The dissolution of Mg-Al hydrotalcites in aqueous solution and its mechanism were investigated
with the dissolution kinetics and thermodynamics at different temperatures and pH. The kinetic model with the outer diffusion and chemical reaction control can be used to describe the dissolution process appropriately
with different controlling steps in various pH ranges. In the pH range from 1.0 to 3.8
the hydrotalcites dissolve completely and the dissolution rate decreases as pH increases
with the dissolution controlled by desorption. In the pH range from 4.2 to 9.4
the hydrotalcites partly dissolve
independent of pH
with the dissolution controlled by surface exchange reaction. On the other hand
the Gibbs free energy change of the dissolution reaction from the Mg-Al hydrotalcite is estimated as 29.516 kJ·mol-1 at 298 K. The result is consistent with the experimental evidence.
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Related Author
YANG Yong
SUN Weizhen
ZHAO Ling
YANG Yong
SUN Weizhen
WANG Miao
LIN Qiaoli
XU Pengguo
Related Institution
State Key Laboratory of Chemical Engineering and Low-carbon Technology, East China University of Science andTechnology
School of Materials Science and Engineering, Lanzhou University of Technology
School of Metallurgy and Energy Engineering, Kunming University of Science and Technology
National Engineering Research Center for Green Recycling of Strategic Metal Resources, CAS Key Laboratory of Green Process Process and Engineering, Institute of Process Engineering, Chinese Academy of Sciences
School of Chemical Engineering, University of Chinese Academy of Sciences