Light Heavy and Semiheavy Water Equilibrium

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Discussion Overview

The discussion centers around the equilibrium process of mixing H2O and D2O, specifically focusing on the time it takes for the system to reach equilibrium and the factors influencing this process, such as temperature and phase. Participants explore the kinetics of hydrogen-deuterium exchange in liquid water at room temperature.

Discussion Character

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

Main Points Raised

  • One participant asks how long it takes for a mix of H2O and D2O to equilibrate, suggesting a range from microseconds to centuries.
  • Another participant emphasizes the importance of temperature and phase, noting that liquid kinetics differ significantly from solid or vapor phases.
  • Participants agree that the process occurs in the liquid phase and can be fast, potentially as quick as mechanical mixing allows.
  • There is a suggestion that the process resembles acid-base reactions, which are typically fast, possibly in the nanosecond range.
  • One participant expresses uncertainty about calculating the equilibrium from first principles due to the complexity of the involved species and reactions.
  • A later reply provides a qualitative explanation of how hydrogen bonds and the presence of H+ ions facilitate rapid exchange between water molecules, although it acknowledges that this explanation is not strictly rigorous.

Areas of Agreement / Disagreement

Participants generally agree that the mixing process is fast in the liquid phase, but there is no consensus on a specific time frame for the equilibrium to be reached. Some participants propose that it could be as quick as nanoseconds, while others suggest a fraction of a second, indicating a range of views on the kinetics involved.

Contextual Notes

Participants note the complexity of the equilibrium involving multiple species, including H2O, HDO, D2O, H+, D+, OH-, and OD-, which complicates the analysis of the reaction kinetics.

Who May Find This Useful

This discussion may be of interest to those studying chemical kinetics, physical chemistry, or anyone exploring the properties of water and deuterium oxide in various phases.

Vanadium 50
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If I start with a mix of half H2O and half D2O, when it equilibrates it will be half HDO, a quarter H2O and a quarter D2O. My question is "how long does this take?". Ballpark is fine - microsecodnds? Days? Centuries?
 
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Vanadium 50 said:
If I start with a mix of half H2O and half D2O, when it equilibrates it will be half HDO, a quarter H2O and a quarter D2O. My question is "how long does this take?". Ballpark is fine - microsecodnds? Days? Centuries?
What temperature/phase(solid, liquid, vapor)? Liquid kinetics are O(m) different from solid/vapor.
 
Liquid water, room temperature. Maybe a little cooler.
 
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Mixing limited, technically this is not much different from acid/base reactions and these are quite fast, in nanosecond range if memory serves me well.
 
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Thanks. I guess I could think of it as an acid-base reaction, between some very week acids and bases. I don't know the pH of D2O, but imagine it's around 7.3.

Calculating from 1st principles looks like a nightmare, since you have a 6-way equilibrium between H2O, HDO, D2O, H+, D+, OH-, and OD-. (Plus the complication of whether H+ is really H3O+) But "a tint fraction oif a second" is a good enough answer for me.
 
I am not sure what that link is meant to say. It's just there.

It dies not mention a time, which is my original question. It does say, indirectly, that water (H2O) has a pH of 7. which is not news. (D2O I looked up and it is 7.4, I estimated 7.3)

I think @Borek answered my question. "As fast as they physically can mix"
 
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Handwavy, but more detailed answer. If you put several water molecules side by side, they will get linked by hydrogen bonds. Resulting four membered ring is highly symmetrical (even if not flat) and the bonds will start oscillating, resulting in a very quick exchange of H and D between water molecules. In the presence of H+ from water autodissociation this is made even easier, as H+ will attach itself to one of the lone electron pairs of a molecule (red outlined part). Charge will delocalize to all hydrogens three hydrogens (as in H3O+), which makes them even more eager to bond to neighbor water molecules, which further speeds up bond oscillations, to the point where charge easily jumps between water molecules, rearranging which hydrogen is attached to each oxygen on the way. That's actually why limiting ion conductivity of H+ is anomalously high, several times higher than that of any other ion - H+ doesn't have to travel by itself, it is charge that jumps (not the case of, say, Na+, which has to meticulously navigate between water molecules).

This explanation is far from being strict, but gives good intuition, and shows why individual water molecules in liquid water are not as "separate" as molecules in other liquids.
 
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