Geophysicists investigated the seismic wave attenuation properties of synthetic mantle rock (peridotite) under simulated upper mantle conditions.
In Study 1, five cylindrical peridotite samples with average mineral grain sizes ranging from to were tested at a constant confining pressure of and a fixed temperature of . A torsional oscillation at a frequency of was applied to each sample, and the resulting shear wave attenuation factor () was recorded.
In Study 2, peridotite samples with a fixed average grain size of were held at while the confining pressure was varied from to to measure .
In Study 3, peridotite samples with a fixed grain size of under a constant confining pressure of were tested across temperatures from to to measure .
Based on the experimental procedures described, which of the following correctly identifies the independent variable, dependent variable, and one controlled variable for Study 1, respectively?
- Grain size of the peridotite sample; shear wave attenuation factor (); confining pressureAnswer
- BShear wave attenuation factor (); grain size of the peridotite sample; temperature
- CConfining pressure; shear wave attenuation factor (); grain size of the peridotite sample
- DGrain size of the peridotite sample; temperature; shear wave attenuation factor ()