Mass loss kinetics and isotope fractionation of Type B CAI melts at 1400 C and solar fO2

Details Mass loss kinetics and isotope fractionation of Type B CAI melts at 1400 C and solar fO2 Mass loss kinetics and isotope fractionation of Type B CAI melts at 1400 C and solar fO2

Mar 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997lpi....28.1161r&link_type=abstract

Conference Paper, 28th Annual Lunar and Planetary Science Conference, p. 161.

Computer Science

1

Carbonaceous Chondrites, Fractionation, Aluminum Compounds, Calcium Compounds, Meteoritic Composition, Melting, Mass Transfer, Evaporation, Magnesium Compounds

Scientific paper

Novel data are presented on the isotope fractionation and rate of mass loss of CAIB composition melts at 1400 C and 1 bar total pressure of gas, with an oxygen fugacity corresponding to solar gas. The two primary effects of such highly reducing conditions are that the rate of mass loss is increased by about three orders of magnitude relative to free evaporation, and there is no detectable fractionation of the Mg isotopes.

Affiliated with

Also associated with

No associations

Rating

Mass loss kinetics and isotope fractionation of Type B CAI melts at 1400 C and solar fO2 does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Mass loss kinetics and isotope fractionation of Type B CAI melts at 1400 C and solar fO2, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Mass loss kinetics and isotope fractionation of Type B CAI melts at 1400 C and solar fO2 will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-873885