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Kouli_etal_2008_Groundwater modelling_BOOK.pdf - Pantelis ...

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In: <strong>Groundwater</strong>: Modelling, Management… ISBN: 978-1-60456-832-5<br />

Editors: L.F. Konig and J.L. Weiss, pp. 133-147 © <strong>2008</strong> Nova Science Publishers, Inc.<br />

Chapter 4<br />

MODELLING OF WATER-SOLID INTERACTIONS:<br />

A DISCUSSION OF DIFFERENT APPROACHES<br />

Marek Šváb 1 and Lenka Wimmerová 2<br />

1 Institute of Chemical Technology in Prague, Technická 5, Prague 6, 166 28, Czech Rep.<br />

2 Dekonta, a.s., Dřetovice 109, Stehelčeves, 273 42, Czech Rep.<br />

Abstract<br />

This contribution contains an explanation and discussion of two different approaches to<br />

the <strong>modelling</strong> of water-solid interactions. The term ‘water-solid interaction’ means all<br />

interactions that are important in the frame of remediation methods, groundwater treatment<br />

and pollution migration, including adsorption, leaching of contaminants, minerals<br />

weathering, etc.<br />

The discussed approaches involve an exact <strong>modelling</strong> of interactions based on chemical<br />

reactions as well as what is known as the ‘semi-empirical’ approach, which is applicable for<br />

very complex systems. On one hand, the exact approach is very promising for a detailed<br />

understanding of particular processes and can be specified by a possible transfer of results<br />

among various systems. On the other hand, the semi-empirical approach can also be a simple<br />

alternative for <strong>modelling</strong> very complex systems.<br />

The calculation of the equilibrium solubility of zinc and copper in water under various<br />

conditions (with and without ammonia as a complexation agent), including detailed speciation<br />

of both m<strong>etal</strong>s complexes, is an example of the exact <strong>modelling</strong>. The influence of ammonia<br />

nitrogen on the solubility of both m<strong>etal</strong>s is obvious: a local solubility maximum occurs at the<br />

pH of 9.4. The results have been confirmed by equilibrium batch experiments with zinc and<br />

copper hydroxides that have proven the local solubility maximum at the pH of 9.4.<br />

The exact <strong>modelling</strong> is further demonstrated by the adsorption of an organic contaminant<br />

from water on three adsorbents in a mixture demonstrating the distribution of the contaminant<br />

between various adsorbents. Although these isotherms are not exact descriptions of particular<br />

sorption reactions, the method of calculation demonstrates the principles of use of the exact<br />

geochemical <strong>modelling</strong> for calculations of competitive sorption on different adsorbents.<br />

As an example of the semi-empirical approach, a mathematical model aimed at predicting<br />

the course of a continuous soil flushing process by use of the input data obtained from simple<br />

batch laboratory experiments is described. An objective of the example is to apply this new<br />

model to soil polluted by zinc and copper (11 949 mg/Kg -1 and 1 895 mg/Kg -1 , respectively)<br />

by flushing this soil with an ammonia nitrogen solution with the pH of 9.4. The model<br />

predicts correctly the period of time needed for the removal of weakly-bound m<strong>etal</strong> fractions,

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