Potential Gradient
Electric Potential Gradient
- An electric field can be defined in terms of the variation of electric potential at different points in the field:
The electric field at a particular point is equal to the negative gradient of a potential-distance graph at that point
- The potential gradient is defined by the equipotential lines
- These demonstrate the electric potential in an electric field and are always drawn perpendicular to the field lines
Equipotential lines around a radial field or uniform field are perpendicular to the electric field lines
- Equipotential lines are lines of equal electric potential
- Around a radial field, the equipotential lines are represented by concentric circles around the charge with increasing radius
- The equipotential lines become further away from each other
- In a uniform electric field, the equipotential lines are equally spaced
- The potential gradient in an electric field is defined as:
The rate of change of electric potential with respect to displacement in the direction of the field
- The electric field strength is equivalent to this, except with a negative sign:
- Where:
- E = electric field strength (V m-1)
- ΔV = change in potential (V)
- Δr = displacement in the direction of the field (m)
- The minus sign is important to obtain an attractive field around a negative charge and a repulsive field around a positive charge
The electric potential around a positive charge decreases with distance and increases with distance around a negative charge
- The electric potential changes according to the charge creating the potential as the distance r increases from the centre:
- If the charge is positive, the potential decreases with distance
- If the charge is negative, the potential increases with distance
- This is because the test charge is positive
Gravitational Potential Gradient
- A gravitational field can be defined in terms of the variation of gravitational potential at different points in the field:
The gravitational field at a particular point is equal to the negative gradient of a potential-distance graph at that point
- The potential gradient is defined by the equipotential lines
- These demonstrate the gravitational potential in a gravitational field and are always drawn perpendicular to the field lines
- The potential gradient in a gravitational field is defined as:
The rate of change of gravitational potential with respect to displacement in the direction of the field
- Gravitational field strength, g and the gravitational potential, V can be graphically represented against the distance from the centre of a planet, r
- Where:
- g = gravitational field strength (N kg-1)
- ΔV = change in gravitational potential (J kg-1)
- Δr = distance from the centre of a point mass (m)
- The graph of V against r for a planet is:
- The key features of this graph are:
- The values for V are all negative
- As r increases, V against r follows a -1/r relation
- The gradient of the graph at any particular point is the value of g at that point
- The graph has a shallow increase as r increases
- To calculate g, draw a tangent to the graph at that point and calculate the gradient of the tangent
- This is a graphical representation of the equation:
where G and M are constant
Worked example
Determine the change in gravitational potential when travelling from 3 Earth radii (from Earth’s centre) to the surface of the Earth.
Assume that the mass of the Earth is 5.97 × 1024 kg and the radius of the Earth is 6.38 × 106 m
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- Earth’s mass, ME = 5.97 × 1024 kg
- Radius of the Earth, rE = 6.38 × 106 m
- Initial distance, r1 = 3 × rE = 3 × (6.38 × 106) m = 1.914 × 107 m
- Final distance, r2 = 1 × rE = 6.38 × 106 m
- Gravitational constant, G = 6.67 × 10−11 m3 kg−1 s−2
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- When travelling from 3 Earth radii to one Earth radii the potential difference is: −4.16 × 107 J kg−1