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66<br />

RADIOCHEMISTRY, STABLE ISOTOPES,<br />

NUCLEAR ANALYTICAL METHODS, GENERAL CHEMISTRY<br />

of chemical and physical interactions between the<br />

heavy metals present in solution and functional<br />

groups of the biosorbent: carboxylic, phosphate,<br />

sulfate, ammino, amidic or hydroxylic [10-12].<br />

Divalent cation binding by calcium alginates was<br />

investigated using a number of techniques. Potentiometric<br />

titration revealed that CA exhibits two<br />

distinct pK a<br />

values: (i) similar to that characteristic<br />

of carboxylic groups, and (ii) comparable to that<br />

of saturated alcohols. Esterification of the biosorbent<br />

species resulted in a significant reduction in<br />

metal sorption (up to 10 times), indicating that<br />

mainly carboxylic groups are responsible for the<br />

sorption. Also the ion-selective electrode (ISE)<br />

studies suggest that sorption of cadmium is mainly<br />

due to an ion exchange mechanism [13]. X-ray photoelectron<br />

spectroscopy (XPS) and the infrared<br />

(FTIR) results indicated that both alcoholic (-OH)<br />

and carboxylic (-COO – ) functional groups present<br />

in the carbohydrate moieties play an important role<br />

in the metal removal from aqueous solutions [14].<br />

Because of the difficulties in direct X-ray investigations<br />

of the carbohydrate derivatives, FTIR<br />

absorption spectra of selected M(II)-alginate complexes<br />

and CA bed (Fig.1) were recorded as a continuation<br />

of our studies [15,16] on species formed<br />

by alginic biosorbent with different metal cations.<br />

Vibrational spectroscopy is the most widely used<br />

technique for studying natural products, being fast,<br />

non-destructive, and demanding small sample<br />

amounts. So, the aim of the presented work was to<br />

continue our studies on transition metal complexes<br />

with biosorbents on the alginate origin.<br />

Main vibrational modes: IR spectra of the investigated<br />

species, especially in the fingerprint region,<br />

are rather complex and reflect the complex nature<br />

of the biomass. Analysis of the main features of the<br />

spectra shows that:<br />

- In the fingerprint spectral window all spectra<br />

exhibit the absorbance bands at approximately<br />

1605, 1420, 1085, 1030, 890 and 820 cm –1 . Proposed<br />

assignment of the bands forming the fingerprint<br />

spectral window has been revised since<br />

publication of the previous paper [16] and is presented<br />

in Table 1.<br />

- The difference between the spectra of CA and<br />

M(II)-alginate is mainly in their absorbance intensities.<br />

While the band intensities of the metal-<br />

-loaded CA in the region of the symmetric carboxylate<br />

stretching mode (1450-1300 cm –1 ) are<br />

significantly higher than that of CA, in the asymmetric<br />

carboxylate stretching modes (about 1610<br />

cm –1 ) a slight decrease in the intensity can be<br />

observed for the transition metal cations upon<br />

the exchange of the calcium cation. The absorbance<br />

bands in pure alginic acid are 1740 and<br />

1240 cm –1 .<br />

- The distance between the ν sym and ν asym absorbance<br />

bands for CA is significantly smaller than<br />

those for M(II)-alginate. It can be related to<br />

the higher symmetry in CA in respect to other<br />

M(II)-alginates, which occurred due to complexation<br />

with metal cation.<br />

- The ν asym (COO) band of the M(II)-alginates are<br />

narrower and sharper than that in the CA spec-<br />

trum. It could be linked with orthodox coordination<br />

spheres, wherein both oxygen-M(II)<br />

bonds have a very similar strength.<br />

- Lack of displacement of the bands related to<br />

vibrations associated with the C-O (both alcoholic<br />

and ether groups) at 1085 and 1030 cm –1 is<br />

observed when calcium cation is replaced by another<br />

divalent cation. Such displacement could<br />

result from different coordination strengths of<br />

the metal and calcium cations to both alcoholic<br />

or ether groups.<br />

- Broad absorption peaks in the region of 3250-3500<br />

cm –1 indicate the existence of hydroxyl groups<br />

involved in H-bond network. The peak observed<br />

at 2930 cm –1 can be assigned as vibration of the<br />

CH group [17,18].<br />

Table 2. Dependence of the ν(COO) sym and ν(COO) asym<br />

peak positions for the Mn(II)-CA on the equilibrium<br />

pH.<br />

The dependence of the main peaks positions<br />

on the equilibrium pH has been analyzed for all<br />

the cations studied. The results are as follows:<br />

- ν(COO) sym<br />

and ν(COO) asym<br />

: Table 2 and Fig.2<br />

present the data obtained for the Mn(II)-alginate.<br />

The complexation mode does not change<br />

within the whole pH range studied [19]. All other<br />

cations behave similarly – neither position nor<br />

shape of both main peaks describing the complexation<br />

mode depends on the solution acidity.<br />

So, the results obtained for other cations are<br />

not shown neither in Table 2, nor in Fig.2.<br />

Fig.2. Spectra of the CA loaded with manganese(II) of<br />

different pH.<br />

- The significant decrease in the intensity of the<br />

3429 cm –1 peak may be explained in terms of<br />

decreasing number of H-bonds, caused by the<br />

dissociation of the hydroxyl groups present in<br />

the uronic moieties.<br />

Because the carboxylate group in the alginate<br />

resin plays an important role in binding metal ions,<br />

the percentage of ionic bonding (PIB) was introduced<br />

to characterize qualitatively the cation-anion<br />

bond formed by the biosorbents [14]:

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