2003
DOI: 10.1016/s0883-2927(03)00013-1
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Decarbonation of geothermal waters by seeding with aragonite crystals coupled with air bubbling

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Cited by 10 publications
(5 citation statements)
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“…The supersaturation coefficient ( Ω ) decrease with the nucleation time allows suggesting the occurrence of an heterogeneous CaCO 3 nucleation. Indeed, it was shown that the metastability of the calcocarbonic system CaCO 3 ‐CO 2 ‐H 2 O can be immediately broken, for more lower supersaturation coefficients, after adding seed particles of calcite, SiO 2 or other inert materials as the PVC. In our experimental conditions, the dependence of CaCO 3 precipitation kinetics on ferric content allows suggesting that iron (III) precipitate plays this role of seed.…”
Section: Resultsmentioning
confidence: 99%
“…The supersaturation coefficient ( Ω ) decrease with the nucleation time allows suggesting the occurrence of an heterogeneous CaCO 3 nucleation. Indeed, it was shown that the metastability of the calcocarbonic system CaCO 3 ‐CO 2 ‐H 2 O can be immediately broken, for more lower supersaturation coefficients, after adding seed particles of calcite, SiO 2 or other inert materials as the PVC. In our experimental conditions, the dependence of CaCO 3 precipitation kinetics on ferric content allows suggesting that iron (III) precipitate plays this role of seed.…”
Section: Resultsmentioning
confidence: 99%
“…This is evident in Figure 6B, where, at flowrates greater than 5 L min -1 , there is no significant increase in the rate at which calcium is removed. The rate of CaCO3 formation could be increased by increasing the operating temperature, which would decrease the 𝐾𝐾 𝑠𝑠𝑠𝑠,𝐶𝐶𝑎𝑎𝐶𝐶𝐶𝐶 3 (Stumm and Morgan, 2012) or by adding seeds, which would increase the 𝑘𝑘 𝐶𝐶𝑎𝑎𝐶𝐶𝐶𝐶 3 (El Fil and Manzola, 2003;Song et al, 2006). The results ultimately show that it is important to have a rate of CO3 2formation greater than the precipitation rate of CaCO3, but the CO2 dissolution rate should be small enough to allow for substantial calcium removal before the buffer capacity of the solution is depleted.…”
Section: Understanding the Processes Involvedmentioning
confidence: 99%
“…The scaling power of real geothermal water, where an extensive scaling takes place in the cooling towers, was also assessed. 33 The geothermal water reaches the surface having a temperature and a pH of about 65°C and 6.8, respectively. Its Ca hardness is around 10 mM with HCO 3 Ϫ concentration of about 2 mM and an ionic strength close to 0.07.…”
Section: Evaluation Of the Novel Saturation Index For Some Experimentmentioning
confidence: 99%