

|
A magnet is an object that has a magnetic field. The word magnet comes from the Greek "magnítis líthos" (μαγνήτης λίθος), which means "magnesian stone". Magnesia is an area in Greece (Now Manisa, Turkey) where deposits of magnetite have been discovered since antiquity.
Contents |
In the modern sense, a magnet is any material that has a magnetic field. It can be in the form of a permanent magnet or an electromagnet. Permanent magnets do not rely upon outside influences to generate their field. Electromagnets rely upon electric current to generate a magnetic field - when the current increases, so does the field. Magnets are attracted to or repelled by other things. If a magnet is strongly attracted to something, then that something is said to have a high permeability. Iron and steel are two examples of materials with very high permeability, and they are strongly attracted to magnets. Liquid oxygen is an example of something with a low permeability, and it is only weakly attracted to a magnetic field. Water has such a low permeability that it is actually repelled by magnetic fields. Everything has a measurable permeability: people, air and even the vacuum of space. The intensity of a magnetic field is measured in units called a "tesla", after the scientist who worked on magnets and electricity.
All normal matter is composed of particles (protons, neutrons, and electrons), and all of these particles have the fundamental property of quantum mechanical spin. Spin gives each one of these particles an associated magnetic field. Because of this, and the fact that the average macroscopic piece of matter contains huge numbers of these particles, it would be expected that all matter would be magnetic. Everyday experience shows that this is not the case.
Within each atom and molecule, the spin of each of these particles is highly ordered as a result of the Pauli Exclusion Principle. However, there is no long range ordering of these spins between atoms and molecules. Without long range ordering, there is no net magnetic field because the magnetic moment of each one of the particles is cancelled by the magnetic moment of other particles.
Permanent magnets are special in that long range ordering does exist. The highest degree of ordering exists within magnetic domains. These domains can be likened to microscopic neighbourhoods in which there is a strong reinforcing interaction between particles, and as a result, a great deal of order. The greater the degree of ordering within and between domains, the greater the resulting field will be.
Long range ordering (and the resulting strong net magnetic field) is one of the hallmarks of a ferromagnetic material.
Electrons play the primary role in generating a magnetic field. Within an atom, electrons can exist either individually or in pairs within any given orbital. When they are paired, the individuals in that pair always have opposite spin (one up, one down). The fact that the spins have opposite orientation means that the two cancel one another. If all electrons are paired, no net magnetic field will be generated.
In some atoms, there are electrons that are unpaired. All magnets have unpaired electrons, but not all atoms with unpaired electrons are ferromagnetic. In order for the material to become ferromagnetic, not only must there be unpaired electrons present, but those unpaired electrons must interact with one another over long ranges such that they are all oriented in the same way. The specific electron configuration of the atoms (as well as the distance between atoms) is what leads to this long range ordering. The electrons find that they can exist in a lower energy state if they all have the same orientation.
An electromagnet, in its simplest form, is a wire that has been coiled into one or more loops. This coil is known as a solenoid. When electric current flows along the coil, a magnetic field is generated around the coil. The orientation of this field can be determined via the right hand rule. The strength of the field is influenced by several factors, including:
The more loops of wire and the greater the current, the stronger the field will be.
If the coil of wire is empty in the center, it will tend to generate a very weak field. Different ferromagnetic or paramagnetic items can be placed in the center of the core with the effect of magnifying the magnetic field, for example an iron nail (soft iron is commonly used for this purpose). The addition of these types of materials can result in a several hundred- to thousand-fold increase of field strength.
At long distances, magnetic fields obey an inverse square law. This means that the field strength is inversely proportional to the distance from the magnet. If the face of an electromagnet is machined to a high degree of precision, it will be able to get much closer to the surface it is trying to attract. Take the case of an electromagnet trying to attract an extremely smooth, flat metal plate. If the electromagnet's face is extremely smooth and flat as well, there will be many more points of contact with the plate, and so the magnetic circuit will have less resistance to the magnetic field.
Electromagnets find uses in many places, ranging from particle accelerators, to junkyard cranes, to MRI machines.
If an electromagnet is strong enough, the magnetic force between neighbouring loops of wire can cause the electromagnet to be crushed by its own magnetic field.
All magnets are dipoles: that is, all magnets have a north and a south pole. The poles are not a pair of things on or inside the magnet. They are a concept used to discuss and describe magnets. In the image at the top of this page, the poles look like specific locations (because the highest surface intensity of the field occurs at the poles), but this does not mean that they are specific locations.
To understand the concept of pole, imagine a row of people who are all facing the same direction and standing in line. While there is a "face" end of the line and a "back" end of the line, there is no one place where all of the faces are and all of the backs are. The person at the front of the face end has a back; and the person at the back end has a face. If you divide the line into two shorter lines, each one of the shorter lines still has a face end and a back end. Even if you pull the line completely apart so that there are just individuals standing around, each one of the individuals still has a face and a back. This can continue without end.
The same holds true with magnets. There is not one place where all of the north or south poles are. If a magnet is divided in two, two magnets will result--and both magnets will have a north and a south pole. Those smaller magnets can then be divided, and all of the resulting pieces will have both a north and south pole. In most instances, if the material continues to be broken into smaller and smaller pieces there will be a point where the pieces are too small to retain a net magnetic field. They won't become individual north or south poles though; instead, they will just lose the ability to maintain a net field. Some materials, however, can be divided down to the molecular level and still maintain a net field with both a north and a south pole. There are theories involving the possibility of north and south magnetic monopoles, but no magnetic monopole (single pole) has ever been found.
A standard naming system for the poles of magnets is important. Historically, the terms north and south reflect awareness of the relationship between magnets and the earth's magnetic field. A freely suspended magnet will eventually orient itself north-to-south, because of its attraction to the north and south magnetic poles of the earth. The end of a magnet that points toward the Earth's geographic North Pole is labeled as the north pole of the magnet; correspondingly, the end that points south is the south pole of the magnet.
The Earth's current geographic north is thus actually its magnetic south. Confounding the situation further, it is known that the Earth's magnetic field has reversed itself in the past, so this system of naming is likely to be backward at some time in the future (see Earth's magnetic field).
Fortunately, by using an electromagnet and the right hand rule, the orientation of the field of a magnet can be defined without reference to the Earth's geomagnetic field.
To avoid the confusion between geographic and magnetic north and south poles, the terms positive and negative are sometimes used for the poles of a magnet. The positive pole is that which seeks geographical north.
Ferromagnetic materials can be magnetised in the following ways:
Permanent magnets can be demagnetized in the following ways:
In an electromagnet, ceasing the flow of current will eliminate the magnetic field. However, a slight field may remain in the core material as a result of hysteresis.
Magnetized items interact with other items in very specific ways.
If a magnet is brought close enough to another magnet, their fields will begin to interact in the following ways:
If a magnet is brought close enough to a ferromagnetic material (that is not magnetized itself), the magnet will strongly attract the ferromagnetic material regardless of orientation. Both the north and south pole of the magnet will attract the other item with equal strength.
By definition, diamagnetic materials weakly repel a magnetic field. This occurs regardless of the north/south orientation field.
By definition, paramagnetic materials are weakly attracted to a magnetic field. This occurs regardless of the north/south orientation of the field.
Calculating the attractive or repulsive force between two magnets is, in the general case, an extremely complex operation, as it depends on the shape, magnetization, orientation and separation of the magnets. However, a formula exists for the simple case of the force between two magnetic poles:
where