C - Lublin
C - Lublin
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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