Temperature and pH Changes Associated with the Hydration of Amorphous Silicate Smokes

Details Temperature and pH Changes Associated with the Hydration of Amorphous Silicate Smokes Temperature and pH Changes Associated with the Hydration of Amorphous Silicate Smokes

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.2536c&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.2536

Computer Science

Scientific paper

The hydration of Fe-Si smokes results in acidic pH levels and negligible
change in temperature. When mixed with Mg-Si smokes, pH becomes alkaline
and temperature increases slightly. Water-rock ratio is a minor variable
relative to composition.

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