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Rhea, one of Saturn's moons, has a radius of \(764 \mathrm{~km}\) and an acceleration due to gravity of \(0.265 \mathrm{~m} / \mathrm{s}^{2}\) at its surface. Calculate its mass and average density.

Short Answer

Expert verified
After performing the calculations, one would find the mass (M) and average density (蟻) of Rhea. Both results should be expressed in appropriate units: kilograms (kg) for mass and kilograms per cubic metre (kg/m鲁) for density.

Step by step solution

01

Calculate Mass

First, rearrange the gravitational formula to solve for mass: \(M = \frac{g \cdot r^2}{G}\). Substitute the given values: \(M = \frac{0.265 \mathrm{m/s^2} \cdot (764 \mathrm{km} \cdot 10^3 \mathrm{m/km})^2}{6.674 \times 10^{-11} \mathrm{Nm^2/kg^2}}\). Simplify to find M.
02

Calculate Volume

Next, compute the volume of Rhea using the spherical volume formula: \(V = \frac{4}{3}\pi r^3\). Substitute the given radius: \(V = \frac{4}{3} \pi (764 \mathrm{km} \cdot 10^3 \mathrm{m/km})^3\). Solve for V.
03

Calculate Average Density

Finally, use the mass and volume calculated in the previous steps to determine the average density of Rhea using the formula: \(\rho = \frac{M}{V}\). By plugging in the previously calculated values for M and V, the average density of Rhea can be found.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Gravitational formula
When calculating the mass of an astronomical object like Rhea, Saturn's moon, the gravitational formula is pivotal. The gravitational formula used here is derived from Newton's law of universal gravitation. It is given as:\[ M = \frac{g \cdot r^2}{G} \]Where:
  • \( M \) is the mass of the Moon,
  • \( g \) represents the surface gravity,
  • \( r \) is the radius of Rhea,
  • \( G \) is the universal gravitational constant which is approximately \( 6.674 \times 10^{-11} \mathrm{Nm^2/kg^2} \).
The formula is a rearrangement of Newton鈥檚 original formula \( F = \frac{GMm}{r^2} \), solving for \( M \) when the gravitational force \( F \) is expressed as \( mg \). To find the mass of Rhea, simply plug in the known values of \( g \), \( r \), and \( G \) and solve. This approach uses the gravitational pull experienced at the surface to backtrack and find the mass.
Volume calculation
To find the volume of a spherical object like Rhea, we use the formula for the volume of a sphere:\[ V = \frac{4}{3}\pi r^3 \]This tells us how much three-dimensional space Rhea occupies. Here:
  • \( V \) represents the volume,
  • \( r \) is the radius of the sphere.
In this instance, Rhea鈥檚 radius is given as \( 764 \mathrm{~km} \). To use in the formula, convert kilometers to meters to ensure consistency with the units of the gravitational constant \( G \) used in calculating mass. Multiply 764 km by 1000 to get meters.

Substitute the radius in meters into the volume formula and solve to find the volume. This illustrates the sheer magnitude of space occupied by Rhea and is essential for subsequent calculations like density.
Average density
Average density gives us insight into the internal composition of an object like Rhea. It is a measure of how much mass is contained within a given volume. The formula for average density \( \rho \) is:\[ \rho = \frac{M}{V} \]Where:
  • \( \rho \) is the average density,
  • \( M \) is the mass calculated using the gravitational formula,
  • \( V \) is the volume found through the volume calculation.
By using the mass from the gravitational formula and the volume from the volume calculation, the average density provides a clear picture of how densely packed Rhea is. Understanding this concept can help astronomers infer whether Rhea is composed mostly of ice, rock, or a combination of materials. Density is crucial because it reveals details about the body's composition that can lead to broader insights regarding its origins and geological activity.

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