The areal velocity of a planet is defined as the rate at which the planet sweeps out area in its orbit. For a planet of mass \( M \) and distance \( r \) from the Sun, the areal velocity \( A \) is given by: \[ A = \frac{dA}{dt} = \frac{1}{2} r^2 \omega, \] where \( r \) is the radius vector and \( \omega \) is the angular velocity.
Step 1: Relationship between angular momentum and areal velocity
The angular momentum \( L \) of a planet is given by: \[ L = M r^2 \omega, \] where \( M \) is the mass of the planet and \( r^2 \omega \) is the angular momentum per unit mass.
Now, using the expression for areal velocity \( A = \frac{1}{2} r^2 \omega \), we can solve for \( r^2 \omega \): \[ r^2 \omega = 2A. \]
Step 2: Final angular momentum
Substitute \( r^2 \omega = 2A \) into the expression for angular momentum: \[ L = M \times 2A = 2MA. \] Thus, the angular momentum of the planet is \( 2MA \), which corresponds to option (C).
Two point charges M and N having charges +q and -q respectively are placed at a distance apart. Force acting between them is F. If 30% of charge of N is transferred to M, then the force between the charges becomes:
If the ratio of lengths, radii and Young's Moduli of steel and brass wires in the figure are $ a $, $ b $, and $ c $ respectively, then the corresponding ratio of increase in their lengths would be: