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| From | cornelius@eisner.decus.org (George Cornelius) |
|---|---|
| Newsgroups | sci.physics |
| Subject | Re: Re:Partial pressure of O2, CO2, etc., in Thailand cave |
| Date | 2018-07-08 01:14 -0400 |
| Organization | Encompasserve |
| Message-ID | <axU$GPEZqWM$@eisner.encompasserve.org> (permalink) |
| References | <a3TEG7FpUeMY@eisner.encompasserve.org> <phs2tm$n6k$1@dont-email.me> |
In article <phs2tm$n6k$1@dont-email.me>, Libor Striz <poutnik4REMOVEnntp@CAPITALSgmail.com> writes: > cornelius@eisner.decus.org (George Cornelius) Wrote in message: >> I am here ignoring the partial pressure of CO2. Of course it >> will be going up as O2 is consumed by the humans in the cavity, >> but since some of the waste product of energy production in the >> body is H2O, there should be a smaller volume of CO2 produced >> than O2 consumed, say, roughly, 2:1. > The major metabolic source of energy - oxidation of glucose - has > the total chemical reaction as > C6H12O6(glucose) + 6 O2 --> > 6 H2O + 6 CO2., Therefore 1:1 Thank you. I had completely forgotten that sugars have a large number of oxygen atoms. Don't recall ever memorizing the chemical formula for glucose although I at one time could tell you one of the others - I suppose sucrose. > For fat, it can be simplified by ommiting the minor glycerol > ester part as just > 2 (CH2)n + 3n O2 --> 2n CO2 + 2n H2O, > so 3:2. > > Large portion of CO2 will be dissolving in water, some small part > of it dissolving the limestone > CO2 + H2O + CaCO3 --> Ca(HCO3)2 Yes, I had long since forgotten the reaction that transforms aqueous CO2 and CaCO3 into limestone, but I knew it existed. And I did expect at least some of the CO2 to dissolve in water. In any case, the outcome is similar to what I proposed, that O2 relative percentages decrease while CO2 changes are not as significant, and this is good because the feeling of suffocation you get in confined spaces is apparently due to excess CO2 and not the lack of oxygen. > The relative humidity will be close to 100%, absolute humidity > in g/me will be near constant as well as temperature. Excessive > water vapour will eventually condense. My assumption as well. > The eventual pressure decrease due decrease of total amount of > gasses will be mostly eliminated by sucking air via limestone > porosity and sucking water to decrease volume and increase > pressure. These effects lead to both absolute and partial > pressure increase of air gasses but CO2, which partial pressure > increase will be much smaller. OK, so porosity effects do apply. As the monsoon season progesses is it possible the limestone becomes closer to being saturated with water and less capable of bearing oxygen and other gases? > 1 % of CO2 reportedly start causing breathing problem, as > increased CO level on blood trigger response of hypothalamus to > intensify breathing to get rid of it . > 10 % has already an anaesthetic effect. ( Quotes Q&A source ) > > The questing remains, what was the initial oxygen concentration > before flooding. Even if the internal space was directly > connected to open air, the cave system is long enough to differ > from average air concentration. E.g oxygen can be spent by > oxidation of iron and manganese minerals and by cave life > forms. Difficult to know unless someone has studied it in the past or someone is routinely recording such things over time. And I doubt if the divers, upon arriving initially, might have both collected an air sample and measured absolute air pressure. I have heard that there were later readings after the reported 15% O2 number and that it has climbed back up to 17%. Perhaps there has been some oxygen replenishment. Plus, despite indications that attempts to run an oxygen line to the cavern had been abandoned, there are reports that there was at least some oxygen transferred, presumably not by carrying in oxygen tanks, in the last few days. George > -- > Libor Striz aka Poutnik ( a pilgrim/wanderer/wayfarer) > > "Humour is the only effective weapon against stupidity." > Miloš Forman > > > ----Android NewsGroup Reader---- > http://usenet.sinaapp.com/
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Partial pressure of O2, CO2, etc., in Thailand cave cornelius@eisner.decus.org (George Cornelius) - 2018-07-07 20:55 -0400
Re: Partial pressure of O2, CO2, etc., in Thailand cave cornelius@eisner.decus.org (George Cornelius) - 2018-07-07 21:30 -0400
Re: Partial pressure of O2, CO2, etc., in Thailand cave cornelius@eisner.decus.org (George Cornelius) - 2018-07-07 22:19 -0400
Re:Partial pressure of O2, CO2, etc., in Thailand cave Libor Striz <poutnik4REMOVEnntp@CAPITALSgmail.com> - 2018-07-08 06:11 +0200
Re: Re:Partial pressure of O2, CO2, etc., in Thailand cave cornelius@eisner.decus.org (George Cornelius) - 2018-07-08 01:14 -0400
Re: Re:Partial pressure of O2, CO2, etc., in Thailand cave Libor Striz <poutnik4REMOVEnntp@CAPITALSgmail.com> - 2018-07-08 07:30 +0200
Re: Re:Partial pressure of O2, CO2, etc., in Thailand cave cornelius@eisner.decus.org (George Cornelius) - 2018-07-09 02:40 -0400
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