Duricrust

A duricrust inselberg near Dori, Burkina Faso

Duricrust is a hard layer on or near the surface of soil. Duricrusts can range in thickness from a few millimeters or centimeters to several meters.

It is a general term (not to be confused with duripan) for a zone of chemical precipitation and hardening formed at or near the surface of sedimentary bodies through pedogenic and (or) non-pedogenic processes. It is typically formed by the accumulation of soluble minerals deposited by mineral-bearing waters that move upward, downward, or laterally by capillary action, commonly assisted in arid settings by evaporation.[1][2][3] Minerals often found in duricrust include silica, iron, calcium, and gypsum.

Duricrusts need to be formed in absolute accumulation, therefore they must have a source, transfer and precipitation. Duricrust is often studied during missions to Mars because it may help prove the planet once had more water. Duricrust was found on Mars at the Viking 2 landing site, and a similar structure, nicknamed "Snow Queen," was found under the Phoenix landing site.[4] Phoenix's duricrust was later confirmed to be water-based.[5]

See also

References

  1. ↑ Dixon, 1994
  2. ↑ Woolnough, 1930
  3. ↑ NADMSC SLTT, 2004
  4. ↑ Rayl, A.J.S. (June 1, 2008). "Holy Cow, Snow Queen! Phoenix Landed on Ice, Team Thinks". The Planetary Society. Retrieved November 12, 2008.
  5. ↑ "Phoenix and the Holy Cow". Astronomy Picture of the Day. November 12, 2008. Retrieved November 12, 2008.

Further reading

External links


This article is issued from Wikipedia - version of the Tuesday, September 29, 2015. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.