“…Numerous laboratory experiments demonstrated that the dissolution of carbonates (calcite and magnesite) is controlled by pH, concentration of HCO 3 À /CO 3 2À ions, and temperature. Despite a number of studies on calcite dissolution in the presence of organic ligands (Perry et al, 2004(Perry et al, , 2005Fredd and Fogler, 1998a,b;Wu and Grant, 2002;Frye and Thomas, 1993;Hoch et al, 2000;Thomas et al, 1993;Compton and Sanders, 1993;Compton and Brown, 1995;Spanos et al, 2006a,b), rarely the effect of variable ligand concentration on the dissolution rate has been rigorously quantified. There are a few data on magnesite dissolution in the presence of ligands at some technologically relevant solution conditions (Hamdona et al, 1995;Demir et al, 2003;Laçin et al, 2005;Bayrak et al, 2006) and Jordan et al (2007) studied ligandcontrolled magnesite dissolution at 100 8C and low pCO 2 in the presence of a single concentration (0.01 M) of organic and inorganic ligands via a combination of macroscopic rate measurements and hydrothermal AFM.…”