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Chemistry and Materials Research                                                               www.iiste.org
ISSN 2224- 3224 (Print) ISSN 2225- 0956 (Online)
Vol 1, No.2, 2011


Application of Appopolite in Adsorption of Heavy Metals (Co and
                    Ni) from Waste Water
                                 Rohini Singh1*,Kavita Kulkarni2, A.D.Kulkarni2


         1. M.Tech Student, Department of Chemical Engineering, BVDU, Pune, India
         2. Associate Professor, BVDU College of Engineering, Pune, India
              Bharati Vidyapeeth Deemed University, College of Engineering, Pune, 411043, India
         * E-mail- richarohini@yahoo.co.in
         E-mail- kskulkarni@bvucoep.edu.in



Abstract
The optimum conditions for adsorption/ion exchange by using a batch method were evaluated by changing
various parameters such as adsorbent amount, initial pH of the solution, mixing temperature and initial metal
ions. The influence of the temperature on the ion-exchange/adsorption process was also examined. The
Langmuir and Freundlich adsorption isotherm equations were derived from the basic empirical equations, and
used for calculation of ion exchange parameters. Adsorption isotherms of Co2+ & Ni2+ ions could be best
modelled by the Langmuir equation. The influences of contact time, metal initial concentration, adsorbent
dosage concentration, and temperature have been studied. The adsorption efficiencies are found to be contact
time dependent, increasing the contact time in the range of 20–180 min. The sorption equilibrium has attained
between 60 and 180 min.
Keywords - Adsorption, Freundlich adsorption isotherm, ion exchange, Langmuir equation, sorption
equilibrium


1. Introduction
There are different types of heavy metals which if present in excess quantities in groundwater, river water,
lakes, canals, dams and other water bodies leads to serious health disorders and various diseases like irritation of
the nose, mouth and eyes and it causes headaches, stomachaches, dizziness, vomiting and diarrhoea.The major
sources of heavy metals in the environment include Metal Extraction, Metal Fabrication and Surface Finishing,
Paint and Pigments as well as the manufacturing of batteries.


2. Zeolites
The term zeolite was originally coined in the 18th century by a Swedish mineralogist named Cronstedt who
observed, upon rapidly heating a natural zeolite that the stones began to dance about as the water evaporated.
Using the Greek words which mean "stone that boils," he called this material zeolite. A commonly used
description of a zeolite is a crystalline aluminosilicate with a cage structure. Technically, we speak of a zeolite
as a crystalline hydrated aluminosilicate whose framework structure encloses cavities (or pores) occupied by
cations and water molecules, both of which have considerable freedom of movement, permitting ion exchange
and reversible dehydration. This definition places it in the class of materials known as "molecular sieves." [The
pores in dehydrated zeolite are 6 Ångstroms in size, while those of a typical silica gel average about 50 Å, and
activated carbon averages 105 Å.] More than 150 zeolite types have been synthesized and 40 naturally occurring
zeolites are known. [The formula of one of the better known zeolites is shown below.] ... Zeolites occur as
hydrates, and all members of the family contain at least one silicon atom per aluminum atom.


Na-A Na2O · Al2O3 · 2SiO2 · 4.5 H2O




                                                        16
Chemistry and Materials Research                                                               www.iiste.org
ISSN 2224- 3224 (Print) ISSN 2225- 0956 (Online)
Vol 1, No.2, 2011

2.1 Natural and Synthetic Formation of Zeolites
Zeolites form in nature as a result of the chemical reaction between volcanic glass and saline water.
Temperatures favoring the natural reaction range from 27°C to 55°C and the pH are typically between 9 and 10.
Nature requires 50 to 50,000 years to complete the reaction. Naturally occurring zeolites are rarely phase-pure
and are contaminated to varying degrees by other minerals [e.g. Fe++, SO4-, quartz, other zeolites, and
amorphous glass]. For this reason, naturally occurring zeolites are excluded from many important commercial
applications where uniformity and purity are essential. Synthetic zeolites hold some key advantages over their
natural analogs. The synthetics can, of course, be manufactured in a uniform, phase-pure state. It is also possible
to manufacture desirable zeolite structures which do not appear in nature. Zeolite A is a well-known example.
Since the principal raw materials used to manufacture zeolites are silica and alumina, which are among the most
abundant mineral components on earth, the potential to supply zeolites is virtually unlimited. Finally, zeolite
manufacturing processes engineered by man require significantly less time than the 50 to 50,000 years
prescribed by nature. Zeolites are microporous crystalline hydrated aluminosilicates that can be considered as
inorganic polymers built from an infinitely extending three-dimensional network (similar to a honeycomb) of
tetrahedral TO4 units, where T is Si or Al, which form interconnected tunnels and cages. Zeolites have been
widely used in heavy metals adsorption experiments due to their unique physical and chemical properties
(crystallinity, thermal stability, well-defined cage structure of molecular size, ion-exchange, etc.). The
advantage of zeolites over resins, apart from their much lower cost (one ton of the natural zeolite clinoptilolite
costs almost €200), is their ion selectivity. Owing to zeolites structural characteristics and their adsorbent
properties, they have been applied as chemical sieves, water softeners and adsorbents. Zeolites can be easily
regenerated by washing them with acidic solutions (e.g. HCl) and this is one more advantage of them because
they      can     be    re-used     many      times    without      losing     their    adsorption       capability.

2.2 Properties of zeolites
2.2.1. Ion exchange
                                            +   +         +
Zeolites usually contain cations (e.g., Na , K , or NH4 ) after the synthesis. These cations are required to
balance the negative net-charge caused by trivalent aluminum cations which are coordinated tetrahedrally by
oxygen anions. By exposing a sodium containing zeolite to a solution containing other cations, the sodium ions
can be exchanged by these other cations provided they are not excluded from the pores due to their size
(including the water molecules coordinating the respective cations).
2.2.2.MolecularSieveEffect/Adsorption
The pore sizes of zeolites are determined by their structures and may be varied slightly by ion-exchanging the
zeolite. By this process smaller cations can be positioned in windows making them wider. Specific cations may
also be positioned on other sites than in the windows, thus leading to even larger open windows. The window
sizes determine the accessibility of the zeolite pore system for other (e.g. organic) molecules.
2.2.3.Acidity
As already mentioned protonated zeolites have acidic properties. The protons which balance the negative charge
of a zeolite framework are not strongly bound to the framework and are able to move within the pores and react
with molecules which penetrate into the zeolite pore system. A protonated zeolite thus can act as a Bronsted
acid. Furthermore, Lewis acidity can be caused by cations within the pores.
2.2.4.Catalysis
Zeolites make extremely active catalysts.... Steric phenomena are very important in zeolite catalysis, and a new
term, "shape selective catalysis," was coined to describe these effects. Extremely selective reactions can be
made to occur over zeolites [when certain products, reactants or transition states are kept from forming within
the pores because of size or shape].


3. Adsorption isotherm
The two isotherms to consider are the Freundlich and Langmuir.
3.1 Langmuir isotherm: The Langmuir sorption isotherm is the best known of all isotherms describing sorption
and it has been successfully applied to many sorption processes. Thus, the Langmuir isotherm model is given by
the equation.



                                                        17
Chemistry and Materials Research                                                              www.iiste.org
ISSN 2224- 3224 (Print) ISSN 2225- 0956 (Online)
Vol 1, No.2, 2011

Ce/qe = 1/(Qmax.KL) + Ce/ Qmax ………………. (1)


Where,
qe = metal concentration on zeolite at equilibrium. (mg of metal ion/g of zeolite)


Qmax and KL are the Langmuir constants related to sorption capacity and sorption energy, respectively. The
values of Qmax (mg/g) and KL(mg–1) can be determined from the linear plot of Ce/qe vs. Ce.


For all cases, the Langmuir model represents a better fit to the experimental data than the
Freundlich model.


Assumptions:
1 .Maximum monolayer coverage (θ=1)
2 .Energetically uniform surface.
3.No interaction between adsorbate atoms/molecules.
4 .The mechanism of adsorption does not change with surface coverage.


ra = Kp(1- θ)
rd = kI θ
At equilibrium,
                  ra= rd
                  θ = Κp/ ( k + Κp)
                               I


                    = Kp/ (1 + Kp)
                    = v / vm


Where, v= volume
           vm= corrected volume
           θ = surface coverage
         (1 - θ) = vacant sites

3.2. Freundlich isotherm:
The Freundlich isotherm, one of the most widely used mathematical descriptions, usually fits the experimental
data over a wide range of concentrations. This isotherm is based on adsorption heterogeneous surfaces, the
exponential distribution of active sites and their energies and adsorption enthalpy changes logarithmically.
This relation is given by:
ln qe= ln KF + (1/n).ln Ce……………………(2)

where,
qe = the amount of metal ions adsorbed per gram of adsorbent at equilibrium (mg/g),
Ce is the equilibrium concentration in mg/l,
KF = roughly an indicator of the adsorption capacity (mg/g)
1/n = a characteristic constant for the adsorption system (g/L).
KF and n can be determined from the graph between ln qe vs ln Ce.


                                                        18
Chemistry and Materials Research                                                              www.iiste.org
ISSN 2224- 3224 (Print) ISSN 2225- 0956 (Online)
Vol 1, No.2, 2011

KF = slope and n = intercept.


4. Conclusion
In the present study, appopolite, natural zeolite has been successfully used for removal of Co and Ni ions from
the aqueous model solution. The maximum adsorption of Co has been found at the dosage 5g/l.
In between cobalt and nickel cobalt exhibited a higher percentage removal. In addition to this:
1. Adsorption of lead, cobalt, and nickel onto appopolite (natural zeolite) has an ion-exchange nature. Three
different stages are observed in the ion exchange adsorption of the metals. The process begins with fast
adsorption on the appopolite micro crystal surface during the first 20 minutes. Nearly 80% of Copper and 75%
of nickel adsorbed during the first stage on the micro crystals surface.
2. The ion exchange of metals is directly proportional to pH value of aqueous solutions. Adsorbtion decreases in
the more acidic medium.
3. The slight difference between adsorption capacity of the appopolite towards Copper and Cadmium from
single and multicomponent solutions may testify to individual sorption centres of the zeolite for each of these
metals.
4. Efficiency of metals removal from solutions by appopolite is inversely proportional to the metal
concentration. The metals from the following order for adsorption efficiency: Pb2+ > Cu2+ > Cd2+ >CO> Ni2+.
5. The data obtained from the studies are applied well to the Langmuir isotherm in comparison to the Freundlich
isotherm.


References
Hiraoki katusuki et.al, “Rapid synthesis of Monodispersed α- Fe2O3 Nanoparticles from Fe(NO3)3 solution by
microwave irradiation”,Journel of the ceramics society of Japan ,112[7]384-387(2004)

J.Salado et.al, “Synthesis and magnetic properties of monodispersed Fe2O3 nanoparticles with controlled
sizes”,Journal of Non-crystalline solids ,354(2008),5207-5209

Brianna R White et.al, “Magnetic ɤ - Fe2O3 nanoparticles coated with poly-L-cysteine for chelation of As(III),
Cu(II), Cd(II), Ni(II), Pb(II), and Zn(II)”,Journal of hazardous materials,161(2009),848-853

Soamwadee chaianansutcharit et.al, “Synthesis of Fe2O3 nanoparticles in different r,eaction media”Ceramics
International ,33(2007),697-699

Jie chen et.al, “Preparation of Fe3O4 nanoparticles with adjustable morphology”,Journal of alloys and
compounds,(2008) ,Article in press.

I.G.Parsons et.al., “Determination of arsenic(III) and arsenic(V) binding to microwave assisted hydrothermal
synthetically prepared Fe3O4,Mn3O4 and MnFe2O4 nanoadsorbents”,Microchemical Journal, 91(2009),100-
106.

Zhong Jie Zhang et.al, “Hydrothermal synthesis and self assembly of magnetite(Fe3O4) nanoparticles with the
magnetic and electrochemical properties”, Journal of crystal growth 310(2008),5453-5457.
Pratap Chutia et.al, “Adsorption of As(V) on surfactant modified natural zeolites”Journal of Hazardous
materials,162(2009),204-211

Yu-Ting Zhou et.al, “Removal of Cu2+ from aquous solution by chitosan-coated magnetic nanoparticles
modified with -ketoglutaric acid”, Journal of colloid and interface science, 330(2009),29-37.

Panagiota Stathi et.al, “Physicochemical study of novel organoclays as heavy metal ion adsorbents for
environmental remediation”,Journal of colloid and interface science, 316(2007),298-309




                                                       19
Chemistry and Materials Research                                               www.iiste.org
ISSN 2224- 3224 (Print) ISSN 2225- 0956 (Online)
Vol 1, No.2, 2011

Comparison &interpretation of adsorption isotherms



Table 1: Isotherm data for Nickel(Ni):

 CO(ppm)     Ce(ppm)     qe= co-   Ln ce         Ln qe        Ce/ qe
                         ce                                             time

       100       69.23     30.77   4.23743429    3.42654019   2.24992     20

       100       48.42     51.58   3.87991295      3.943134   0.93874     60

       100       48.14     51.86   3.87411343    3.94854778   0.92827    120

       100        47.8      52.2   3.86702564    3.95508249   0.91571    180

       300         120       180   4.78749174    5.19295685   0.66667     20

       300       100.8     199.2   4.61313836    5.29430935   0.50602     60

       300       89.25    210.75   4.49144142     5.3506726   0.42349    120

       300        85.4     214.6     4.4473461   5.36877583   0.39795    180

       500       194.7     305.3   5.27145991     5.7212949   0.63773     20

       500      166.89    333.11   5.11733491    5.80847277   0.50101     60

       500         173       327   5.15329159    5.78996017   0.52905    120

       500       150.2     349.8   5.01196774    5.85736156   0.42939    180




                                                    20
Chemistry and Materials Research                                                  www.iiste.org
ISSN 2224- 3224 (Print) ISSN 2225- 0956 (Online)
Vol 1, No.2, 2011




Table 2: Isotherm data for Cobalt(Co):




 CO(ppm)     Ce(ppm)     qe= co-    Ln ce        Ln qe        Ce/ qe
                         ce                                                time

 100         31.06       68.94      3.43592082   4.23323656   0.4505367    20

 100         28.056      71.944     3.33420251   4.27588804   0.38996998   60

 100         27.763      72.237     3.3237042    4.27995238   0.38433213   120

 100         25.17       74.83      3.22565281   4.31521887   0.33636242   180

 300         55.357      244.643    4.01380312   5.49980001   0.22627666   20

 300         52.49       247.51     3.96062268   5.51145099   0.21207224   60

 300         48.49       251.51     3.88135759   5.52748275   0.19279552   120

 300         45.23       254.77     3.81176058   5.54036118   0.17753268   180

 500         94.81       405.19     4.55187489   6.00435609   0.23398899   20

 500         89.63       410.37     4.49569009   6.01705919   0.21841265   60

 500         82.21       417.79     4.40927695   6.03497891   0.1967735    120

 500         81.85       418.15     4.4048883    6.03584022   0.19574315   180




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11.application of appopolite in adsorption of heavy metals (co and ni) from waste water

  • 1. Chemistry and Materials Research www.iiste.org ISSN 2224- 3224 (Print) ISSN 2225- 0956 (Online) Vol 1, No.2, 2011 Application of Appopolite in Adsorption of Heavy Metals (Co and Ni) from Waste Water Rohini Singh1*,Kavita Kulkarni2, A.D.Kulkarni2 1. M.Tech Student, Department of Chemical Engineering, BVDU, Pune, India 2. Associate Professor, BVDU College of Engineering, Pune, India Bharati Vidyapeeth Deemed University, College of Engineering, Pune, 411043, India * E-mail- richarohini@yahoo.co.in E-mail- kskulkarni@bvucoep.edu.in Abstract The optimum conditions for adsorption/ion exchange by using a batch method were evaluated by changing various parameters such as adsorbent amount, initial pH of the solution, mixing temperature and initial metal ions. The influence of the temperature on the ion-exchange/adsorption process was also examined. The Langmuir and Freundlich adsorption isotherm equations were derived from the basic empirical equations, and used for calculation of ion exchange parameters. Adsorption isotherms of Co2+ & Ni2+ ions could be best modelled by the Langmuir equation. The influences of contact time, metal initial concentration, adsorbent dosage concentration, and temperature have been studied. The adsorption efficiencies are found to be contact time dependent, increasing the contact time in the range of 20–180 min. The sorption equilibrium has attained between 60 and 180 min. Keywords - Adsorption, Freundlich adsorption isotherm, ion exchange, Langmuir equation, sorption equilibrium 1. Introduction There are different types of heavy metals which if present in excess quantities in groundwater, river water, lakes, canals, dams and other water bodies leads to serious health disorders and various diseases like irritation of the nose, mouth and eyes and it causes headaches, stomachaches, dizziness, vomiting and diarrhoea.The major sources of heavy metals in the environment include Metal Extraction, Metal Fabrication and Surface Finishing, Paint and Pigments as well as the manufacturing of batteries. 2. Zeolites The term zeolite was originally coined in the 18th century by a Swedish mineralogist named Cronstedt who observed, upon rapidly heating a natural zeolite that the stones began to dance about as the water evaporated. Using the Greek words which mean "stone that boils," he called this material zeolite. A commonly used description of a zeolite is a crystalline aluminosilicate with a cage structure. Technically, we speak of a zeolite as a crystalline hydrated aluminosilicate whose framework structure encloses cavities (or pores) occupied by cations and water molecules, both of which have considerable freedom of movement, permitting ion exchange and reversible dehydration. This definition places it in the class of materials known as "molecular sieves." [The pores in dehydrated zeolite are 6 Ångstroms in size, while those of a typical silica gel average about 50 Å, and activated carbon averages 105 Å.] More than 150 zeolite types have been synthesized and 40 naturally occurring zeolites are known. [The formula of one of the better known zeolites is shown below.] ... Zeolites occur as hydrates, and all members of the family contain at least one silicon atom per aluminum atom. Na-A Na2O · Al2O3 · 2SiO2 · 4.5 H2O 16
  • 2. Chemistry and Materials Research www.iiste.org ISSN 2224- 3224 (Print) ISSN 2225- 0956 (Online) Vol 1, No.2, 2011 2.1 Natural and Synthetic Formation of Zeolites Zeolites form in nature as a result of the chemical reaction between volcanic glass and saline water. Temperatures favoring the natural reaction range from 27°C to 55°C and the pH are typically between 9 and 10. Nature requires 50 to 50,000 years to complete the reaction. Naturally occurring zeolites are rarely phase-pure and are contaminated to varying degrees by other minerals [e.g. Fe++, SO4-, quartz, other zeolites, and amorphous glass]. For this reason, naturally occurring zeolites are excluded from many important commercial applications where uniformity and purity are essential. Synthetic zeolites hold some key advantages over their natural analogs. The synthetics can, of course, be manufactured in a uniform, phase-pure state. It is also possible to manufacture desirable zeolite structures which do not appear in nature. Zeolite A is a well-known example. Since the principal raw materials used to manufacture zeolites are silica and alumina, which are among the most abundant mineral components on earth, the potential to supply zeolites is virtually unlimited. Finally, zeolite manufacturing processes engineered by man require significantly less time than the 50 to 50,000 years prescribed by nature. Zeolites are microporous crystalline hydrated aluminosilicates that can be considered as inorganic polymers built from an infinitely extending three-dimensional network (similar to a honeycomb) of tetrahedral TO4 units, where T is Si or Al, which form interconnected tunnels and cages. Zeolites have been widely used in heavy metals adsorption experiments due to their unique physical and chemical properties (crystallinity, thermal stability, well-defined cage structure of molecular size, ion-exchange, etc.). The advantage of zeolites over resins, apart from their much lower cost (one ton of the natural zeolite clinoptilolite costs almost €200), is their ion selectivity. Owing to zeolites structural characteristics and their adsorbent properties, they have been applied as chemical sieves, water softeners and adsorbents. Zeolites can be easily regenerated by washing them with acidic solutions (e.g. HCl) and this is one more advantage of them because they can be re-used many times without losing their adsorption capability. 2.2 Properties of zeolites 2.2.1. Ion exchange + + + Zeolites usually contain cations (e.g., Na , K , or NH4 ) after the synthesis. These cations are required to balance the negative net-charge caused by trivalent aluminum cations which are coordinated tetrahedrally by oxygen anions. By exposing a sodium containing zeolite to a solution containing other cations, the sodium ions can be exchanged by these other cations provided they are not excluded from the pores due to their size (including the water molecules coordinating the respective cations). 2.2.2.MolecularSieveEffect/Adsorption The pore sizes of zeolites are determined by their structures and may be varied slightly by ion-exchanging the zeolite. By this process smaller cations can be positioned in windows making them wider. Specific cations may also be positioned on other sites than in the windows, thus leading to even larger open windows. The window sizes determine the accessibility of the zeolite pore system for other (e.g. organic) molecules. 2.2.3.Acidity As already mentioned protonated zeolites have acidic properties. The protons which balance the negative charge of a zeolite framework are not strongly bound to the framework and are able to move within the pores and react with molecules which penetrate into the zeolite pore system. A protonated zeolite thus can act as a Bronsted acid. Furthermore, Lewis acidity can be caused by cations within the pores. 2.2.4.Catalysis Zeolites make extremely active catalysts.... Steric phenomena are very important in zeolite catalysis, and a new term, "shape selective catalysis," was coined to describe these effects. Extremely selective reactions can be made to occur over zeolites [when certain products, reactants or transition states are kept from forming within the pores because of size or shape]. 3. Adsorption isotherm The two isotherms to consider are the Freundlich and Langmuir. 3.1 Langmuir isotherm: The Langmuir sorption isotherm is the best known of all isotherms describing sorption and it has been successfully applied to many sorption processes. Thus, the Langmuir isotherm model is given by the equation. 17
  • 3. Chemistry and Materials Research www.iiste.org ISSN 2224- 3224 (Print) ISSN 2225- 0956 (Online) Vol 1, No.2, 2011 Ce/qe = 1/(Qmax.KL) + Ce/ Qmax ………………. (1) Where, qe = metal concentration on zeolite at equilibrium. (mg of metal ion/g of zeolite) Qmax and KL are the Langmuir constants related to sorption capacity and sorption energy, respectively. The values of Qmax (mg/g) and KL(mg–1) can be determined from the linear plot of Ce/qe vs. Ce. For all cases, the Langmuir model represents a better fit to the experimental data than the Freundlich model. Assumptions: 1 .Maximum monolayer coverage (θ=1) 2 .Energetically uniform surface. 3.No interaction between adsorbate atoms/molecules. 4 .The mechanism of adsorption does not change with surface coverage. ra = Kp(1- θ) rd = kI θ At equilibrium, ra= rd θ = Κp/ ( k + Κp) I = Kp/ (1 + Kp) = v / vm Where, v= volume vm= corrected volume θ = surface coverage (1 - θ) = vacant sites 3.2. Freundlich isotherm: The Freundlich isotherm, one of the most widely used mathematical descriptions, usually fits the experimental data over a wide range of concentrations. This isotherm is based on adsorption heterogeneous surfaces, the exponential distribution of active sites and their energies and adsorption enthalpy changes logarithmically. This relation is given by: ln qe= ln KF + (1/n).ln Ce……………………(2) where, qe = the amount of metal ions adsorbed per gram of adsorbent at equilibrium (mg/g), Ce is the equilibrium concentration in mg/l, KF = roughly an indicator of the adsorption capacity (mg/g) 1/n = a characteristic constant for the adsorption system (g/L). KF and n can be determined from the graph between ln qe vs ln Ce. 18
  • 4. Chemistry and Materials Research www.iiste.org ISSN 2224- 3224 (Print) ISSN 2225- 0956 (Online) Vol 1, No.2, 2011 KF = slope and n = intercept. 4. Conclusion In the present study, appopolite, natural zeolite has been successfully used for removal of Co and Ni ions from the aqueous model solution. The maximum adsorption of Co has been found at the dosage 5g/l. In between cobalt and nickel cobalt exhibited a higher percentage removal. In addition to this: 1. Adsorption of lead, cobalt, and nickel onto appopolite (natural zeolite) has an ion-exchange nature. Three different stages are observed in the ion exchange adsorption of the metals. The process begins with fast adsorption on the appopolite micro crystal surface during the first 20 minutes. Nearly 80% of Copper and 75% of nickel adsorbed during the first stage on the micro crystals surface. 2. The ion exchange of metals is directly proportional to pH value of aqueous solutions. Adsorbtion decreases in the more acidic medium. 3. The slight difference between adsorption capacity of the appopolite towards Copper and Cadmium from single and multicomponent solutions may testify to individual sorption centres of the zeolite for each of these metals. 4. Efficiency of metals removal from solutions by appopolite is inversely proportional to the metal concentration. The metals from the following order for adsorption efficiency: Pb2+ > Cu2+ > Cd2+ >CO> Ni2+. 5. The data obtained from the studies are applied well to the Langmuir isotherm in comparison to the Freundlich isotherm. References Hiraoki katusuki et.al, “Rapid synthesis of Monodispersed α- Fe2O3 Nanoparticles from Fe(NO3)3 solution by microwave irradiation”,Journel of the ceramics society of Japan ,112[7]384-387(2004) J.Salado et.al, “Synthesis and magnetic properties of monodispersed Fe2O3 nanoparticles with controlled sizes”,Journal of Non-crystalline solids ,354(2008),5207-5209 Brianna R White et.al, “Magnetic ɤ - Fe2O3 nanoparticles coated with poly-L-cysteine for chelation of As(III), Cu(II), Cd(II), Ni(II), Pb(II), and Zn(II)”,Journal of hazardous materials,161(2009),848-853 Soamwadee chaianansutcharit et.al, “Synthesis of Fe2O3 nanoparticles in different r,eaction media”Ceramics International ,33(2007),697-699 Jie chen et.al, “Preparation of Fe3O4 nanoparticles with adjustable morphology”,Journal of alloys and compounds,(2008) ,Article in press. I.G.Parsons et.al., “Determination of arsenic(III) and arsenic(V) binding to microwave assisted hydrothermal synthetically prepared Fe3O4,Mn3O4 and MnFe2O4 nanoadsorbents”,Microchemical Journal, 91(2009),100- 106. Zhong Jie Zhang et.al, “Hydrothermal synthesis and self assembly of magnetite(Fe3O4) nanoparticles with the magnetic and electrochemical properties”, Journal of crystal growth 310(2008),5453-5457. Pratap Chutia et.al, “Adsorption of As(V) on surfactant modified natural zeolites”Journal of Hazardous materials,162(2009),204-211 Yu-Ting Zhou et.al, “Removal of Cu2+ from aquous solution by chitosan-coated magnetic nanoparticles modified with -ketoglutaric acid”, Journal of colloid and interface science, 330(2009),29-37. Panagiota Stathi et.al, “Physicochemical study of novel organoclays as heavy metal ion adsorbents for environmental remediation”,Journal of colloid and interface science, 316(2007),298-309 19
  • 5. Chemistry and Materials Research www.iiste.org ISSN 2224- 3224 (Print) ISSN 2225- 0956 (Online) Vol 1, No.2, 2011 Comparison &interpretation of adsorption isotherms Table 1: Isotherm data for Nickel(Ni): CO(ppm) Ce(ppm) qe= co- Ln ce Ln qe Ce/ qe ce time 100 69.23 30.77 4.23743429 3.42654019 2.24992 20 100 48.42 51.58 3.87991295 3.943134 0.93874 60 100 48.14 51.86 3.87411343 3.94854778 0.92827 120 100 47.8 52.2 3.86702564 3.95508249 0.91571 180 300 120 180 4.78749174 5.19295685 0.66667 20 300 100.8 199.2 4.61313836 5.29430935 0.50602 60 300 89.25 210.75 4.49144142 5.3506726 0.42349 120 300 85.4 214.6 4.4473461 5.36877583 0.39795 180 500 194.7 305.3 5.27145991 5.7212949 0.63773 20 500 166.89 333.11 5.11733491 5.80847277 0.50101 60 500 173 327 5.15329159 5.78996017 0.52905 120 500 150.2 349.8 5.01196774 5.85736156 0.42939 180 20
  • 6. Chemistry and Materials Research www.iiste.org ISSN 2224- 3224 (Print) ISSN 2225- 0956 (Online) Vol 1, No.2, 2011 Table 2: Isotherm data for Cobalt(Co): CO(ppm) Ce(ppm) qe= co- Ln ce Ln qe Ce/ qe ce time 100 31.06 68.94 3.43592082 4.23323656 0.4505367 20 100 28.056 71.944 3.33420251 4.27588804 0.38996998 60 100 27.763 72.237 3.3237042 4.27995238 0.38433213 120 100 25.17 74.83 3.22565281 4.31521887 0.33636242 180 300 55.357 244.643 4.01380312 5.49980001 0.22627666 20 300 52.49 247.51 3.96062268 5.51145099 0.21207224 60 300 48.49 251.51 3.88135759 5.52748275 0.19279552 120 300 45.23 254.77 3.81176058 5.54036118 0.17753268 180 500 94.81 405.19 4.55187489 6.00435609 0.23398899 20 500 89.63 410.37 4.49569009 6.01705919 0.21841265 60 500 82.21 417.79 4.40927695 6.03497891 0.1967735 120 500 81.85 418.15 4.4048883 6.03584022 0.19574315 180 21
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