2023
DOI: 10.1021/acsenvironau.2c00061
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Climate Change and the Sea: A Major Disruption in Steady State and the Master Variables

Abstract: Since the beginning of the industrial revolution, humans have burned enormous quantities of coal, oil, and natural gas, rivaling nature’s elemental cycles of C, N, and S. The result has been a disruption in a steady state of CO2 and other greenhouse gases in the atmosphere, a warming of the planet, and changes in master variables (temperature, pH, and pε) of the sea affecting critical physical, chemical, and biological reactions. Humans have also produced copious quantities of N and P fertilizers producing wid… Show more

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Cited by 5 publications
(2 citation statements)
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“…The diagenesis of calcium carbonates, including their dissolution and recrystallization, is important in both marine and freshwater systems because of its impact on the ocean carbon budget, ocean acidification , and for CO 2 capture and storage technologies . Underlying these diagenetic factors, the two most common CaCO 3 polymorphs (aragonite and calcite) have low but different values for equilibrium solubility constants . In this work, we use solid-state NMR and infrared spectroscopy to follow the manifestation of calcite-to-aragonite phase conversion processes when powders of these two phases are cosuspended in water.…”
mentioning
confidence: 99%
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“…The diagenesis of calcium carbonates, including their dissolution and recrystallization, is important in both marine and freshwater systems because of its impact on the ocean carbon budget, ocean acidification , and for CO 2 capture and storage technologies . Underlying these diagenetic factors, the two most common CaCO 3 polymorphs (aragonite and calcite) have low but different values for equilibrium solubility constants . In this work, we use solid-state NMR and infrared spectroscopy to follow the manifestation of calcite-to-aragonite phase conversion processes when powders of these two phases are cosuspended in water.…”
mentioning
confidence: 99%
“…6 Underlying these diagenetic factors, the two most common CaCO 3 polymorphs (aragonite and calcite) have low but different values for equilibrium solubility constants. 7 In this work, we use solid-state NMR and infrared spectroscopy to follow the manifestation of calcite-toaragonite phase conversion processes when powders of these two phases are cosuspended in water. Moreover, we identify at the molecular level a mechanism that inhibits the phase conversion: surface embedding of a dissolved phosphatebearing additive.…”
mentioning
confidence: 99%