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• W2152693230 abstract "The Phoenix mission investigated patterned ground and weather in the northern arctic region of Mars for 5 months starting 25 May 2008 (solar longitude between 76.5 degrees and 148 degrees ). A shallow ice table was uncovered by the robotic arm in the center and edge of a nearby polygon at depths of 5 to 18 centimeters. In late summer, snowfall and frost blanketed the surface at night; H(2)O ice and vapor constantly interacted with the soil. The soil was alkaline (pH = 7.7) and contained CaCO(3), aqueous minerals, and salts up to several weight percent in the indurated surface soil. Their formation likely required the presence of water." @default.
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• W2152693230 date "2009-07-03" @default.
• W2152693230 modified "2023-10-16" @default.
• W2152693230 title "H ₂ O at the Phoenix Landing Site" @default.
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• W2152693230 doi "https://doi.org/10.1126/science.1172339" @default.
• W2152693230 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/19574383" @default.
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