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New answer posted
8 months agoContributor-Level 10
5.11 Given:
The angle of declination, = 12
The angle of dip, = 60
Horizontal component of Earth's magnetic field, = 0.16 G
If Earth's magnetic field be B, we can relate B and as
B = = = 0.32 G
Therefore, the Earth's magnetic field lies in the vertical plane, 12west of the geographic meridian, making an angle of 60 (upward) with the horizontal direction. Its magnitude is 0.32 G.
New answer posted
8 months agoContributor-Level 10
5.10 Given:
Horizontal component of Earth's magnetic field, = 0.35 G
Angle made by the needle with the horizontal plane, = 22
If the Earth's magnetic field at that location be B,
then = B
B = = = 0.377 G
Therefore, the strength of Earth's magnetic field at that location is 0.377 G
New answer posted
8 months agoContributor-Level 10
5.9 Number of turns, n = 16
Radius of the coil, r = 10 cm = 0.1 m
Cross-section of the coil, A = = = 0.0314
Current in the coil, I = 0.75 A
Magnetic field strength, B = 5.0 T
Frequency of oscillation of the coil, = 2/s
Magnetic moment, M = NIA = 16 = 0.377 A
Frequency is given by the relation, = , where I = moment of Inertia of the coil
I = = = 1.19 kg
New answer posted
8 months agoContributor-Level 10
5.8 (a) Number of turns, n = 2000
Area of cross-section, A = 1.6
Current, I = 4.0 A
The magnetic moment along the axis of the solenoid is calculated as
M = nAI = 2000 1.6 = 1.28 A
(b) Magnetic field, B = 7.5 T
Angle between magnetic field and the axis of the solenoid, = 30
Torque
= 1.28 7.5
= 4.8 Nm
New answer posted
8 months agoContributor-Level 10
5.7 Magnetic moment, M = 1.5 J/T
Magnetic field strength, B = 0.22 T
Initial angle between the axis and the magnetic field, = 0 and the final angle, = 90
Work required to make the magnetic moment normal to the direction of the magnetic field is given as:
W = -MB( cos cos ) = - 1.5 - cos 0 ) = 0.33 J
Initial angle between the axis and the magnetic field, = 0 and the final angle, = 180
Work required to make the magnetic moment normal to the direction of the magnetic field is given as:
W = -MB( cos cos ) = - 1.5 - cos 0 ) = 0.33 J
For case
Torque , here = = 90
= 1.5 = 0.33 J
Torque , here = = 180
= 1.5 =
New answer posted
8 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
8 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
8 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
8 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
8 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
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