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Calcite precipitation from aqueous solutions with different calcium and hydrogen carbonate concentrations.
| Content Provider | Semantic Scholar |
|---|---|
| Author | Zeppenfeld, Kai |
| Copyright Year | 2010 |
| Abstract | This paper describes the influence of different Ca 2 + and HCO 3 − concentrations on the precipitation of calcite in aqueous solutions. Mixtures of CaCl 2 and NaHCO 3 solutions with different concentrations were stirred, covering a wide range of supersaturation and precipitation of calcite. The resulting reduction of the Ca 2 + concentration was recorded as a function of time by measuring the electric conductivity and the pH value. The nucleation rate increased with increasing supersaturation and can be described with the classical theory of nucleation. For different solutions with similar values of supersaturation, the hydrogen carbonate/calcium ratio had no significant influence on the rate of nucleation. At a given calcium concentration the precipitation rate increased with increasing supersaturation. This effect was more pronounced at higher supersaturations. Measurements at similar values of supersaturation showed that the calcite precipitation rate increased with increasing hydrogen carbonate/calcium ratio. These results can be explained by applying a surface complexation model. The crystal surface concentrations of the two species > CaCO 3 − and > CO 3 − and the adsorption of CaCO 3 0 ion pairs are responsible for catalysing calcite precipitation. |
| Starting Page | 482 |
| Ending Page | 491 |
| Page Count | 10 |
| File Format | PDF HTM / HTML |
| DOI | 10.2166/aqua.2010.076 |
| Volume Number | 59 |
| Alternate Webpage(s) | https://watermark.silverchair.com/482.pdf?token=AQECAHi208BE49Ooan9kkhW_Ercy7Dm3ZL_9Cf3qfKAc485ysgAAAhAwggIMBgkqhkiG9w0BBwagggH9MIIB-QIBADCCAfIGCSqGSIb3DQEHATAeBglghkgBZQMEAS4wEQQMy5XG3Gt7_p1QqSNmAgEQgIIBw1TBM918DBsFVxxDzrAd55FVcS1lJXl-iKocYEnJq9ATRq0b8NtUumrHXvz4iNZHs7e6czBG1_I2M8_fTfPek5a0QORyKu2kBF27F6Brc7jNYa2XZDjIU-RnkwLRoh2hLds4vPUW4oF5Jt7hUKu4GC0thmyMOnkzgrSGC2F83lpOD0coj01DI7NWOLuA2Jacit_aVw5p6eKzBzhlvSMwSJTGG7Nx1rlCp1RTgW4R8hAK6shMZEdP9aBA3UORLPivRbX6h8s3Z5pwOmlIpGTUk4xRk6mMIgTB6ywqrxwLKv1RKjAeNZCsC84pVJ0xPVMugx97KUF8g5VXbdImKCiPlKzN_BvdgKvdDROQZ36RqgxNVa5G6G84GeEn3qZVaNXfh2S5ipUk_2b_nwKjsUo3pjFXDsX2Xw9RUarAccAAbaArkDgGNBAnJK7KwxfzQYG5cPlFm5wkSrguTPOVNc4_JJrlLVYH6bXk_6yjxVk4bZ_zjH6uumy7rAAPMnUbFmWTw_cuA0GuzleFirjwu57aKVIA6bFl6U_FtZ57aYRU3fOlMtEYraolRr0a0MfuVy9JKi95YuNBwwrKIlyBpoeBocoAQ0U |
| Alternate Webpage(s) | https://doi.org/10.2166/aqua.2010.076 |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |
