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Electrolytic conductivity of preparations with Na-montmorillonite without<br />

aluminum is (8.9-36.3 mS), with aluminum (8.1-15.7 mS), of preparations with<br />

mica without aluminum (8.7-10.7 mS), with aluminum (8.8-39.4 mS), and of the<br />

preparations with kaolinite without aluminum (9.6-18 mS), with aluminum (9-26.7<br />

mS). An important influence of the pH value of the suspension was stated on the<br />

value of electrolytic conductivity. The greatest correlation was found in the<br />

organic-mineral preparations with kaolinite and with aluminum (r=0.93***) and in<br />

the preparations with mica without aluminum (r=0.75 *** ). It was proved that the<br />

greatest degree of reaction of the humic acids with Na-montmorillonite and with<br />

mica took place at pH 5, and with kaolinite at pH 7 (in the above mentioned<br />

combinations with aluminum). Aluminum clearly stimulated the increase in the<br />

degree of complexity of humic acids with minerals.<br />

Specific surface area is a very good parameter that characterizes the structure<br />

of the organic-mineral adsorbent. Specific surface area was determined using the<br />

initial part of the water vapour adsorption isotherm at 20°C within an adsorbate<br />

relative pressure range of 0,P/P 0 , 0.35 in accordance with the Brunauer, Emmet and<br />

Teller (BET) equation [Brunauer et al. 1938]. Water vapour adsorption were<br />

determined at 20°C gravimetrically (by weight), using a vacuum dryer in a<br />

temperature-controlled room according to Stawiński at al. (1999). The results of<br />

the specific surface area were statistically analyzed, including analysis of variance<br />

using the Statgraf software, and regression analysis using the Excel software. The<br />

calculated relations were then described with a linear equation, logarithm and<br />

power equation. The description of the relation analysis was made using the most<br />

fitted function.<br />

The variability of surface phenomena during the formation of synthetic<br />

organic-mineral bindings is proved by different values of the specific surface area.<br />

The specific surface area of the bindings with Na-montmorillonite without<br />

aluminum ranges between 87 and 150.4 m 2 /g; with aluminum 145.6 to 152.8 m 2 /g;<br />

for bindings with mica without aluminum 83.2 to 150.4 m 2 /g; with aluminum 145.6<br />

to 152.8 m 2 /g; for bindings with kaolinite without aluminum 14.1 to 43 m 2 /g; with<br />

aluminum 15.9 to 38.5 m 2 /g. A significant influence of the pH value of the<br />

suspension on the size of the specific surface area was stated. The highest<br />

correlation was observed in the bindings with kaolinite (r=0.93 ***). It was proven<br />

that the addition of aluminum to the bindings with Na-montmorillonite<br />

significantly influenced the growth of the specific surface area at pH 5, in bindings<br />

with mica-at pH 7, and in bindings with kaolinite- at pH 3 and 4. At pH 3 there was<br />

a significant decrease in that value and there was an increase at pH 4. The greatest<br />

degree of reaction was stated in bindings with Na-montmorillonite (without Al) at<br />

pH 5 , with mica (without Al) at pH 7, and with kaolinite at pH 5,6 and 7.<br />

95

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