Discussion Overview
The discussion centers on the possibility of generating HOD clathrate by creating an interface between HOD and methane gas. Participants explore the theoretical implications and challenges associated with forming HOD clathrate, particularly in comparison to existing studies on methane hydrates involving H2O and D2O.
Discussion Character
- Exploratory, Technical explanation, Debate/contested
Main Points Raised
- One participant inquires about the feasibility of generating HOD clathrate, noting the lack of literature on the subject compared to methane hydrates with H2O and D2O.
- Another participant mentions that pure HOD will equilibrate to a mixture of HOD, H2O, and D2O due to water's self-ionization.
- A participant speculates that the bulk of HOD would equilibrate before it could freeze to methane clathrate and questions the partitioning of 'heavy methane'.
- Further discussion suggests that attempts to create bulk HOD ice would result in a mixture before clathrate formation could occur, citing differential ionization rates and equilibria.
- One participant asserts that pure HOD clathrate cannot be made due to self-ionization of liquid HOD, recommending reliance on existing D2O studies instead.
- Concerns are raised about the stability of HOD in the liquid phase, which may explain the scarcity of literature on HOD clathrate.
- A participant expresses a desire for alternative opinions but suggests that the discussion may be reaching a conclusion.
Areas of Agreement / Disagreement
Participants generally agree that pure HOD clathrate cannot be formed due to the self-ionization of HOD. However, there are differing views on the implications of this and the potential for further exploration of the topic.
Contextual Notes
The discussion highlights limitations related to the stability of HOD in the liquid phase and the potential for equilibria to affect clathrate formation. There are unresolved questions regarding the specifics of HOD's behavior in relation to methane clathrate synthesis.
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