2. ENVIRONMENTAL ChEMISTRy & TEChNOLOGy 2.1. Lectures
2. ENVIRONMENTAL ChEMISTRy & TEChNOLOGy 2.1. Lectures
2. ENVIRONMENTAL ChEMISTRy & TEChNOLOGy 2.1. Lectures
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Chem. Listy, 102, s265–s1311 (2008) Environmental Chemistry & Technology<br />
P70 SELECTION OF PACKING MATERIALS FOR<br />
bIOFILTER DEVELOPMENT<br />
IVETA ŠTYRIAKOVá and ALEXAnDRA VAŠKOVá<br />
Institute of Geotechnics of the Slovac Academy of Sciences,<br />
Watsonova 45, 043 53 Košice, Slovakia,<br />
bacil@saske.sk<br />
Introduction<br />
natural materials that are available in large quantities<br />
may have potential as inexpensive sorbents. Cost effective<br />
alternative technologies or sorbents for treatment of metals<br />
contaminated waste streams are needed. A study 1 reported<br />
that zeolites, clinoptilolite in particular, demonstrate strong<br />
affinity for Pb and other heavy metals. Adsorbing Cd and<br />
Zn examined by both modifications with natural bentonite 2 .<br />
Results showed that the acid-treatment decreased the adsorption<br />
capacity, while the heat treatment did improve capacity.<br />
Retention of Pb and Zn on pure calcite was the subject of a<br />
number of investigations 3,4 . On the contrary, the number of<br />
sorption studies of both ions on magnesite is very limited.<br />
Investigations on the biosorption mechanism of heavy<br />
metals show that the metal ions are deposited by adsorption<br />
to the functional groups present on the cell wall. Dead as well<br />
as living cells are used in the removal of metal ions 5,6 . The<br />
batch adsorption experiments demonstrate that the surface<br />
complexation approach can be used successfully to quantify<br />
the adsorption of Cd in a mixed B. subtilis – quartz system as<br />
functions of both pH and solute/sorbent ratios 7 .<br />
We are interested in the surface complexation approach<br />
of zeolite, bentonite, calcite, magnezite and also these materials<br />
with bacteria in the behavior various heavy metals in the<br />
batch experiments. The objectives of this work were to determine<br />
the differences of mineral/water and mineral-bacteria/<br />
water interface in sorption capacities of metals.<br />
Experimental<br />
The biosorption experiments were carried out in Erlenmeyer<br />
flasks which contained 10 g samples and 100 ml<br />
medium. The medium contained (per liter) 0.5 g naH 2 PO 4 ,<br />
1.0 g (nH 4 ) 2 SO 4 , 0. g naCl, and 2 g glucose. The flasks were<br />
inoculated with a mixture of Bacillus cereus and B. megaterium<br />
(0.1 g wet bacteria dm –3 ) that had been previously isolated<br />
from Horná Prievrana. The two strains were purified by<br />
heat treatment at 80 °C for 15 min followed by streak plating<br />
on nutrient agar cultures. The isolates were identified with<br />
the BBL Crystal Identification System (Becton, Dickinson<br />
and Co., Franklin Lakes, nJ). For identification, the isolates<br />
were cultivated on Columbia agar plates per manufacturer’s<br />
instructions.<br />
The flasks were incubated under dynamic conditions<br />
(150 rev min –1 ) for 3 hours at 25 °C. The liquid phase was<br />
contained individual metals in 0.5mM concentration in the<br />
forms ZnSO 4 , CuSO 4 , PbCO 3 . The spent media (leachates)<br />
were sampled for metal analysis. The chemical controls<br />
s476<br />
did not receive an inoculum but were incubated under otherwise<br />
similar conditions.<br />
Solid residues were analyzed by X-ray diffraction using<br />
a Philips X’Pert SW–binary diffractometer with CuKα radia tion (40 kV, 50 mA), equipped with an automatic divergence<br />
slit, sample spinner, and a graphite secondary monochromator.<br />
Data were collected for 2–60 °2Θ with a step width of<br />
0.05 ° and a counting time of 30 s per 0.05 °. The mineralogy<br />
has been evaluated in quantitative terms from X-ray powder<br />
diffraction patterns using a Rietveld-based data processing<br />
technique.<br />
Quantitative changes in the liquid phase were measured<br />
with a Model 30 Varian atomic absorption spectrometer<br />
(Varian, Inc., Melbourne, Vic., Australia).<br />
Batch experiments were conducted to measure:<br />
• Zn, Cu, Pb and zeolite adsorption in a mixed singly<br />
metals – zeolite – Bacillus system<br />
• Zn, Cu, Pb and bentonite adsorption in a mixed singly<br />
metals – bentonite – Bacillus system second<br />
• Zn, Cu, Pb and quartz sands adsorption in a mixed singly<br />
metals – quartz sands – Bacillus system<br />
• Zn, Cu, Pb and calcite adsorption in a mixed singly<br />
metals – calcite – Bacillus system<br />
• Zn, Cu, Pb and magnezite adsorption in a mixed singly<br />
metals – magnezite – Bacillus system<br />
Z e o l i t e<br />
The natural materials, zeolite was obtained from nižný<br />
Hrabovec location in Slovakia. The mineralogical composition<br />
of zeolite was clinoptilolite 51–68 %, quartz + cristobalite<br />
9–20 %, feldspars 8–13 %, mica 13 % and iron minerals<br />
0.3 %.<br />
Table I<br />
Chemical composition of zeolite<br />
Components SiO 2 Al 2 O 3 Fe 2 O 3 MgO na 2 O<br />
% wt. 67.0 1<strong>2.</strong>3 1.3 0.7 0.7<br />
B e n t o n i t e<br />
The natural materials, zeolite was obtained from Lastovce<br />
location in Slovakia. The mineralogical composition<br />
of bentonite was smectite 63%, quartz 21%, kaolinite 11%,<br />
feldspars 4-6% and calcite 2%.<br />
Table II<br />
Chemical composition of bentonite<br />
Components SiO 2 Al 2 O 3 Fe 2 O 3 MgO na 2 O<br />
% wt. 59.2 18.6 <strong>2.</strong>8 4.2 0.7<br />
Q u a r t z S a n d s<br />
The natural materials, zeolite was obtained from nižný<br />
Hrabovec location in Slovakia. The mineralogical composi