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A '''magnetic field''' is a [[vector]] field responsible for generating forces on electrically charged objects and magnets.  Magnetic fields are generated by magnetic [[dipole]]s, moving [[electric charge]]s, or changing [[electric field]]s.
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A '''magnetic field''' is a [[vector field]] responsible for generating [[force]]s on electrically charged objects and magnets.  Magnetic fields are generated by magnetic [[dipole]]s, moving [[electric charge]]s, or changing [[electric field]]s.
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Magnetic fields are linked to electric fields; [[light]], for instance, is a propagating electric and magnetic [[wave]].  Relativistically, a magnetic force in one [[inertial frame]] corresponds to an electric force in another.
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Magnetic fields are related to electric fields; together they are part of [[electromagnetism]]. For instance, [[light]] is a propagating electric and magnetic [[wave]].  Relativistically, a magnetic force in one [[inertial frame of reference]] corresponds to an electric force in another.
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When trying to determine the magnetic forces and fields, the [[right hand rule]] often proves useful.
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==Mathematics==
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Magnetic fields are often denoted using the letter B. The magnetic force acting on a particle travelling at a [[velocity]] v can be written as:
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<math>
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\vec{F} = q \left( \vec{v} \times \vec{B} \right)
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</math>
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where q is the electrical charge on the particle.<ref>[http://hyperphysics.phy-astr.gsu.edu/hbase/Forces/funfor.html#c3 Magnetic force on hyperphysics]</ref> The [[cross product]] means that the force will always act at a right angle to both the field and the velocity and if the velocity is [[parallel]] to the field, no force will act. As the force always acts perpendicular to the velocity, a charged particle in a uniform (constant) magnetic field will undergo [[circular motion]]. The [[magnitude]] of the force can also be written as:
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<math>
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F = qvB \sin{\theta}
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</math>
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where θ is the angle between the velocity and magnetic field. The direction can then be found using the [[right hand rule]].
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===Force on a Current Carrying Wire===
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An electrical [[current]] is rate of flow of charge past a point. By considering a wire with length L, the equation IL=nqv can be derived, where I is the current flowing along that wire and n is the "number density" (the number of charge carriers per unit length). This means that the force on a straight current carrying wire in a '''uniform''' magnetic field can be found as:
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<math>
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F = BIL \sin{\theta}
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</math>
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with θ now being the angle between the wire and the magnetic field.
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===Magnetic Field Produced by a Current Carrying Wire===
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Any electrical current creates a magnetic field. The magnetic field around a straight wire circulates around the wire. Its strength at a point depends only on the perpendicular distance to the wire and the size of the current:
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<math>
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B = \frac{\mu_0 I}{2 \pi r}
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</math>
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where r is the distance to the wire and μ<sub>0</sub> is the [[constants|permeability of free space]].
    
==Earth's Magnetic Field==
 
==Earth's Magnetic Field==
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[[Image:magnetic_field.gif|right|thumb|The View of "Answers in Genesis"]]
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[[Image:magnetic_field.gif|right|thumb|Change in the Earth's magnetic field according to Humphreys' model ]]
 
The magnetic field of [[Earth]] is directional nearly north-to-south, although slightly askance, meaning that "magnetic north" is not the same as "true north," and a person who is orienteering must take into account this change of declination, although it is truly only marginally relevant, unless you are close to either pole.<ref>Boy Scout Handbook.</ref>  This field has been decaying at a rapid rate of about about 5% per century, which casts doubt on the theory that the [[Earth]] is billions of years old.<ref>K.L. McDonald and R.H. Gunst, 'An analysis of the earth’s magnetic field from 1835 to 1965,’ ESSA Technical Report, IER 46-IES 1, U.S. Govt. Printing Office, Washington, 1967.</ref>  This decay suggests that, at some point, the poles will invert.
 
The magnetic field of [[Earth]] is directional nearly north-to-south, although slightly askance, meaning that "magnetic north" is not the same as "true north," and a person who is orienteering must take into account this change of declination, although it is truly only marginally relevant, unless you are close to either pole.<ref>Boy Scout Handbook.</ref>  This field has been decaying at a rapid rate of about about 5% per century, which casts doubt on the theory that the [[Earth]] is billions of years old.<ref>K.L. McDonald and R.H. Gunst, 'An analysis of the earth’s magnetic field from 1835 to 1965,’ ESSA Technical Report, IER 46-IES 1, U.S. Govt. Printing Office, Washington, 1967.</ref>  This decay suggests that, at some point, the poles will invert.
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Scientists have speculated about the history of Earth's magnetic field.  One group that makes use of the [[Bible]] as a resource for science suggests that the history of the Earth's magnetic field is as depicted to the right.<ref>http://www.answersingenesis.org/creation/v20/i2/magnetic.asp</ref>
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Scientists have speculated about the history of Earth's magnetic field.  One group that makes use of the [[Bible]] as a resource for science suggests that the history of the Earth's magnetic field is as depicted to the right.<ref name=answersingenesis>[https://answersingenesis.org/astronomy/earth/the-earths-magnetic-field-and-the-age-of-the-earth/ answersingenesis.org]</ref> The model, created by [[Russell Humphreys]], can be summarised as:
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* Creation of the Earth's magnetic field when God created the Earth
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* A decay in its strength until the time of the [[Great Flood]]
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* A series of very rapid reversals during the Flood, perhaps once every one or two weeks<ref name=answersingenesis/>
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* Fluctuations continue for around two thousand years after the Flood
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* The steady decay of the field resumes
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This model suggests the magnetic field of the [[Earth]] must be less than 10,000 years old
    
== References ==
 
== References ==
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<references/>
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{{reflist}}
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==See also==
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*[[Electric field]]
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*[[Electromagnetism]]
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*[[Maxwell's equations]]
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[[Category:Physics]]
 
[[Category:Physics]]
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[[Category:Electromagnetism]]
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