2019
DOI: 10.1201/9781315138770
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Carbon Dioxide Equilibria and their Applications

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Cited by 106 publications
(82 citation statements)
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“…The inhibition of bacterial growth due to high CO 2 concentration environment is thought to be occurred through the diffusion of H 2 CO 3 across the bacterial membrane that altering intracellular pH (Wolfe, ). These changes increased at low temperatures because of the higher solubility of CO 2 at decreased temperatures and may affect enzymes involved in metabolic pathways within the cell (Butler, ). Moreover, high CO 2 concentrations may inhibit decarboxylation reactions, in which CO 2 is released by feedback mechanisms.…”
Section: Resultsmentioning
confidence: 99%
“…The inhibition of bacterial growth due to high CO 2 concentration environment is thought to be occurred through the diffusion of H 2 CO 3 across the bacterial membrane that altering intracellular pH (Wolfe, ). These changes increased at low temperatures because of the higher solubility of CO 2 at decreased temperatures and may affect enzymes involved in metabolic pathways within the cell (Butler, ). Moreover, high CO 2 concentrations may inhibit decarboxylation reactions, in which CO 2 is released by feedback mechanisms.…”
Section: Resultsmentioning
confidence: 99%
“…Dissolved CO 2 can also be hydrated to form carbonic acid; however, its concentration is ∼10 −3 of the concentration of dissolved CO 2 . Therefore, the hydrated and dissolved CO 2 may be considered as a single species . The associated rate and equilibrium constants for these reactions are taken from previous literature reports: K1=3.35x10-2Matm-1 , K2=4.44x107M-1 , k2f=5.93x103M-1s-1 , k2r=1.34x10-4s-1 , K3=4.66x103M-1 , k3f=1.00x108M-1s-1 , k2r=2.15x104s-1 .…”
Section: Methodsmentioning
confidence: 99%
“…CO 2A was calculated from an assumed mole fraction of CO 2 in the atmosphere (CO 2X ) and relating it to a CO 2 concentration in the water by using Henry's law: normalCnormalO2normalA=KH×0.25emnormalCnormalO2normalX0.25em×0.25emPnormalAnormalTnormalM0.25em=KH×pnormalCnormalO2 where CO 2A is the equilibrium CO 2 concentration (µmol L −1 ); K H is the temperature‐dependent Henry's constant (L atm mol −1 ) [ Butler , ]; CO 2X is the partial pressure of CO 2 in the atmosphere, assumed to be 390 ppmv; and P ATM is the atmospheric pressure, in atmospheres, calculated from either observed barometric pressure or from the reported elevation of the monitoring location. ΔCO 2 was then calculated as normalΔnormalCnormalO2=0.25emnormalCnormalO2normalW0.25emnormalCnormalO2normalA. …”
Section: Methodsmentioning
confidence: 99%
“…Aerobic metabolism couples the production and consumption of O 2 and CO 2 such that the molar departures of the gases from atmospheric equilibrium, ΔO 2 and ΔCO 2 , respectively, are expected to have predictable behavior. However, in water with relatively high pH (~8.0 or higher), the hydrated form of CO 2 , H 2 CO 3 , can ionize to H + + HCO 3 − [ Butler , ], and so ΔCO 2 and −ΔO 2 will be neither equivalent nor related by a fixed stoichiometry. In high‐pH/high‐alkalinity waters, some of the CO 2 added or removed through reactions such as primary production and aerobic respiration will exist in the ionized form.…”
Section: Introductionmentioning
confidence: 99%