Juvenile Water

juvenile water

[′jü·vən·əl ′wȯd·ər]
(hydrology)
McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-Hill Companies, Inc.
The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.

Juvenile Water

 

groundwater that enters the subterranean hydrosphere from the depths of the earth for the first time. The term was proposed in 1902 by E. Seuss, who believed that juvenile water was associated with magmatic chambers, from which it was discharged into the upper parts of the crust with gaseous products.

According to current ideas, the formation of juvenile water is linked to the general processes of degasification of mantle material in the course of metamorphism and magmatism. Juvenile water reaching the crust mixes with water of different origin found there. An increased content of carbon dioxide, helium, and oxygen in groundwater is an indirect indicator of juvenile water.

REFERENCES

Kadik, A. A., E. B. Lebedev, and N. I. Khitarov. Voda v magmaticheskikh rasplavakh. Moscow, 1971.
Vulkanizm iglubiny Zemli. Moscow, 1971.
The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.
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