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Monoatomic Elements
- 5-30-2003
- Categorized in: Advanced Science, Monatau Extreme
Monoatomic elements are nothing more than elements which are chemically isolated, i.e. instead of 60 atoms of Carbon are 34 atoms of Silicon being bound together in something called a Buckministerfullerene or a knobbier version of the same. The significance lies in the fact that when a single element metal progresses from a normal metallic state to a monoatomic state, it passes through a series of chemically different states. These include:
Other elements which have many of these same properties are the Precious Metals, which include Ruthenium, Rhodium, Palladium, Silver, Osmium, Iridium, Platinum, and Gold. All of these elements have to greater or lesser degree, the same progression as gold does in continuously reducing the number of atoms chemically connected. Many of these precious elements are found in the same ore deposits, and in their monoatomic form are often referred to as the White Powder of Gold.
Monoatomic elements apparently exist in nature in abundance. Precious Metal ores are, however, not always assayed so as to identify them as such. Gold miners, for example, have found what they termed “ghost gold” -- “stuff” that has the same chemistries as gold, but which were not yellow, did not exhibit normal electrical conductivity, and were not identifiable with ordinary emission spectroscopy. Thus they were more trouble than they were worth, and generally discounted.
However, in a technique called “fractional vaporization”, the monoatomic elements can be found and clearly identified via a more advanced emission spectroscopy. This fact was first discussed by David Radius Hudson, who was attempting to separate gold and silver from raw ore -- but was hindered by the ghost gold which had no apparent intrinsic value.
The process involved placing a sample on a standard carbon electrode, running a second carbon electrode down to a position just above the first, and then striking a Direct Current arc across the electrodes. The electrical intensity of the arc would ionize the elements in the sample such that each of the elements would give off specific, identifying frequencies of light. By measuring the specific frequencies of light (the spectrum of the element or elements), one could then identify which elements were in the sample. Typically, such spectroscopic analysis involves striking the arc for 10 to 15 seconds, at the end of which, the carbon electrodes are effectively burned away. According to the majority of American spectroscopists, any sample can be ionized and read within those 15 seconds.
In the advanced technique, the carbon electrodes are sheathed with an inert gas (such as Argon). This allows the emission spectroscopy process to be continued far beyond the typical 15 seconds, in order to fully identify all of the elements in their various forms.
When this was done, in the first seconds, the ghost gold might be identified as iron, silicon, and aluminum. But as the process continued for as long as 300 seconds, palladium began to be read at about 90 seconds, platinum at 110 seconds, ruthenium at 130 seconds, rhodium at 145 seconds, iridium at 190 seconds, and osmium at 220 seconds. These latter readings were the monoatomic elements. Commercially available grades of these metals were found to be including only about 15% of the emission spectroscopic readings.
The mining activity of what is considered the best deposit in the world for six of these elements (Pd, Pt, Os, Ru, Ir, and Rh) yields one-third of one ounce of all these precious metals per ton of ore. But this is based on the standard spectroscopic analysis. When the burn is continued for up to 300 seconds, the same ores might easily yield emission lines suggesting: 6 to 8 ounces of palladium, 12 to 13 ounces of platinum, 150 ounces of osmium, 250 ounces of ruthenium, 600 ounces of iridium, and 1200 ounces of rhodium! Over 2200 ounces per ton, instead 1/3 of 1 ounce per ton! [Keep in mind that rhodium typically sells for $3,000/ounce, while gold sells for $300/ounce!]
The distinguishing characteristic between the first and second readings of the emission spectroscopy for the precious metals is that all of them come in two basic forms. The first is the traditional form of metals: yellow Gold, for example. The second is the very non-traditional form of the metal: the monoatomic state. The chemistries and physics of these two different states of these metals are radically different. More importantly, when the atoms are in the monoatomic state, things really begin to get interesting!
A key to understanding monoatomic elements is to recognize that the monoatomic state results in a rearrangement of the electronic and nuclear orbits within the atom itself. This is the derivation of the term: Orbitally-Rearranged Monoatomic Element (ORME).
- An alloy of numerous atoms of the same element, which exhibit all the characteristics normally associated with the metal: electrical conductivity, color, specific gravity, density, and so forth. The atom’s intrinsic temperature might be room temperature.
- A combination of significantly fewer atoms of the same element, which no longer exhibit all of the characteristics normally associated with the metal. For example, the electrical conductivity or color might change. The atom’s intrinsic temperature drops, for example, to 50 to 100 oK (or about two hundred degrees below zero oC).
- A Microcluster of far few atoms -- typically on the order of less than one hundred atoms, and as few as a dozen or so atoms. The metal characteristics begin to fall off one by one until the so-called metal is hardly recognized. The intrinsic temperature has now fallen to the range of 10 to 20 oK, only slightly above Absolute Zero.
- A Monoatomic form of the element -- in which each single atom is chemically inert and no longer possesses normal metallic characteristics; and in fact, may exhibit extraordinary properties. The atom’s intrinsic temperature is now about 1 oK, or close enough to Absolute Zero that Superconductivity is a virtually automatic condition.
Other elements which have many of these same properties are the Precious Metals, which include Ruthenium, Rhodium, Palladium, Silver, Osmium, Iridium, Platinum, and Gold. All of these elements have to greater or lesser degree, the same progression as gold does in continuously reducing the number of atoms chemically connected. Many of these precious elements are found in the same ore deposits, and in their monoatomic form are often referred to as the White Powder of Gold.
Monoatomic elements apparently exist in nature in abundance. Precious Metal ores are, however, not always assayed so as to identify them as such. Gold miners, for example, have found what they termed “ghost gold” -- “stuff” that has the same chemistries as gold, but which were not yellow, did not exhibit normal electrical conductivity, and were not identifiable with ordinary emission spectroscopy. Thus they were more trouble than they were worth, and generally discounted.
However, in a technique called “fractional vaporization”, the monoatomic elements can be found and clearly identified via a more advanced emission spectroscopy. This fact was first discussed by David Radius Hudson, who was attempting to separate gold and silver from raw ore -- but was hindered by the ghost gold which had no apparent intrinsic value.
The process involved placing a sample on a standard carbon electrode, running a second carbon electrode down to a position just above the first, and then striking a Direct Current arc across the electrodes. The electrical intensity of the arc would ionize the elements in the sample such that each of the elements would give off specific, identifying frequencies of light. By measuring the specific frequencies of light (the spectrum of the element or elements), one could then identify which elements were in the sample. Typically, such spectroscopic analysis involves striking the arc for 10 to 15 seconds, at the end of which, the carbon electrodes are effectively burned away. According to the majority of American spectroscopists, any sample can be ionized and read within those 15 seconds.
In the advanced technique, the carbon electrodes are sheathed with an inert gas (such as Argon). This allows the emission spectroscopy process to be continued far beyond the typical 15 seconds, in order to fully identify all of the elements in their various forms.
When this was done, in the first seconds, the ghost gold might be identified as iron, silicon, and aluminum. But as the process continued for as long as 300 seconds, palladium began to be read at about 90 seconds, platinum at 110 seconds, ruthenium at 130 seconds, rhodium at 145 seconds, iridium at 190 seconds, and osmium at 220 seconds. These latter readings were the monoatomic elements. Commercially available grades of these metals were found to be including only about 15% of the emission spectroscopic readings.
The mining activity of what is considered the best deposit in the world for six of these elements (Pd, Pt, Os, Ru, Ir, and Rh) yields one-third of one ounce of all these precious metals per ton of ore. But this is based on the standard spectroscopic analysis. When the burn is continued for up to 300 seconds, the same ores might easily yield emission lines suggesting: 6 to 8 ounces of palladium, 12 to 13 ounces of platinum, 150 ounces of osmium, 250 ounces of ruthenium, 600 ounces of iridium, and 1200 ounces of rhodium! Over 2200 ounces per ton, instead 1/3 of 1 ounce per ton! [Keep in mind that rhodium typically sells for $3,000/ounce, while gold sells for $300/ounce!]
The distinguishing characteristic between the first and second readings of the emission spectroscopy for the precious metals is that all of them come in two basic forms. The first is the traditional form of metals: yellow Gold, for example. The second is the very non-traditional form of the metal: the monoatomic state. The chemistries and physics of these two different states of these metals are radically different. More importantly, when the atoms are in the monoatomic state, things really begin to get interesting!
A key to understanding monoatomic elements is to recognize that the monoatomic state results in a rearrangement of the electronic and nuclear orbits within the atom itself. This is the derivation of the term: Orbitally-Rearranged Monoatomic Element (ORME).
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You may find links that lead to
interesting information, or there
may be links to undesirable sites.
If you find any of these undesirables,
PLEASE let us know the URLs so
we can block them from our campaign. |