Geophysicists study the rheology of magma to predict volcanic eruption styles. A volcanologist formulated a hypothesis regarding the combined effects of pressure () and water content () on the viscosity () of rhyolitic magma at a constant temperature of :
*Hypothesis*: Increasing decreases by disrupting silicate network bonds. However, because higher compresses the melt and opposes this bond disruption, the viscosity-reducing effect of adding water (defined as the factor by which decreases when is increased from to ) will become weaker as increases.
To test this hypothesis, the volcanologist measured the viscosity of rhyolitic magma samples at under different combinations of and . The results are shown in the table below:
| Trial | Pressure (, ) | Water content (, ) | Viscosity (, ) |
|---|---|---|---|
| 1 | 50 | 0.1 | |
| 2 | 50 | 1.0 | |
| 3 | 50 | 3.0 | |
| 4 | 150 | 0.1 | |
| 5 | 150 | 1.0 | |
| 6 | 150 | 3.0 | |
| 7 | 300 | 0.1 | |
| 8 | 300 | 1.0 | |
| 9 | 300 | 3.0 |
Which of the following statements best describes how the volcanologist should modify the hypothesis in light of these results?
- Modify the hypothesis to state that the viscosity-reducing effect of water becomes stronger as pressure increases, because the factor by which viscosity decreases when water is added increases as pressure increases.Answer
- BModify the hypothesis to state that the viscosity-reducing effect of water becomes weaker as pressure increases, because the absolute decrease in viscosity when water is added is smallest at .
- CRetain the hypothesis because at each pressure, increasing the water content from to decreases the magma viscosity.
- DModify the hypothesis to state that increasing pressure increases magma viscosity, because compaction at higher pressures prevents water from effectively lubricating the silicate network.