Discussion Overview
The discussion revolves around the water pressure beneath the ice of Europa, one of Jupiter's moons, and the feasibility of exploring this environment with machines or structures. Participants explore various aspects including the ice thickness, pressure calculations, and the challenges of penetrating the ice layer.
Discussion Character
- Exploratory
- Technical explanation
- Debate/contested
- Experimental/applied
Main Points Raised
- One participant inquires about the potential water pressure under Europa's ice and whether it could be manageable for machines.
- Another participant asks for the surface gravity of Europa and the specific depth of interest, suggesting the need for a formula to calculate pressure based on depth.
- It is noted that scientists estimate Europa's ice shell thickness to be between 10 to 15 miles (15 to 25 kilometers).
- Participants discuss the depth capabilities of submarines, referencing the Los Angeles class submarine and suggesting it could potentially operate at depths of 2,160 meters on Europa.
- There is a question about whether the ice layer could support its own weight without the pressure from the water below, comparing it to a solid ball with varying internal pressures.
- Concerns are raised about the challenges of breaking through the ice, with one participant suggesting mechanical and thermal methods for penetration.
- Another participant proposes the idea of a submarine that could test the concept by diving through Antarctic ice to Lake Vostok before attempting to reach Europa, questioning the thermal conductivity of ice at extreme temperatures.
- Discussion includes the idea that submersibles may not need to worry about pressure if gas pockets are removed from their construction, allowing for deeper exploration.
- It is suggested that a combination of drilling and heating may be the most effective method for penetrating the ice layer.
Areas of Agreement / Disagreement
Participants express various viewpoints on the feasibility of exploring beneath Europa's ice, with no clear consensus on the best methods or the implications of pressure and ice thickness. Multiple competing views remain regarding the challenges and potential solutions for exploration.
Contextual Notes
Limitations include assumptions about the ice thickness, the specific conditions under which exploration would occur, and the technical capabilities of proposed machines or structures. The discussion does not resolve the mathematical or physical challenges presented.