On the effects of temperature on the intensity of magnetic forces; and on the diurnal variation of the terrestrial magnetic intensity
The details of the author’s experiments upon the above subjects are given in an extended series of tables, commencing with a temperature of — 3° Fahr. up to 127° Fahr. Mr. Christie found that as the temperature of the magnets increased, their intensity diminished, in direct contradiction to the notion of destroying magnetism by intense cold. From a temperature of 80° the intensity decreased rapidly as the temperature increased, and at above 100° a portion of the power of the magnet was permanently destroyed. In regard to the diurnal changes in the terrestrial intensity, the author’s experiments lead him to suggest the following queries for the consideration of those who may have an opportunity of making such observations:—Does the time of the minimum intensity correspond with the time at which the sun is on the magnetic meridian ? Does the time of maximum intensity correspond to the sun’s passing the plane of the equator of the dipping-needle ? Does any change take place in the intensity while the sun is below the horizon ? Are any periodical effects corresponding to the time of rotation of the sun about its axis observable ? Is the diurnal change of intensity at the time of new moon sensibly different from what it is at the time of quadrature ? If the moon do produce an effect on the needle, it is evidently less than that of the sun;—should we then attribute it to solar heat, or to the magnetism of the sun ?