Magnetic Flux "Ø"
What it is
Magnetic flux is to charge as momentum is to mass. Flux opposes a change in the velocity of a charge, much as momentum opposes a change in the velocity of a mass. A change in momentum generates a physical force while a change in flux generates an electro-motive force ( voltage). To slow down a mass we must dissipate its' momentum. To slow down a charge, we must dissipate its' flux.

Flux is commonly visualized as magnetic lines passing through a given area.


History
Natural magnets (lodestones) were reported by the Chinese over 4500 years ago. Magnetized needles were used as direction indicators about 3000 years ago.

The words magnet and magnetism are derived from the Greek word "magnetite". Magnetite, a magnetic oxide of iron, was mined in Magnesia and mentioned in Greek texts as early as 800 BC. Thales of Miletus (640-547 BC), who lived nearby, was the first to study magnetic forces. He knew that magnetite attracts iron and that rubbing amber (a fossil tree resin that the Greeks called elektron) would make it attract lightweight objects such as feathers.

Not much was learned about magnetism until 1819 when Hans Oersted (1777-1851) passed an electrical current through a wire and noticed that a nearby compass needle deflected. This stimulated a great interest in magnetism and led to rapid advances.

Michael Faraday (1791-1851) conceptualized most of the electro-magnetic concepts. James Maxwell (1831-1879) expressed Faraday's concepts mathematically and expanded upon them to include dielectric displacement, permeability, electro-magnetic radiation and so on.


Common equations
voltage = flux / time
magnetic field strength (B) = flux / area
flux = current * length * permeability
flux density = magnetic vector potential / distance
flux density = magnetic vector potential x del    ( del = distance^-1)

Units
webers
Maxwells
line of force
volt seconds
megalines
unit poles

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