Albert Roy Davis & Walter C. Rawls

Magnetism and Its Effects on Living Systems

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CHAPTER () THE MAGNETIC EXPOSURE OF SEEDS:

CHAPTER () TRUE NATURE OF MAGNETIC FIELDS:

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On page 22 (below picture) we present the updated concepts from our findings, initially made in 1936 as to the division of the two poles' energies,
each separated one from the other and each having a different potential, value, in electronic magnetic currents. The south ( S) pole
is positive in respect to the north ( N) pole, which is negative. Referring to page 22 you will see that in the use of a straight
bar or long cylinder magnet, the two poles can be used each separated one from the other, and only the pole you wish to work with is then applied for exposure of any system you may wish to apply it to. The conventional horseshoe magnet is not suitable for  use in the application of only the one pole's energies as the poles of the horseshoe magnet are too close together to allow isolation to the degree we can have, by the use of the straight type of magnet. 

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THE CABLE EFFECT:

The Magnetic Blueprint of Life

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NORTH POLE OF THE N-1 MAGNET:

Some of the findings from forty years of well-documented research into magnetic effects on biological systems using the North
pole of the N-1 magnet are:

Surface Tension of Water:

EXAMPLE 1:

To demonstrate one effect of a North unipolar magnetic field on water, 500 ccs of common tap water at 65-75°F was placed in a glass beaker such that the water was exposed only to the energies of the North pole field. The measurable field at the beaker was
adjusted to 1000 gauss. Conventional techniques were used to determine the surface tension, in dynes, of a control sample of the
tap water before exposure. Following exposure for a specified period, the surface tension, in dynes, was again determined. This
test was repeated for a number of water samples for different exposure periods. Table I sets forth the resulting surface tension,
in dynes, above or below the measured control sample as a function of exposure time. Inasmuch as absolute values of surface tension will vary, depending upon variables such as geography and water source, it is only the difference in surface tension between exposed and unexposed water which is believed to be significant. 

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It is apparent from these tests that exposure of water to the North pole field of a magnet increases the surface tension of the water. Maximum effect of the North magnetic field appears to be attained in about three to four minutes. Increased exposure does not appear to increase the effect on the surface tension of water. 

EXAMPLE 2: 

The tests of Example I were repeated except that plastic beakers were used and the polarity of the electromagnet was reversed to
expose the samples to 1000 gauss of South unipolar field energies. The same surface tension determinations were made after each
exposure and compared with the control sample. Table II sets forth the results. 

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Exposure of water to South pole magnetic fields decreases surface tension. Maximum effect of the South magnetic field appears to be attained in about three to five minutes. Increased exposure time does not appear to significantly increase the effect on the surface tension of water. 

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