Namaste, future engineers! Welcome to this deep dive into the fascinating world of Gravitational Field and Potential. In our previous discussions, we understood Newton's Law of Gravitation, which described the force of attraction between two point masses. But how does this force "act at a distance"? This is where the concept of a
field comes into play. Just like a king has his 'sphere of influence,' every mass creates a 'gravitational field' around itself, and any other mass entering this field experiences a gravitational force.
Let's begin our journey by building these concepts from the ground up, progressively moving towards the complexities required for JEE Main & Advanced.
### 1. The Gravitational Field (or Gravitational Field Intensity)
Imagine you place a small test mass, $m_0$, at some point in space. If it experiences a gravitational force, then there must be a gravitational field present at that point, created by other masses.
#### 1.1 Definition and Derivation for a Point Mass
The
gravitational field intensity (often simply called gravitational field) at a point in space is defined as the gravitational force experienced by a unit test mass placed at that point. It's a vector quantity, as it has both magnitude and direction.
Let's say a source mass $M$ creates a gravitational field. If we place a test mass $m_0$ at a distance $r$ from $M$, the gravitational force on $m_0$ is given by Newton's Law:
$vec{F} = -frac{GMm_0}{r^2}hat{r}$
where $hat{r}$ is a unit vector pointing from $M$ to $m_0$, and the negative sign indicates an attractive force (towards $M$).
According to our definition, the gravitational field intensity $vec{g}$ is:
$vec{g} = frac{vec{F}}{m_0}$
Substituting the expression for $vec{F}$:
$vec{g} = frac{-frac{GMm_0}{r^2}hat{r}}{m_0}$
$vec{g} = -frac{GM}{r^2}hat{r}$
*
Magnitude: $g = frac{GM}{r^2}$
*
Direction: Towards the source mass $M$.
*
Units: The units of gravitational field intensity are Newtons per kilogram (N/kg) or, equivalently, meters per second squared (m/sยฒ), which is the unit of acceleration. This tells us that gravitational field intensity is essentially the
acceleration due to gravity at that point.
#### 1.2 Principle of Superposition
If there are multiple source masses $M_1, M_2, M_3, ...$, the net gravitational field at any point is the vector sum of the gravitational fields produced by each individual mass.
$vec{g}_{net} = vec{g}_1 + vec{g}_2 + vec{g}_3 + ...$
This principle is fundamental for calculating fields due to complex distributions.
### 2. Gravitational Field Due to Various Mass Distributions
Let's apply our understanding to some common geometries:
#### 2.1 Gravitational Field Due to a Uniform Spherical Shell
Consider a uniform spherical shell of mass $M$ and radius $R$.
*
Case 1: Outside the shell (r > R)
For any point outside the shell, it can be proven (using integral calculus or Gauss's Law for Gravitation, which is analogous to Electrostatics) that the entire mass of the shell behaves as if it were concentrated at its center.
Therefore, the gravitational field intensity is:
$g_{out} = frac{GM}{r^2}$ (directed towards the center)
*
Case 2: Inside the shell (r < R)
This is a crucial result. For any point inside a uniform spherical shell, the net gravitational field intensity is
zero. Imagine a point inside the shell. We can draw a double cone originating from this point. The mass elements cut by the cones on opposite sides of the point will exert forces that precisely cancel each other out.
$g_{in} = 0$
*
At the surface (r = R):
$g_{surface} = frac{GM}{R^2}$
Region |
Distance (r) |
Gravitational Field (g) |
|---|
Outside the shell |
r > R |
$frac{GM}{r^2}$ |
On the surface |
r = R |
$frac{GM}{R^2}$ |
Inside the shell |
r < R |
0 |
#### 2.2 Gravitational Field Due to a Uniform Solid Sphere
Consider a uniform solid sphere of mass $M$ and radius $R$.
*
Case 1: Outside the sphere (r > R)
Similar to the spherical shell, for any point outside a uniform solid sphere, the entire mass can be considered to be concentrated at its center.
Therefore:
$g_{out} = frac{GM}{r^2}$ (directed towards the center)
*
Case 2: Inside the sphere (r < R)
This is where it gets interesting and is a frequent topic in JEE. For a point inside the sphere, only the mass of the sphere *enclosed within the radius r* contributes to the gravitational field. The outer shell of mass (from r to R) does not contribute (as per the spherical shell result).
Let the density of the sphere be $
ho = frac{M}{frac{4}{3}pi R^3}$.
The mass enclosed within a radius $r$ ($M_{in}$) is:
$M_{in} =
ho cdot frac{4}{3}pi r^3 = left(frac{M}{frac{4}{3}pi R^3}
ight) cdot frac{4}{3}pi r^3 = M frac{r^3}{R^3}$
Now, treat this enclosed mass $M_{in}$ as a point mass at the center. The field at distance $r$ is:
$g_{in} = frac{GM_{in}}{r^2} = frac{G(M frac{r^3}{R^3})}{r^2}$
$g_{in} = frac{GMr}{R^3}$ (directed towards the center)
* At the center (r = 0): $g_{center} = 0$.
* At the surface (r = R): $g_{surface} = frac{GMR}{R^3} = frac{GM}{R^2}$. (This matches the outside formula at r=R).
Region |
Distance (r) |
Gravitational Field (g) |
|---|
Outside the sphere |
r > R |
$frac{GM}{r^2}$ |
On the surface |
r = R |
$frac{GM}{R^2}$ |
Inside the sphere |
r < R |
$frac{GMr}{R^3}$ |
At the center |
r = 0 |
0 |
The field $g$ increases linearly from 0 at the center to $frac{GM}{R^2}$ at the surface, and then decreases as $1/r^2$ outside the sphere.
#### 2.3 Gravitational Field Due to a Uniform Ring on its Axis
Consider a uniform ring of mass $M$ and radius $R$. We want to find the field at a point $P$ on its axis, at a distance $x$ from its center.
* Let's take a small mass element $dm$ on the ring. The distance from $dm$ to $P$ is $s = sqrt{R^2 + x^2}$.
* The field due to $dm$ at $P$ is $dg = frac{G dm}{s^2}$.
* This $dg$ has two components: one along the axis ($dg_x$) and one perpendicular to the axis ($dg_y$).
* Due to symmetry, the perpendicular components from all diametrically opposite elements will cancel out. Only the axial components add up.
* The axial component of $dg$ is $dg_x = dg cos heta$, where $cos heta = frac{x}{s}$.
* So, $dg_x = frac{G dm}{s^2} frac{x}{s} = frac{G dm cdot x}{(R^2 + x^2)^{3/2}}$.
* To find the total field, integrate $dg_x$ over the entire ring:
$g = int dg_x = int_0^M frac{G x}{(R^2 + x^2)^{3/2}} dm$
Since $G, x, R$ are constants for the integration,
$g = frac{Gx}{(R^2 + x^2)^{3/2}} int_0^M dm$
$g = frac{GMx}{(R^2 + x^2)^{3/2}}$ (directed towards the center of the ring if $x>0$)
*
Special Cases:
* At the center of the ring (x = 0): $g = 0$. This makes sense due to symmetry.
* Far away from the ring (x >> R): $g approx frac{GMx}{(x^2)^{3/2}} = frac{GMx}{x^3} = frac{GM}{x^2}$. The ring behaves like a point mass.
*
Maximum Field: The field intensity is maximum at some point on the axis. To find this, we differentiate $g$ with respect to $x$ and set it to zero ($frac{dg}{dx} = 0$). This yields $x = pm frac{R}{sqrt{2}}$.
### 3. Gravitational Potential Energy (U)
Just like any conservative force, the gravitational force can be associated with a potential energy.
#### 3.1 Definition and Derivation
The
gravitational potential energy of a system of two masses is the work done by an external agent to bring the masses from infinite separation to their current separation without any change in kinetic energy (i.e., slowly). Alternatively, it's the negative of the work done by the gravitational force in the same process.
Consider two point masses $M$ and $m$ initially at infinite separation. We bring $m$ from infinity to a distance $r$ from $M$.
The gravitational force on $m$ at a distance $x$ from $M$ is $F_g = -frac{GMm}{x^2}$ (attractive).
The work done by the gravitational force is:
$W_g = int_{infty}^{r} vec{F}_g cdot dvec{x} = int_{infty}^{r} -frac{GMm}{x^2} dx = -GMm left[ -frac{1}{x}
ight]_{infty}^{r}$
$W_g = -GMm left( -frac{1}{r} - (-frac{1}{infty})
ight) = -GMm left( -frac{1}{r} - 0
ight)$
$W_g = frac{GMm}{r}$
The change in potential energy is $Delta U = -W_g$. Since we define potential energy to be zero at infinite separation ($U_infty = 0$), the potential energy at distance $r$ is:
$U_r - U_infty = -W_g$
$U_r - 0 = -frac{GMm}{r}$
$U = -frac{GMm}{r}$
*
Negative Sign: The negative sign indicates that the gravitational force is attractive. Energy must be supplied to separate the masses, meaning their bound state has negative potential energy. This implies that the system is stable and attractive.
*
Reference Point: Gravitational potential energy is conventionally taken as zero when the masses are infinitely far apart.
*
Units: Joules (J).
*
Scalar Quantity: Potential energy is a scalar.
#### 3.2 Gravitational Potential Energy of a System of Multiple Point Masses
For a system of more than two point masses, the total gravitational potential energy is the sum of the potential energies of all unique pairs of masses.
For three masses $m_1, m_2, m_3$:
$U_{total} = U_{12} + U_{13} + U_{23} = -frac{Gm_1m_2}{r_{12}} - frac{Gm_1m_3}{r_{13}} - frac{Gm_2m_3}{r_{23}}$
### 4. Gravitational Potential (V)
Just as gravitational field is force per unit mass,
gravitational potential is gravitational potential energy per unit mass. It's a scalar quantity.
#### 4.1 Definition and Derivation for a Point Mass
The
gravitational potential at a point in space is defined as the gravitational potential energy per unit test mass placed at that point. It's also the work done by an external agent (per unit mass) to bring a test mass from infinity to that point without acceleration.
If a source mass $M$ creates a field, and a test mass $m_0$ at distance $r$ has potential energy $U = -frac{GMm_0}{r}$, then the gravitational potential $V$ is:
$V = frac{U}{m_0}$
$V = -frac{GM}{r}$
*
Negative Sign: Similar to potential energy, the negative sign indicates attraction and that potential decreases as we approach the mass.
*
Reference Point: Potential is zero at infinity ($V_infty = 0$).
*
Units: Joules per kilogram (J/kg).
*
Scalar Quantity: Potentials can be added algebraically.
#### 4.2 Relationship between Gravitational Field and Potential
Gravitational field is related to gravitational potential by:
**$vec{g} = -
abla V$** (where $
abla$ is the gradient operator)
In one dimension (e.g., for a point mass or spherical distribution, where potential depends only on $r$):
$g = -frac{dV}{dr}$
This means the gravitational field points in the direction of decreasing potential. If you know the potential, you can find the field by taking its negative gradient. Conversely, if you know the field, you can find the potential by integrating:
$V_B - V_A = -int_A^B vec{g} cdot dvec{r}$
#### 4.3 Principle of Superposition for Potential
For a system of multiple point masses, the total gravitational potential at any point is the algebraic sum of the potentials due to individual masses.
$V_{net} = V_1 + V_2 + V_3 + ...$
### 5. Gravitational Potential Due to Various Mass Distributions
#### 5.1 Gravitational Potential Due to a Uniform Spherical Shell
Consider a uniform spherical shell of mass $M$ and radius $R$.
*
Case 1: Outside the shell (r > R)
Similar to the field, the shell behaves as if its mass is concentrated at the center for points outside.
$V_{out} = -frac{GM}{r}$
*
Case 2: Inside the shell (r < R)
Here, the field inside is zero ($g_{in}=0$). Using the relation $dV = -g dr$:
$V_r - V_R = -int_R^r g_{in} dr = -int_R^r 0 dr = 0$
So, $V_r = V_R$. This means the potential inside the shell is constant and equal to the potential at its surface.
$V_{in} = V_{surface} = -frac{GM}{R}$
$V_{in} = -frac{GM}{R}$
Region |
Distance (r) |
Gravitational Potential (V) |
|---|
Outside the shell |
r > R |
$-frac{GM}{r}$ |
On the surface |
r = R |
$-frac{GM}{R}$ |
Inside the shell |
r < R |
$-frac{GM}{R}$ |
The potential is constant inside and smoothly transitions to decreasing outside.
#### 5.2 Gravitational Potential Due to a Uniform Solid Sphere
Consider a uniform solid sphere of mass $M$ and radius $R$.
*
Case 1: Outside the sphere (r > R)
$V_{out} = -frac{GM}{r}$
*
Case 2: Inside the sphere (r < R)
This is another crucial derivation for JEE Advanced. We use $V_r - V_infty = -int_infty^r vec{g} cdot dvec{r}$.
We break the integral into two parts: from $infty$ to $R$, and from $R$ to $r$.
$V_r = -int_infty^R g_{out} dr - int_R^r g_{in} dr$
$V_r = -int_infty^R frac{GM}{r^2} dr - int_R^r frac{GMr}{R^3} dr$
$V_r = -GM left[ -frac{1}{r}
ight]_infty^R - frac{GM}{R^3} left[ frac{r^2}{2}
ight]_R^r$
$V_r = -GM left( -frac{1}{R} - 0
ight) - frac{GM}{2R^3} (r^2 - R^2)$
$V_r = frac{GM}{R} - frac{GM r^2}{2R^3} + frac{GM R^2}{2R^3}$
$V_r = frac{GM}{R} - frac{GM r^2}{2R^3} + frac{GM}{2R}$
$V_{in} = -frac{GM}{2R^3}(3R^2 - r^2)$
*
At the surface (r = R):
$V_{surface} = -frac{GM}{2R^3}(3R^2 - R^2) = -frac{GM}{2R^3}(2R^2) = -frac{GM}{R}$. (Matches the outside formula).
*
At the center (r = 0):
$V_{center} = -frac{GM}{2R^3}(3R^2 - 0) = -frac{3GM}{2R}$
This means the potential at the center is $1.5$ times the potential at the surface (in magnitude). It's the lowest (most negative) potential.
Region |
Distance (r) |
Gravitational Potential (V) |
|---|
Outside the sphere |
r > R |
$-frac{GM}{r}$ |
On the surface |
r = R |
$-frac{GM}{R}$ |
Inside the sphere |
r < R |
$-frac{GM}{2R^3}(3R^2 - r^2)$ |
At the center |
r = 0 |
$-frac{3GM}{2R}$ |
The potential is parabolic inside (most negative at center) and then increases as $1/r$ outside (still negative).
#### 5.3 Gravitational Potential Due to a Uniform Ring on its Axis
Consider a uniform ring of mass $M$ and radius $R$. We want to find the potential at a point $P$ on its axis, at a distance $x$ from its center.
* Take a small mass element $dm$ on the ring. The distance from $dm$ to $P$ is $s = sqrt{R^2 + x^2}$.
* The potential due to $dm$ at $P$ is $dV = -frac{G dm}{s} = -frac{G dm}{sqrt{R^2 + x^2}}$.
* Since potential is a scalar, we can simply integrate $dV$ over the entire ring:
$V = int dV = int_0^M -frac{G}{sqrt{R^2 + x^2}} dm$
Since $G, R, x$ are constants for the integration,
$V = -frac{G}{sqrt{R^2 + x^2}} int_0^M dm$
$V = -frac{GM}{sqrt{R^2 + x^2}}$
*
Special Cases:
* At the center of the ring (x = 0): $V = -frac{GM}{R}$. This is the minimum (most negative) potential on the axis.
* Far away from the ring (x >> R): $V approx -frac{GM}{sqrt{x^2}} = -frac{GM}{x}$. The ring behaves like a point mass.
### 6. JEE Advanced Perspective and Important Considerations
*
Calculus is Key: For continuous mass distributions (rods, discs, non-uniform spheres), integration techniques are indispensable for calculating both field and potential.
*
Sign Conventions: Always be mindful of the negative signs in potential and potential energy equations. They signify the attractive nature of gravity and the choice of zero potential at infinity.
*
Vector vs. Scalar: Gravitational field is a vector, so fields from multiple sources add vectorially. Gravitational potential is a scalar, so potentials from multiple sources add algebraically. This makes calculating potential often simpler.
*
Relationship: Remember the powerful relation $vec{g} = -
abla V$. It's a quick way to find one from the other.
*
Work Done: Work done by gravity in moving a mass $m$ from A to B is $W_{AB} = U_A - U_B = -m(V_B - V_A)$. Work done by an external agent is $W_{ext} = U_B - U_A = m(V_B - V_A)$.
*
Hollow vs. Solid Sphere: The distinction between hollow shells and solid spheres for internal points is critical for both field and potential.
* Hollow: $g_{in}=0$, $V_{in}=$ constant.
* Solid: $g_{in} propto r$, $V_{in} propto (3R^2-r^2)$.
*
Gravitational Self-Energy: This is the work done by an external agent to assemble a mass distribution (e.g., a solid sphere) from infinitesimal particles brought from infinity. It is a more advanced concept, often derived by integrating the potential energy of adding successive shells of mass. For a uniform solid sphere of mass M and radius R, the self-energy is
$U_{self} = -frac{3GM^2}{5R}$. This concept is usually tested in JEE Advanced.
By mastering these concepts and their derivations, you'll be well-equipped to tackle a wide range of problems involving gravitational fields and potentials in your JEE preparation! Keep practicing with examples involving various configurations of masses.