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Hydrogen Cycle
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This section presents new scientific theory surrounding the hydrogen cycle. Unlike conventional thought that supports the concept of a hydrogen cycle explained in biological terms, this new proposed theory suggests explanation of the basic energy cycle of the planet in terms that involve the planet's core, crust, oceans and atmosphere.
To begin, let's take a brief look below at the cycle as science explains it today, extracted from Wikipedia.org.
Hydrogen is one of the constituents of water. It recycles as in other biogeochemical cycles. It is actively involved with the other cycles like the carbon cycle, nitrogen cycle ,sulfur cycle and oxygen cycle as well.
Anaerobic fermentation of organic substances to carbon dioxide and methane is a collaborative effort involving many different biochemical reactions, processes and species of microorganisms. One of these many processes that occur is termed "interspecies hydrogen transfer". This process has been described as integral to the symbiosis between certain methane-producing bacteria (methanogens) and nonmethanogenic anaerobes. In this symbiosis, the nonmethanogenic anaerobes degrade the organic substance and produce -among other things- molecular hydrogen (H2). This hydrogen is then taken up by methanogens and converted to methane via methanogenesis. One important characteristic of interspecies hydrogen transfer is that the H2 concentration in the microbial environment is very low. Maintaining a low hydrogen concentration is important because the anaerobic fermentative process become increasingly thermodynamically unfavorable as the partial pressure of hydrogen increases.
Extracted from Wikipedia.org
We believe the hydrogen cycle is much more complex than what is described above, as it forms the fundamental energy system of the planet.
Hydrogen is the most abundant element identified by science, comprising 75% of all matter by mass; and it would be logical to presume that it plays a very big part in the make-up and functioning of the universe. In our atmosphere, hydrogen, in its diatomic state (H2) as pure hydrogen, is only a very tiny component. However, when you account for the amount of hydrogen bonded to many other atoms in molecules such as water, the amount of hydrogen is much higher.
Water is a hydrogen transport mechanism that allows hydrogen to move slowly through the environment and then out of the atmosphere. Water is comprised of two thirds hydrogen and one third oxygen (H2O). While hydrogen is positive by nature, oxygen is negative, and these characteristics allow hydrogen and oxygen to form water. If hydrogen is ignited in an oxygen environment, the only byproduct is water and heat. This makes hydrogen a very unique atom in terms of both physics and chemistry, and as such, is a critical element in the functioning of DiAxiom's NOHRMAN (H+e) System outlined in more detail elsewhere on this site.
The Hydrogen cycle theory will be described as three separate systems within our planet's energy system. The first of these is the charging cycle. This is where hydrogen first enters into our environment. The second system is the discharge cycle and is where hydrogen leaves the lower atmosphere of the planet. The third is the release cycle where hydrogen leaves the upper atmosphere to join the plasma of the solar system.
Hydrogen is in a constant state of flux from the core of the planet, into the magma layer, crust, oceans, atmosphere and finally, out into space. It is the movement of this hydrogen that, within the proposed theory, causes the formation of water on our planet, volcanoes to occur, and to a great extent, our weather systems.
