liquefaction
noun: the conversion of a solid or a gas into a liquid
Schauberger
It is known, for example, that for the liquefaction of brown coal (lignite) appropriate catalysts are required. Here there is no uniformity, because everything is bipolar and therefore it is necessary to make a clear distinction between positive and negative catalysts. The chemical reaction itself is of no interest biologically speaking, and the whole thing must be considered from a higher standpoint, otherwise it would be impossible, for example, to liquefy hard coal (anthracite), i.e. to transfer it to the next higher state of evolvement. This also applies to calcium (combusted marble) and other insoluble basic substances. That a falling temperature gradient is of decisive importance for biological processes of development, has already been emphasised elsewhere. Since science, which thinks too mechanistically, has also failed to grasp this, it would unable to understand the naturalesque interpretation of the concept of 'reaction', which here is to be understood as a process of ur-genesis. Without this there would be no reproduction or further development, which is responsible for higher-grade emulsions, namely the inner fusion (marriage) of etherialised primary substances in the 4th spacial dimension. As long as the [The Energy Evolution - Harnessing Free Energy from Nature, The Catalysts]
Just a small heat-influence is enough to separate the higher factors from more inferior ones contained in good water. As the condensing reversionary elements of retro-development, the latter appear and become visible in the form of substantial physical matter. It should therefore be quite obvious that with the high temperatures known to be necessary for contemporary methods of coal liquefaction, the identical processes of separation and concentration must take place in increased measure. [The Energy Evolution - Harnessing Free Energy from Nature, The Liquefaction of Coal by Means of Cold Flows]
(2) "A process for the liquefaction of gases by the Joule–Thomson effect. In this process devised by Carl von Linde (1842-1934) for liquefying air, the air is freed of carbon dioxide and water and compressed to 150 atmospheres. The compressed gas is passed through a copper coil to an expansion nozzle within a Dewar flask. The emerging air is cooled by the Joule–Thomson effect as it expands and then passes back within a second copper coil that surrounds the first coil. Thus the expanded gas cools the incoming gas in a process that is said to be regenerative. Eventually the air is reduced to its critical temperature and, at the pressure of 150 atmospheres (well above its critical pressure), liquefies. The process is used for other gases, especially hydrogen and helium. Hydrogen has first to be cooled below its inversion temperature (see Joule–Thomson effect) using liquid air; helium has first to be cooled below its inversion temperature using liquid hydrogen." [Collins Dictionary of Science. Oxford University Press, Great Britain, 1984, ISBN 0-19-211593-6.] — Ed [The Energy Evolution - Harnessing Free Energy from Nature, The Liquefaction of Coal by Means of Cold Flows]
This product of synthesis is characterised by the fact that the ratio between oxygen and its carbone counterpart is 4% : 96%, because all the remaining oxygen has been transformed into fertilising substances and then bound. Therefore the new product of synthesis has the highest negative valency and is of geospheric character. Certain factors relating to these processes should be noted: In the scientific synthesising process heat has a shrivelling effect on the decisive formative substance in its nascent state, while physical pressure ruptures its outer envelope. In the case of coal liquefaction by means of cold flows the increasing cooling on the developmental path acts to increase the potential. However, since the increase in the potential of the true formative substance is of a purely energetic nature, it would be unable to break through the outer envelope had this not been mechanically abraded through the circumvolution and inner rotation (gyrate within and about itself|about itself and its own axis) caused by the increasing frictional pressure arising from the doubly increased velocity of the whole water-body. These differences demand the closest attention and consideration. The product of synthesis obtained by means of cold flows, binds itself into its own waste product (juvenile water). Therefore apart from a new, fresh and more highly cultured energy, an associated carrier-substance of the highest order is also created at the expense of the gradually transforming (internally reconstituted) stocks of old water. This two-fold transformation represents the increase and the qualitative improvement of what has been quantitatively increased (the growth of water). The finished product is a crystal-clear water that has neither taste, nor smell, nor colour, because in this product of synthesis all kinds of things are on the loose or have been loosed (emancipated), i.e. they have been raised to the [The Energy Evolution - Harnessing Free Energy from Nature, The Liquefaction of Coal by Means of Cold Flows]
See Also