funny at times, but generally he's ok, when not .. trying to catch you out(so he can laugh at you) .. is fine for anyone who has come here to be amused but I’m not in that category. I’m here to learn as much as I can about the science relevant to my question. So far the only person on this blog to help improve my understanding is you through your questions.
Regarding Quote .. you still haven't said what it is about Co2 that causes it to act so differently to the other elements, surely HE should move more, in ice if it's smaller and lighter? .. one day I may be able to fully answer the first part with confidence. All that I can say for the moment is that it is something to do with the bonding between the one C and two O atoms that make up a molecule and the interaction of each molecule with other molecules (N2, O2, Ar, CH4, H2O, etc. Why not put that question to The Naked Scientists.
As for the second part, He, being smaller even than CO2, does experience size-dependent fractionation, as described in the paper “Evidence for molecular size dependent gas fractionation in firn air derived from noble gases, oxygen, and nitrogen measurements” by Huber et al (http://icebubbles.ucsd.edu/Publications/Huber_closeoff_EPSL2006.pdf).It is worthwhile looking more closely at that paper, because as well as answering your question about He directly, it expands on my earlier comment (on 14/04/2011 21:38:13) about Huber, Severinghaus (one of the co-arthors) and that magic 0.36nm molecule diameter Quote Abstract .. For smaller gas species (mainly He and Ne) the fractionation factors are linearly correlated to the molecule size, whereas for diameters greater than about 3.6 Å the fractionation seems to be significantly smaller or even negligible .. Note that Table 2 presents the molecular diameters used in their model and the close-off fractionation factor it produced for 8 of the atmospheric gases, including CO2 and He, but also note that those diameters are collision, not kinetic. Fig. 8 presents a useful graph of 7 of those computer-modelled close-off fractionation factors, with He down at the bottom of the curve, but note which one is missing, dear old CO2. I mentioned in that earlier comment that I had asked Severinghaus why he used collision rather than kinetic diameter and if he had tried his model using CO2’s 0.33nm kinetic diameter instead of its 0.39nm collision diameter. As I said, he chose not to respond directly to those questions. Have a guess where CO2 would have been if he had used kinetic diameter, which I hypothesise is the appropriate measure.
That is why I challenge the conclusion that Quote .. Close-off fractionation factors for different gases depend strongly on the diameter. The mass of the molecule is less important, since the effect on isotope ratios is very low. The critical size of about 3.6 Å seems to be an upper limit up to which molecules fractionate during the close-off process in the firn. A possible explanation for this could be the diffusion of molecules through channels in the ice lattice. From our findings we believe that the effect of close-off fractionation is nonexistent or at least very small for isotope ratios and for large molecules, like Xe, Kr, N2, CO2, CH4, and N2O. This is an important confirmation for the integrity of polar ice cores as a climate archive of the ancient atmospheric composition of these gases ..
But I’m only a retired Chartered Electrical Engineer and Geezer reasonably says Quote .. I find it interesting that anyone who is unaware of why ice cubes float in water might think they are qualified to call into question the scientific credentials of anyone else .. That is why during the past year I have requested help from “experts” like Severinghaus, Alley, Bender, etc. etc. etc.
and now from this “ .. media-savvy group of physicians and researchers from Cambridge University .. ”, but I’m still not getting an answer.
Actually Pete lets just ask the main crux of your question.Why Do climatologists ignore the kinetic movement of CO2 in ice, as that could, and probably does effect the ice core Co2 levels?Anyone?
.. But it relates to your general question, and is only an issue "if" kinetics of Co2 in ice are true, and as far as I can tell that is still part of your main question and so not answered either. Surely first we find out if the kinetic factors are real then ask why does the Co2 move. I asked you because I believed you understood the kinetic science but didn't understand why they ignored it ..
.. (physical chemistry) The distance between the centers of two molecules taking part in a collision at the time of their closest approach
.. The kinetic diameter can be understood as the diameter of a pore needed to let that specific molecule pass ..
.. Separating of water .. in particular with H2, CO, CO2, CH4 and higher alkanes ..
.. separation on size is possible, when the components to be separated are small enough in kinetic diameter to migrate through the zeolite pores and the components from which they have to be separated have a kinetic diameter that is too large ..
.. some assistance in generating a scientific paper ..
.. It's never a good sign if a scientist ignores your question relating to their research, it's either an unknown variables ..
.. need time to formulate a responce and so felt it was too much hassle
.. whizzing all over TNS and those in the "Scientific Community" who are obviously conspiring ..
I came across this blog while searching for detailed pictures of ice extracted from deep down an ice sheet. I have a question that has been puzzling me for over a year now and remains unanswered despite asking it of experts in the subject ..
Climate Change and Ice Cores. Dr Eric Wolff from the British Antarctic Survey
The Naked Scientists are a media-savvy group of physicians and researchers from Cambridge University ..
Who are we?”
So what's your question here Pete?
.. why do paleo-climatologists use collision diameter in preference to kinetic diameter when considering the migration of air molecules through firn and ice ..
I don't recall claiming any expertise in migration of molecules through any medium, so it's no surprise you find me lacking in that arena ..
About my suggestion that you put a question to the Naked Scientists of why CO2 acts in the way that it does you said Quote .. But it relates to your general question, and is only an issue "if" kinetics of Co2 in ice are true, and as far as I can tell that is still part of your main question and so not answered either. Surely first we find out if the kinetic factors are real then ask why does the Co2 move. I asked you because I believed you understood the kinetic science but didn't understand why they ignored it .. I thought that I had made it clear that the “experts” to whom I have put my question are aware of the size-dependent fractionation that occurs (in your terminology “the kinetic factors are real”) but use a different (in my hypothesis an incorrect) measure of the estimated size of molecules when modelling their movement within the porous firn.
You and Geezer, appear to defend The Naked Scientists because they may not have expertise in climate science. I would not be here if they had not given me the impression of having a to, section within their "Environment" area specifically on Climate Change and having their representatives advising on it. If I don’t have expertise then I admit it. Surely it is not asking too much for a simple statement on their “About” page making it clear in what areas they are competent to speak?