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The magnetising field required to be applied in opposite direction to reduce residual magnetism to zero is called (a) coercivity (b) retentivity [c) hysteresis (d) None of the above

Short Answer

Expert verified
(a) coercivity

Step by step solution

01

Understanding the Concept

To solve this problem, it's important to understand the key terms related to magnetism. Retentivity, coercivity, and hysteresis are terms used to describe different aspects of magnetism, particularly in the context of a magnetic hysteresis loop.
02

Defining Coercivity

Coercivity is defined as the intensity of the external magnetic field that must be applied to a ferromagnetic material to reduce its magnetization to zero after the material has been magnetized to saturation. This is exactly what the problem describes: applying a magnetizing field in the opposite direction to reduce residual magnetism to zero.
03

Defining Retentivity

Retentivity refers to the residual magnetism that remains in a ferromagnetic material after an external magnetizing field is removed. It is different from coercivity, as it describes the ability of the material to retain a certain amount of magnetization after being magnetized.
04

Identifying Key Term

Considering the definitions and the context provided in the problem, the magnetizing field applied in the opposite direction to reduce the residual magnetism to zero relates to coercivity. This is because coercivity is specifically defined by this action.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Retentivity
Retentivity is an essential concept in magnetism that refers to a material's ability to retain a certain level of magnetization after an external magnetic field is removed. It's a measure of the residual magnetism that remains locked inside a ferromagnetic material. When a material is magnetized to its saturation point and then the magnetizing force is turned off, the degree of remaining magnetism is called retentivity. Retentivity is a critical property for materials that are used to create permanent magnets. For instance, if you want to design a strong and durable magnet, you would choose a material with high retentivity so that it can maintain its magnetization over time. Key points to remember about retentivity:
  • Indicates the level of residual magnetism in a material.
  • High retentivity is desired for making permanent magnets.
  • It helps in understanding how well a material can maintain its magnetism without needing an external force.
Understanding retentivity helps you predict how different materials will behave in magnetic applications and is essential in various technological advancements.
Hysteresis
Hysteresis in magnetism is the phenomenon where the magnetization of a material lags behind the applied magnetic field. This occurs because the magnetic domains within a ferromagnetic material do not re-align instantaneously with changes in the external magnetic field. The hysteresis loop is a graphical representation of this lagging behavior, showing the relationship between the magnetic field applied to a material and its resulting magnetization. The loop showcases several key points:
  • The initial magnetization curve starts as the magnetic domains align with the applied field.
  • After reaching saturation, where all domains are aligned, the field is reduced, and the curve shows where the material retains some magnetization (retentivity).
  • The point where the material needs an opposite field to demagnetize completely is its coercivity.
Hysteresis explains why ferromagnetic materials dissipate energy when they undergo cyclical magnetization and demagnetization, impacting the efficiency of devices like transformers and electric motors. This behavior is crucial for understanding magnetic losses and guiding material selection in engineering applications.
Magnetism
Magnetism is a fundamental physical phenomenon arising from the motion of electric charges, resulting in attractive and repulsive forces between objects. At the atomic level, magnetism is primarily due to electrons orbiting the nucleus and their intrinsic magnetic moments related to their spin. Magnetic materials are usually classified into three categories:
  • Ferromagnetic materials: These materials, like iron, can be magnetized by an external magnetic field and retain their magnetization once the field is removed.
  • Paramagnetic materials: These materials are weakly attracted to magnetic fields and do not retain any significant magnetization in the absence of an external field.
  • Diamagnetic materials: These materials create an opposing magnetic field when exposed to a magnetic field and are usually weakly repelled.
Understanding magnetism is crucial, as it encompasses the principles that govern the operation of a wide array of devices, ranging from simple compasses to complex MRI machines. In developing technologies, comprehending the behavior of different materials under magnetic fields is essential for crafting efficient and effective solutions to practical challenges.

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Most popular questions from this chapter

A magnet is placed on a paper in a horizontal plane for locating neutral points. A dip needle placed at the neutral point will be horizontal at the (a) magnetic poles (b) magnetic equator (c) latitude angle \(45^{\circ}\) (d) latitude angle of \(60^{*}\)

At a certain place, the horizontal component of the earth's magnetic field is \(B_{0}\) and the angle of dip is \(45^{\circ}\). The total intensity of the field at that place will be (a) \(B_{0}\) (b) \(\sqrt{2} B_{0}\) (c) \(2 B_{0}\) (d) \(B_{0}^{1}\)

A paramagnetic sample shows a net magnetisation of \(8 \mathrm{Am}^{-1}\) when placed in an external magnetie field of \(0.6 \mathrm{~T}\) at a temperature of \(4 \mathrm{~K}\). When the same sample is placed in an external magnetic field of \(0.2 \mathrm{~T}\) at a temperature of \(16 \mathrm{~K}\), the magnetisation will be [NCFRT Exemplar] (a) \(\frac{32}{3} \mathrm{Am}^{-1}\) (b) \(\frac{2}{3} \mathrm{Am}^{-1}\) (c) \(6 \mathrm{Am}^{-1}\) (d) \(2.4 \mathrm{Am}^{-1}\)

Magnetic field of earth is identical to magnetic field of a giant magnet held \(20^{\circ}\) west of geographic \(N-\mathrm{S}\) at the centre of earth. At equator, horizontal component of earth is 0.32 G. Vertical component can be calculated from the relation \(V=H \tan \delta\), where \(\delta\) is angle of dip at the place. The value of \(\delta=0^{\circ}\) at equator and \(8=90^{\circ}\) at poles. At a particle place, \(V=H\). The angle of dip is (a) 45 * (b) \(90^{\circ}\) (c) \(0^{\circ}\) (d) None of these

Match the following column I with column II Column I Column II I. Magnetic moment A. \(\left[\mathrm{ML}^{-} \mathrm{T}^{-2} \mathrm{~A}^{-1}\right]\) II. Permeability B. Vector III. Intensity of magnetisation C. \(\mathrm{Nm}^{\mathrm{I}} / \mathrm{Wb}\) IV. Magnetic induction D. Scalar Code (a) \(1-\mathrm{A}, \mathrm{II}-\mathrm{B}, \mathrm{III}-\mathrm{C}, \mathrm{N}-\mathrm{D}\) (b) \(1-C, I I-D, I \|-B, I V-A\) (c) \(1-\mathrm{D}, \mathrm{II}-\mathrm{C}, \mathrm{III}-\mathrm{A}, \mathrm{IV}-\mathrm{B}\) (d) \(\mathrm{L}-\mathrm{B}, \mathrm{Il}-\mathrm{A}, \mathrm{m}-\mathrm{B}, \mathrm{N}-\mathrm{D}\)

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