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| sunshinewarrior |
Posted: Wed Apr 09, 2008 7:30 am Post subject: Pyroclastic flow |
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 Forum Ph.D.

Joined: 26 Sep 2007 Posts: 948 Location: London
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Iâve put this in Earth Sciences because thatâs where pyroclastic flow appears to be most used.
My understanding (though the wiki Iâve linked seems to suggest otherwise), was that pyroclastic flow was characterised by a combination of solids and heated gas, and it was in that context that I wanted to raise this question.
Say that I (hypothetically, and anyway it was in a different country where it is allowed and I was younger â in fact not yet of age so I canât be held responsible..) had some experience of using hash. Now as the article suggests, a common method for use involves preparing âfor smoking by heating it with a flame for a couple of seconds, producing some bubbling or sizzling. It then softens and can be crumbled into tiny pieces or formed into shapes to obtain maximum surface area when burning.â
Hereâs my question, if anyone has enough chemistry/geology/whatever to tell. When one âroastsâ hash, is the subsequent crumbly nature due to something akin to pyroclastic flow? Does the heating raise the temperature of trapped gases/volatiles in the hash, thereby reducing the structural integrity of the solid?
Admins/mod, if this has in any way violated the terms of use, please feel free to delete, and accept my apologies.
cheer
shanks |
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| Zitterbewegung |
Posted: Wed Apr 09, 2008 8:12 am Post subject: |
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 Forum Sophomore

Joined: 24 Dec 2007 Posts: 173
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Ummmmmmm......not quite.
Pyroclastic flows in general are basically an avalanche of "acidic" (in geological terms, not chemically speaking i.e. high silica content and thus high viscosity + high content of trapped volatile components) lava ejected from a strato-vulcano. This is basically a self-amplifying process as after the lava got ejected the pressure is of course released. This in turn causes the bubbles of volcanic gasses trapped inside the lava chunks to expand. They go more or less "popp" and release more hot gasses and decreasing the avérage size of the lava chunks effectively creating a self sustaining air cushion under the pyroclastic flow. This cussion accelerates the downhill mtion of the avalanche sucking in even more air. Did you ever see a dust avalanche in the mountains? More or less like this but a little bit hotter
To give you a better conception: Try standing behind a jet powering up it's engines to the max. On top of this jet is a truck loaded with tons of slag directly from a blast furnace. The truck dumps the slag in the exhaust of the throttle-full-open turbine while you are just a couple of feet away.
Have fun. _________________ I love deadlines. I like the whooshing sound they make as they fly by |
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| sunshinewarrior |
Posted: Wed Apr 09, 2008 8:31 am Post subject: |
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 Forum Ph.D.

Joined: 26 Sep 2007 Posts: 948 Location: London
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| Zitterbewegung wrote: |
| Ummmmmmm......not quite. |
But but but...
| Zitterbewegung wrote: |
| They go more or less "popp" and release more hot gasses and decreasing the avérage size of the lava chunks effectively creating a self sustaining air cushion under the pyroclastic flow. This cussion accelerates the downhill mtion of the avalanche sucking in even more air. |
It's exactly that sort of air cushion effect that I'm talking about. Obviously neither the temperatures nor pressures are comparable, but is there nothing analogous about them at all? |
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| Zitterbewegung |
Posted: Thu Apr 10, 2008 2:50 am Post subject: |
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 Forum Sophomore

Joined: 24 Dec 2007 Posts: 173
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| Quote: |
| It's exactly that sort of air cushion effect that I'm talking about. Obviously neither the temperatures nor pressures are comparable, but is there nothing analogous about them at all? |
Well, in one case you have some resin that is not really easy to crumble when cold. The pyroclastic flow consists of a high silica melt interspersed with allready cooled chuncks in it. I do not see a common property here or do I miss the point?  _________________ I love deadlines. I like the whooshing sound they make as they fly by |
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| sunshinewarrior |
Posted: Thu Apr 10, 2008 3:23 am Post subject: |
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 Forum Ph.D.

Joined: 26 Sep 2007 Posts: 948 Location: London
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| Zitterbewegung wrote: |
| Quote: |
| It's exactly that sort of air cushion effect that I'm talking about. Obviously neither the temperatures nor pressures are comparable, but is there nothing analogous about them at all? |
Well, in one case you have some resin that is not really easy to crumble when cold. The pyroclastic flow consists of a high silica melt interspersed with allready cooled chuncks in it. I do not see a common property here or do I miss the point?  |
Perhaps I was led astray by University Challenge - one of the bonus question sets consisted of asking about the difference between three types of flowing mixtures - gas + liquid, liquid + solid, and gas + solid, which last they said was the characteristic of pyroclastic flow. It was the idea of a flowing combination of gas and solid that got me thinking. |
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| Bunbury |
Posted: Fri Apr 11, 2008 7:32 am Post subject: |
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Forum Ph.D.

Joined: 26 Sep 2007 Posts: 690
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| A flowing combination of gas plus solid is what goes on in a circulating fluidized bed boiler furnace and in any number of pneumatic conveying systems. That University Challenge question seems open to a broad range of answers. (I'm amazed it's still on. Just checked - it started in 1962.) |
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| Ophiolite |
Posted: Fri Apr 11, 2008 7:38 am Post subject: |
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 Forum Radioactive Isotope

Joined: 25 Jul 2005 Posts: 4450 Location: Scotland
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| Bunbury wrote: |
| (I'm amazed it's still on. Just checked - it started in 1962.) |
This is a reincarnation. Jeremy Paxman instead of Bamber Gascoine. I think the old one was on ITV, not BBC also, but I may be wrong.
I could answer almost none of the questions in 1962, now I find many of them ridiculously easy. I must have learned something in four and a half decades.  _________________ The Universe is not only weirder than we imagine it is weirder than we can imagine. J.B.S.Haldane. |
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| sunshinewarrior |
Posted: Fri Apr 11, 2008 7:54 am Post subject: |
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 Forum Ph.D.

Joined: 26 Sep 2007 Posts: 948 Location: London
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| So pyroclastic can't be used as a catch-all term for all solid+gas flows or substances. Bother. I shall probably call them pyroclastics anyway - it's catchy. |
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| Zitterbewegung |
Posted: Fri Apr 11, 2008 8:01 am Post subject: |
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Joined: 24 Dec 2007 Posts: 173
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Ummmpfff.....now I get it. Long week, no brain left. Good example by bunburry btw. _________________ I love deadlines. I like the whooshing sound they make as they fly by |
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| Bunbury |
Posted: Fri Apr 11, 2008 8:07 am Post subject: |
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Forum Ph.D.

Joined: 26 Sep 2007 Posts: 690
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| sunshinewarrior wrote: |
| So pyroclastic can't be used as a catch-all term for all solid+gas flows or substances. Bother. I shall probably call them pyroclastics anyway - it's catchy. |
Now, a pyroclastic coprolite - that would be something to see. |
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| sunshinewarrior |
Posted: Fri Apr 11, 2008 8:46 am Post subject: |
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 Forum Ph.D.

Joined: 26 Sep 2007 Posts: 948 Location: London
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| Bunbury wrote: |
| sunshinewarrior wrote: |
| So pyroclastic can't be used as a catch-all term for all solid+gas flows or substances. Bother. I shall probably call them pyroclastics anyway - it's catchy. |
Now, a pyroclastic coprolite - that would be something to see. |
Well... if you ever visit London...  |
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