27 Geochemistry, Organic (Posters)
Sunday, 31 October 2010
8:00 AM - 6:00 PM
Hall D
CARBON ISOTOPIC FRACTIONATION AS A FUNCTION OF CHARRING TEMPERATURE DURING THE PRODUCTION OF BIOCHAR
Paper number: 27-8
Program: Technical Sessions
Time: 8:00 AM – 6:00 PM
Authors
-
David W. RutherfordU.S. Geological Survey, Denver, CO
-
Colleen E. RostadU.S. Geological Survey, Denver, CO
-
Nabil M.R. SaadPicarro, Inc, Sunnyvale, CA
Abstract
13C concentration decreases in both the switch grass and pine wood biochars as formation temperature increase from 250o to 600oC. The 13C concentration then increases as charring temperature increases from 700o to 900oC. These changes are most likely due to the kinetic isotope effect. From 250o to 600oC, carbon atoms in the original cellulose, hemicellulose, and lignin structural components react to form graphene structures. Under these conditions, the 13C atoms will react slightly more slowly that the 12C atoms and therefore, there will be a depletion of 13C in the resulting graphene structures. At the higher temperatures increases in 13C concentrations in the chars indicate that the reverse is taking place and that the graphene structures are being degraded to volatile compounds that are depleted in 13C. These results are consistent with earlier reported results on the formation of aromatic carbons during initial charring followed by loss of aromatic carbon with prolonged charring.