PHOSPHORUS AS A MARKER IN C-11
It has been noted by several people that C-11, which they have produced from shallow coastal seawater, did not
have the psycho or biological activity of LIQUID-CHITM , which is produced from
deep sea Pacific Ocean water. It is possible that phosphorous content may explain this anomaly.
Phosphorus may be an indicator of potency and should be monitored in all source material and precipitates for
this reason. Soluble phosphorus leached from the land and transferred to the oceans eventually forms
insoluble calcium phosphate and sinks to the sea floor as sediment.
In most parts of the oceans this sedimented phosphorus is lost as a source of nutriment. However, due to
the earth’s rotation and the way that ocean currents move, there are regions, mostly on the west coasts of
continents, where currents upwell against the continental shelf. The result of this upwelling is that these
sediments are returned to the surface where they may reenter the biological food chain.
The following table illustrates the point:
Phosphorus abundance in parts per million
| Atlantic surface water |
.0015 |
| Atlantic deep water |
.042 |
| Pacific surface water |
.0015 |
| Pacific deep water |
.084 |
| LIQUID-CHITM |
.22 |
The difference between the Atlantic and Pacific Oceans may be attributable to phosphorus leached from volcanic
ejecta in the ring of fire region.
It has been noted that M-State materials exhibit specific gravity even in solution and that stratification takes
place in the oceans. The upwelling currents that return phosphorus to the near surface may be doing the same with
ORMUS.
For these reasons, phosphorus content should be monitored as an indicator of potency when producing C-11.
This, together with the parting procedure posted at www.subtleenergies.com/ormus/tw/wm-assay.htm, should enable one to make the best possible C-11
concentrate.
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