Re: Inertial Drives

Jerry W. Decker ( (no email) )
Fri, 30 Jan 1998 01:31:40 -0800

Hi Folks!

Went back to reread the Reynolds files and they were just as amazing as
the first few times I read them, check out this very specific quote from
http://keelynet.com/energy/reynold1.txt ;

Dilatancy refers to the shear-induced expansion of a mass of solid
particles. Reynolds' used dilatancy to explain the curious behavior of
beach sand. Walking on the beach is easy on the wet sand near the water,
but difficult in dry sand.

When walking on wet beach sand, each time a heel strikes the surface, the
area surrounding the impact appears to turn dry or white. This dry area
appears to propagate from the point of impact like some sort of field.
According to Reynolds (2),

it is in many ways analogous to a gravitational field.

When a close-packed mass of sand is subjected to a deforming force, the
particles attempt to slide past one another. This results in an
expansion or dilation of the deformed volume.

The action of expansion or dilation can be understood by making two
fists, holding them in front of you and placing the knuckles of one fist
into the spaces between the knuckles of the other fist. Your knuckles
should now be "geared" to each other with the open spaces (interstices)
at a minimum.

Now, if one set of knuckles is moved up or down relative to the other, a
point of maximum open "packing" is reached then the top of one knuckle is
directly on top of another. This represents the maximum expansion or
dilation of the volume containing the sheared "particles", i. e.,
knuckles.

In sand, for the sheared volume to expand, water must flow in to fill the
interstices. The sheared portion of sand underfoot therefore sucks water
away from the surrounding mass of wet sand and its surface turns white or
dry. This gearing action is responsible for the strength of the sand and
also for the rigidity of bricks of coffee packaged in flexible plastic
foil bags.
-----------------------
So, this gravity seepage theory, means it has to have a 'seepage'
constant, a specific amount of time, based on the density of the
mass (and ameliorated/influenced by surrounding masses to some
degree)...if we can BEAT THAT SEEPAGE TIME, we can CONTROL GRAVITY and
Inertia, just as Puthoff's paper 'ZPE as the cause of Inertia' indicates.
A related document by Haisch is; http://www.jse.com/haisch/mercury.html

I sent Hal an email describing this tendril/seepage effect which seems to
have been proven by Aspdens experiment...he responded by saying he
thought it was a novel and interesting concept, wanting more information,
so that is why I posted the Reynolds files to KeelyNet, subsequently
sending him the URLs via email so he could read the files. He never
commented on them but I never asked what he thought, guess I should.

--                Jerry W. Decker   /   jdecker@keelynet.com          http://keelynet.com    /  "From an Art to a Science"       Voice : (214) 324-8741    /   FAX :  (214) 324-8741   KeelyNet - PO BOX 870716 - Mesquite - Republic of Texas - 75187