Two models are proposed to explain the heat source maintaining the liquid water ocean beneath the icy crust of Saturn's moon, Enceladus.
Tidal Heating Model
Orbital resonance with other moons causes gravitational tidal flexing of Enceladus's rocky core. This flexing generates significant frictional heat concentrated in the core, maintaining core temperatures above and driving high-temperature hydrothermal activity at the core-ocean boundary.
Radioactive Decay Model
The primary heat source is the decay of radioactive isotopes within the core. This decay produces a low-intensity, uniform heat flux. Because radioactive isotopes have decayed over billions of years, current core temperatures are predicted to be low, not exceeding .
Spacecraft measurements detect silica () nanoparticles in the plumes erupting from Enceladus's south polar fractures. Laboratory experiments demonstrate that these nanoparticles can only form when liquid water interacts with rock at temperatures of at least .
Which of the following statements best describes how this finding relates to the two models?
- It supports the Tidal Heating Model and contradicts the Radioactive Decay Model, because the required formation temperature for silica nanoparticles is within the range predicted by the Tidal Heating Model but exceeds the limit predicted by the Radioactive Decay Model.Answer
- BIt contradicts the Tidal Heating Model and supports the Radioactive Decay Model, because the presence of silica nanoparticles indicates that Enceladus has a cold core below .
- CIt contradicts both models, because the formation temperature of is incompatible with both the high temperatures of the Tidal Heating Model and the low temperatures of the Radioactive Decay Model.
- DIt supports both models, because both tidal flexing and radioactive decay are expected to produce core temperatures high enough to facilitate the chemical reactions that form silica nanoparticles.