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wat e r r e s e a r c h 4 6 ( 2 0 1 2 ) 4 0 6 3e4 0 7 0
Available online at w
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Laboratory study on the adsorption of Mn2D on suspendedand deposited amorphous Al(OH)3 in drinking waterdistribution systems
Wendong Wang a,*, Xiaoni Zhang a, Hongping Wang b, Xiaochang Wang a, Lichuan Zhou a,Rui Liu c, Yuting Liang d
a School of Environmental and Municipal Engineering, Xi’an University of Architecture and Technology, Xi’an, Shaanxi 710055, ChinabQujiang Drinking Water Purification Plant, Water Industry Operations Company of Xi’an, Xi’an 710061, ChinacDepartment of Environmental Technology and Ecology, Yangtze Delta Region Institute of Tsinghua University, Zhejiang, Jiaxing 314006,
ChinadSchool of Environmental and Safety Engineering, Changzhou University, Changzhou 213164, China
a r t i c l e i n f o
Article history:
Received 18 November 2011
Received in revised form
6 May 2012
Accepted 10 May 2012
Available online 18 May 2012
Keywords:
Aluminum hydroxide
Drinking water
Pipe scale
Water quality
* Corresponding author. Department of EnviYanta Road, Xi’an, Shaanxi 710055, China. T
E-mail address: [email protected] (W. W0043-1354/$ e see front matter ª 2012 Elsevdoi:10.1016/j.watres.2012.05.017
a b s t r a c t
Manganese (II) is commonly present in drinking water. This paper mainly focuses on the
adsorption of manganese on suspended and deposited amorphous Al(OH)3 solids. The
effects of water flow rate and water quality parameters, including solution pH and the
concentrations of Mn2þ, humic acid, and co-existing cations on adsorption were investi-
gated. It was found that chemical adsorption mainly took place in drinking water with pHs
above 7.5; suspended Al(OH)3 showed strong adsorption capacity for Mn2þ. When the total
Mn2þ input was 3 mg/L, 1.0 g solid could accumulate approximately 24.0 mg of Mn2þ at
15 �C. In drinking water with pHs below 7.5, because of Hþ inhibition, active reaction sites
on amorphous Al(OH)3 surface were much less. The adsorption of Mn2þ on Al(OH)3 changed
gradually from chemical coordination to physical adsorption. In drinking water with high
concentrations of Ca2þ, Mg2þ, Fe3þ, and HA, the removal of Mn2þ was enhanced due to the
effects of co-precipitation and adsorption. In solution with 1.0 mg/L HA, the residual
concentration of Mn2þ was below 0.005 mg/L, much lower than the limit value required by
the Chinese Standard for Drinking Water Quality. Unlike suspended Al(OH)3, deposited
Al(OH)3 had a much lower adsorption capacity of 0.85 mg/g, and the variation in flow rate
andmajor water quality parameters had little effect on it. Improved managements of water
age, pipe flushing and mechanical cleaning were suggested to control residual Mn2þ.
ª 2012 Elsevier Ltd. All rights reserved.
1. Introduction Environment and Health/Institute of Occupational Medicine,
Manganese (Mn) is an element that is ubiquitous in the envi-
ronment. It is commonly found in drinking water and is
essential for humanhealth at low concentrations (Institute for
ronmental and Civil Engiel.: þ86 135 7254 7081; faang).
ier Ltd. All rights reserved
2004). However, excessive concentrations of Mn could result
inmetallic tasting water andmany health problems. Jose et al.
(2009) found that excessive intake of manganese could cause
nervous system damage, leading to Parkinson’s disease, and
neering, Xi’an University of Architecture and Technology, No. 13,x: þ86 29 8220 2729.
.
wat e r r e s e a r c h 4 6 ( 2 0 1 2 ) 4 0 6 3e4 0 7 04064
injure arterial breastwork and the myocardium. Wasserman
et al. (2006) identified a significant negative relationship
betweenMn2þ and the intellectual function of 142 10-years-old
children drinking well water. In addition, the accumulation of
manganese-containing sediments can lead to reduced water
pressure and flow in pipes (Sly et al., 1990; USEPA, 2008). The
World Health Organization has set a guideline of 0.4 mg/L for
manganese intake control from drinking water (World Health
Organization, 2008); and the limit value in the Chinese Stan-
dard for DrinkingWater Quality (GB5749-2006) is 0.1 mg/L.
Manganese primarily exists in the form of divalent
manganese cation (Mn2þ) in drinking water. In neutral and
alkaline environments, Mn2þ is difficult to be oxidized
(Sommerfeld, 1999). Although chlorine or KMnO4 oxidation
combined with sand filtration is usually applied for Mn2þ
removal, its concentration in the treated water is still difficult
to meet the local requirements (Seppanen, 1993; Mo, 2010). It
was presumed that the concentration ofMn2þwas constant as
the water passes through pipelines (Schock, 2005). Conse-
quently, regulatory monitoring of Mn2þ is only required at
entry points of the drinkingwater distribution system (DWDS),
presuming that its concentration could not increase and that
suchmonitoring is sufficiently toprotectpublichealth (Schock,
2005; Wang et al., 2011). In fact, as the effects of pollutants
accumulationand sedimentation, the concentrationofMn2þ is
variable (USEPA, 2006), and the variation of water quality such
as solution pHmay cause a sudden release of Mn2þ.Aluminum-containing scale commonly exists in the DWDS
(Snoeyink et al., 2003; Wang et al., 2010). Many studies have
found that amorphous Al(OH)3 exists a good adsorption
capacity to many pollutants (Schock and Holm, 2003). Julien
et al. (1994) studied the adsorption of organic acids to pre-
formed Al(OH)3 and found a correlation between removal
efficiency and the number and ionization of functional
groups. Generally, the removal efficiency increased with
a greater number of functional groups on the organic acids
and thus with greatermolecular weight. Sudden reductions in
lead levelswere observed during pipe rig testing in a Rochester
case study that was coincided with the opening of a new
filtration plant and appeared to be related to aluminum
deposition on lead piping materials (Kirmeyer et al., 1999).
However, the adsorption of Mn2þ on amorphous Al(OH)3 has
not yet been considered in the literature.
The objective of this paper was to (1) study the adsorption
of Mn2þ in DWDS with suspended and deposited amorphous
Table 1 e Effecting factors and their levels selected in the expe
Experiments Para. Units
Adsorption of Mn2þ on Al(OH)3 scale pH e
Mn2þ mg/L
v mL/s
Adsorption of Mn2þ on Al(OH)3 suspension Ca2þ mg/L
Mg2þ mg/L
Fe3þ mg/L
HA mg/L
Para., parameters; Var., variable.
Al(OH)3 formation; (2) investigate the effects of major water
quality parameters including solution pH, dissolved organic
matter, and co-existing cations on the adsorption process; and
(3) reveal the reaction mechanism between amorphous
Al(OH)3 and Mn2þ. On the basis of the conclusions obtained in
this study, some DWDS operation management suggestions
were also given.
2. Experimental materials and methods
2.1. Adsorption of Mn2þ on suspended Al(OH)3
0.20 g of air-dried Al(OH)3 made from the hydrolysis of
Al2(SO4)3 at pH 6.5 was put into 500 mL test tubes with 240 mL
of deionized water. Then, 10.0 mL of 25.0 mg/L MnCl2 was
added. The tubes were stirred using a magnetic stirrer for
5 min. Then, the mixtures were sampled and centrifuged at
5000 rpm for 20 min. The amount of residual Mn2þ was
determined by analyzing the supernatant. The sorption coef-
ficient (Kd) was calculated as the ratio of the amount of Mn2þ
being adsorbed to the solid and the amount of residual Mn2þ
in the water at equilibrium, as shown in Eq. (1) (Dzombak and
Morel, 1990):
¼ AlOH0:5� þMn2þ/ ¼ AlOMn0:5þ þHþ (1)
The effects of the primary co-existing ions, including
calcium, magnesium, iron, and humic acids (HA), on the
adsorption of Mn2þ were investigated. HA was filtrated with
a 0.45 mm polycarbonate membrane to remove the insoluble
matter, and it was subsequently filtered with an ultrafiltration
membrane with a 500 Da molecular weight cutoff. In this
experiment, all thewater quality parametersweremaintained
at the values in the ranges of actual drinking water (Table 1).
The co-existing cations were added three times, correspond-
ing to their low, middle, and high levels in actual drinking
water respectively. Solution pH was adjusted with 0.50 mol/L
NaOH and 0.50 mg/L HNO3.
2.2. Manganese (II) adsorption on deposited amorphousAl(OH)3 scale
A laboratory scale DWDS was set up as shown in Fig. 1.
Drinking water was drawn from a tank and pumped to the
riments (15 �C).
Mn2þ pH Selected level
Low Middle High
1.0 Var. 6.5 7.5 8.5
Var. 7.5 0.0 1.0 2.0
1.0 7.5 0.2 0.5 1.0
1.0 7.5 20.0 60.0 100.0
1.0 7.5 5.0 25.0 50.0
1.0 7.5 0.1 0.3 0.5
1.0 7.5 1.0 5.0 10.0
water tankInfluent
Pump
Pressure gauge
Pipe system Discharge
Fig. 1 e Drinking water distribution system used in the
experiment.
wat e r r e s e a r c h 4 6 ( 2 0 1 2 ) 4 0 6 3e4 0 7 0 4065
pipe system. To exclude the effects of othermetals introduced
by pipe corrosion and metal element stripping, polyvinyl
chloride (PVC) pipes were used in the system. Deionized water
was used for modeling drinking water preparation. The water
quality parameters were adjusted by placing specified
volumes of 0.50 mol/L NaOH, 0.50 mg/L HNO3, 100 mg/L
Al2(SO4)3, and 50.0 mg/L MnCl2 into the tank. Reagent grade
chemicals were used except where noted.
The tank was placed in an incubator to maintain the
water temperature at 15 �C. Water samples were taken from
the effluent, and deposited Al(OH)3 were scraped from the
pipeline, respectively. To accelerate the precipitation of
Al(OH)3, the initial pH and aluminum concentration of the
solution were maintained at 6.5 and 50.0 mg/L, respectively.
After 5 days of operation, a white gelatinous pipe coating,
mainly composed of Al(OH)3 was generated. Then, stopped
adding Al2(SO4)3 and introduced 1.0 mg/L Mn2þ to the system
in stage I. To insure that the added metal elements were fully
mixed with the Al(OH)3 scale, the flow velocity was main-
tained at 0.5 mL/s, which was much lower than the normal
value.
When the concentration of Mn2þ residual in the effluent
was stable, the effects of flow velocity, solution pH, and
manganese concentration on Mn2þ adsorption were investi-
gated in stage II (Table 1). Water samples were taken at
different time intervals and filtered through a 0.45 mm poly-
carbonate membrane for water quality determination.
5 10 15 20
0.00
0.02
0.04
0.06
0.08 pH 8.5 pH 7.5 pH 6.5
Reaction time (min)
Res
idua
l Mn2+
(m
g/L
)
C = 1.0 mg/LC = 0.5 mg/LC = 0.1 mg/L
Fig. 2 e Manganese (II) adsorption in solutions with an
amorphous Al(OH)3 suspension.
2.3. Manganese (II) adsorption prediction method
The formation of surface complexes is conceptualized simi-
larly to that happened in solutions. The application of the
surface acid/base reactions could explain the protolytic
behavior of many different oxides (Schindler, 1981). The mass
action laws for surface complexation reactions are also
treated similarly to those involving soluteesolute
interactions.
The amount of Mn2þ adsorbed by suspended amorphous
Al(OH)3 was predicted applying the VISUAL MINTEQ software,
by defining the concentrations of all components, solution pH,
water temperature, ion strength, and adsorption parameters
including the number of the surfaces (1 surface), adsorption
model (Diffused Layer Model), solid concentration (0.05 mg/L),
site concentration (1.0 mmol/mmol), and the sorption coeffi-
cient (Kd) (Pommerenk and Schafran, 2005). Moreover,
manganese speciation including the solids that might
precipitate from solution was also calculated.
2.4. Water quality and solid analysis methods
The concentrations of aluminum, calcium, magnesium, iron,
and manganese were determined using an ICP-AES (IRIS
intrepid-II, Thermo Scientific, USA). Sample aliquots were
digested with trace metal grade nitric acid to pH < 2 for 12 h
prior to analysis. The concentration of HA was determined by
a TOC analyzer (TOC-Vwp, Shimazu Company, Japan); pHwas
determined using a pHmeter (Model 828, ThermoOrion, USA),
temperature was determined with a thermometer (Model
TTM1-JM-6200IM, Yuan-Da Technology Corporation, China).
All parameters were analyzed according to the standard
methods described in GB/T 5750.4-2006 of China.
To observe the surface characteristics of amorphous
Al(OH)3, scanning electron microscopy combined with an
energy dispersive spectrometer (SEM/EDS) (JSM-6490LV, JEOL
Ltd., Japan) and a X-ray diffractometry (Ultima IV, Rigaku
Corporation, Japan) were applied. The SEM/EDS samples were
sputter-coated with gold before conducting surface scanning
and elemental component analysis. To verify the valence
information of manganese, the X-ray photoelectron spec-
troscopy (K-Alpha, Thermo Scientific, USA) of the amorphous
Al(OH)3 solid after adsorption was also observed. Specific area
was measured using a Micromeritic Gemini model VII 2390
and an adsorption volumetric system with a pressure trans-
ductor (MKS Baratron 170 M). 100 mg of the sample was kept
under N2 flow at 60 �C for 4 h. The assays were performedwith
N2 as the adsorbate at 77 K.
3. Results and discussion
3.1. Manganese (II) adsorption in the suspended Al(OH)3solution
Static adsorption experiments were conducted in shaking
flasks. The residual concentrations of Mn2þ were stable with
reaction time at pH 6.5, while the addition of Mn2þ led to
a notable increase in residual Mn2þ (Fig. 2). By increasingMn2þ
input from 0.1 to 0.5 mg/L after 6 min of adsorption, the
0.0 0.5 1.0 1.5 2.0 2.5 3.0
0
5
10
15
20
25
q (
mg/
g)
Mn2+
input ( mg/L)
Model fitting results
Fig. 3 e Adsorption isotherm of Mn2D on amorphous
Al(OH)3 suspension at pH 7.5.
wat e r r e s e a r c h 4 6 ( 2 0 1 2 ) 4 0 6 3e4 0 7 04066
residual concentration of Mn2þ increased notably from
0.01 mg/L to approximately 0.04 mg/L. The increment of
residual Mn2þ was about 0.03 mg/L, much lower than the
increment of Mn2þ input. Increasing Mn2þ input further to
1.0 mg/L after 14 min of adsorption, similar experimental
results were obtained, indicating that the adsorption of Mn2þ
on Al(OH)3 was a fast process, andmost of the Mn2þ input was
removed. Compared with the solution at pH 6.5, residual
concentrations of Mn2þ were much lower (below 0.005 mg/L)
at pH 7.5 and 8.5 and less affected by the amount of Mn2þ
input (Fig. 2). Residual Mn2þ was not detected, even in the
solution with 1.0 mg/L Mn2þ input.
The distribution of manganese in the system was calcu-
lated using Visual MINTEQ software, while maintaining the
solution pH at 7.5e8.5. Because of the presence of amorphous
Al(OH)3, little manganese hydroxide or other manganese-
containing solids formed in the reaction. Nearly all of the
Mn2þ input was adsorbed by Al(OH)3 solid or remained in the
solution. From the X-ray diffraction spectrum of the solids
formed after adsorption, it was also difficult to observe the
peaks contributed by Mn(OH)2, MnCO3, and other manganese-
containing crystals. Both Mn(III) and Mn(IV) were not found in
amorphous Al(OH)3 after adsorption. Accordingly, the high
removal ratio of Mn2þ at pHs above 7.5 was not attributed by
chemical precipitation but mainly by the adsorption of Mn2þ
on amorphous Al(OH)3.
Table 2 e Adsorption equilibrium between amorphous Al(OH)
Total Mn (mmol) ¼AlOH0.5� (mmol) Mn2þ (mmol)
18.2 624 1.0
36.4 609 3.8
54.5 596 9.6
72.7 581 12.6
90.9 565 14.5
To observe the adsorption capacity of amorphous Al(OH)3,
the adsorption isotherm of Mn2þ was drawn in Fig. 3. The
adsorption of Mn2þ onto amorphous Al(OH)3 followed the rules
of type I adsorption isotherm at pH 7.5. When the total Mn2þ
input was 3 mg/L, 1.0 g amorphous Al(OH)3 could adsorb
approximately 24.0 mg of Mn2þ. On the basis of the concentra-
tions of total and residual Mn2þ, the adsorption constant (Kd) of
Mn2þ was calculated (Table 2). The specific surface area and
surface site density of amorphous Al(OH)3 were assumed to be
constant at 900 m2/g and 1.0 mmol/mmol, respectively
(Pommerenk and Schafran, 2005). Applying the diffuse layer
adsorption model, residual Mn2þ concentrations were pre-
dicted. In solutions with total Mn2þ input below 0.5 mg/L, the
experimentaldatafittedwellwith themodelfitting result;while
when the concentration of totalMn2þ inputwas above 1.0mg/L,
it was lower than the model fitting results, which might be
connectedwith the availability of the reaction sites in solutions
with high Mn2þ contents. Considering the concentration of
Mn2þ in drinking water usually lower than 0.5 mg/L (Mo, 2010),
the method was still valid for Mn2þ adsorption prediction.
At pHs above 7.5, the amount ofMn2þ removed fromdrinking
water was close to the amount adsorbed by amorphous Al(OH)3(Fig. 4), indicating that the reaction constant and adsorption
model selected were suitable and that amorphous Al(OH)3showed good adsorption capacity in a weak alkaline solution.
These observations agreed with the conclusions made by
Violante and Huang (1985), validating the data obtained in Fig. 4.
Besides, from Eq. (1), it could be concluded that the adsorption of
Mn2þ onto amorphous Al(OH)3 was highly pH dependent. The
chemical adsorption process would be inhibited in acidic condi-
tions (Gustafsson and Bhattacharya, 2007). However, the deter-
mined values of residual Mn2þ were lower than the predicted
values at pHs below 7.5.
Compared with chemical adsorption as the formation of
inner-sphere or strong outer-sphere bonds betweenMn2þ and
the surface structural cation, the contribution of physical
adsorption to Mn2þ removal was higher under acidic condi-
tions (Venema et al., 1996). As the existence of van der waals
force, part of the Mn2þ was removed. In Fig. 5, it was shown
that the original surface of amorphous Al(OH)3 solid was
irregular; while after Mn2þ adsorption it became much
smoother. However, as the combination strength caused by
physical adsorption was usually weaker than that caused by
chemical adsorption, flow velocity and drinking water quality
might lead to a sudden desorption of Mn2þ. In order to insure
drinking water supply safety, decreasing Mn2þ concentration
in the treated water and improving drinking water supply
network management are suggested.
3 and Mn2D at 15 �C.
¼AlOMn0.5þ (mmol) pH LogKd LogKd
17.2 6.5 �2.06 �2.43
32.5 6.5 �2.36
44.9 6.5 �2.61
60.1 6.5 �2.58
76.5 6.5 �2.53
6.5 7.0 7.5 8.0 8.5
0.0
0.2
0.4
0.6
0.8
1.0
Residual Mn2+
(calculated value)
Residual Mn2+
(determined value)
Adsorbed Mn2+
(calculated value)
Mn2+
(m
g/L
)
pH
Fig. 4 e Theoretical concentrations of Mn2D adsorbed by
amorphous Al(OH)3 at different solution pH values.
wat e r r e s e a r c h 4 6 ( 2 0 1 2 ) 4 0 6 3e4 0 7 0 4067
Elemental analysis showed that aluminum and oxygen
were the major elements of the aluminum-containing solids
that formed in both static and dynamic adsorption experi-
ments (Table 3). The Al/O molar ratio was approximately 1:3,
which corresponded well with the elemental composition
characteristics of amorphous Al(OH)3. Manganese was not
detected until after adsorption. The molecular weight percent
of Mn2þ was approximately 1.91%. Every gram of amorphous
Al(OH)3 could adsorb 18.5 mg of Mn2þ, close to the experi-
mental value. These results further indicated that amorphous
Al(OH)3 had a large adsorption capacity for Mn2þ, especially in
basic conditions.
3.2. Manganese (II) adsorption on deposited amorphousAl(OH)3
Experiments were conducted applying synthetic water with
pH, temperature, and initial Mn2þ concentration maintained
at 7.5, 15 �C, and 1.0 mg/L, respectively, after the formation of
amorphous Al(OH)3 pipe scale. The variation of residual Mn2þ
with flow volume was studied. Initially, the concentration of
residual Mn2þ in the bulk water was the lowest, at approxi-
mately 0.85 mg/L (Fig. 6). However, as the total flow increased,
the amount of Mn2þ that remained in the drinking water also
increased. When the total flow volume was 2.0 L, the
concentration of Mn2þ in the effluent increased to 1.0 mg/L
which was closed to the total Mn2þ input.
Manganese speciation was calculated applying Visual
MINTEQ under the same water quality condition. In the
absence of amorphous Al(OH)3 formation, more than 99% of
the Mn2þ would exist in the water. When amorphous Al(OH)3scale formed in the pipeline, part of the Mn2þ was adsorbed,
which had been shown in Section 3.1. At the end of stage I,
Al(OH)3 reached its maximum adsorption capacity. The
amount of Mn2þ adsorbed by deposited amorphous Al(OH)3was approximately 0.85 mg/g, much less than the value
removed from suspended amorphous Al(OH)3, whichmight be
related to its surface characteristics. Although the XRD
spectra of deposited and suspended Al(OH)3 solids were
similar to each other, both in an amorphous state, the specific
surface area of the deposited Al(OH)3 was about 160 m2/g,
much lower than that of suspended Al(OH)3, 920 m2/g. To
investigate the effects of major parameters on Mn2þ adsorp-
tion, the systems were operated under different conditions in
stage II, as shown in Fig. 6.
When the amount ofMn2þ addition decreased from 1.0mg/
L to 0 mg/L, the concentration of residual Mn2þ decreased
suddenly to 0.001mg/L, indicating that the adsorption of Mn2þ
on deposited amorphous Al(OH)3 was stable. The amount of
Mn2þ released from pipe scale was much lower than the
acceptable value 0.1 mg/L, which was good for drinking water
supply safety. However, when the added concentration of
Mn2þ was increased from 1.0 mg/L to 2.1 mg/L, the concen-
tration of residual Mn2þ reached 2.1 mg/L quickly, further
indicating that Al(OH)3 scale had reached its maximum
adsorption capacity (Fig. 6). When the flow rate increased
from 0.5 to 1.0 mL/s, the concentration of residual Mn2þ
increased from 0.94 mg/L to 1.12mg/L gradually, this might be
linked to the flushing effects of the pipe water at higher flow
velocity (Friedman et al., 2003). Maintaining low flow velocity
was suggested for residual Mn2þ control in the tap water.
Similar to the effects of flow velocity, the variation of
solution pH also had little effect on the adsorption of Mn2þ on
deposited amorphous Al(OH)3 in basic conditions (Fig. 6). At
pH 7.5e8.5, the amount ofMn2þ residual in drinkingwaterwas
stable at about 1.0 mg/L. Unlike the case at pH 8.5, the
concentration of residual Mn2þ fluctuated in the range of
0.85e1.05 mg/L at pH 6.5, which might be connected with the
weak combination between amorphous Al(OH)3 and Mn2þ
under acidic conditions (Fonseca et al., 2006). Elemental
analysis revealed that manganese was not detected in the
freshly formed scale; however, after adsorption, its molecular
weight ratio increased to approximately 0.15%. Every gram of
amorphous scale could adsorb 1.1 mg of Mn2þ, close to the
experimental value.
In this study, Al(OH)3 scale was prepared prior to Mn2þ
adsorption. Most of the Mn2þ was mainly adsorbed by the
reaction sites on its surface only, leading to much less Mn2þ
removed from water (Hiemstra and van Riemsdijk, 1996). In
actual DWDS, however, amorphous Al(OH)3 usually formed
simultaneously with the removal of pollutants. Metal
elements not only existed on the surface but also inside of
Al(OH)3 scale (Lauer and Lohman, 1994). It could be concluded
that in the formation process of amorphous Al(OH)3 scale, its
adsorption capacity for Mn2þ was strong; however, when
Al(OH)3 formation was halted or its structure was destroyed
due to the variation of water quality, its adsorption capacity
would drastically decrease or even leading to a suddenly
release ofMn2þ. Accordingly, removing contaminant reservoir
should be conducted regularly in DWDS management.
3.3. Effects of water quality on Mn2þ adsorption
In addition to solution pH and manganese concentration, the
influence of co-existing cations on the adsorption ofMn2þwas
also examined. Considering Ca2þ, Mg2þ, and Fe3þ commonly
existing in drinking water, their concentrations are usually
higher than other elements (Schock, 2005). Dissolved organic
Fig. 5 e Morphological characteristics of amorphous Al(OH)3 before (a) and after (b) Mn2D adsorption.
wat e r r e s e a r c h 4 6 ( 2 0 1 2 ) 4 0 6 3e4 0 7 04068
matter is mainly produced by living organisms or formed by
secondary synthesis reactions (Desroches and Dayde, 2000;
Liu et al., 2007). As a commonly existing organic matter in
drinking water, HA could react both with aluminum-
containing solids and Mn2þ by the formation of stable
complexes (Pommerenk and Schafran, 2005). Their effects on
Mn2þ adsorption on amorphous Al(OH)3 were also investi-
gated at pH 6.5 with 1.0 mg/L Mn2þ addition.
The presence of co-existing materials could promote the
removal of Mn2þ from drinking water. When the concentra-
tion of Ca2þ was 20 mg/L, residual Mn2þ was approximately
0.08 mg/L after 10 min adsorption (Fig. 7). Increasing the
concentration of Ca2þ to 60 mg/L, the residual Mn2þ increased
to about 0.035 mg/L after 22.0 min adsorption. When the
concentration of Ca2þ was at its highest value (100 mg/L), the
residual Mn2þ concentration was approximately 0.03 mg/L.
Similar experimental results were obtained when Mn2þ co-
existed with Mg2þ, Fe3þ, and HA in solution. However, the
contribution of these co-existing materials differed greatly
from each other. Their promoting capacity on Mn2þ removal
could be listed from strong to weak as follows:
HA > Fe3þ > Mg2þ > Ca2þ.Co-precipitation and enhanced adsorption induced by the
co-existing cations are the major reasons leading to further
removal of Mn2þ from drinking water (Knocke et al., 1991).
With a solution pH of 6.5, the solubility of Fe(OH)3 (III) was the
lowest, and the solubility of CaCO3 was the highest among the
cations selected in the experimental water quality condition.
Table 3 e Elements composition of amorphous Al(OH)3 before
Elements Before adsorption After adso
Weight (%) Mole (%) Weight (%)
O 62.84 74.33 62.7
Al 33.57 23.54 32.64
S 3.60 2.12 2.75
Mn 0.00 0.00 1.91
The amount of Fe(OH)3 solid formed was also more than
Mg(OH)2 and CaCO3. Besides the accessibility of adsorption
sites, the adsorption capacity of Fe(OH)3 for Mn2þ was also
stronger than that ofMg(OH)2 and CaCO3 (Buamah et al., 2008),
leading tomoreMn2þ removed from the systemwith Fe(III) co-
existing.
Unlike the co-existing cations, the HA used in this experi-
ment, with an average molecular weight below 500 Da, was
soluble. Its reactive characters can be explained by a series of
oxygen-containing functional groups, which includes
carboxyl, phenolic-OH, enolic, and alcoholic-OH, and carbonyl
(Wang et al., 2010). One HA molecular usually contains many
different active reaction sites (Tipping, 1994), which provide
more combining sites for Mn2þ and Al(OH)3 solid. With the
effects of bridging adsorption, nearly all of the Mn2þ was
removed.
Accordingly, in solutionswith CaCO3, Mg(OH)2, and Fe(OH)3solid formation and HA, Mn2þ removal ratio was higher due to
the effects of co-precipitation and adsorption. Even in solution
with only 1.0 mg/L HA, the concentration of residual Mn2þ in
the water body was determined to be below 0.005 mg/L.
However, it should be noted that this study has only investi-
gated the adsorption and precipitation processes of Mn2þ at
the lab scale, and its oxidation process was not considered.
Not withstanding its limitation, this study does suggest the
adsorption rules hold true for the adsorption of Mn2þ on
amorphous Al(OH)3 formed in DWDS when there is no
oxidation reaction with the residual Mn2þ.
(a) and after (b) adsorption.
rption (suspension) After adsorption (scale)
Mole (%) Weight (%) Mole (%)
74.51 63.33 74.05
23 33.29 23.12
1.84 3.23 2.76
0.65 0.15 0.07
0 5 10 15 20 25 30
0.00
0.05
0.10
0.15
Stage 3: coexisting cations at high-level
Stage 2: coexisting cations at mid-level
Stage 1: coexistingcations at low-level
Mn2+
con
cent
rati
on (
mg/
L )
Adsorption time ( min )
Ca Fe Mg HA
Fig. 7 e Effects of Ca2D, Mg2D, Fe3D, and HA on the
adsorption of Mn2D on amorphous Al(OH)3 suspension.
0 2500 5000 25000 26000 27000 28000 29000
0.8
1.0
2.0
2.2
Stage ΙΙ
Mn
conc
entr
atio
n (
mg/
L)
V ( mL )
v=0.2 mL/s v=1.0 mL/s pH 6.5 pH 8.5 C = 2.1 mg/L
Stage Ι
Fig. 6 e Variation of Mn2D remained in drinking water with
the total flow volume before and after water quality and
flow velocity adjustment in the system with amorphous
Al(OH)3 scale formation.
wat e r r e s e a r c h 4 6 ( 2 0 1 2 ) 4 0 6 3e4 0 7 0 4069
4. Conclusions
The adsorption of Mn2þ on amorphous Al(OH)3 is a complex
process. In drinking water with solution pHs above 7.5,
chemical adsorption mainly took place; Al(OH)3 suspension
showed a strong adsorption capacity to Mn2þ. In drinking
water with solution pHs below 7.5, as the inhibition of Hþ
increased, active reaction sites on the solid surfaceweremuch
less. Thus, the adsorption process of Mn2þ on amorphous
Al(OH)3 changed gradually from chemical coordination to
physical adsorption with a decreasing solution pH.
In drinking water with high concentrations of Ca2þ, Mg2þ,and Fe3þ, the adsorption of Mn2þ on amorphous Al(OH)3 was
enhanced due to the effects of co-precipitation and adsorption
contributed by the newly formed CaCO3, Mg(OH)2, Fe(OH)3,
and other solids. Different from the effects of co-existing
cations, dissolved organic matter, especially HA, enhanced
the adsorption of Mn2þ due to the effect of bridge connecting.
Even in solution with only 1.0 mg/L HA (average molecular
weight of less than 500 Da), the concentration of residualMn2þ
in the water body could be controlled below 0.005 mg/L, much
lower than the standard required level.
In the formation of amorphous Al(OH)3 scale, the adsorp-
tion capacity for Mn2þ was the highest, at about 24.0 mg/g,
when the Mn2þ input was 3 mg/L at 15 �C. In solution with HA
and CaCO3, Mg(OH)2, and Fe(OH)3 solids, its removal ratio was
higher. When the Al(OH)3 scale stopped growing, its adsorp-
tion capacity decreased significantly to approximately
0.85 mg/g. Better management of water age and sediment
accumulation was suggested to control the concentration of
Mn2þ in the tap water. Moreover, flushing and mechanical
cleaning should also be conducted regularly.
Acknowledgments
This research was supported by Changjiang Scholars and
Innovative Research Team in University (PCSIRT) (IRT0853),
the National Natural Science Foundation of China (21007050),
and Changzhou University Research Fund (ZMF1002127). We
are also grateful for anonymous reviewers for their helpful
suggestions and advices.
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