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Force On A Current Loop In A Magnetic Field01:17

Force On A Current Loop In A Magnetic Field

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Magnetic forces on wires carrying current are most frequently applied in motors. A DC motor is a device that converts electrical energy into mechanical work. In motors, wire loops are enclosed in a magnetic field. When current flows through the loops, the magnetic field applies torque, which causes the shaft to rotate. The direction of the current is reversed once the loop's surface area is lined up with the magnetic field, causing a constant torque on the loop. During the process, commutators...
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Torque On A Current Loop In A Magnetic Field01:13

Torque On A Current Loop In A Magnetic Field

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The most common application of magnetic force on current-carrying wires is in electric motors. These consist of loops of wire, which are placed between the magnets with a magnetic field. When current flows through the loops, the magnetic field applies torque, which causes the shaft to rotate, thus converting electrical energy to mechanical energy.
Consider a rectangular current-carrying loop containing N turns of wire, placed in a uniform magnetic field. The net force on a current-carrying loop...
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Faraday Disk Dynamo01:23

Faraday Disk Dynamo

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A Faraday disk dynamo is a DC generator, producing an emf that is constant in time. It consists of a conducting disk that rotates with a constant angular velocity in the magnetic field, perpendicular to the disk's plane. The rotation of the disk causes a change in magnetic flux, which induces an emf, causing opposite charges to develop on the rim and in the center of the disk. The polarity of the induced emf can be determined by the direction of the magnetic field and the direction of the...
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Electric Generator: Alternator01:25

Electric Generator: Alternator

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Electric generators induce an emf by rotating a coil in a magnetic field. A simple alternator is an AC generator that creates electrical energy that varies sinusoidally with time. A simple alternator consists of a conducting loop that is placed inside a uniform magnetic field. The loop is connected to split rings connected to the external circuit with the help of brushes.
The magnetic flux passing through the coil varies sinusoidally as the loop rotates inside the magnetic field. This...
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Potential Due to a Magnetized Object01:24

Potential Due to a Magnetized Object

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Magnetic dipoles in magnetic materials are aligned when placed under an external magnetic field. For paramagnets and ferromagnets, dipole alignment occurs in the direction of the magnetic field. However, the dipoles align opposite to the field in the case of diamagnets. This state of magnetic polarization due to the external field is called magnetization. Magnetization is defined as the dipole moment per unit volume. It plays a similar role to polarization in electrostatics.
The vector...
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MOS Capacitor01:25

MOS Capacitor

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A Metal-Oxide-Semiconductor (MOS) capacitor is a fundamental structure used extensively in semiconductor device technology, particularly in the fabrication of integrated circuits and MOSFETs (metal-oxide-semiconductor field-effect transistors). The MOS capacitor consists of three layers: a metal gate, a dielectric oxide, and a semiconductor substrate.
The metal gate is typically made from highly conductive materials such as aluminum or polysilicon. Beneath the metal gate lies a thin layer of...
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A 100 KW Class Applied-field Magnetoplasmadynamic Thruster
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El Moho eléctrico Moho.

A G Jones1, I J Ferguson

  • 1Geological Survey of Canada, Ottawa, Ontario. ajones@NRCan.gc.ca

Nature
|February 24, 2001
PubMed
Resumen
Este resumen es generado por máquina.

Los datos sísmicos revelan el límite entre la corteza y el manto, o discontinuidad de Mohorovičić (Moho), pero los estudios eléctricos no han sido concluyentes. Nuevos datos electromagnéticos de Canadá.

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Área de la Ciencia:

  • La geofísica es la geofísica.
  • Sismología Sismología Sismología.
  • El electromagnetismo es el electromagnetismo.

Sus antecedentes:

  • La discontinuidad de Mohorovičić (Moho) marca el límite entre la corteza terrestre y el manto, identificado por los cambios en la velocidad sísmica.
  • Estudios electromagnéticos anteriores no han detectado un cambio de conductividad correspondiente en el Moho.
  • Las mediciones de laboratorio sugieren un contraste de conductividad en el Moho, que no se observa en los estudios de campo.

Objetivo del estudio:

  • Para investigar las firmas electromagnéticas en las profundidades de Moho.
  • Para conciliar las discrepancias entre las observaciones sísmicas y electromagnéticas en el límite entre la corteza y el manto.
  • Para explorar las propiedades eléctricas del manto superior debajo de un cratón anómalo.

Principales métodos:

  • Análisis de datos electromagnéticos del cratón Slave, en el norte de Canadá.
  • Comparación de la conductividad observada con las mediciones de laboratorio en rocas del manto.
  • Utilizando la conductividad anómala baja de la corteza terrestre del cráter Slave para obtener imágenes Moho de alta resolución.

Principales resultados:

  • Se detectó un cambio gradual distinto en la conductividad eléctrica a profundidades de Moho.
  • El cratón Slave exhibe una conductividad crustal total excepcionalmente baja (<1 Siemens).
  • La conductividad del manto superior debajo del Moho es dos órdenes de magnitud más alta de lo predicho por los estudios olivinos.

Conclusiones:

  • Los métodos electromagnéticos pueden resolver los cambios de conductividad en el Moho.
  • La alta conductividad en el manto superior indica una fase de conducción conectada.
  • Este hallazgo desafía los modelos existentes de composición y propiedades de la frontera entre la corteza y el manto.