If the distance between sun and earth were reduced to half its present value, then the number of days in one year would have been
129
To solve this problem, we need to apply Kepler's Third Law of Planetary Motion, also known as the Law of Periods. This law describes the relationship between the orbital period of a planet and the semi-major axis (average distance) of its orbit around the Sun.
Kepler's Third Law states that the square of the orbital period (\(T\)) of a planet is directly proportional to the cube of the semi-major axis (\(R\)) of its orbit. Mathematically, this can be expressed as:
\[T^2 \propto R^3\]
This proportionality can also be written as:
\[\frac{T^2}{R^3} = \text{constant}\]
This means that for any two objects orbiting the same central body (like planets orbiting the Sun), the ratio of the square of their periods to the cube of their average distances will be the same.
Let's denote the initial conditions (present value) with subscript '1' and the new conditions (reduced distance) with subscript '2'.
According to Kepler's Third Law:
\[\frac{T_1^2}{R_1^3} = \frac{T_2^2}{R_2^3}\]
Now, we can substitute the given values into the equation:
\[T_2^2 = T_1^2 \left( \frac{R_2}{R_1} \right)^3\]
Substitute \(T_1 = 365\) days and \(R_2 = \frac{R_1}{2}\):
\[T_2^2 = (365)^2 \left( \frac{\frac{R_1}{2}}{R_1} \right)^3\]
Simplify the ratio of distances:
\[T_2^2 = (365)^2 \left( \frac{1}{2} \right)^3\]
Calculate the cube of \(\frac{1}{2}\):
\[T_2^2 = (365)^2 \left( \frac{1}{8} \right)\]
To find \(T_2\), take the square root of both sides:
\[T_2 = \sqrt{\frac{(365)^2}{8}}\]
\[T_2 = \frac{365}{\sqrt{8}}\]
We know that \(\sqrt{8} = \sqrt{4 \times 2} = 2\sqrt{2}\).
\[T_2 = \frac{365}{2\sqrt{2}}\]
To rationalize the denominator, multiply the numerator and denominator by \(\sqrt{2}\):
\[T_2 = \frac{365 \times \sqrt{2}}{2\sqrt{2} \times \sqrt{2}}\]
\[T_2 = \frac{365 \times \sqrt{2}}{2 \times 2}\]
\[T_2 = \frac{365 \times \sqrt{2}}{4}\]
Using the approximate value \(\sqrt{2} \approx 1.414\):
\[T_2 = \frac{365 \times 1.414}{4}\]
\[T_2 = \frac{516.11}{4}\]
\[T_2 \approx 129.0275\]
Therefore, if the distance between the Sun and Earth were reduced to half its present value, the number of days in one year would be approximately 129 days.
| Parameter | Current Value | New Value |
|---|---|---|
| Orbital Period (\(T\)) | \(T_1 = 365\) days | \(T_2 = ?\) |
| Distance (\(R\)) | \(R_1\) | \(R_2 = R_1 / 2\) |
Using the relationship \(T^2 \propto R^3\), we calculated \(T_2\) to be approximately 129 days.
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