SlideShare a Scribd company logo
1
External Field of a Bar Magnet and Inverse Square Law
BACKGROUND: Since early times the existence of magnetic force has been known;
certain kinds of rocks called ‘lodestone’ would attract pieces of iron. Also, forces of
attraction and repulsion between two pieces of lodestone were observed to depend on
their relative orientation. A freely suspended lodestone would always point in the same
direction; the end which pointed toward the geographic North was labeled the North (or
N) pole and that pointing toward the geographic South was labeled the South (or S) pole.
It therefore would appear that the earth acts like a giant bar magnet with its South
magnetic pole in the Northern hemisphere and its North magnetic pole in the Southern
hemisphere since opposite magnetic poles attract each other.
A single modern concept of a magnetic eld always accompanies an electric current
or a moving charge. A circulating electric current in an atom and its electronic spin will
produce a magnetic eld. Permanent magnets, such as a bar magnet made from iron
alloys (ferromagnetic materials), have small clusters of adjacent atoms, called magnetic
domains. The unpaired spins in the atoms of a magnetic domain are aligned to produce a
sizeable magnetic eld. In an unmagnetized piece of a magnetic material, these domains
are randomly oriented and their magnetic elds well-nigh cancel each other out.
However, under the inuence of a sufficiently strong external magnetic eld, the domains
become generally aligned in the direction opposite of that of the external eld. Now the
magnetic elds of the individual domains add up to produce a magnetic eld, as in a bar
magnet.
OBJECT: To investigate the magnetic eld about a bar magnet and to show that it varies
inversely as the square of the distance from an isolated magnetic pole.
APPARATUS: Long bar magnet, drawing board, compass (one small and one large, if
possible), aluminum plate guide for bar magnets, iron filings, and paper.
THEORY: The magnetic eld is a vector eld since its strength or intensity may be
dened as the force on a unit North pole. Somewhat analogous to electric elds,
magnetic elds can be represented by lines so that the strength of the eld is
represented by the density of lines and its direction represented by a tangent to these
lines. We illustrate below the magnetic eld of a bar magnet in Fig. 5.1 and an
expanded view near the North pole of a long bar magnet in Fig. 5.2.
2
Figure 5.1: Magnetic Field of a Permanent Bar Magnet.
Figure 5.2: The Magnetic Field Near the North Pole of a Bar Magnet.
It is seen from Fig. 5.1 that the magnetic lines of force always from closed loops.
The location of the poles is generally uncertain and we will suppose that the pole is
situated inside the magnet at a distance d from the end of the magnet.
In Fig. 5.2, the same number of lines thread through the lengths ℓ1, ℓ2 and ℓ3
which are located at r1, r2, and r3 from the end of the magnet. The strength of the
magnetic eld at a point is described by the number of lines per unit area crossing a small
area perpendicular to the eld at that point. The magnetic eld is inversely proportional
to the square of the distance from the pole. Together these statements for the average
value of B will give:
,
)(
1
,
1
22
dr
BandB
+
∝∝
l (1)
or
ℓ = c(r + d), (2)
where c is the propotionality constant and d is the distance between the pole and edge of
the bar magnet. However, bear in mind that the inuence of the South pole (visible in the
bending of the magnetic lines of force as in Fig. 5.1) renders this relation approximate.
PROCEDURE:
1. Place the bar magnet in the center of the paper with its South pole facing North. A
compass needle, in the absence of any external magnetic elds other than that of
the Earth, will align itself in the N–S direction Make sure that it is a strongly
magnetized magnet. Draw the magnet outline.
2. Place the small compass near the North pole of the magnet and make a dot on the
paper at each end of the compass arrow. Move the compass forward till its South
pole is over the dot of the previous North pole location.
3
3. Plot at least 10 to 12 lines of force by moving the compass, marking arrow
positions and repositioning the compass. Take care that these lines originating
from the North pole are nearly equally spaced at the starting point.
4. Draw a smooth curve through the series of dots and place arrows indicating that
these lines emanate from the North pole.
5. Locate the points where the compass needle has no tendency to turn in any
direction. These points are called neutral points and should indicate where the
magnetic eld of the Earth and that of the magnet are equal and opposite to each
other.
6. To further visualize the magnetic field of a bar magnet, position the bar magnet
beneath a sheet of paper. Sprinkle iron filings above the paper and magnet and tap
the box slightly so that the filings will align along the magnetic field lines.
CALCULATIONS:
1. Measure several ℓ’s (ℓ1, ℓ2,...), keeping them much smaller than the length of the
bar magnet, and the corresponding r’s (r1,r2,...). The closer (as compared to the
length of the bar magnet) you are to the pole for these measurements, the better
your results will be since the magnetic eld will more closely resemble that of an
isolated magnetic pole, for with Eq. (1) applies.
2. Plot ℓ versus r using the computer. The linearity of this plot, implied by Eq. (1), is
only approximate because Eq. (1) itself holds only approximately as explained
above. (This is the reason for keeping the ℓ’s as small as possible compared to the
length of the bar magnet.) Determine the value of d from the intercept with the
axis displaying r in the ℓ– r plot.

More Related Content

DOC
PPTX
Physics w1 electromagnetism
PPTX
X cbse physics chapter 13
PPTX
MAGNETISM,EARTH MAGNETIC FIELD
PPT
ALL ABOUT MAGNET
PDF
Lecture 8 3_n_8_4_magnetic_force
PPTX
Magnets & magnetic fields
PPT
Magnetic force
Physics w1 electromagnetism
X cbse physics chapter 13
MAGNETISM,EARTH MAGNETIC FIELD
ALL ABOUT MAGNET
Lecture 8 3_n_8_4_magnetic_force
Magnets & magnetic fields
Magnetic force

What's hot (18)

PPTX
Magnetic fields
PPT
MAGNETIC FIELD INTENSITY
PPTX
Earths magnetism
PPT
Magnetism and matter
PDF
Lecture 8 1_magnetic_field
PDF
Physics 1 chapter-5
PPTX
Earth magnetic field
PPTX
Magnets and magnetism
PPT
Grade 11, U5 L1-Natural Magnetism
PPTX
Earths magnetic field
PPT
Magnetism
PPT
Magnets and magnetism
PPTX
Magnetism physics
PPT
Magnetism
PPTX
electromagnetic induction ( part 1 )
PPTX
Magnetism
PDF
Magnetic field sensing
Magnetic fields
MAGNETIC FIELD INTENSITY
Earths magnetism
Magnetism and matter
Lecture 8 1_magnetic_field
Physics 1 chapter-5
Earth magnetic field
Magnets and magnetism
Grade 11, U5 L1-Natural Magnetism
Earths magnetic field
Magnetism
Magnets and magnetism
Magnetism physics
Magnetism
electromagnetic induction ( part 1 )
Magnetism
Magnetic field sensing
Ad

Similar to 5 external fieldbarmagnet (20)

PPTX
Earths magnetism part 1
PDF
Unit IV_ Fundamentals of Magnetism and application
DOC
Eoc 2
PPTX
Class XII Physics Chapter 5' with you.pptx
PPTX
1. preliminary understanding of magnetism
PPT
Ch 21 Magnetic Fields and Forces
PPS
PREFINAL
PPTX
Ch-13-Magnetic-effect-of electric -current.pptx
PPT
Magnetism (1).ppt
PPT
Magnetism.ppt
PPTX
MAGNETIC FIELDS-1.pptx
PPTX
Part of PHY_003 for JUBEB CLASS for physics
PPT
Magnetism by wasay zia
PPTX
magnetism-lecture.pptx
PPTX
Electromagnetic
PPSX
Magnetic effect of electric current
PPTX
Electromagnetic induction, grade 12 physics
PPTX
Magnetism and Electromagnetism
PPTX
Magnetism Lesson in Physics for Engineers
PPTX
ELEMENTARY PHYSICS FOR 100 LEVEL STUDENTS
Earths magnetism part 1
Unit IV_ Fundamentals of Magnetism and application
Eoc 2
Class XII Physics Chapter 5' with you.pptx
1. preliminary understanding of magnetism
Ch 21 Magnetic Fields and Forces
PREFINAL
Ch-13-Magnetic-effect-of electric -current.pptx
Magnetism (1).ppt
Magnetism.ppt
MAGNETIC FIELDS-1.pptx
Part of PHY_003 for JUBEB CLASS for physics
Magnetism by wasay zia
magnetism-lecture.pptx
Electromagnetic
Magnetic effect of electric current
Electromagnetic induction, grade 12 physics
Magnetism and Electromagnetism
Magnetism Lesson in Physics for Engineers
ELEMENTARY PHYSICS FOR 100 LEVEL STUDENTS
Ad

5 external fieldbarmagnet

  • 1. 1 External Field of a Bar Magnet and Inverse Square Law BACKGROUND: Since early times the existence of magnetic force has been known; certain kinds of rocks called ‘lodestone’ would attract pieces of iron. Also, forces of attraction and repulsion between two pieces of lodestone were observed to depend on their relative orientation. A freely suspended lodestone would always point in the same direction; the end which pointed toward the geographic North was labeled the North (or N) pole and that pointing toward the geographic South was labeled the South (or S) pole. It therefore would appear that the earth acts like a giant bar magnet with its South magnetic pole in the Northern hemisphere and its North magnetic pole in the Southern hemisphere since opposite magnetic poles attract each other. A single modern concept of a magnetic eld always accompanies an electric current or a moving charge. A circulating electric current in an atom and its electronic spin will produce a magnetic eld. Permanent magnets, such as a bar magnet made from iron alloys (ferromagnetic materials), have small clusters of adjacent atoms, called magnetic domains. The unpaired spins in the atoms of a magnetic domain are aligned to produce a sizeable magnetic eld. In an unmagnetized piece of a magnetic material, these domains are randomly oriented and their magnetic elds well-nigh cancel each other out. However, under the inuence of a sufficiently strong external magnetic eld, the domains become generally aligned in the direction opposite of that of the external eld. Now the magnetic elds of the individual domains add up to produce a magnetic eld, as in a bar magnet. OBJECT: To investigate the magnetic eld about a bar magnet and to show that it varies inversely as the square of the distance from an isolated magnetic pole. APPARATUS: Long bar magnet, drawing board, compass (one small and one large, if possible), aluminum plate guide for bar magnets, iron filings, and paper. THEORY: The magnetic eld is a vector eld since its strength or intensity may be dened as the force on a unit North pole. Somewhat analogous to electric elds, magnetic elds can be represented by lines so that the strength of the eld is represented by the density of lines and its direction represented by a tangent to these lines. We illustrate below the magnetic eld of a bar magnet in Fig. 5.1 and an expanded view near the North pole of a long bar magnet in Fig. 5.2.
  • 2. 2 Figure 5.1: Magnetic Field of a Permanent Bar Magnet. Figure 5.2: The Magnetic Field Near the North Pole of a Bar Magnet. It is seen from Fig. 5.1 that the magnetic lines of force always from closed loops. The location of the poles is generally uncertain and we will suppose that the pole is situated inside the magnet at a distance d from the end of the magnet. In Fig. 5.2, the same number of lines thread through the lengths ℓ1, ℓ2 and ℓ3 which are located at r1, r2, and r3 from the end of the magnet. The strength of the magnetic eld at a point is described by the number of lines per unit area crossing a small area perpendicular to the eld at that point. The magnetic eld is inversely proportional to the square of the distance from the pole. Together these statements for the average value of B will give: , )( 1 , 1 22 dr BandB + ∝∝ l (1) or ℓ = c(r + d), (2) where c is the propotionality constant and d is the distance between the pole and edge of the bar magnet. However, bear in mind that the inuence of the South pole (visible in the bending of the magnetic lines of force as in Fig. 5.1) renders this relation approximate. PROCEDURE: 1. Place the bar magnet in the center of the paper with its South pole facing North. A compass needle, in the absence of any external magnetic elds other than that of the Earth, will align itself in the N–S direction Make sure that it is a strongly magnetized magnet. Draw the magnet outline. 2. Place the small compass near the North pole of the magnet and make a dot on the paper at each end of the compass arrow. Move the compass forward till its South pole is over the dot of the previous North pole location.
  • 3. 3 3. Plot at least 10 to 12 lines of force by moving the compass, marking arrow positions and repositioning the compass. Take care that these lines originating from the North pole are nearly equally spaced at the starting point. 4. Draw a smooth curve through the series of dots and place arrows indicating that these lines emanate from the North pole. 5. Locate the points where the compass needle has no tendency to turn in any direction. These points are called neutral points and should indicate where the magnetic eld of the Earth and that of the magnet are equal and opposite to each other. 6. To further visualize the magnetic field of a bar magnet, position the bar magnet beneath a sheet of paper. Sprinkle iron filings above the paper and magnet and tap the box slightly so that the filings will align along the magnetic field lines. CALCULATIONS: 1. Measure several ℓ’s (ℓ1, ℓ2,...), keeping them much smaller than the length of the bar magnet, and the corresponding r’s (r1,r2,...). The closer (as compared to the length of the bar magnet) you are to the pole for these measurements, the better your results will be since the magnetic eld will more closely resemble that of an isolated magnetic pole, for with Eq. (1) applies. 2. Plot ℓ versus r using the computer. The linearity of this plot, implied by Eq. (1), is only approximate because Eq. (1) itself holds only approximately as explained above. (This is the reason for keeping the ℓ’s as small as possible compared to the length of the bar magnet.) Determine the value of d from the intercept with the axis displaying r in the ℓ– r plot.