Earth:Cold-water geyser

From HandWiki
Revision as of 09:51, 5 February 2024 by John Stpola (talk | contribs) (fix)
(diff) ← Older revision | Latest revision (diff) | Newer revision → (diff)
Short description: Natural explosive eruption of cold water
Tall, thin geyser erupts as bystanders watch.
Andernach Geyser, (Germany), the world's highest cold-water geyser

Cold-water geysers are geysers that have eruptions whose water spurts are propelled by CO
2
-bubbles, instead of the hot steam which drives the more familiar hot-water geysers: The gush of a cold-water geyser is identical to the spurt from a freshly-opened bottle of soda pop. Cold-water geysers look quite similar to their steam-driven counterparts; however, their CO
2
-laden water often appears whiter and more frothy.[1]

Mechanism

In cold-water geysers, the supply of CO
2
-laden water lies confined in an aquifer, in which water and CO
2
are trapped by less permeable overlying strata. The more familiar hot-water geysers derive the energy for their eruptons from the proximity to (relatively) near-surface magma. In contrast, whereas cold water geysers might also derive their supply of CO
2
from magmatic sources, by definition of "cold-water", they do not also obtain sufficient heat to provide steam pressure, and their eruptions are propelled only by the pressure of dissolved CO
2
. The magnitude and frequency of such eruptions depend on various factors such as plumbing depth, CO
2
concentrations and refresh rate, aquifer water yield, etc.

The water and its load of CO
2
powering a cold-water geyser can escape the rock strata overlying its aquifer only through weak segments of rock, like faults, joints, or drilled wells. A borehole drilled for a well, for example, can unexpectedly provide an escape route for the pressurized water and CO
2
to reach the surface. The column of water rising through the rock exerts enough pressure on the gaseous CO
2
so that it remains in the water as dissolved gas or small bubbles. When the pressure decreases due to the widening of a fissure, the CO
2
bubbles expand, and that expansion displaces the water above and causes the eruption.

Examples

File:Wallenborn-brubbel.ogv Notable cold-water geysers include:

  • Saratoga Springs, New York
  • Crystal Geyser, near Green River, Utah[1][2]

Other cold-water geysers include:

  • Caxambu, Brazil[3]
  • Herľany, Slovakia
  • Sivá Brada, Slovakia
  • Wallender Born (a.k.a. Brubbel), Germany
  • Wehr Geyser Germany
  • Andernach Geyser (a.k.a. Namedyer Sprudel), Germany

References

  1. 1.0 1.1 "Carbon dioxide-driven, cold water geysers". University of California, Santa Barbara. 6 May 2005. http://www.uweb.ucsb.edu/~glennon/crystalgeyser/index.htm. 
  2. "The operation and geography of carbon-dioxide-driven, cold-water geysers". GOSA Transactions 9: 184–192. 2005. 
  3. Bonotto, Daniel Marcos (2016). "Hydrogeochemical study of spas groundwaters from southeast Brazil". Journal of Geochemical Exploration 169: 60–72. doi:10.1016/j.gexplo.2016.07.016.