Published July 29, 2019 | Version v1
Software Restricted

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

  • 1. Woods Hole Oceanographic Institution
  • 2. Woods Hole Oceanographic Institution, University of Science and Technology of China

Description

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.

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The IsoCave app is currently available to academic researchers under the Creative Commons Attribution-NonCommercial-No Derivatives 4.0 International (CC BY-NC-ND 4.0) license. By requesting access to this app, you agree to comply with the terms specified in this license (https://creativecommons.org/licenses/by-nc-nd/4.0/).

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Additional details

Funding

Carbonate Formation Induced by CO2 Degassing: Controls on the Isotopic Compositions and Implications for Clumped Isotope Thermometry 1530253
U.S. National Science Foundation

References

  • 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.