“…We determined D H 2 O vs. C H 2 O relationships for each concentration profile in several ways: (1) by direct calculation using BoltzmannMatano methods (Crank, 1975;Sauer and Freise, 1962;den Broeder, 1969;Dayananda, 1983), which makes no assumptions about the functional form of the relationship; (2) by assuming simple functional forms for the relationship between D H 2 O and C H 2 O (e.g., D H 2 O is a linear function of C H 2 O (e.g., Shaw, 1974), or D H 2 O is an exponential function of C H 2 O (e.g., Delaney and Karsten, 1981)); or (3) by assuming a specific diffusion model based on the speciation of water dissolved in silicate melt (e.g., Stolper, 1982a,b;Behrens and Nowak, 1997;Nowak and Behrens, 1997;Zhang, 1999;Doremus, 2000;. By comparing the results of these various approaches to characterizing the D H 2 O vs. C H 2 O relationship, we can evaluate the confidence and detail with which this relationship can be determined from diffusion profiles of the sort we have obtained (i.e., that extend over a significant C H 2 O range).…”