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Gravitational Potential due to Uniform solid sphere is considered one of the most asked concept.
16 Questions around this concept.
Which of the following most closely depicts the correct variation of the gravitation potential V(r) due to a large planet of radius R and uniform mass density ? (figures are not drawn to scale)
In a gravitational field potential V at a point, P is defined as negative of work done per unit mass in changing the position of a test mass from some reference point to the given point.
Note-usually reference point is taken as infinity and potential at infinity is taken as Zero.
We know that
$
W=\int \vec{F} \cdot \overrightarrow{d r}
$
So $V=-\frac{W}{m}=-\int \frac{\vec{F} \cdot \overrightarrow{d r}}{m}$
And $\vec{I}=\frac{\vec{F}}{m}$
$
V=-\int \vec{I} \cdot \overrightarrow{d r}
$
$V \rightarrow$ Gravitational potential
$I \rightarrow$ Field Intensity
$d r \rightarrow$ small distance
We can also write
$
I=-\frac{d V}{d r}
$
Means a negative gradient of potential gives the intensity of the field.
The negative sign indicates that in the direction of intensity the potential decreases.
- It is a scalar quantity.
. Unit $\rightarrow$ Joule $/ \mathrm{kg}$ or $\mathrm{m}^2 / \mathrm{sec}^2$
- Dimension : $\left[M^0 L^2 T^{-2}\right]$
Gravitational Potential at a distance 'r'
If the field is produced by a point mass then
$
\begin{aligned}
& I=\frac{G M}{r^2} \\
& V=-\int \vec{I} \cdot \overrightarrow{d r} \\
& \text { So } \\
& V=-\frac{G M}{r}
\end{aligned}
$
at $r=\infty \quad V=0=V_{\max }$
Gravitational Potential difference
In the gravitational field, the work done to move a unit mass from one position to the other is known as Gravitational Potential difference.
If the point mass M is producing the field
Point A and B are shown in the figure.
=Gravitational potential at point A
=Gravitational potential at point B
$r_B \rightarrow$ the distance of mass at $B$
$r_A \rightarrow$ distance of mass at $A$
$\Delta V=$ The gravitational potential difference in bringing unit mass m from point A to point B in the gravitational field produced by $M$.
$
\begin{aligned}
& \Delta V=V_B-V_A=\frac{W_{A \rightarrow B}}{m} \\
& \Delta V=-G M\left[\frac{1}{r_B}-\frac{1}{r_A}\right]
\end{aligned}
$
Superposition of Gravitational potential
The net gravitational potential at a given point due to different point masses (M1,M2,M3…) can be calculated by doing a scalar sum of their individuals Gravitational potential.
$\begin{aligned} V & =V_1+V_2+V_3 \cdots \\ & =-\frac{G M_1}{r_1}-\frac{G M_2}{r_2}-\frac{G M_3}{r_3} \cdots \\ V & =-G \sum_{i=1}^{i=n} \frac{M_i}{r_i} \\ M_i & \rightarrow \text { mass } \\ r_i & \rightarrow \text { distances }\end{aligned}$
Point of zero potential
Let m1 and m2 are separated at a distance d from each other
And P is the point where net Gravitational potential $V=V_1+V_2=0$
Then P is the point of zero Gravitational potential
Let point $P$ is at distance $x$ from $m_1$
Then For point $P$
$
\begin{aligned}
& V=V_1+V_2=0 \\
& -\frac{G m_1}{r_1}-\frac{G m_2}{r_2}=0 \\
& -\frac{G m_1}{x}-\frac{G m_2}{d-x}=0 \\
& \quad x=\frac{m_1 d}{m_1-m_2}
\end{aligned}
$
For Uniform circular ring
$r=$ distance from ring
$a \rightarrow$ radius of Ring
$V \rightarrow$ Potential
At a point on its Axis
$
V=-\frac{G M}{\sqrt{a^2+r^2}}
$
At the center
$
V=-\frac{G M}{a}
$
For Uniform disc
$a \rightarrow$ Radius of disc
M-mass of disc
- At the center of the disc
$
V=-\frac{2 G M}{a}
$
- At a point on its axis
$
V=-\frac{2 G M}{a^2}\left(\sqrt{a^2+x^2}-x\right)
$
For Spherical shell
$R \rightarrow$ Radius of shell
$r \rightarrow$ distance from the center of the shell
- Inside the surface
$
\begin{aligned}
r & <R \\
V & =-\frac{G M}{R}
\end{aligned}
$
- on the surface
$
\begin{aligned}
r & =R \\
V & =-\frac{G M}{R}
\end{aligned}
$
- Outside the surface
$
\begin{aligned}
r & >R \\
V & =-\frac{G M}{r}
\end{aligned}
$
Uniform solid sphere
$R \rightarrow$ Radius of sphere
$M \rightarrow$ Mass of sphere
$r \rightarrow$ distance from the center of sphere
- Inside the surface
$
\begin{aligned}
r & <R \\
V & =-\frac{G M}{2 R}\left[3-\left(\frac{r}{R}\right)^2\right]
\end{aligned}
$
- on the surface
$
V_{\text {surface }}=-\frac{G M}{R}
$
- Outside the surface
$
V=-\frac{G M}{r}
$
- Tip-
$
\text { V centre }=\frac{3}{2} V \text { sur face }
$
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