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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?
What temperature/phase(solid, liquid, vapor)? Liquid kinetics are O(m) different from solid/vapor.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?
I believe he is talking about hydrogen-deuterium exchange, not just mixing.Bystander said:https://en.wikipedia.org/wiki/Norwegian_heavy_water_sabotage ;
Totally forgot about this. Liquid phase? Fast as you can mechanically mix/stir it together.
Light water, or H2O, consists of two hydrogen atoms and one oxygen atom. Heavy water, or D2O, contains deuterium, a hydrogen isotope with an extra neutron. Semiheavy water, or HDO, has a mixture of regular hydrogen and deuterium.
The equilibrium between light, heavy, and semiheavy water occurs through the process of isotopic exchange, where hydrogen atoms in water molecules can exchange with deuterium atoms. This process reaches equilibrium based on the relative concentrations of light and heavy water.
Studying the equilibrium between light, heavy, and semiheavy water can provide insights into chemical reactions, biological processes, and environmental studies. It can also be used in isotope labeling experiments and nuclear magnetic resonance spectroscopy.
The equilibrium between light, heavy, and semiheavy water can be measured using techniques such as mass spectrometry, infrared spectroscopy, and nuclear magnetic resonance. These methods can determine the relative concentrations of different isotopes in water samples.
Yes, the equilibrium between light, heavy, and semiheavy water can be influenced by factors such as temperature, pressure, and the presence of catalysts. Changes in these conditions can affect the rate of isotopic exchange and the distribution of isotopes in water molecules.