### Heat Sources of Enceladus' Ocean
Enceladus, a small icy moon of Saturn, possesses a global subsurface liquid water ocean beneath its icy crust. Scientists debate the primary mechanism responsible for generating the heat necessary to maintain this liquid ocean.
Hypothesis 1
The ocean is kept warm primarily by *tidal dissipation*. As Enceladus orbits Saturn, gravitational forces from Saturn and neighboring moons continuously flex Enceladus’s porous, rocky core. This flexing creates frictional heating in the rock, which directly warms the water circulating through the core. This mechanism is highly dynamic, concentrating heat generation in active zones and producing localized hydrothermal temperatures exceeding .
Hypothesis 2
The ocean is kept warm primarily by *radiogenic heating*. The rocky core of Enceladus contains unstable radioactive isotopes, such as potassium-40 () and uranium-235 (). The decay of these isotopes releases a steady flow of thermal energy. Because the isotopes are uniformly distributed throughout the core, this decay produces a gentle, uniform warmth, with maximum core temperatures reaching no higher than .
New Evidence
Astronomers analyzing data from a space probe detect nanometer-sized silica () particles in the plumes of vapor erupting from Enceladus’s southern polar crust. Laboratory experiments show that these specific nanometer-sized silica particles can only form when mineral-rich water is heated to temperatures above and subsequently mixed with cold water.
Based on this information, how does the detection of the nanometer-sized silica particles in Enceladus's plumes affect the two hypotheses?
- AIt supports Hypothesis 2 and weakens Hypothesis 1, because the uniform heat from radioactive decay is required to sustain the chemical environment needed to precipitate silica.
- BIt weakens both Hypothesis 1 and Hypothesis 2, because the high temperature requirement indicates that Enceladus has a completely molten core, contradicting both hypotheses.
- It supports Hypothesis 1 and weakens Hypothesis 2, because the particles require hydrothermal temperatures that are attainable under Hypothesis 1 but exceed the maximum temperature predicted by Hypothesis 2.Cevap
- DIt supports both Hypothesis 1 and Hypothesis 2, because both tidal dissipation and radiogenic heating would lead to the widespread deposition of silica throughout the ice shell.