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C - Lublin

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PRACTICAL REMARKS<br />

The titration curve of a soild, and especially of the soil, may include free<br />

acidic ions adsorbed on the surface (exchange acidity), which are not surface acidic<br />

groups. Therefore there exist a danger of interpretation of exchange acidity in<br />

terms of variable charge. To avoid the latter prior to the titration, the soil suspensions<br />

should be exchange acidity depleted. This can be done by standard neutral<br />

salt washing. We use fivefold centrifuging with excess of 1 mole dm -3 NaCl solution<br />

of pH=3 that provides the lack of Al (ICP AES) in the supernatants. The<br />

washed sample can be directly used for the titration, provided its mass is known.<br />

Next 1 mole dm -3 NaCl suspension containing around 1.00g (dry mass) of the<br />

sodium homoionic form of the solid is kept at pH≈2.9 by additions of small increments<br />

of 1 mole dm -3 HCl for half an hour of mixing. During additional 3 min.<br />

mixing the pH is controlled, and if changed by more than 0.02 unit, the suspension<br />

is centrifuged and the pretreatment repeated. From the final suspension, half of the<br />

supernatant (weighing) and the remaining suspension are titrated with 0.100 mole<br />

dm -3 NaOH in 1 mole dm -3 NaCl solution with the rate of 30 µl/min. The amount of<br />

the titer consumed between pH 3 to 9 is recorded with a step of 0.2 pH unit. The<br />

measurements are performed in four replicates. Usually the deviation of the titration<br />

curves is lower for the suspensions (around 5%) and higher for the supernatants<br />

(around 15%). If washing of the solid and the pretreatment for the titration<br />

are properly performed, the titration curves of the supernatants are similar to a titration<br />

curve of 1 mole dm -3 NaCl pH=3 solution, which indicates also that the dissolution<br />

of the solid phase under experimental conditions is negligible. This is important<br />

to note that in the above procedure the equilibrium conditions are not reached,<br />

so the titration curves can be used rather for comparative purposes. 24 hours equilibrium<br />

titration of a soil consumes up to twice as much titer as the continuous<br />

titration described here and a high dissolution of the solid phase occurs as is indicated<br />

by high deviation of the titration curves of the supernatants from the titration<br />

curve of NaCl solution (Jozefaciuk and Shin, 1996a).<br />

Applying constant and high concentration of neural salt during titration has a<br />

few advantages. It minimizes adsorption of exchange protons at low initial pH<br />

value and their further titration (replacing exchange protons by neutral salt cations),<br />

dilution effects (changes of variable charge with salt concentration), dissolution of<br />

solid phase, and allows for a better development of variable surface charge (surface<br />

groups dissociation is less hindered by electrostatic effects at high ionic strengths).<br />

Some results of the application of the back-titration method in analysis of<br />

various materials are presented in Józefaciuk (2002) for minerals, Józefaciuk and<br />

Szatanik-Kloc (2002) for plant roots, Jozefaciuk et. al. (2002) for soils.<br />

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