65_HS1-834228961_62-HQ-83894_Section_006

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that powe,. to accompl·iah thts end would haue t o bs dert ued
from the cracking of on atomic /uel such as heauy water.
In that connection hs atateB that the tonoaphers
surroundtng the earth radtates postttue tono toward the
earth's surface.
Jfany of these are diaatpatsd by oombtntng
wtth part'tcles in the atmos.ohorc with tht1 result -that poatt·ive
ton3 are mora concentrated· near the earth's surface than
higher above it. He reasons that a dtsk could be ratsed
tn the atr by emittin9 a great quantity of nogattua ions
through tto upper surface and causing a decrease tn preaaure
whtch would result in the pree3urc underneath the disk
/orctng it upward.
lle indicates that aonowhere between
thtt surface o/ the earth and the ionosphere thi3 presaure
would equaltae at which point the disk could go no htgher.
It could then be moued horizontally by emitting negative
tona tn ~he dtrection in which tt ta ·aestred to moue.
llr. Eekhout stated that he did not feel such a
deutce could be re~ote controlled atnce tt would probably
not be poastble to maintain radt o contact with tt.
Ile
/eels, however, that the occupants of such a deutce ~ould
be /ullU protected stnce accordtng to the electrtcal theory
demonstrated by Tara.day's Cage the current tnuolued tn the
propul.aton of auch a deviae woU.Zd concentrate ttsel/ around
the edges of the disk.
The for~gotng ta Jurntehed for your t~formatton.
{NOTE ON YELLOW: Eekhout was interviewed at 2:15 p. m.
5- 5-52, by Super vi sor v. H. Bailey by reference from Ur.
Nichols' Office.
Bureau files contain no data identifiable
wi t h him. )
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