A Mills Dynasty?
[Atomic Physics] [Max Planck Institute for Nuclear Physics]
Introduction
" The study of simple systems has been of particular interest since the very first days of physics. Simple systems, consisting of just a few particles do not show the puzzling variety of phenomena known from solid state physics, for example. But they offer invaluable insights into the the properties of particles and fundamental forces. To gain a first understanding of atomic physics it is a much more promising approach to study hydrogen instead of complex molecules, for instance.
The object of our studies is one of these simple systems: the Positronium negative ion. This exotic entity is a bound state of a positron and two electrons. It is similar to the negative ion of hydrogen (H-). In fact, it is the most simple three body problem imaginable."
Professor Allen Mills is at the University of California Riverside (UCR)
"Allen Paine Mills, Jr.; Observation of the Positronium Negative Ion; Phys. Rev. Letters 46, 717; 1981"
"Allen Paine Mills, Jr.; Measurement of the Decay Rate of the Positronium Negative Ion; Phys. Rev. Letters 50, 671; 1983"
Here is where a Stable Mass ~ 2.5+ Electron (ELECTRONIUM) can form and get in Groundwater/Rainwater in
the Earth or from the Potassium-Argon in the Oceans.
It would explain Randy Mills' "Fractional Orbit Hydrino" High Energy Release.
The Stable Argon-40 (~1% in the air) can also contain the Electronium Particle.
"Potassium-argon or K-Ar dating is a geochronological method used in many geoscience disciplines. It is based on measuring the products of the radioactive decay of potassium (K), which is a common element found in materials such as micas, clay minerals, tephra and evaporites.
Potassium (K) exisits in 3 isotopes - 39K (92.23%), 40K (0.00118%), 41K (6.73%)."
"The radioactive isotope 40K decays to 40Ar and 40Ca with a half-life of 1.26x109 years. 40Ca is the most common form of Ca, however, so the increase in abundance due to K decay results in a negligible increase in total abundance making it less useful as a geochronometer. The 40Ar isotope is much less abundant however, and is therefore a more useful isotope."
"As argon is a gas, it is able to escape from molten rock. However, when the rock solidifies, the decayed 40Ar will begin to accumulate in the crystal lattices. In order to determine the 40Ar content of a rock, it must be melted and the isotopic composition of the released gas measured via mass spectrometry. It is also necessary to separately measure the amount of 40K in the sample. This can be measured using flame photometry or atomic absorption spectroscopy. The ratio between the 40Ar and the 40K is related to the time elapsed since the rock was cool enough to trap the Ar. This is the key principle behind K-Ar dating"
