dipole(redirected from DIPOL)
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in electricity and magnetism, point where electric or magnetic force appears to be concentrated. A single electric charge located at a point is sometimes referred to as an electric monopole.
..... Click the link for more information. , in electricity and magnetism.
Any object or system that is oppositely charged at two points or poles, such as a magnet, a polar molecule, or an antenna element. The properties of a dipole are determined by its dipole moment, that is, the product of one of the charges by their separation directed along an axis through the centers of charge. See Dipole moment
An electric dipole consists of two electric charges of equal magnitude but opposite polarity, separated by a short distance (see illustration); or more generally, a localized distribution of positive and negative electricity without net charge whose mean positions of positive and negative charge do not coincide.
Molecular dipoles which exist in the absence of an applied field are called permanent dipoles, while those produced by the action of a field are called induced dipoles. See Polar molecule
The term magnetic dipole originally referred to the fact that a magnet has two poles and, because of these two poles, experiences a torque in a magnetic field if its axis is not along a magnetic flux line of the field. It is now generalized to include electric circuits which, because of the current, also experience torques in magnetic fields. See Magnet
An electric dipole whose moment oscillates sinusoidally radiates electromagnetic waves and is known as a hertzian dipole; it is of interest in developing the theory of electromagnetic radiation. For practical purposes, a half-wave dipole, consisting of two collinear conducting rods, fed at the center, whose combined length equals half the wavelength of the radiation to be transmitted or received, is often used as an antenna element, either by itself or in an array, or as a feed for a reflector. See Electromagnetic radiation
dipole(dÿ -pohl) A simple linear balanced antenna that is fed from its center. It usually consists of two equal-length straight opposing elements, although these may sometimes be folded back on themselves and their far ends joined together in the middle to form a folded dipole. The elements may be of any length but the overall length of the dipole is usually a multiple of half a wavelength of the received (or transmitted) radio wave; the reactive component of the impedance seen at its feed point is then small.
A half-wave dipole has two elements of length one-quarter of a wavelength each and has a radiation resistance of about 70 ohms. A full-wave dipole is twice as long as a half-wave dipole and has a radiation resistance of several thousand ohms. The gain of a half-wave dipole over an isotropic radiator is about two decibels.
There are two types of dipole, electric and magnetic.
Electric dipole. An electric dipole is the aggregate of two opposite point charges that are equal in absolute value and that are separated by a certain distance. The main characteristic of an electric dipole is the dipole moment, which is a vector directed from the negative charge to the positive charge (see Figure 1), whose magnitude is equal to the product of the charge e and the distance l between the two charges: p = eI. The dipole moment determines the electric field of the dipole at a great distance R from the dipole (R » l), as well as the effect of the external electric field on the dipole.
In regions remote from the dipole its electric field E decreases with distance as 1/R3, that is, faster than the field of the point charge (~t/R2). The components of field intensity E along the axis of the dipole (Ep) and perpendicular to p (E1) are proportional to the dipole moment. In the cgs (Gaussian) system of units, they are
Ep = (p/R3) (3 cos2 θ − 1) = (3p/R3) (cos θ sin θ)
where θ is the angle between p and the radius vector R of the point in space where the field of the diode is being measured; the total intensity . Thus, the field intensity on the axis of the diode for θ = 0 is twice that for θ = 90°. For both of these angles the field intensity has only the component Ep. At θ = 0 the direction of the field intensity is parallel to p; at 0 = 90° it is antiparallel (see Figure 2).
The effect of the external electric field on the dipole is also proportional to the magnitude of its dipole moment. A homogeneous field generates a rotational moment M = pE sin α (α is the angle between the vector of intensity of the external electric field E and the dipole moment p; see Figure 3),
which tends to turn the dipole in such a way that its dipole moment is oriented in the direction of the field. In a nonhomogeneous electric field the dipole is acted upon not only by the rotational moment but also by a force tending to pull the dipole into the region of a stronger field (see Figure 4).
The electric field of any neutral system approximately coincides with the field of an equivalent dipole if the distance from the system is much greater than its dimensions. An equivalent dipole is one that has the same dipole moment as the charge system in question. (That is, at great distances from the system, the field is insensitive to the details of charge distribution.) Therefore, in many cases an electric dipole is a good approximation for describing such a system at distances much greater than the system’s dimensions. For example, the molecules of many substances may be regarded approximately as electric dipoles (in the simplest case, such molecules consist of two ions with opposite charges); the atoms and molecules in the external field, which separates their positive and negative charges somewhat, acquire a field-induced dipole moment and themselves become microscopic dipoles.
Electric dipoles whose dipole moment changes with time (as a consequence of a change in their length l or charges e) are sources of electromagnetic radiation.
Magnetic dipole. The study of the interactions of the poles of permanent magnets (C. Coulomb, 1785) led to the idea of the existence of magnetic charges analogous to electric charges. A pair of such charges, of equal magnitude but opposite sign, was regarded as a magnetic dipole (having a magnetic dipole moment). Later it was found that magnetic charges do not exist and that magnetic fields are created by moving electric charges—that is, electric currents. However, the preservation of the concept of a magnetic dipole was found to be expedient, since at great distances from a closed conductor loop through which current is flowing, the magnetic fields are identical to the fields that would be produced by a magnetic dipole (at great distances from the dipole, the magnetic field of a magnetic dipole is computed according to the same formulas as are used for the electrical field of an electric dipole, except that the magnetic moment of the current is substituted for the electrical moment of a dipole). The magnetic moment of a current system is defined by the magnitude and distribution of the currents. In the simplest case, with a current I flowing through a loop with radius a, the magnetic moment in the cgs system is p = ISn/c, where S = πa2 is the area of the loop; the unit vector n, drawn from the center of the loop, is directed in such a way that, when viewed from its end, the current is seen as flowing counterclockwise (see Figure 5); and c is the speed of light.
The analogy between a magnetic dipole and a current-carrying conductor loop may also be followed in examining the effects of the magnetic field on a current. In a homogeneous magnetic field the current-carrying conductor loop is subjected to a force moment that tends to rotate the loop in such a way that its magnetic moment assumes the direction of the field; in a nonhomogeneous field such closed-loop currents (“magnetic dipoles”) are pulled into the region of greatest field intensity. This interaction of a magnetic field and a magnetic dipole is the basis of some physical processes, such as the separation of particles with different magnetic moments (nuclei, atoms, or molecules), whose magnetic moments depend on the motion of the charged elementary particles of which they are composed, as well as on the magnetic moments associated with the spin of the particles. A beam of such particles separates upon passing through a nonhomogeneous magnetic field because the change in the trajectory of a particle (caused by the field) is greater for particles with greater magnetic moments.
However, the analogy between a magnetic dipole and a current-carrying conductor loop (the equivalence theory) is not complete. For example, in the center of a conductor loop
the magnetic field intensity is not only not equal to the field intensity of an “equivalent” dipole but is also of opposite direction (see Figure 6). The magnetic lines of feree, as distinct from electrical lines offeree, which originate and terminate in charge locations, are closed.
REFERENCESFeynman, R., R. Layton, and M. Sands. Feinmanovskie lektsii po fizike, fasc. 5: Elektrichestvo i magnetizm. Moscow, 1966. Chapter 6. [Translated from English.]
Kalashnikov, S. G. Elektrichestvo. Moscow, 1956. Section 17. (Obshchii kurs fiziki, vol. 2.)
Kirenskii, L. V. Magnetizm, 2nd ed. Moscow, 1967.
Tamm, I. E. Osnovy teorii elektrichestva, 7th ed. Moscow, 1957.
G. IA. MIAKISHEV and V. I. GRIGOR’EV