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Grad Students Find Missing Link in Early Martian Water Cycle

  • Researchers Mohammad Afzal Shadab and Eric Hiatt, pursuing their graduate studies at The University of Texas at Austin, have created a model to examine how water moved through early Mars’ surface down to underground aquifers.
  • Their computer model simulates how water took between 50 and 200 years to seep from Mars’ surface down to an aquifer about a mile underground.
  • The findings suggest much of Mars’ ancient water was trapped underground and less was available to replenish surface lakes, lakes, or the atmosphere through evaporation.
  • Their model suggests that the underground water may have formed a reservoir at least 300 feet deep, and Hiatt noted that the water infiltrating the Martian crust was not escaping into space.
  • This research revises Mars’ early hydrology picture, implying limited surface water stability and supporting future missions focused on subsurface water and astrobiology.
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Phys.org broke the news in United Kingdom on Monday, May 19, 2025.
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