
Rev. Téc. Ing. Univ. Zulia. Vol. 42, No. 1, 2019, Enero-Abril, pp. 03-47
11Cu (II) Chemisorption on Calcined Substrates made with an Oxidic Refractory
Introduction
Transitional metal adsorption in variable charge
soils have been well studied by several authors [1, 2] but
has not been treated for the case of calcined substrates
prepared with oxidic refractory lithological materials. In
both cases the Fe and Al, as well as Mn and Ti amphoteric
oxides are the most important source of variable charge;
these amphoteric surfaces can be either protonated or
deprotonated by acid or alkaline treatment to create
positive or negative charges on the oxides surfaces, leading
to cation and anion adsorption reactions respectively,
according to equation (1) [3].
(1)
The literature also suggest a mechanism for
which the adsorption of transitional metals on these
kind of surfaces, through the formation of a covalent
bond between the metal ion and the oxidic surface, called
chemisorption, according to equation (2) where M could
be any transitional metal.
(2)
Such kind of reaction modifies the surface
charge through more positive values, which allows
anion adsorption, and produces acidification through the
formation of H3O+ ion. This process is defined as specific
adsorption or chemisorption, which has the tendency to
be irreversibility. In previous publications [4, 5] copper
adsorptions on calcined substrates prepared with some
of these refractory lithologic materials which have surface
variable charges were described. This physicochemical
characteristic is due to the presence of amphoteric oxides
in the material, such as Fe, Al, Mn and Ti, previously
described in the literature [6, 7]. As a consequence of these
particular properties, these lithological materials are
versatile for preparing calcined adsorbing substrates and
their applications in water treatment. Furthermore, due
to their capacity for anion/cation exchange, heavy metals,
oxyanions and organic matter are removed by adsorption
processes. In previous publications the application to
water softening [8], cation adsorption reactions [4], anion
adsorption reactions [9, 10] and water treatment [11]
have been described. The objective of this paper is to
complement the information presented by the previous
articles with new findings which support the hypothesis
of the chemisorption of cupper ions on the oxidic surface
of these calcined substrates, in order to continue working
on this project. Moreover, according to the theoretic
model described above, H3O+ ion must be one of the
reaction products, producing acidification in the solution.
Therefore, by following up the pH evolution during the
adsorption reaction it should show this acidification
process.
Experimental Section
lithologic material have been described in the literature
[7]. Being an arid zone, the soils are classified as aridisols
[12], presenting serious limitations for agronomical uses.
However, some of these lithological materials are used by
potters for making kitchen hardware and constructions
materials like bricks and crockery using thermal treatment
due to its refractory properties. Calcined subtrates were
prepare according to the procedure described in the
literature [4 - 6], so by using the granulometric fraction
between 425 – 250 mm for the determination of the
zero charge point, the pH and the electrical conductivity
the BET technique using isothermal N2 adsorption. The
procedure for the deprotonation reaction of the calcined
substrate (substrate activation) is also described in the
same literature were the substrate is chemically treated
excess of alkali is wash out with distillate water until
it reaches pH 7, and later it dries in a furnace at 120oC.
The determination of Point of Zero Charge (PZC) of raw
the material, (RM), calcined non-activated (NAS) and
activated substrates (AS) was performed according to
the method described by the literature [13, 14]. The pH
was measured at different ionic strength against pH in
aqueous extract and pH0 was recorded on a graphic of
pH against pHH2O which gives de pHo at the intersection
of pHH2O axe. The adsorption study was performed by
triplicate, in isothermal conditions at 20 ± 2 oC for 24 h,
using batch equilibration procedure by treating 2 g of
calcined substrate with 5, 10, 15, 20, 25, 30 and 40 mL of
0.001 M Cu+2, in closed vessels. Then the Cu+2 equilibrium
concentration were determined by the complexometric
titration at pH 10 with a 0.001 M EDTA standard solution
and NET as metalochromic indicator. Thus, adsorption
isotherms were obtained by plotting the amount of copper
adsorbed (mmol g-1 substrate) against the equilibrium
Langmuir equation [15-17]. The pH and the EC variations
were measured using the same batch equilibration
procedure, in triplicate samples, by treating 2 g of raw
material, activated and non-activated calcined substrate,
with increasing volume of 0.001 M, 0.01 M and 0.1 M of