A Manual of Physical Measurements
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MAGNETIC FIELDS The magnetic induction B at any point is measured by the number of lines of induction per unit crosssection and its unit is therefore the line per square centimeter. The magnetic flux $ through a given area is simply the number of lines of induction through this area A, or 1 (225) 150. Exercise 76. Determination of H. (First Method). The lines of magnetic induction due to the earth's field run from South to North, although deviating in some places by an ap- preciable angle from ...the geographical North and South line. This angle is called the angle of declination. The lines of induction are also inclined towards the horizontal plane, making in Ann Arbor an angle of 72 with the horizon. This is the angle of magnetic inclination or the magnetic dip. It should be noted that neither the magnetic decimation nor the dip is constant. They not only vary from place to place over the earth's surface, but they also- vary slightly from year to year and from day to day in the same place.
What to read after A Manual of Physical Measurements?
You can find similar books in the "Read Also" column, or choose other free books by Anthony Zeleny to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
MAGNETIC FIELDS The magnetic induction B at any point is measured by the number of lines of induction per unit crosssection and its unit is therefore the line per square centimeter. The magnetic flux $ through a given area is simply the number of lines of induction through this area A, or 1 (225) 150. Exercise 76. Determination of H. (First Method). The lines of magnetic induction due to the earth's field run from South to North, although deviating in some places by an ap- preciable angle from ...the geographical North and South line. This angle is called the angle of declination. The lines of induction are also inclined towards the horizontal plane, making in Ann Arbor an angle of 72 with the horizon. This is the angle of magnetic inclination or the magnetic dip. It should be noted that neither the magnetic decimation nor the dip is constant. They not only vary from place to place over the earth's surface, but they also- vary slightly from year to year and from day to day in the same place.
What to read after A Manual of Physical Measurements?
You can find similar books in the "Read Also" column, or choose other free books by Anthony Zeleny to read onlineMoreLess
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