An electric potential at a point in a static
electric field is given by the
line integral {{Equation box 1 where is an arbitrary path from some fixed reference point to ; it is uniquely determined up to a constant that is added or subtracted from the integral. In electrostatics, the
Maxwell-Faraday equation reveals that the
curl \nabla\times\mathbf{E} is zero, making the electric field
conservative. Thus, the line integral above does not depend on the specific path chosen but only on its endpoints, making V_\mathbf{E} well-defined everywhere. The
gradient theorem then allows us to write: {{Equation box 1 This states that the electric field points "downhill" towards lower voltages. By
Gauss's law, the potential can also be found to satisfy
Poisson's equation: \mathbf{\nabla} \cdot \mathbf{E} = \mathbf{\nabla} \cdot \left (- \mathbf{\nabla} V_\mathbf{E} \right ) = -\nabla^2 V_\mathbf{E} = \rho / \varepsilon_0 where is the total
charge density and \mathbf{\nabla}\cdot denotes the
divergence. The concept of electric potential is closely linked with
potential energy. A
test charge, , has an
electric potential energy, , given by U_ \mathbf{E} = q\,V. The potential energy and hence, also the electric potential, is only defined up to an additive constant: one must arbitrarily choose a position where the potential energy and the electric potential are zero. These equations cannot be used if {{nowrap|\nabla\times\mathbf{E}\neq\mathbf{0},}} i.e., in the case of a
non-conservative electric field (caused by a changing
magnetic field; see
Maxwell's equations). The generalization of electric potential to this case is described in the section .
Electric potential due to a point charge The electric potential arising from a point charge, , at a distance, , from the location of is observed to be V_\mathbf{E} = \frac{1}{4 \pi \varepsilon_0} \frac{Q}{r}, where is the
permittivity of vacuum, is known as the
Coulomb potential. Note that, in contrast to the magnitude of an
electric field due to a point charge, the electric potential scales respective to the reciprocal of the radius, rather than the radius squared. The electric potential at any location, , in a system of point charges is equal to the sum of the individual electric potentials due to every point charge in the system. This fact simplifies calculations significantly, because addition of potential (scalar) fields is much easier than addition of the electric (vector) fields. Specifically, the potential of a set of discrete point charges at points becomes V_\mathbf{E}(\mathbf{r}) = \frac{1}{4\pi\varepsilon_0} \sum_{i=1}^n\frac{q_i}\, where • is a point at which the potential is evaluated; • is a point at which there is a nonzero charge; and • is the charge at the point . And the potential of a continuous charge distribution becomes V_\mathbf{E}(\mathbf{r}) = \frac{1}{4\pi\varepsilon_0} \int_R \frac{\rho(\mathbf{r}')} \mathrm{d}^3 r'\,, where • is a point at which the potential is evaluated; • is a region containing all the points at which the charge density is nonzero; • is a point inside ; and • is the charge density at the point . The equations given above for the electric potential (and all the equations used here) are in the forms required by
SI units. In some other (less common) systems of units, such as
CGS-Gaussian, many of these equations would be altered. == Generalization to electrodynamics ==