Solid diprotium saturated vapour density

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Discussion Overview

The discussion revolves around the equilibrium vapour density of bulk solid diprotium at a temperature of 2.7 K. Participants explore the relationship between temperature and vapour density, as well as the implications of these values in different contexts, such as molecular clouds and global warming.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • One participant inquires about the precise equilibrium vapour density of solid diprotium at 2.7 K and notes that the density of saturated vapour decreases exponentially with temperature.
  • Another participant questions the focus on solid diprotium instead of regular hydrogen and suggests that approximate values might suffice in practical applications.
  • A participant provides a vapor pressure equation for solid hydrogen and calculates the log P at 2.7 K to be about -13, while expressing uncertainty about the accuracy of this extrapolation.
  • Concerns are raised regarding the reliability of the vapor pressure values derived from the Antoine equation, with one participant unable to reproduce the mentioned pressures.
  • Another participant introduces a different equation for vapor pressure and presents calculations that yield slightly divergent results for pressures at 2.7 K, suggesting a range of 10^-13 to 10^-11.5 mm Hg.
  • Participants discuss the relevance of these pressures in the context of molecular clouds, noting the differences in standard units and the potential for solid formation in such environments.

Areas of Agreement / Disagreement

Participants express differing views on the reliability of vapor pressure calculations and the relevance of solid diprotium in various contexts. There is no consensus on the precise equilibrium vapour density or the applicability of the Antoine equation at low temperatures.

Contextual Notes

Some participants note limitations in the available data for temperatures around 2.7 K, as well as the challenges of extrapolating values beyond measurable ranges. The discussion highlights the complexity of vapor pressure calculations and the need for careful consideration of assumptions.

snorkack
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What precisely is the equilibrium vapour density of bulk solid diprotium surface now, at 2,7 K?

The density of the world falls with some power of temperature (which one?). The density of saturated vapour falls exponentially.
At which temperature shall the world saturate with respect to bulk solid diprotium?
 
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What has your research brought you so far ? Any reason you don't like hydrogen and focus on the isotope that's overwhelmingly dominant anyway ?
Google is your friend
http://www.tvu.com/PEngPropsSH2Web.htm
https://www1.eere.energy.gov/hydrogenandfuelcells/tech_validation/pdfs/fcm01r0.pdf
https://en.wikipedia.org/wiki/Solid_hydrogen
https://nvlpubs.nist.gov/nistpubs/jres/47/jresv47n2p63_a1b.pdf

Can you give some more context ? What are you trying to find ? What, for example is the reason you want it 'precisely' (without giving a definition) ? In an age of global warming it might be good enough to use approximate values from physical property approximation expressions and equations of state :rolleyes: ?

Anyway, why look at solid hydrogen when first the oceans freeze, then O2 and N2 condense etc etc ?
snorkack said:
The density of the world falls with some power of temperature (which one?)
The temperature of the earth, of course :wink:
But if the 'which' refers to the power, then I'd start with 1 (see iron/nickel or rock)
 
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BvU said:
What has your research brought you so far ?
Tables tend to break off at temperatures far above 2,7 K.
BvU said:
That one was useful.
Vapor pressure of the solid (20.4 K equilibrium hydrogen) follows the equation

log P (mm Hg) = A + B/T + CT,

where A = 4.62, B = -47.02, C = 0.02023, although the vapor pressures for a mixtures closer to normal hydrogen are somewhat lower [3]
For 2,7 K, I get log P at about -13.
BvU said:
Can you give some more context ? What are you trying to find ? What, for example is the reason you want it 'precisely' (without giving a definition) ? In an age of global warming it might be good enough to use approximate values from physical property approximation expressions and equations of state :rolleyes: ?

Anyway, why look at solid hydrogen when first the oceans freeze, then O2 and N2 condense etc etc ?
The temperature of the earth, of course :wink:
But if the 'which' refers to the power, then I'd start with 1 (see iron/nickel or rock)
Um. Ices are already dust.
Hydrogen and helium are as yet gases, even in molecular clouds.
How does that present equilibrium vapour pressure, of 10-13 mm Hg, compare with pressure in molecular clouds?
 
Dunno, but outer space is different from 'the world' . With a few H atoms per m3 there's no chance of solid formation.

snorkack said:
For 2,7 K, I get log P at about -13
wouldn't trust those numbers: with those values in the Antoine eqn I can't even reproduce the pressures they mention ! and 2.7 K is extrapolating way out...

snorkack said:
compare with pressure in molecular clouds
Those guys have funny 'standard units' P/kB of 104 to 107 cm-3 K, it seems (nice exercise: convert to mm Hg -- I get 10-15 to 10-12 , so perhaps a case of oops! -- but I may well be mistaken. It's past bedtime here )

But then again, when you google 'interstellar ice' or 'volatiles' ... :rolleyes:

Let me know if and how you find inroads for this diprotonium ice !
 
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BvU said:
wouldn't trust those numbers: with those values in the Antoine eqn I can't even reproduce the pressures they mention ! and 22.7 K is extrapolating way out...
Sure, but I could not find actual measurements for 2,7 K.
Do you expect that the pressure would be subject to some sort of Antoine equation?
 
Here's another (table 6) with eqn ##A + B/T + B'\ln T##
Perhaps you can sort out he references mentioned here (section 2.2.30) ; data are on P 6-288
 
BvU said:
Here's another (table 6) with eqn ##A + B/T + B'\ln T##
Page 17. For eH2, it gives A as 2,5 (for Torr), B as -85,3, B' as 2,9.
For 2,7 K, that would mean B/T=-31,6, ln T=1, B´/ln T=2,9
then ln Q=2,5-31,6+2,9=5,4-31,6=-26,2
log Q=ln Q/2,303=-11,5

Thus, two sources give P as 10-13 and 10-11,5 mm Hg respectively. Appreciable divergence, but not unreasonably big seeing how these are extrapolated out of the measurable range. Same ballpark.
How do these numbers - 10-13...10-11 mm Hg - compare to the present pressures in molecular clouds?
 

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