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total flux [mol.m –2 ]<br />

0.7<br />

0.65<br />

0.6<br />

0.55<br />

0.5<br />

0.45<br />

0.4<br />

0 1 2 3 4 5<br />

pH<br />

total flux [mol.m –2 ]<br />

0.4<br />

0 1 2 3 4 5 6<br />

F<strong>in</strong>ally the total diffusion flux showed complex dependency on the ionic strength <strong>of</strong><br />

copper(II) solution. For small NaCl additions, the decrease <strong>of</strong> total flux comes with the<br />

<strong>in</strong>crease <strong>of</strong> ionic strength, on the contrary substantial <strong>in</strong>crease appeares <strong>in</strong> higher NaCl<br />

concentration range. Former decrease can be caused by decrease <strong>of</strong> HA sorption ability,<br />

competitive diffusion <strong>of</strong> Na + ions or by affect<strong>in</strong>g Cu 2+ solvation. The later <strong>in</strong>crease is not very<br />

clear. It can be supposed that <strong>in</strong> the solution with high ionic strength bigger Cu 2+ clusters are<br />

solvated and easily took out from the solution.<br />

CONCLUSIONS<br />

This paper deals with the study <strong>of</strong> copper(II) ions non–stationary diffusion <strong>in</strong> humic gel.<br />

Ma<strong>in</strong> aim was to determ<strong>in</strong>ate the <strong>in</strong>fluence <strong>of</strong> <strong>in</strong>dividual copper(II) solution properties on the<br />

total diffusion flux across the solution–gel <strong>in</strong>terface.<br />

It was proved that copper(II) ions diffusion across the phase <strong>in</strong>terface is affected ma<strong>in</strong>ly by<br />

the <strong>in</strong>itial concentration <strong>of</strong> copper <strong>in</strong> the solution and by the time duration <strong>of</strong> the diffusion.<br />

The <strong>in</strong>fluence <strong>of</strong> other solution properties, such as its pH or ionic strength as well as the type<br />

<strong>of</strong> copper(II) salt anion is far less important however show <strong>in</strong>terest<strong>in</strong>g dependencies.<br />

Although the applied apparatus was very simple and could be improved for follow<strong>in</strong>g<br />

experiments (the higher solution volumes should be used) experimental data are fitted well by<br />

the theoretical calculations, so it can be said that this method presented itself suitable for the<br />

wide spectrum <strong>of</strong> diffusion experiments us<strong>in</strong>g humic gel as a very usefull natural–like model.<br />

REFERENCES<br />

[1] Klučáková, M.: Hum<strong>in</strong>ový gel jako model pro studium transportu těžkých kovů<br />

v přírodních systémech. CHEMagazín 2004, Vol. 14, No. 3, p. 8–9. ISSN 1210–7409<br />

[2] Klučáková, M., Kaláb, M., Pekař, M., Lapčík, L.: Study <strong>of</strong> Structure and properties <strong>of</strong><br />

Humic and Fulvic Acids. II. Study <strong>of</strong> Adsorption <strong>of</strong> Cu + ions to Humic Acids Extracted<br />

from Lignite, J.Polym.Mater 19 (3) 2002<br />

[3] Malenovská, M.: Studium difúzních procesů v hum<strong>in</strong>ových gelech. 55 stran. Diplomová<br />

práce na VUT, FCH Brno 2005. Vedoucí diplomové práce Ing. Mart<strong>in</strong>a Klučáková<br />

PhD.<br />

[4] Sedláček, P..: Difúze kovových iontů v hum<strong>in</strong>ových gelech. 70 stran. Diplomová práce<br />

na VUT, FCH Brno 2006. Vedoucí diplomové práce Doc. Ing. Mart<strong>in</strong>a Klučáková PhD.<br />

[5] Klučáková, M., Pekař, M.: Diffusion <strong>of</strong> Metal Cations <strong>in</strong> Humic Gels. In Humic<br />

Substances: Nature´s most Versatile Materials (E. Ghabbour, G. Davies Eds.), Francis<br />

& Taylor, New York, 2004, p. 263–74<br />

0.7<br />

0.65<br />

0.6<br />

0.55<br />

0.5<br />

0.45<br />

ionic strength [mol.dm –3 ]<br />

Fig. 8 Total diffusion flux dependency on solution pH (left) and ionic strength (right)<br />

Sborník soutěže Studentské tvůrčí č<strong>in</strong>nosti Student 2006 a doktorské soutěže O cenu děkana 2005 a 2006<br />

Sekce DSP 2006, strana 227

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