Copper(II) Carbonate Complexation in Seawater

Robert H. Byrne, William L. Miller

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Abstract

<p> <p id="x-x-SP0005"> Cupric carbonate and cupric bicarbonate complexation constants were determined in natural seawater and in a variety of synthetic media. The formation constants of CuHCO <sub> 3 </sub> <sup> + </sup> , CuCO <sub> 3 </sub> <sup> 0 </sup> and Cu(CO <sub> 3 </sub> ) <sub> 2 </sub> <sup> 2&minus; </sup> at 25&deg;C and zero ionic strength are: log <em> &beta; </em> <sub> <em> H </em> </sub> <sup> 0 </sup> = 1.8, log <em> &beta; </em> <sub> 1 </sub> <sup> 0 </sup> = 6.82 and log <em> &beta; </em> <sup> 0 </sup> <sub> 2 </sub> = 10.6. Formation constants of these species appropriate to 0.7 molar ionic strength and 25&deg;C are log <em> &beta; </em> <sub> <em> H </em> </sub> &sim;- 1, log <em> &beta; </em> <sub> 1 </sub> = 5.73, log <em> &beta; </em> <sub> 2 </sub> = 9.3. Our results indicate that the inorganic speciation scheme of Cu(II) in seawater is dominated by CuCO <sub> 3 </sub> <sup> 0 </sup> and that the ternary species, CuCO <sub> 3 </sub> OH <sup> &minus; </sup> , is of substantial importance. </p></p>
Original languageAmerican English
JournalGeochimica et Cosmochimica Acta
Volume49
DOIs
StatePublished - Jan 1 1985

Disciplines

  • Life Sciences

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