ESPECIALLY THE MAGNETIC ORIENTATION OF PARTICLES
Abstract
Experimental results are given spectral analysis of rock granite-aplite in order to reveal the chemical composition of magnetic rock ores. DF-24 was used to measure spectral analysis, and the method proposed earlier . As used to measure the natural residual magnetization. Experimental studies have shown that the magnetic phenomena in mountain granite-aplite and the conditions for the formation of natural residual magnetization in it are very specific and the following factors are observed: ferromagnetic grains are very small from 1 to 10 microns.
The paper considers the features of magnetic orientation, in order to reveal how magnetized particles are deposited in water, how the value of the magnetic moment – µ changes in a constant magnetic field-H. Weленыfound errors of inclinati n
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