Boaz Chung Yi Heng’s research while affiliated with University of Nottingham and other places

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Publications (1)


Figure 3. Bjerrum plots and the corresponding saturation states at different pH values for (a) rainwater, (b) limestone quarry water, (c) seawater, and (d) reverse osmosis concentrate
Figure 4. Effect of partial pressure of CO2 on (a) saturation state (Ωcal) and (b) pH.
Figure 6. Bjerrum plots for AWL effluents of increasing DIC concentrations
Figure 7. The effect of diluting an AWL reactor effluent with seawater on (a) pH, and (b) Ωcal without degassing (solid line) and equilibrating with ambient air pCO2 of 415 μatm prior to dilution (dotted lines)
Analyses of the water sources studied
A preliminary study of calcite saturation states with varying pH and salinity
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January 2024

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Boaz Chung Yi Heng

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Dominic Foo

The present work explores accelerated weathering of limestone (AWL) as an option to combat the climate change problem posed by the still growing carbon footprint. AWL is a promising low-technology solution that sequesters CO2 through the dissolution of calcium carbonate (CaCO3) in water to form calcium bicarbonate. One aspect of the feasibility of its application is whether the newly formed bicarbonate will remain in solution for the long term. This paper examines the carbonate equilibria for various water bodies by combining Bjerrum plots with the calcite saturation value, omega. The hydrochemistry software, aqion, was used to simulate a range of water compositions with different salinities at various conditions. The study compares saturation states of rainwater, limestone quarry water, seawater, and reverse osmosis concentrate, with their respective dissolved inorganic carbon (DIC) concentrations, across the full range of pH values. The areas of stability and instability can be observed from the generated plots in order to be able to design effective AWL processes. A key issue for successful implementation of AWL is operating within the CaCO3 saturation limit and ensuring dissolved material does not subsequently reprecipitate.

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Citations (1)


... It is important to note here that a pH of 8 is sufficiently alkaline to shift the CO2-HCO3 − -CO3 2− equilibrium towards HCO3 − . This can be illustrated using Bjerrum diagrams for seawater [42][43][44]. All of the dissolved CO2 gas is therefore converted to HCO3 − and CO3 2− . ...

Reference:

Water Separation and Formation of Cells with Differential Aeration as Factors Controlling Corrosion of Steel Pipelines in a Crude Oil Storage Facility
A preliminary study of calcite saturation states with varying pH and salinity