Polarity (physics)

In physics, polarity is the condition of having both negative and positive charges—in particular, having magnetic or electrical poles. Polarity, which is found at the atomic level as well as the planetary level, may be strong or weak.

Magnetic poles come in pairs. Batteries are polar—having positive and negative terminals—and Earth has an electromagnetic field that has north and south poles. The stronger the polarity is, the greater the effect will be in attracting or repelling other objects.

Atomic and Molecular Polarity

Atoms have a core, which contains one or more protons and neutrons as well as orbitals called electrons. Protons have a positive charge, electrons have a negative charge, and neutrons are neutral. If the atom contains an equal number of protons and electrons, the atom is neutral. Atoms with unequal numbers of protons and electrons are called ions. Cations have fewer electrons and a positive charge, while anions have more electrons and a negative charge. Opposites attract, and likes repel.

When two atoms share electrons, they form a covalent bond. These bonds are polar when the electrons are not equally shared and nonpolar when the electrons are equally shared. Multiple covalent bonds may compose a molecule. When a molecule is asymmetrical, it has a net polarity, which means it has more negative charge on one end and an excess of positive charge. This polar molecule acts as an electric dipole and may interact with electric fields. The stronger the charge is, the greater the attraction will be between molecules. The closer the molecules are, the stronger the attraction between them will be.

Molecular polarity influences the properties of matter. For example, the strong polar attraction between water molecules (hydrogen and oxygen) is responsible for the high temperature needed to cause water to boil and enter a gaseous state. Hydrogen bonds are strong, and the polar dipole force of water molecules is difficult to disrupt. The molecules stick together, holding a liquid form and resisting a change of state until enough kinetic energy is applied to force apart the molecules.

Electricity

An electric direct current is the flow of electrons through a conductive material, such as wire, through a complete circuit. The power source, such as a battery, must be polar and operates because molecular opposites attract. It pushes the current from a negative terminal and draws it in at the other end of the circuit at the positive terminal, completing the circuit. This directional flow of current electricity is the electric field line. A moving electric charge will create an electromagnetic field. A moving magnetic field will produce an electric field.

Magnetism and Magnetic Fields

All objects have some degree of magnetism, but in most, it is so weak that it has no effect. Other objects, in particular some metals, are strongly magnetic and attract or repel other magnetic objects. Permanent magnets, such as iron, are made of molecules that line up because of their magnetic fields. All magnets have magnetic fields, in which the objects exert magnetic influence. The effects take place along magnetic field lines, which are the paths of the magnetic influence. The field lines come together at the magnet's poles.

In addition to permanent magnets, electricity can create magnetic force. An example is a large crane-supported magnet that can be used to move scrap metal or junk cars. By wrapping conductive wire around a core of iron or other metal that can be magnetized and adding an electric current, the movement of the current through the wire creates a magnetic field. The magnetic field lines circle the coil of wire. Reversing the current will also reverse the direction of the magnetic field, and cutting off the electricity removes the magnetic field. Adding more turns of wire makes such magnets stronger.

Planetary Polarity

A magnetic field surrounds Earth. Most magnetic objects on Earth are attuned to the magnetically attractive poles of the planet, the magnetic north pole and the magnetic south pole. Magnetic energy flows through Earth's axis. At the magnetic north pole, this energy exits Earth, divides, and flows southward. At the southern point of the axis, the magnetic energy rejoins and enters Earth's core again. Like any dipolar or bar magnet, the magnetic north pole—which is negatively charged—pushes out energy, while the magnetic south pole pulls in energy. For example, a compass needle's point must be positively charged to point to magnetic north.

The polarity of the planet is not constant, and the magnetic north and south poles are not aligned with the geographic poles. The magnetic north pole is moving north about forty miles a year, and the strength of the magnetic field fluctuates. Earth's magnetic field is most likely generated by its composition: a solid core surrounded by a liquid metal. The iron in the core probably generates electric currents that geophysicists believe create the magnetic field. They describe this as a dynamo effect. Over the planet's history, the poles have been reversed many times.

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