282
MAGNETIC OBSEEVATIONS.
K — Moment of inertia of the magnet, including its suspending stirrup and other
appendages.
tz = Ratio of the circumference to the diameter of the circle = 3-1415927. . .
]x. = The increase in the magnetic moment of the magnet, produced by the inducing
action of a magnetic force equal to the unity of the English system of
absolute measurement.
r0 = Apparent distance between the centres of the deflecting and suspended magnets
in the observations of deflection.
r = Distance corrected for error of graduation and temperature.
u0 = Observed angle of deflection.
P = A constant depending upon the distribution of magnetism in the deflecting
and suspended magnet.
m = Magnetic moment of the deflecting or vibrating magnet.
X = Horizontal component of the earth's magnetic force.
~ = Approximate value of
X0 X
-=7 = Value of -=p before the application of the correction
X X
(-!)■
Formulae for calculating mX:
T, = Tn 1 —
oca )
0 I 86400 16
Formulae for calculating
X
= Va r3 sin uQ.
tri ( P \
~ X I1 ~
m
~X
In reference to our observations of Intensity in general, and particularly to the
instruments employed, we add the following details:
T0 (= observed time of one vibration of the magnet). The time was noted at the
precise moment when the point of the scale most distant from the centre
MAGNETIC OBSEEVATIONS.
K — Moment of inertia of the magnet, including its suspending stirrup and other
appendages.
tz = Ratio of the circumference to the diameter of the circle = 3-1415927. . .
]x. = The increase in the magnetic moment of the magnet, produced by the inducing
action of a magnetic force equal to the unity of the English system of
absolute measurement.
r0 = Apparent distance between the centres of the deflecting and suspended magnets
in the observations of deflection.
r = Distance corrected for error of graduation and temperature.
u0 = Observed angle of deflection.
P = A constant depending upon the distribution of magnetism in the deflecting
and suspended magnet.
m = Magnetic moment of the deflecting or vibrating magnet.
X = Horizontal component of the earth's magnetic force.
~ = Approximate value of
X0 X
-=7 = Value of -=p before the application of the correction
X X
(-!)■
Formulae for calculating mX:
T, = Tn 1 —
oca )
0 I 86400 16
Formulae for calculating
X
= Va r3 sin uQ.
tri ( P \
~ X I1 ~
m
~X
In reference to our observations of Intensity in general, and particularly to the
instruments employed, we add the following details:
T0 (= observed time of one vibration of the magnet). The time was noted at the
precise moment when the point of the scale most distant from the centre