Magnetism and Matter
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New answer posted
4 months agoContributor-Level 10
5.6 Magnetic field strength, B = 0.25 T
Magnetic moment, M = 0.6 J/T
The angle , between the axis of the solenoid and the direction of the applied field is 30 . Therefore, the torque acting on the solenoid is given as
= 0.6 = 7.5 J
New answer posted
4 months agoContributor-Level 10
5.5 Number of turns, n = 800
Area of the cross-section, A = 2.5
Current flowing, I = 3.0 A
A current carrying solenoid behaves like a bar magnet because a magnetic field develops along its axis (along the length).
The magnetic moment associated is calculated as M = nIA = 800 2.5 J/T= 0.6 J/T
New answer posted
4 months agoContributor-Level 10
5.4 Moment of the bar magnet, M = 0.32 J/T
Magnetic field, B = 0.15 T
The bar magnet is aligned along the magnetic field. This system is considered as being in stable equilibrium. Hence, the angle , between the bar magnet and the magnetic field is 0 .
Potential energy of the system = -MBcos = - 0.32 = -4.8 J
When the bar magnet is oriented 180 to the magnetic field, it becomes unstable equilibrium.
Potential energy = - MBcos = - 0.32 = 4.8 J
New answer posted
4 months agoContributor-Level 10
5.3 Magnetic field strength, B = 0.25 T
Torque on the bar magnet, = 4.5 J
Angle between the bar magnet and the external magnetic field, = 30
From the relation T = MB , where M = Magnetic moment, we get
M = = = 0.36 J/T
Hence the magnetic moment is 0.36 J/T
New answer posted
4 months agoContributor-Level 10
5.2 (a) Earth's magnetic field changes with time. It takes a few hundred years to change by an appreciable amount. The variation in earth's magnetic field with the time cannot be neglected.
(b) Earth's core contains molten iron. This form of iron is not ferromagnetic. Hence this is not considered as a source of earth's magnetism.
(c) The radioactivity in earth's interior is the source of energy that sustains the currents in the outer conducting regions of earth's core. These charged currents are considered to be responsible for earth's magnetism.
(d) The change of earth's magnetic field got weakly recorded in rocks during their solidif
New answer posted
4 months agoContributor-Level 10
5.1 (a) Earth's magnetic field can be specified by three following independent quantities
Magnetic declination
Angle of dip
Horizontal component of earth's magnetic field.
(b) The angle of dip at a point depends on how far the point is located with respect to North pole or South pole. The angle of dip will be more in Britain than Southern India as Britain is closer to Magnetic North pole than South India to the Magnetic South pole.
(c) It is a hypothesis that a huge bar magnet is embedded deep in Earth's ground with its north pole near magnetic south pole of earth and south pole is near magnetic north pole of earth. Magnetic field lines
New answer posted
5 months agoContributor-Level 10
The net magnetic flux through any closed surface is zero, according to Gauss's Law for magnetism.
Mathematically,
? B · dA = 0.
It states that all magnetic field lines that enter a surface must exit from it as well. In this way, it is different from the electric charges which can exist independently as positive and negative.
New answer posted
5 months agoContributor-Level 10
The Earth's magnetic field makes a magnetic inclination or dip with the horizontal plane at a particular location. It shows how much the magnetic field is tilted from the horizontal. It gets tilted due to the Earth's magnetic nature. The formula is:
tan I = B_V / B_H,
where B_V is the vertical component and B_H is the horizontal component of the Earth's magnetic field.
New answer posted
5 months agoContributor-Level 10
The angle between the magnetic north (the direction a compass points) and the geographic north (true north) is the magnetic declination. This angle can change over time due to changes in the Earth's magnetic field and varies with location on Earth. It is important for navigation where accurate directional orientation is crucial, especially in marine and aviation transport. The declination helps in avoiding navigational errors as it ensures that compass readings are corrected.
New answer posted
5 months agoContributor-Level 10
The Earth's magnetic field makes a magnetic inclination or dip with the horizontal plane at a particular location. It shows how much the magnetic field is tilted from the horizontal. It gets tilted due to the Earth's magnetic nature. The formula is:
tan I = B_V / B_H,
where B_V is the vertical component and B_H is the horizontal component of the Earth's magnetic field.
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