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Magnetic Force
The MF1-A consists of a pair of coils in the Helmholtz configuration and a small magnetized disk mounted so it can rotate in a gimbal which is suspended from a spring. By using Hooke's Law, a measurement of the spring's deflection can be used to infer the magnetic force on the disk. The spring can be calibrated by attaching one-gram steel ball bearings and the coils may be used individually or together in two ways:
There are four main objectives: 1. To demonstrate that there is no net magnetic force on a magnetic dipole in a region of uniform magnetic field. The coils are connected in series with the current circulating in the same direction in both coils. In the presence of a uniform field of 65 Gauss, the spring does not elongate or compress. This almost always surprises students who expect the dipole to move up or down depending upon the orientation of the dipole with respect to the field. The observation that the dipole only rotates to align itself along the field forces the students to reconsider their preconceived ideas about magnetism. 2. To show that a net magnetic force on a dipole exists only in the presence of a magnetic field gradient, a spatially varying field. For these experiments the coils are connected in series with the currents flowing in opposite directions, creating a field gradient along the axis.
Using the physical parameters of the MF1-A coils, students can calculate the field gradient at any axial position. After calibrating the spring, students can measure the magnetic force as a function of field gradient. The magnitude of the magnetic moment can be plotted from the slope of the student data shown in Figure 1. The measurements shown were made at the midpoint of the coils.
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