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    Research and Science Today No. 2(4)/2012

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    THE KINETICS OF CALCITE DISSOLUTION PRECIPITATION

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    The channel-flow cell method is used to establish the dissolution/precipitation kinetics of calcite under wide ranges of bulk Ca1+ concentration (0-10 mM) and solution flow rate (10-30.3 cm3 s-1) for different bulk pH values. Detailed mathematical modeling of the heterogeneous reaction, and accompanying solution processes leads to the following rate equation based on a model in which Ca2+ and CO2- 3 undergo Langmuirian adsorption on the calcite surface: Dnet/mol cm-2s-1 = kbKCaKCO3 { KSP - [Ca2+]o[CO2- 3]O (1 + KCo[Ca2+]o(1 + KCO3 [CO3]o)} Here Dnet is the net flux of dissolving calcium ions, kb is a rate constant, Ksp, is the solubility product of calcite corrected for the ionic strength of the solution, KA (A = Ca2+ or CO2- 3) are Langmuirian adsorption constants, and [ ]o denotes the concentration at the Outer Helmholtz Plane. © 1993 Academic Press. All rights reserved

    Unsteady aerodynamic characteristics of a dual-element airfoil

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