## Magnetic field

 prefLabel Magnetic Field definition Pertaining to the magnetic field generated by the Earth, consisting of both the dipole and non-dipole components. relatedMatch narrower inScheme closeMatch broader Abstract from DBPedia A magnetic field is a vector field that describes the magnetic influence of electric charges in relative motion and magnetized materials. A charge that is moving parallel to a current of other charges experiences a force perpendicular to its own velocity. The effects of magnetic fields are commonly seen in permanent magnets, which pull on magnetic materials (such as iron) and attract or repel other magnets. Magnetic fields surround and are created by magnetized material and by moving electric charges (currents) such as those used in electromagnets. They exert forces on nearby moving electrical charges and torques on nearby magnets. In addition, a magnetic field that varies with location exerts a force on magnetic materials. Both the strength and direction of a magnetic field vary with location. As such, it is described mathematically as a vector field. In electromagnetics, the term "magnetic field" is used for two distinct but closely related fields denoted by the symbols B and H. In the International System of Units, H, magnetic field strength, is measured in the SI base units of ampere per meter (A/m). B, magnetic flux density, is measured in tesla (in SI base units: kilogram per second2 per ampere), which is equivalent to newton per meter per ampere. H and B differ in how they account for magnetization. In a vacuum, B/ and H are the same; but in a magnetized material, B/ and H differ by the magnetization M of the material at that point in the material. Magnetic fields are produced by moving electric charges and the intrinsic magnetic moments of elementary particles associated with a fundamental quantum property, their spin. Magnetic fields and electric fields are interrelated and are both components of the electromagnetic force, one of the four fundamental forces of nature. Magnetic fields are used throughout modern technology, particularly in electrical engineering and electromechanics. Rotating magnetic fields are used in both electric motors and generators. The interaction of magnetic fields in electric devices such as transformers is conceptualized and investigated as magnetic circuits. Magnetic forces give information about the charge carriers in a material through the Hall effect. The Earth produces its own magnetic field, which shields the Earth's ozone layer from the solar wind and is important in navigation using a compass.磁場（じば、英語: Magnetic field）は、電気的現象・磁気的現象を記述するための物理的概念である。工学分野では、磁界（じかい）ということもある。 単に磁場と言った場合は磁束密度Bもしくは、「磁場の強さ」Hのどちらかを指すものとして用いられるが、どちらを指しているのかは文脈により、また、どちらの解釈としても問題ない場合も多い。後述のとおりBとHは一定の関係にあるが、BとHの単位は国際単位系（SI）でそれぞれWb/m², A/m であり、次元も異なる独立した二つの物理量である。Hの単位はN/Wbで表すこともある。なお、CGS単位系における、磁場（の強さ）Hの単位は、Oeである。この項では一般的な磁場の性質、及びHを扱うこととする。 磁場は、空間の各点で向きと大きさを持つ物理量（ベクトル場）であり、電場の時間的変化または電流によって形成される。磁場の大きさは、+1のN極が受ける力の大きさで表される。磁場を図示する場合、N極からS極向きに磁力線の矢印を描く。 小学校などの理科の授業では、砂鉄が磁石の周りを囲むように引きつけられる現象をもって、磁場の存在を教える。このことから、磁場の影響を受けるのは鉄だけであると思われがちだが、強力な磁場の中では、様々な物質が影響を受けるという事が分かる。最近では、磁場や電場（電磁場、電磁波）が生物に与える影響について関心が寄せられている。 data publication(s) found by GCMD Science Keywords) Hourly mean values geomagnetic observatory Huancayo (HUA), 1935 to 1985Alternate_Mag_Absolutes - A software package for Magnetic Absolute Measurements with arbitrarily distributed DI Theodolite OrientationsIndCoils_FGE - A software package for merging Fluxgate and Induction Coil dataGeomagnetic Observatory St. Helena, preliminary hourly mean values 2010, XYZ componentsPreliminary minute mean values of geomagnetic observatory Villa Remedios, Bolivia, August 2010Preliminary minute mean values of geomagnetic observatory Villa Remedios, Bolivia, for January 2013Permanent Magnetotelluric Reference Station Wittstock, GermanyCompilation of palaeomagnetic data from sediments and volcanic rocks spanning 30,000 to 50,000 years ago used to create the temporally continuous global spherical harmonic geomagnetic field model LSMOD.1LSMOD.1 - Global paleomagnetic field model for 50 -- 30 ka BPPreliminary minute means Geomagnetic Observatory Tatuoca (TTB), 2008 to 2017Hall current densities derived from CHAMP scalar magnetic field data during six magnetic storms 2003 and 2005LSMOD.2 - Global paleomagnetic field model for 50 -- 30 ka BP