cr@baso4: an acid rain-indicating material
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12810 Chem. Commun., 2011, 47, 12810–12812 This journal is c The Royal Society of Chemistry 2011
Cite this: Chem. Commun., 2011, 47, 12810–12812
CR@BaSO4: an acid rain-indicating materialw
Hong-Wen Gao* and Xin-Hui Xu
Received 1st September 2011, Accepted 6th October 2011
DOI: 10.1039/c1cc15435d
The CR@BaSO4 hybrid was synthesized, characterized and
used as an acid rain-indicating (ARI) material. A painted ARI
umbrella was discolored after exposure to simulated acid rain of
pH 5 or less and returned to the initial color after the rain
stopped. Such a functionalized material may make acid rain
visual to remind people in real-time.
Acid rain was first observed in the mid 19th century, when
some people noticed that forests located downwind of large
industrial areas showed signs of deterioration.1 It occurs when
large amounts of gases such as sulphur dioxide and nitrogen
dioxide are released into the air. Acid rain (pH o 5.6) affects
us in many different ways.2 Breathing and lung problems in
children and adults who have asthma have been linked to acid
air pollution.3 It can also damage non-living things. For
example, it destroys forests and biodiversity,4 pollutes lakes
and soil5 and corrodes buildings.6 At worst, it can damage
non-replaceable statues, and sculptures that are part of our
nation’s heritage.7 Some of the most acidic rain ever recorded
fell in the UK in 1974 and was measured to have a pH of 2.4.8
In December 1982, a sample of fog taken at Corona del Mar in
Southern California had a pH of 1.69. This extremely high
acidity developed after a two-day ground-level temperature
inversion in the Los Angeles basin.9 Places showing significant
impact of acid rain around the globe include most of eastern
and north-western Europe e.g. Poland, Scandinavia, Sweden
and Norway, northern and eastern America and south-eastern
Canada.10 In China, most of the acid rain effected areas are
located between the south of the Yangtze River and the east of
the Qinghai–Tibet Plateau, where the total area is approximately
1 200000 square kilometers. Early on the 15th of November 1990,
President Bush signed Amendments to the Clean Air Act. Title IV
of the Amendments authorized the Environmental Protection
Agency to establish an Acid Rain Program, the overall goal of
which is to reduce sulphur dioxide and nitrogen dioxide emissions.9
During the next two decades, many governments have introduced
laws to reduce these emissions.11 Over the years the scope and
intensity of acid rain has only been known by the relevant
government and research institutions. It is difficult for most people
to distinguish the acidity of rainfall on-site. It is necessary to
develop a way of visually detecting acid rain. This work aims
to prepare a potential acid rain-indicating material, which is
filled into the acrylic-based emulsion paint used to paint
common rain gear to visually remind people of acid rain in
real-time.
Congo red (CR, C.I. 22120) chemically named benzidinediazo-
bis-1-naphthylamine-4-sulfonic acid with a bright red color and
low toxicity is widely used in textiles, printing and paper-
making, etc. CR is still usually used in chemical laboratories as
a conventional acid–base indicator. It dissociates into a mixture
of H2L (blue), HL� (red) and L2� (red) with a transition range
of pH 3–5.2, which just corresponds to the scope of acid rain. It
is not readily reactive with the conventional ions in rain e.g.
Ca2+, Mg2+, Na+, Cl�, SO42�, CO3
2� etc. Barium sulfate
(BaSO4) isn’t dissolved in acidic aqueous media. It is usually
used as a filler in paint, paper, rubber and plastic in order to
increase the hardness and whiteness. The hybridization of CR
into BaSO4 obeyed the Langmuir sorption isotherm when
freshly formed (Fig. S1 A, ESIw). It indicated that the CR
was bound to the BaSO4 particles’ surface in a monolayer via
the affinity of Ba with –SO3�.12 The saturation mole ratio (N)
of CR to BaSO4 was calculated to be 1/60 and their binding
constant (K) to be 2.61 � 105 M�1. Therefore, CR was
immobilized firmly onto BaSO4. The reaction rate of CR is
less than 40% when the initial mole ratio of CR to BaSO4 is
more than 0.02 (Fig. S1 B, ESIw). According to the recom-
mended procedure, the CR@BaSO4 hybrid formed contained
1.6% C and 0.4% N by elemental analysis. The mole ratio of
CR to BaSO4 is calculated to be 1/85 in the hybrid. Weight loss
(about 5%) of CR@BaSO4 appeared obviously at around
720 1C, which is much higher than the decomposition temperature
of CR e.g. 360 and 410 1C (Fig. S2, ESIw). The thermal stability
of CR embedded in the hybrid obviously increased. CR was
calculated to occupy 3.3% of the hybrid, i.e. the mole ratio 1/83
of CR to BaSO4, which corresponds with the above analysis.
The CR@BaSO4 hybrid (40%) aqueous liquid is a thick
dark-red semifluid (Fig. 1Aa). Many rough elliptic particles/
sheets (50–200 nm of size) layered together to form the
irregular particles of 1–10 mm (Fig. 1A) (Fig. S3, ESIw). Theyare similar to MB@BaSO4 but different from CR@CaCO3.
13
From TEM, some regular thin layers were found inside the
CR@BaSO4 hybrid (Fig. 1Ba–b and Ca), where the thickness
of CR and BaSO4 layers were both approximately 1 nm. There
are two –SO3� groups located at the head and tail of CR so
that CR prostrated between adjacent BaSO4 layers to form a
State Key Laboratory of Pollution Control and Resource Reuse,College of Environmental Science and Engineering, Tongji University,Shanghai 200092, China. E-mail: [email protected];Fax: 86-21-65988598; Tel: 86-21-65988598w Electronic supplementary information (ESI) available: Experimentaldetails and Fig. S1 to S9. See DOI: 10.1039/c1cc15435d
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This journal is c The Royal Society of Chemistry 2011 Chem. Commun., 2011, 47, 12810–12812 12811
firm complex (Fig. 1Cb). Such an interlayer stacked structure
will prevent CR leaching in the aqueous solution.
Owing to a large number of –SO3� groups embedded in the
CR@BaSO4 hybrid (Fig. 1Cb), the hybrid carried a great
deal of negative charge confirmed by the z-potential analysis(Fig. S4, ESIw), e.g. �34.1 mV at pH 5.6, �28.5 mV at pH 4,
and �20.6 mV at pH 3. Without doubt, the CR@BaSO4
hybrid may adsorb H+. From the acid dissociation constant
(Ka) of CR, pKa 4.1,14 the [H2L]2/[HL�][L2�] ratio was
calculated to be 13 at pH 3, resulting in a blue hue, 1.3 at
pH 4, a bluish-purple hue and only 0.03 at pH 5.6, a red hue.
The CR@BaSO4 hybrid is also insoluble in aqueous media.
This was confirmed from an immersion experiment on the
hybrid (Fig. S5, ESIw), where the color was not stripped when
the hybrid was immersed in aqueous solution for 330 days and
acidic media for 24 h. Therefore, it is feasible to use this hybrid
as an acid rain-indicating material.
The simulated acid rains flowed across the ARI paint plates
and the color changed from red to blue (Fig. S6, ESIw). Also,
the blue color darkened with a decrease in pH from 5.6 to 3.5.
The blue color of the ARI paint plate also deepened with an
increase of the water flow time. Though the most obvious color
change of the ARI paint plates appeared after 15 min, the color
difference was clearly distinguishable at 5 min. Without doubt,
the ARI paint may indicate acid rain in real-time.
The absorption by the ARI paint of visible light between
450 and 550 nm decreased with a decrease of pH and that of
light between 600 and 750 nm increased (Fig. S7, ESIw). Thus,the reflection of blue-green light from the ARI paint plates
increased and that of the red light decreased. In accordance
with the visual observation above.
The quantitative color difference (DE) of the ARI
paint may be calculated by the relation
DE ¼ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiða0 � a1Þ2 þ ðb0 � b1Þ2 þ ðL0 � L1Þ2
q,15 where the
symbol a is redness–greenness, b yellowness–blueness and
L lightness–darkness. The subscripts 0 and 1 refer to the ARI
paint plate measured before and after exposure to rain. A DE of
7 occurs when the critical color difference is distinguished by
100% of observers.16 When the rain ceased for 1 h, DE values of
all of the plates were determined to be less than 4, i.e. they
returned to the initial red (Fig. S6, ESIw). Therefore, CR was
immobilized firmly into BaSO4 and not leached during rain.
CR is one kind of azo dye that is easily decomposed under
ultraviolet light irradiation. When an ARI paint plate was
exposed to strong sunshine for 18 h, DE was determined to
be 10. However, DE changed from 0.4 to 4.5 when the plate
was placed indoors for 10 to 270 days. Therefore, the ARI
paint is suitable for painting on the surface of rain gear but
unfit for painting on the external wall of a building.
The ARI umbrella test indicated that the four sectors coated
with ARI paint changed from red to blue with a reduction of
pH (Fig. 2B–E). During exposure to pH 5.6 simulated acid
rain, the sectors painted with the ARI paint changed little and
could not be readily differentiated (Fig. 2B). The DE of sector a
was determined to be 3.5 against the dry umbrella (Fig. 2A).
When the pH of simulated acid rain is less than 5, the color
change of the ARI paint sectors was obviously distinguishable
in comparison with the adjacent sectors (Fig. 2C–E). The DE of
sector a was determined to be 9 at pH 5, 15 at pH 4.5 and 23 at
pH 4 (Fig. 2F). Thus, the ARI umbrella testing indicated that
the ARI paint is suitable for indicating acid rain of pH r 5.
The raining duration indicated that the color change of the
ARI paint sectors was easily differentiated after exposure to
rain for 5 min with pH 4.5 of simulated acid rain (Fig. S8,
ESIw). The blue color darkened slightly with the passing of
time, which is similar to the ARI plate’s appearance above.
Thus, the ARI umbrella may indicate acid rain rapidly.
In order to investigate the repeatable use of the ARI
umbrella, it was exposed to three cycles of pH 4.5 simulated
acid rain. The results indicated that the repeated raining
seldom influenced the acid rain-indicating function of the
Fig. 1 Morphology and structure of the CR@BaSO4 hybrid. A: SEM image, Aa: the CR@BaSO4 hybrid liquid (40%); B and C: TEM images,
Ba, Bb and Ca: layer structure area inside the hybrid, Cb: cartoon illustration of CR binding to the BaSO4 layers.
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12812 Chem. Commun., 2011, 47, 12810–12812 This journal is c The Royal Society of Chemistry 2011
ARI umbrella (Fig. S9, ESIw). In addition, the ARI paint
sectors returned to the initial color after the rain had ceased
for 1 h. Therefore, the ARI umbrella can be used repeatedly
during rainfall.
In conclusion, acid rain as a form of serious air pollution17 is
recognized as one of the most serious global environmental
problems. It has brought great losses to the global economy and
civilization. This work developed a facile preparation of an ARI
material, i.e. a CR@BaSO4 hybrid synthesized by conventional
organic–inorganic hybridization. When characterizing the
structure and morphology, the CR@BaSO4 hybrid contained
a great deal of negative charges and the thermal stability of
CR when firmly embedded increased up to 720 1C. The ARI
paint was prepared by mixing the CR@BaSO4 hybrid with
acrylic-based emulsion paint and was then coated on an
umbrella. The ARI umbrella discolored sensitively after
5 min of exposure to simulated acid rain of pH o 5 and
returned to the initial color after the rain ceased for 1 h.
During airing an ARI umbrella seldom discolored, i.e. the
color difference (DE) was less than 7 when placed indoors for
9 months. Such a new-type of functionalized material provides
the public with an on-site method of observation for acid rain.
Surely, with every citizen all over the world acting forcefully,
air pollution and acid rain problems may eventually be solved.
The authors acknowledge financial support from the National
Key Technology R&D Program of China (Grant No.2008-
BAJ08B13) and the Key Project of State Key Laboratory of
Pollution Control and Resource Reuse (2011–2014).
Notes and references
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9 A. Nixon,T. Curran,Government of Canada, Science andTechnology Division, Acid Rain, http://dsp-psd.pwgsc.gc.ca/Collection-R/LoPBdP/CIR/7937-e.htm.
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Fig. 2 Change of the ARI umbrellas after 5 min of rain with various simulated acid rains. (A) Before raining; (B to E) pH 5.6, 5.0, 4.5 and 4.0; (F)
change in DE of the above ARI umbrellas (B to E, area a) during raining.
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