Effect of temperature and polymorph mineral solubility on average modeled dissolution rates.

• Main Authors: Justin B. Ries, Megan Switzer
• Format: Dataset
• Language: unknown
• Published: Biological and Chemical Oceanography Data Management Office (BCO-DMO) 2018
• Subjects: oceans; Ocean acidification
• Online Access: https://search.dataone.org/view/sha256:bfa770512c6e877dc626c41e8d510b5d480bfee4fb6792fbec533c391e72139b

<p>Effect of temperature and polymorph mineral solubility (high-Mg calcite &gt; aragonite &gt; low-Mg calcite) on average modelled dissolution rate over Ω_A = 0.2 - 5.0 (using Ω_A increments of 0.2) at 10.1 °C (± 0.02) and 25.0 °C (± 0.02).&nbsp; Results ranked by magnitude of temperature effect on average dissolution rate. Ω_A = saturation state of seawater with respect to aragonite.</p> <p>See also related datasets for seawater chemistry, calcification rates, and dissolution rates.&nbsp;<br /> <a href=\"https://bco-dmo.org/dataset/723864\">Seawater chemistry</a>&nbsp;<br /> <a href=\"https://bco-dmo.org/dataset/723866\">Calcification rates</a><br /> <a href=\"https://bco-dmo.org/dataset/723867\">Dissolution rates</a></p> <p>These data are published in:</p> <p>Ries, J.B., Ghazaleh, M.N., Connolly, B., Westfield, I., Castillo, K.D., 2016, Impacts of ocean acidification and warming on the dissolution kinetics of whole-shell biogenic carbonates.&nbsp; Geochimica et Cosmochimica Acta 192: 318–337. doi:&nbsp;<a href=\"https://www.doi.org/10.1016/j.gca.2016.07.001\">10.1016/j.gca.2016.07.001</a></p> <p>Please see manuscript for complete methodology.&nbsp;</p> <p>&nbsp;</p>