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Review of second-order models for adsorption systems

Yuh-Shan Ho

School of Public Health, Taipei Medical University, 250 Wu-Hsing Street, Taipei 11014, Taiwan

Received 24 November 2004; received in revised form 2 April 2005; accepted 29 December 2005 Available online 7 February 2006

Abstract

Applications of second-order kinetic models to adsorption systems were reviewed. An overview of second-order kinetic expressions is described

in this paper based on the solid adsorption capacity. An early empirical second-order equation was applied in the adsorption of gases onto a solid.

A similar second-order equation was applied to describe ion exchange reactions. In recent years, a pseudo-second-order rate expression has been

widely applied to the adsorption of pollutants from aqueous solutions onto adsorbents. In addition, the earliest rate equation based on the solid

adsorption capacity is also presented in detail.

© 2006 Elsevier B.V. All rights reserved.

Keywords: Kinetics; Second-order; Pseudo-second-order; Biosorption; Sorption

1. Introduction

Predicting the rate at which adsorption takes place for a

given system is probably the most important factor in adsorption

system design, with adsorbate residence time and the

reac-tor dimensions controlled by the system’s kinetics. A number

of adsorption processes for pollutants have been studied in an

attempt to find a suitable explanation for the mechanisms and

kinetics for sorting out environment solutions. In order to

inves-tigate the mechanisms of adsorption, various kinetic models

have been suggested. In recent years, adsorption mechanisms

involving kinetics-based models have been reported. Numerous

kinetic models have described the reaction order of adsorption

systems based on solution concentration. These include

first-order

[1]

and second-order

[2]

reversible ones, and first-order

[3]

and second-order

[4]

irreversible ones, pseudo-first-order

[5]

and pseudo-second-order ones

[6]

based on the solution

concentration. On the other hand, reaction orders based on the

capacity of the adsorbent have also been presented, such as

Lagergren’s first-order equation

[7]

, Zeldowitsch’s model

[8]

,

and Ho’s second-order expression

[9–12]

.

This paper describes an earlier adsorption rate equation based

on the solid capacity for a system of liquids and solids

[7]

, the

Elovich equation for adsorption of gases onto a solid and

apply-∗Tel.: +886 2 2736 1661x6514; fax: +886 2 2738 4831.

E-mail address: [email protected].

ing a second-order rate equation for gas/solid and solution/solid

adsorption systems

[8]

, a second-order rate expression for ion

exchange reactions

[13]

, and a pseudo-second-order expression

[9]

.

2. Modeling

2.1. Second-order rate equation

A linear form of the typical second-order rate equation is

1

C

t

= k

2

t +

1

C

0

,

(1)

where C

t

is the equilibrium concentration (mg/dm

3

), C

0

the

ini-tial concentration (mg/dm

3

), t the time (min), and k

2

is the rate

constant (dm

3

/mg min).

Early applied second-order rate equations in solid/liquid

sys-tems described reactions between soil and soil minerals

[14,15]

.

Others applied which the second-order rate equation included

the adsorption of fluoride onto acid-treated spent bleaching earth

[16]

; and the adsorption of water using the dealumination of

HZSM-5 zeolite by thermal treatment

[17]

. Moreover,

Varsh-ney et al. reported the kinetics of adsorption of the pesticide,

phosphamidon, on beads of an antimony(V) phosphate cation

exchanger during the first 15 min

[18]

.

0304-3894/$ – see front matter © 2006 Elsevier B.V. All rights reserved. doi:10.1016/j.jhazmat.2005.12.043

(2)

2.2. Lagergren’s equation

As early as 1898

[7]

, Lagergren described liquid–solid phase

adsorption systems, which consisted of the adsorption of oxalic

acid and malonic acid onto charcoal. Lagergren’s first-order rate

equation is the earliest known one describing the adsorption rate

based on the adsorption capacity. It is summarised as follows:

d

x

d

t

= k(X − x),

(2)

where X and x (mg/g) are the adsorption capacities at equilibrium

and at time t (min), respectively, and k is the rate constant of the

first-order adsorption (1/min).

Eq.

(2)

was integrated with the boundary conditions of t = 0

to t = t and x = 0 to x = x to yield

ln



X

X − x



= kt

(3)

and

x = X(1 − e

−kt

)

.

(4)

Eq.

(3)

may be rearranged to a linear form:

log(

X − x) = log(X) −

k

2

.303

t.

(5)

In order to distinguish kinetics equations based on

concentra-tions of solution from adsorption capacities of solids,

Lager-gren’s first-order rate equation has been called pseudo-first-order

[10,19–22]

. An early known application of Lagergren’s kinetics

equation to adsorption was undertaken by Trivedi et al.

[23]

for

the adsorption of cellulose triacetate from chloroform onto

cal-cium silicate. During the last four decades, the kinetics equation

has been widely applied to the adsorption of pollutants from

aqueous solutions

[24]

.

2.3. Elovich’s equation

Elovich’s equation is another rate equation based on the

adsorption capacity. In 1934

[8]

, the kinetic law of

chemisorp-tion was established though the work of Zeldowitsch. The rate of

adsorption of carbon monoxide on manganese dioxide

decreas-ing exponentially with an increase in the amount of gas adsorbed

was described by Zeldowitsch

[8]

. It has commonly been called

the Elovich equation in the following years:

d

q

d

t

= a e

−αq

,

(6)

where q is the quantity of gas adsorbed during the time t,

α the

initial adsorption rate, and a is the desorption constant during any

one experiment. The integrated form of Eq.

(6)

can be written

in the form

q =



2

.3

α



log(

t + t

0

)



2

.3

α



log

t

0

(7)

with

t

0

=

1

αa

.

(8)

With a correctly chosen t

0

, the plot of q as a function of log(t + t

0

)

should yield a straight line with a slope of 2.3/

α; Eq.

(8)

then

gives a which obviously represents the initial rate of adsorption

for q = 0. The test thus involves one single disposable parameter,

t

0

, which is found by trial; if t

0

is too small, the curve is

con-vex, and if t

0

is too large, it is concave to the axis of log(t + t

0

)

[25]

. This Elovich equation is commonly used to determine the

kinetics of chemisorption of gases onto heterogeneous solids,

and is quite restricted, as it only describes a limiting property

ultimately reached by the kinetic curve

[26]

.

To simplify Elovich’s equation, Chien and Clayton

[27]

assumed that a

αt  1 and by applying the boundary conditions

of q = 0 at t = 0 and q = q at t = t, then Eq.

(6)

becomes

[28]

:

q = α ln(aα) + α ln(t).

(9)

Thus, the constants can be obtained from the slope and the

inter-cept of a straight line plot of q against ln(t). Recently, Rudzinski

and Panczyk

[29]

published an exhaustive analysis of existing

rationalizations for the Elovich equation found in the literature

for the kinetics of adsorption onto heterogeneous surfaces.

In earlier years, numerous applications of Elovich’s

equa-tion to the adsorpequa-tion of gases onto solid systems were reported

[30,31]

. During the last three decades, the equation has been

widely used to describe the kinetics of adsorption of gases

onto solids

[29,32–35]

. The most frequently cited paper for the

application of Elovich’s equation to adsorption systems was an

alternative to Elovich’s equation for kinetics of adsorption of

gases onto solids

[33]

. An earlier application of the rate

equa-tion of Elovich was the exchange of

32

P between the goethite

(␣-FeOOH) crystal surface and the solution phase

[36]

. The

application of Elovich equation to the kinetics of phosphate

release and adsorption in soils

[27]

is the most frequently cited

paper on the adsorption in solution/solid systems. In addition, the

Elovich equation has also been used to describe the adsorption

of pollutants from aqueous solutions in recent years

[19,37,38]

.

2.4. Ritchie’s equation

In 1977

[33]

, Ritchie reported a model for the adsorption of

gaseous systems. Assumptions were made as follows:

θ is the

fraction of surface sites which are occupied by an adsorbed gas,

n the number of surface sites occupied by each molecule of the

adsorbed gas, and

α is the rate constant. Assuming that the rate

of adsorption depends solely on the fraction of sites which are

unoccupied at time t, then

d

θ

d

t

= α(1 − θ)

n

.

(10)

Eq.

(10)

integrates to

1

(1

− θ)

n−1

= (n − 1)αt + 1 for n = 1

(11)

or

θ = 1 − e

−αt

for

n = 1.

(12)

(3)

It is assumed that no site is occupied at t = 0. When introducing

the amount of adsorption, q, at time t, Eq.

(11)

becomes

q

n−1

(

q

− q)

n−1

= (n − 1)αt + 1

(13)

and similarly Eq.

(12)

becomes

q = q

(1

− e

−αt

)

,

(14)

where q

is the amount of adsorption after an infinite time.

In earlier years, Sobkowsk and Czerwi´nski

[39]

presented a

rate equation for the reaction of carbon dioxide adsorption onto

a platinum electrode:

d

θ

d

t

= k(1 − θ)

n

,

(15)

where

θ = Γ /Γ

denotes the surface coverage by the reaction

products,

Γ and Γ

the surface concentrations at time t and after

completion of the reaction, respectively, k the rate constant, and

n is the order of the reaction.

When n = 1,

−ln(1 − θ) = k

1

t.

(16)

When n = 2,

θ

1

− θ

= k

2

t.

(17)

Sobkowsk and Czerwi´nski

[39]

concluded that the first-order

is only for low surface concentrations of a solid, confirmed by

using plots of

−ln(1 − θ) versus time as Eq.

(16)

, and the

second-order is for higher concentrations of a solid, confirmed by using

plots of

θ/(1 − θ) versus time as Eq.

(17)

. In addition, Trasatti and

Formaro reported that the plot of

−ln(1 − θ) versus time is not

linear for very long times, when the coverage reaches a

station-ary value for the adsorption of glycolaldehyde onto a platinum

electrode

[40]

. In the case of the sorption of basic dyes from

aqueous solution onto sphagnum moss peat, Ho and McKay

[22]

found that log(q

e

− qt) versus time was only applicable in

the early stage of the reaction. In the case of adsorption of gases

onto a solid surface, Sobkowsk and Czerwi´nski reported that

the first-order rate equation could only be used for a low surface

concentration of gases adsorbed onto a solid surface, and the

second-order rate evaluation could be applied to higher

concen-trations

[39]

.

Several adsorption results were examined using the Ritchie

equation

[33]

. In the early years, the Elovich equation was

applied to describe gas and vapour adsorption systems, such

as the adsorption of carbon monoxide during the oxidation

of polyvinylidene chloride

[41]

, the chemisorption of

hydro-gen onto graphon

[42]

, the measuring of the kinetics of the

chemisorption of H

2

onto a MoS

2

+ Al

2

O

3

catalyst

[43]

, and the

adsorption of water vapour by Vycor fibre

[44]

. These systems

did not fit the Elovich equation very well. Ritchie

[33]

examined

these results using Eq.

(13)

when n = 2. Eq.

(13)

becomes

q

(

q

− q)

= αt + 1.

(18)

The value for q

is obtained from the intercept at (1/t) = 0 on

a plot of (1/q) against (1/t). Ritchie found a good linear

rela-tionship between t and q

/(q

− q) for the results of Austin et

al.

[41]

, Bansal et al.

[42]

, Deitz and Turner

[44]

, and Samuel

and Yeddanapalli

[43]

. In recent years, the Ritchie equation

has also been applied to solution/solid adsorption systems, for

example, the adsorption of cadmium ions onto bone char

[37]

,

and the adsorption of Cd(II) onto acid-treated jackfruit peel

[45]

.

2.5. Second-order rate expressions

In 1984

[13]

, Blanchard et al. presented the overall exchange

reaction of NH

4+

ions fixed in zeolite by divalent metallic ions

in the solution which can be written:

Z

(2NH4+)

+ M

2+

→ Z

(M2+)

+ 2NH

4+

,

(19)

where Z

(2NH4+)

and Z

(M2+)

are the amounts of NH

4+

ion fixed in

the zeolite (meq/g), and M

2+

and NH

4+

are the concentrations

(meq/dm

3

).

The authors assumed that the metallic concentration varies

very slightly during the first hours, and the kinetic order is two

with respect to the number (n

0

− n) of available sites for the

exchange; thus, the differential equation can be written as

d

n

d

t

= K[n

0

− n]

2

(20)

and integration gives

1

(

n

0

− n)

− α = Kt,

(21)

where n is the amount of M

2+

fixed or the amount of NH

4+

released at each instant, n

0

the exchange capacity, and K is the

rate constant.

Considering the boundary condition n = 0 for t = 0, it follows

that

α = 1/n

0

. By plotting 1/(n

0

− n) as a function of time, a

straight line must be obtained, the slope of which gives the rate

constant, K, and the intercept gives the exchange capacity. In

recent years, the Blanchard second-order expression has been

used to describe the kinetics of exchange processes between

sodium ions from zeolite A and cadmium, copper, and nickel

ions from solutions

[46]

.

An expression of second-order rate based on solid capacity

has also been presented for the kinetics of adsorption of

diva-lent metal ions onto peat

[9–12]

. Peat contains polar functional

groups such as aldehydes, ketones, acids, and phenolics. These

groups can be involved in chemical bonding and are

respon-sible for the cation exchange capacity of the peat. Thus, the

peat–copper reaction may be represented in two ways

[47]

:

2P

+ Cu

2+

↔ CuP

2

(22)

and

2HP

+ Cu

2+

↔ CuP

2

+ 2H

+

,

(23)

(4)

In an attempt to present the equation representing adsorption

of divalent metals onto sphagnum moss peat during agitation,

the assumption was made that the process may be second-order

and that chemisorption occurs involving valency forces through

sharing or the exchange of electrons between the peat and

diva-lent metal ions as covadiva-lent forces. The rate of the second-order

reaction may be dependent on the amount of divalent metal ions

on the surface of the peat, and the amount of divalent metal

ions adsorbed at equilibrium

[9,12]

. The rate expression for the

adsorption described by Eqs.

(24)

and

(25)

is

d(P)

t

d

t

= k[(P)

0

− (P)

t

]

2

(24)

or

d(HP)

t

d

t

= k[(HP)

0

− (HP)

t

]

2

,

(25)

where (P)t

and (HP)t

are the number of active sites occupied

on the peat at time, t, and (P)

0

and (HP)

0

are the number of

equilibrium sites available on the peat.

The driving force, (q

e

− qt), is proportional to the available

fraction of active sites. The kinetic rate equations can be

rewrit-ten as follows:

d

q

t

d

t

= k(q

e

− q

t

)

2

,

(26)

where k is the rate constant of adsorption (g/mg min), q

e

the

amount of divalent metal ions adsorbed at equilibrium (mg/g),

and qt

is the amount of divalent metal ions on the surface of the

adsorbent at any time, t (mg/g).

Separating the variables in Eq.

(26)

gives

d

q

t

(

q

e

− q

t

)

2

= k dt

(27)

and integrating this for the boundary conditions t = 0 to t = t and

q

t

= 0 to qt

= qt, gives

q

t

=

q

2 e

kt

1

+ q

e

kt

(28)

which is the integrated rate law for a second-order reaction. Eq.

(28)

can be rearranged to obtain

q

t

=

1

t

kq2 e

+

t qe

(29)

which has a linear form of

t

q

t

=

1

kq

2 e

+

1

q

e

t

(30)

and

h = kq

2 e

,

(31)

where h is the initial adsorption rate (mg/g min) as qt/t

approaches 0, and Eq.

(29)

can be rearranged to obtain

q

t

=

1

t

h

+

qte

(32)

and

t

q

t

=

1

h

+

1

q

e

t.

(33)

The rate of a reaction is defined as the change in concentration of

a reactant or product per unit time. Concentrations of products

do not appear in the rate law because the reaction rate is studied

under conditions where the reverse reactions do not contribute

to the overall rate. The reaction order and rate constant must

be determined by experiments. In order to distinguish the

kinet-ics equation based on the concentration of a solution from the

adsorption capacity of solids, this second-order rate equation

has been called a pseudo-second-order one

[9]

. The

pseudo-second-order model constants can be determined experimentally

by plotting t/qt

against t. Although there are many factors which

influence the adsorption capacity, including the initial adsorbate

concentration

[12,48–51]

, the reaction temperature

[10,12,50]

,

the solution pH value

[52,53]

, the adsorbent particle size

[48]

and

dose

[12,48,51]

, and the nature of the solute

[12,54]

, a kinetic

model is concerned only with the effect of observable

parame-ters on the overall rate. The pseudo-second-order expression has

been successfully applied to the adsorption of metal ions, dyes,

herbicides, oils, and organic substances from aqueous solutions

(

Table 1

).

Recently, a theoretical analysis of the pseudo-second-order

model was reported

[139]

. The advantage of the Azizian

deriva-tion is that when the initial concentraderiva-tion of solute is low, then

the adsorption process obeys the pseudo-second-order model.

Conversely pseudo-first-order models can be applied to higher

initial concentrations. The rate constant of the

pseudo-second-order model is a complex function of the initial concentration of

the solute.

Table 2

shows a comparison of second-order rate equations

of Sobkowsk and Czerwi´nski

[39]

, Ritchie

[33]

, Blanchard et al.

[13]

, and Ho

[9]

. In earlier years, Sobkowsk and Czerwi´nski used

the second-order rate equation based on the adsorption capacity

of a solid for higher concentrations of solids with the rate of

reaction of carbon dioxide adsorption onto a platinum electrode

[39]

. Ritchie presented a second-order empirical equation to test

the adsorption of gases onto solids

[33]

. Blanchard et al. reported

a similar rate equation for the exchange reaction of NH

4+

ions

fixed in zeolite by divalent metallic ions in solution

[13]

. Ho

described adsorption which included chemisorption and gave

a different idea of the second-order equation called a

pseudo-second-order rate expression

[9]

.

In many cases, the equilibrium adsorption capacity is

unknown, and chemisorption tends to become immeasurably

slow and the amount adsorbed is still significantly smaller than

the equilibrium amount

[140]

. On the other hand, achieving

equi-librium takes a long time in some adsorption systems

[141–143]

.

However, the pseudo-second-order equation has the following

advantages: it does not have the problem of assigning an

effec-tive adsorption capacity, i.e., the adsorption capacity, the rate

constant of pseudo-second-order, and the initial adsorption rate

all can be determined from the equation without knowing any

parameter beforehand.

(5)

Table 1

Pseudo-second-order kinetic model of various related systems from the literature

Adsorbent Adsorbate References

2-Mercaptobenzimidazole clay

Hg(II) [55]

Activated carbon 2,4-Dichlorophenoxy-acetic acid

[56]

Activated carbon Cd(II) [57]

Activated carbon Cd(II) [58]

Activated carbon Cd(II), Ni(II) [59]

Activated carbon Congo red [60]

Activated carbon Direct blue 2B, Direct green B

[61]

Activated carbon Hg(II) [62]

Activated carbon Hg(II) [63]

Activated carbon Methylene blue [64]

Activated carbon Paraquat dichloride [65]

Activated carbon Co(II) [66]

Activated carbon Pb(II) [67]

Activated carbon Pb(II) [68]

Activated carbon Pb(II), Hg(II), Cd(II), Co(II)

[69]

Activated clay Basic red 18, Acid blue 9 [70]

Aeromonas caviae Cr(VI) [71]

Alginate Ni(II) [72]

Anaerobic granular sludges Ni(II), Co(II) [73]

Aspergillus niger Acid blue 29 [74]

Aspergillus niger Basic blue 9 [75]

Aspergillus niger Congo red [76]

Aspergillus niger Pb(II), Cd(II), Cu(II), Ni(II) [77]

Azadirachta indica (Neem)

leaf

Congo red [78]

Azadirachta indica (Neem)

leaf

Pb(II) [79]

Baker’s yeast Cd(II) [80]

Banana stalk Musa

paradisiacal

Hg(II) [81]

Beech leaves Cd(II) [11]

Bentonite Acid red 57, Acid blue 294 [82]

Bi2O3 Cr(VI) [11]

Blast furnace slag, dust, sludge, carbon slurry

Chlorophenols [83]

Bottom ash Cu(II), Pb(II) [11]

Calabrian pine bark Zn(II), Pb(II) [84]

Calcined alunite Phosphorus [85]

Calcined Mg–Al–CO3

hydrotalcite

Cr(VI) [86]

Cassava waste biomass Cu(II), Cd(II) [87]

Chitin Cd(II) [88]

Chitin, chitosan, Rhizopus

arrhizus

Cr(VI), Cu(II) [38]

Chitosan Cu(II) [89]

Chitosan Ni(II) [90]

Clinoptilolite Pb(II) [91]

Coconut coir pith 2,4-Dichlorophenol [92]

Coconut coir pith Cr(VI) [93]

Coir Cu(II), Pb(II) [94]

Cypress leaves Pb(II) [11]

Date pits Methylene blue [95]

Date pits Phenol [96]

Diatomaceous clay Methylene blue [97]

Dolomite Phosphate [98]

Fly ash Congo red [99]

Fly ash Omega chrome red ME,

o-cresol, p-nitrophenol

[100]

Fly ash Victoria blue, OCL, PNP,

OCRME

[11]

Table 1 (Continued)

Adsorbent Adsorbate References

Grafted silica Pb(II), Cu(II) [101]

Grape stalks Cr(VI) [102]

Iron oxide-coated sand As(V), As(III) [103]

Jordanian low-grade phosphate

Pb(II) [104]

Juniper fiber Cd(II) [105]

Juniper fiber Phosphorus [106]

Mesoporous silicate Phosphate [107]

Mg–Al–CO3hydrotalcite Cr(VI) [108]

Microcystis Ni(II), Cr(VI) [109]

Microporous titanosilicate ETS-10

Pb(II) [110]

Mixed clay/carbon Acid blue 9 [111]

Mucor rouxii Pb(II), Cd(II), Ni(II), Zn(II) [112]

Myriophyllum spicatum Pb(II), Zn(II), Cd(II) [113]

Na-bentonite Oil [114]

Oil shale 4-Nitrophenol [115]

Peat Basic blue 69, Acid blue 25 [11]

Peat Basic green 4, Basic violet

4, Basic blue 24

[116]

Peat Cu(II) [117]

Peat Cu(II) [11]

Peat Cu(II) [118]

Peat-resin particle Basic magenta, Basic brilliant green

[119]

Perlite Cd(II) [120]

Perlite Methylene blue [121]

Pith Basic red 22, Acid red 114 [122]

Reed leaves Cd(II) [11]

Rhizopus oligosporus Cu(II) [123]

Rhodotorula aurantiaca Pb(II) [124]

Sago Cu(II), Pb(II) [125]

Sawdust Cd(II), Pb(II) [126]

Sawdust Phenol [127]

Schizomeris leibleinii Pb(II) [128]

Sepiolite Pb(II) [129]

Spent grain Pb(II), Cd(II) [130]

Sphagnum moss peat Chrysoidine, Astrazon blue, Astrazone blue

[22]

Sphagnum moss peat Cu(II), Ni(II) [131]

Sphagnum moss peat Cu(II), Ni(II), Pb(II) [12]

Sugar beet pulp Pb(II) [132]

Sugar beet pulp Pb(II), Cu(II), Zn(II), Cd(II), Ni(II) [133] Surfactant-modified clinoptilolite Phosphate [134] TNSAC Phosphate [11]

Tree fern Basic red 13 [135]

Tree fern Cd(II) [136]

Tree fern Cu(II) [49]

Tree fern Pb(II) [50]

Vermiculite Cd(II) [137]

Waste tyres, sawdust Cr(VI) [138]

Wollastonite Ni(II) [11]

(6)

Table 2

Comparison of second-order models

Author Year Linear form Plot

Sobkowsk and Czerwi´nski 1974 1−θθ = k2t 1−θθ vs. t

Ritchie 1977 qq∞ ∞−q = αt + 1 qq−qvs. t Blanchard et al. 1984 n1 0−n− α = Kt 1 n0−nvs. t Ho 1995 qtt = 1 k2q2e + 1 qet t qtvs. t

3. Conclusion

Adsorption rate equations have considered the adsorption

capacities of solids since Lagergren’s first-order equation was

presented. Several rate equations were reported with the same

idea in the following years. In earlier years, Elovich’s

equa-tion and Ritchie’s equaequa-tion were applied to the adsorpequa-tion of

gases onto solid faces. Later, application of these equations

to the adsorption of pollutants from aqueous solutions were

investigated. A second-order rate equation was used to describe

chemisorption for the adsorption of gases used to describe ion

exchange reactions. The pseudo-second-order rate expression

was used to describe chemisorption involving valency forces

through the sharing or exchange of electrons between the

adsor-bent and adsorbate as covalent forces, and ion exchange. In

recent years, the pseudo-second-order rate expression has been

widely applied to the adsorption of pollutants from aqueous

solu-tions. The advantage of using this model is that there is no need

to know the equilibrium capacity from the experiments, as it can

be calculated from the model. In addition, the initial adsorption

rate can also be obtained from the model.

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