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  4. Inhibition of calcite precipitation by natural organic material: Kinetics, mechanism, and thermodynamics
 
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Inhibition of calcite precipitation by natural organic material: Kinetics, mechanism, and thermodynamics

Journal
Environmental Science and Technology
Journal Volume
39
Journal Issue
17
Pages
6420-6428
Date Issued
2005
Author(s)
Lin, Y.-P.
Singer, P.C.
Aiken, G.R.
YI-PIN LIN  
DOI
10.1021/es050470z
URI
https://scholars.lib.ntu.edu.tw/handle/123456789/463050
URL
https://www.scopus.com/inward/record.uri?eid=2-s2.0-24644483584&doi=10.1021%2fes050470z&partnerID=40&md5=3b2c7b6674059ac8a42be689d5d1eeb1
Abstract
The inhibition of calcite precipitation by natural organic material (NOM) in solutions seeded with calcite was investigated using a pH-stat system. Experiments were carried out using three NOMs with different physical/chemical properties. For each of the materials, inhibition was found to be more effective at lower carbonate/calcium ratios and lower pH values. The reduction in the precipitation rate could be explained by a Langmuir adsorption model using a conditional equilibrium constant. By identification of the type of site on the NOM molecules that is involved in the adsorption reaction, the "conditional" equilibrium constants obtained at different solution compositions converged to a single "nonconditional" value. The thermodynamic data determined at 25°C and 1 atm suggest that the interaction between NOM molecules and the calcite surface is chemisorptive in nature and that adsorption is an endothermic reaction driven by the entropy change. The greatest degree of inhibition was observed for the NOM with the highest molecular weight and aromatic carbon content. For a given type of NOM, the degree of inhibition of calcite precipitation was dictated by the balance between the enthalpy change and the entropy change of the adsorption reaction. © 2005 American Chemical Society.
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[SDGs]SDG6

Type
journal article

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