IsoCave: An Isotope-Enabled Reaction-Diffusion Model of Speleothem Formation

IsoCave is an isotope-enabled reaction-diffusion model of speleothem formation that quantitatively simulate the evolution of solution carbonate chemistry, carbonate precipitation, and stable isotope composition, including carbon isotope (d13C), oxygen isotope (d18O), triple oxygen isotope (D'17O) and clumped isotope composition (D47, D48 and D49), of DIC in the drip water and of carbonate precipitates during speleothem formation. License: Creative Commons Attribution-NonCommercial-No Derivatives 4.0 International (CC BY-NC-ND 4.0) Please cite the following reference when using the IsoCave code: Guo, W., Zhou, C. (2019) Patterns and controls of disequilibrium isotope effects in speleothems: Insights from an isotope-enabled reaction-diffusion model and implications for quantitative thermometry, Geochimica et Cosmochimica Acta, 267, 196-226. Guo, W. (2019) IsoCave: An Isotope-Enabled Reaction-Diffusion Model of Speleothem Formation, http://doi.org/10.5281/zenodo.3253242. This work was supported by the U.S. National Science Foundation [NSF-EAR-1530253], the American Chemical Society Petroleum Research Fund, the Andrew W. Mellon Foundation Endowed Fund For Innovative Research and the Investment in Science Fund at Woods Hole Oceanographic Institution