MadSci Network: Earth Sciences |
Hello, Richard! Let's start with a "quick tour" of magnetism in iron. Taken on an atom-by- atom basis, iron is always magnetic so long as the electron clouds of the atoms are not "overly excited". This atomic-sized magnetism arises from the particular configuration of the electrons in the iron atom. However, unless we can somehow line up the atom-sized magnets so their individual magnetic fields are pointing in the same direction, we will not sense any net magnetic field. So long as the iron is cool enough, the atoms will align locally into "groups" that are effectively small magnets and are called magnetic domains. Within each domain, all the iron atoms have their magnetic fields lined up. Without something (i.e. a magnetic field) forcing them to align, these domains are randomly oriented and thus their individual magnetic fields cancel out in the aggregate. Now let's hit your questions one by one: Richard: Is iron in its raw form magnetic, or does it have to magnetized? Mad Scientist: See above for the "typical" state of iron. Richard: How do you magnetize something? If you had a piece if iron how would you make it magnetic without a magnet to rub up against it? Motion of some kind maybe? Mad Scientist: To magnetize something, you must force the domains to line up so their magnetic fields are mostly parallel. Rubbing something may help speed up the process, because it heats the material and the domains reorient more quickly as the temperature goes up. (Aside: a magnetized material has a point known as its Curie temperature at which it will lose its magnetic properties due to thermal jiggling randomizing the domains. If the material then cools down below the Curie temperature without a magnetic field present, it will not have any net magnetic field as the cooling domains will freeze into place in random directions. If it cools down with a field present, that field will tend to reorient the domains and the iron will end up magnetized). The source of the magnetic field used does not need to be a physical magnet; you can also use the magnetic field generated by a solenoid, for example. Richard: Two pieces of iron rubbing against each other, would that make them magnetic? Mad Scientist: Not in the absence of a magnetic field, but the Earth's magnetic field is always around unless you take steps to exclude it with shielding. The magnetization arising from the Earth's weak field may not be much, but there should be some. Note that as lavas coming up from the mantle freeze into place along the Mid-Atlantic Ridge, the Earth's field magnetizes the iron in the rock enough so that the pattern of the reversals of the Earth's field through time can be observed. Richard: How is magnetism achieved, [in laymans terms if possible]? Mad Scientist: Think of iron as a collection of zillions of tiny magnets, each of which is a single iron atom. Left to themselves, they will line up in little groups (the magnetic domains), but the number of domains is very large and they are randomly oriented in space. So all their magnetic fields end up averaging out to zero or close to it. To achieve a magnetized material, we force the domains to line up with each other by applying a magnetic field. To get further information, I'd suggest an introductory text in materials science, or perhaps a freshman/sophomore physics text (generally physics texts are not quite so useful when discussing material properties, but they certainly cover the basics of electromagnetic theory).
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