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WORLD’S NATURAL SALTIEST POND DON JUAN POND

WORLD’S NATURAL SALTIEST POND

 DON JUAN POND 


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ESPITE  being in Antarctica, the Don Juan Pond doesn’t freeze! And that too when temperatures hover around - 500C.
          Don Juan Pond is a small, extremely salty, ankle-lake located in the McMurdo Dry Valleys of Antarctica, nestled I Wright Valley between the Asgard Mountain Range and the Olympus Mountain Range. The pond was discovered in 1961 and pilots Lt John Hickey who discovered it.
          Don Juan Pond is the saltiest natural body of water on Earth with a salinity level of over 40%, which is around 18 times saltier than the ocean. Or some eight times as salty as the Dead Sea. Although the lake is located n one of the coldest regions of Antarctica, it is so salty that it never freezes even when the surface temperature drops to -500 C during Austral winter, making it one of the unique places for the investigation of habitability n extreme conditions n earth and possible for  life on Mars.
          The major solute in the pond is calcium chloride salt (CaCl2). Earlier it was believed that the salinity of the pond was contributed by the ground water. However, according to a study published in Nature Publishing Group’s open access journal, Scientific Reports, the pond gets its salt from precipitation.
          The researchers explained the process of deliquesce during which, when the humidity in the air spikes, surface salt near the pond absorbs the available moisture. Those water-loaded salts then stream through the loose soil until they reach the permafrost layer beneath. There they stay until the occasional stream of snow melt washes the salts down the channel and into the pond.
          And this is how the world’s saltiest natural water body is able to remain liquid in one of the coldest and driest places on earth.
          Head and Dickson from Brown University approached Antarctica as a model for the cold, dry desert of Mars. According to them Don Juan Pond could tell us something about the possibilities of flowing water on Mars, both in the pas and in the present.

           

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