Marie Mauriaucourt1,2, Shanfeng Jiang2, Anamaria Soare2, Aalbert Zwijnenburg2, Noushine Shahidzadeh1. 1. University of Amsterdam, Van der Waals-Zeeman Institute, Institute of Physics, Science Park 904, 1098 XH Amsterdam, The Netherlands. 2. Nouryon, Research, Development & Innovation Salt, Industrial Chemicals, Zuthpenseweg 10, 7418 AJ Deventer, The Netherlands.
Abstract
Caking constitutes a major problem for the flowability, transport, packaging, and consumption of hygroscopic granular crystalline materials such as salt. Sodium chloride is the most abundant salt on the earth and known to form strong lumps, mainly due to cycles of water uptake and water evaporation. We report on a multiscale study of the anticaking effect of the bio-based additive Fe-mTA, a metal-organic complex of iron (III) and meso-tartrate. Drying-deliquescence cycling experiments are performed to reproduce the situation in which the salt undergoes repeated humidity fluctuations. Our results show that Fe-mTA acts as a nucleation promoter and growth inhibitor by inducing roughness on the surface of crystals. To directly study the effect of Fe-mTA down to the micrometer scale, we study liquid capillary bridges between two macroscopic salt crystals by applying droplets of salt solution with various levels of additives. Scanning electron microscopy and three-dimensional (3D) laser scanning confocal profilometry results show that Fe-mTA produces a surface roughness at the micron scale. This roughness decreases the effective contact area between crystals and promotes the spreading of the liquid bridge; consequently, the formation of a solid bridge between grains with water evaporation is avoided, thus preventing the caking phenomenon and, in addition, preventing adhesion of the crystals to solid substrates.
Caking constitutes a major problem for the flowability, transport, packaging, and consumption of hygroscopic granular crystalline materials such as salt. Sodium chloride is the most abundant salt on the earth and known to form strong lumps, mainly due to cycles of water uptake and water evaporation. We report on a multiscale study of the anticaking effect of the bio-based additive Fe-mTA, a metal-organic complex of iron (III) and meso-tartrate. Drying-deliquescence cycling experiments are performed to reproduce the situation in which the salt undergoes repeated humidity fluctuations. Our results show that Fe-mTA acts as a nucleation promoter and growth inhibitor by inducing roughness on the surface of crystals. To directly study the effect of Fe-mTA down to the micrometer scale, we study liquid capillary bridges between two macroscopic salt crystals by applying droplets of salt solution with various levels of additives. Scanning electron microscopy and three-dimensional (3D) laser scanning confocal profilometry results show that Fe-mTA produces a surface roughness at the micron scale. This roughness decreases the effective contact area between crystals and promotes the spreading of the liquid bridge; consequently, the formation of a solid bridge between grains with water evaporation is avoided, thus preventing the caking phenomenon and, in addition, preventing adhesion of the crystals to solid substrates.
Sodium
chloride (NaCl), commonly known as salt, is an essential
nutrient for life and one of the most abundant minerals on the earth.
Once considered a luxury, salt is nowadays an ordinary material with
a wide range of applications ranging from cooking to large-scale industrial
use. Once produced, salt is stored and transported in different ways
for various applications. For handling purposes, its flowability as
a granular material is of major concern. However, salt is strongly
subject to caking, a phenomenon where individual salt grains agglomerate
together[1] (Figure ) and form big lumps of solid material. This
phenomenon is due to the salt’s hygroscopic properties in combination
with fluctuations in humidity and/or temperature of the environment.
To prevent the caking phenomenon and to prevent crystals from agglomerating,
additives known as anticaking agents are added to the salt.[2,3]
Figure 1
Caked
salt.
Caked
salt.For NaCl, the most widely used
anticaking agent is based on ferrocyanide
or [Fe(CN)6]−4.[2,4,5] The sodium salt in its hydrous form is also known
as yellow prussiate of soda (YPS). To be effective, only 2.5 ppm (equivalent
to 2.5 mg/kg) of YPS is required in salt. However, YPS has important
drawbacks.[5] In the chlorine-alkali industry,
one of the most important industries using sodium chloride, YPS can
enter the membrane electrolyzers and iron deposits as Fe(OH)[3] on or in the membranes and potentially affects
the electrodes. Thus, it may lead to increased power consumption and
a shortened lifetime of membranes and electrodes. Moreover, in electrolyzers,
cyanide is (partially) transformed to the harmful derivative NCl3 that may lead to explosions even at the ppm level in liquid
chlorine. To avoid these disadvantages, a new type of bio-based anticaking
agent has been developed based on tartrate derivatives originating
from grapes processing for the wine industry.[6−8] This additive
is a complexation product between sodium tartrate (with its three
stereoisomers, as shown in Figure ) and iron (III) chloride. Since iron meso-tartrate
is the key functional complex in the additive, the anticaking agent
is called Fe-mTA or mTA. It has been shown to be quite effective even
at low concentrations with an industrial dosing level of only 3 ppm
by weight. It also shows clear advantages in the membrane electrolysis
process. Before entering electrolyzers, the Fe-mTA complex falls apart.
The iron precipitates as Fe(OH)3, which is subsequently
removed by means of filtration. Tartrate is converted into HCl and
CO2 in the electrolyzers and no chlorinated components
are formed.[6] In addition, Fe-mTA is also
biodegradable and cyanide-free.
Figure 2
Stereoisomers of tartaric acid: (a) levo-tartaric
acid (L-TA),
(b) dextro-tartaric acid (D-TA), and (c) meso-tartaric acid (mTA).
Stereoisomers of tartaric acid: (a) levo-tartaric
acid (L-TA),
(b) dextro-tartaric acid (D-TA), and (c) meso-tartaric acid (mTA).Previously, Bode et al.[9,10] studied
the anticaking
mechanism of YPS and Fe-mTA at the molecular level and showed the
dominant mechanism to be a step-pinning phenomenon, where a molecule
of the additive blocks the monoatomic step growth on the surface,
and in this way influences the surface morphology of the growing crystals
at the atomic scale. Townsend et al.[11] suggested
a link between the phenomenon of salt creeping and anticaking. Creeping
is the evaporation-driven extension of crystallites beyond the solution
boundary of a liquid on a solid substrate.[12] It was concluded that the amplitude of creeping can be used as a
good indication of the effectiveness of an anticaking agent. Although
these studies offer important insights into the action of anticaking
agents, they cannot fully explain the mechanism of anticaking itself
at the macroscopic scale.Here, we report on the mechanism of
anticaking of sodium chloride
using Fe-mTA, at a larger scale than molecular ones, by combining
microscopic and macroscopic-scale experiments. We performed several
drying-deliquescence cycles to simulate humidity fluctuations at the
root of the caking phenomenon. On the microscale, the impact of the
anticaking additive on the nucleation of sodium chloride was investigated
via crystallization by evaporating microdroplets of salt solutions
deposited on glass slides followed by multiple deliquescence-drying
cycles. In addition, the impact of the additive as a growth promoter
or inhibitor was determined by small-volume evaporation experiments
in microcapillaries, where controlled precipitation of one (crystal)
nucleus was studied.[13−15] Finally, at the macroscale, the mechanism of anticaking
was determined by performing capillary bridge experiments between
two macroscopic NaCl crystals.
Materials and Methods
Three types
of salt solutions are used:Undersaturated pure NaCl solutions
at a concentration of 5.9 molal;NaCl solutions (5.9 molal)
with Fe-mTA at 80 ppm;NaCl solutions (5.9 molal) with Fe-mTA
at 160 ppm.The Fe-mTA dosage of 80 ppm in solutions corresponds
to typical
industrial dosing levels on the final salt product. Solutions were
prepared using ultrapure Millipore water, NaCl salt of Pharmaceutical
grade with a very low percentage of impurities (Sanal P, purity >
99.9%), and mTA solution, both products provided by Nouryon. The characteristics
of the solutions are summarized in Table . The addition of the mTA at such low concentrations
does not change the physicochemical properties of the salt solution
at 5.9 molal. The surface tension, density, and contact angles on
the glass slide and NaCl crystal are the same for 160 and 80 ppm to
within the experimental accuracy.
Table 1
Physicochemical Properties
of Salt
Solutions Used in This Study
solution
water
NaCl solution 5.95 m
NaCl solution + Fe-mTA (80 ppm)
NaCl solution + Fe-mTA (160 ppm)
density (g/cm3)
1.0193 ± 0.0022
1.197 ± 0.0083
1.1948 ± 0.0051
1.1926 ± 0.0017
surface tension γ (mN/m)
71.86 ± 0.05
80.53 ± 0.15
80.87 ± 0. 15
80.51 ± 0.2
contact
angle on the glass slide θg (°)
N/A
20.4 ± 1.8
19.6 ± 1.7
18.9 ± 2.1
contact angle on the NaCl crystal θc (°)
N/A
12.6 ± 1.5
12.4 ± 1.5
12.5 ± 2.8
Microscopic studies are done by evaporating
aqueous salt solutions
of known initial concentrations, as described in Table , either as droplets (initial
droplet volume ∼0.57 ± 0.08 μL) on cleaned Corning
GlassTM slides or introduced into glass microcapillaries (500 μm
in diameter). By fixing the temperature (T ∼
21 ± 2 °C) and controlling the relative humidity (RH) of
the ambient air in the climatic chamber,[13] the evaporation rate of the solution is controlled. The relative
humidity in our mini-climatic chamber is fixed by introducing an airflow
with a controlled partial water vapor pressure. This is created by
first flowing the air through the water at a given temperature T1 in a water bath thermostat (for drying experiments,
around 9–12 °C depending on the day and the temperature
of the lab). The airflow that is saturated with water vapor at temperature T1 is subsequently conducted to the mini-climatic
chamber at a temperature T2 (∼21
°C: laboratory environment). Consequently, the relative humidity
of the mini-climatic chamber is fixed by the following equationwhere RH
is the relative humidity (%), pw is the
partial vapor pressure, and pws is the
saturated vapor pressure at the laboratory
temperature (2.64 kPa at 21 °C). Since the flowing air is saturated
with water vapor, for example, at 9 °C, the partial vapor pressure
is equal to the saturated vapor pressure at T1(1.26 kPa at 9 °C), and the relative humidity will be
settled at ∼50%. Our system permits us to control a wide range
of relative humidities very precisely; hence, under a phase-contrast
microscope and using direct imaging we investigate the kinetics of
dissolution of crystals in contact with liquid water and also their
deliquescence in contact with water vapor, followed by recrystallization
during the evaporation. Experiments were done with unconfined (droplets
evaporation) or confined geometries (cylindrical microcapillaries
of 500 μm) to investigate the robustness of the results obtained.
Measuring the volume change during evaporation of the solution inside
the microcapillaries allows one to determine the supersaturation at
the onset of precipitation; this is done by recording the displacement
of the two menisci while simultaneously visualizing the onset of crystal
growth in the solution directly with an optical microscope coupled
to a CCD camera.Liquid bridges between mm-scale NaCl crystals
are studied as a
controlled macroscale caking scenario. First, NaCl crystals are grown
for 3 months in Petri dishes by slow evaporation of an initially undersaturated
salt solution to obtain large and very pure crystals. Two crystals
of similar size and perfectly square corners are glued onto two cover
slides, which in turn are attached to a cleaned Corning GlassTM glass
slide using double-sided tape in such a way that the crystals touch
only at their corners (Figure a,b). Salt solution droplets of 1 μL are applied at
the contact point, forming a liquid capillary bridge between the two
crystals (Figure c).
An inverted Leica microscope and three-dimensional (3D) laser scanning
confocal profilometer (Keyence) are used to investigate the drying
of the capillary bridge between the two crystals.
Figure 3
(a) Schematic of the
experiment to study macroscale capillary bridges
between two salt crystals. (b) Photograph of two NaCl crystals touching
at their corners. (c) Liquid capillary bridge formed at the contact
point between the two crystals, after depositing a droplet (1 μL)
of salt solution.
(a) Schematic of the
experiment to study macroscale capillary bridges
between two salt crystals. (b) Photograph of two NaCl crystals touching
at their corners. (c) Liquid capillary bridge formed at the contact
point between the two crystals, after depositing a droplet (1 μL)
of salt solution.
Results and Discussion
Evaporation-Induced
Crystallization
Figure shows the evaporation of droplets
of salt NaCl solutions (5.9 molal) with different Fe-mTA concentrations
(80 and 160 ppm) on cleaned glass slides at RH = 50% and T = 21 °C. With the evaporation of water, the NaCl concentration
increases progressively until the spontaneous precipitation of crystals
in the droplets.[16,17] For all solutions, i.e., with
and without Fe-mTA, the first crystals are formed close to the contact
line at the liquid/air interface.[16] This
nucleation, close to the edge of the droplet, is due to a higher concentration
of the solute near the contact line where evaporation is strongest.
Clearly, the presence of the additive does not affect the location
of the nucleation, i.e., liquid/air interface. For all salt solutions
with and without additives, an inward motion of the crystals toward
the center of the droplet (Figure ) can be observed. With the growth of the crystal,
it becomes confined between the free surface and the solid substrate;
the resulting deformation of the liquid/air interface due to this
geometrical constraint results in capillary forces that push the crystal
toward the center of the drop.[16]
Figure 4
Temporal evolution
of the crystal morphology in drying microdroplets
of pure salt (top row), NaCl + 80 ppm Fe-mTA (middle row), and NaCl
+ 160 ppm Fe-mTA (bottom row).
Temporal evolution
of the crystal morphology in drying microdroplets
of pure salt (top row), NaCl + 80 ppm Fe-mTA (middle row), and NaCl
+ 160 ppm Fe-mTA (bottom row).For the pure salt solution, as expected, a cubic growth of the
crystals is observed after its precipitation (Figure , top row). For salt solutions with Fe-mTA,
the morphology of the crystal is observed that changes with time:
the crystal growth mode starts as cubic at the onset of precipitation,
followed by the emergence of significant surface roughness and the
development of branched patterns (Figure , middle and bottom rows). In addition, in
the presence of Fe-mTA, the crystals do not adhere to the substrate
like the pure salt after complete drying.The supersaturation
levels (m/ms, with ms being the concentration at saturation) reached
at the onset of crystals precipitation for the salt solutions with
and without Fe-mTA were determined by evaporation experiments in microcapillaries
under the same environmental conditions. The high supersaturation
achieved here prior to precipitation in experiments done in such small
volumes compared to bulk crystallization is in good agreement with
the previously reported results.[13,15,18]In addition, the results, summarized in Table , show that there
are no major differences
between the 80 and 160 ppm as the error bars indeed indicate. However,
the difference between the pure salt and salt with m-TA is significant,
which shows the role of m-TA as a nucleation enhancer.
Table 2
Supersaturation (m/ms) Levels at the
Onset of Crystal Precipitation
supersaturation S at nucleation
NaCl solution
1.6 ± 0.03
NaCl solution + 80 ppm Fe-mTA
1.4 ± 0.11
NaCl solution +160 ppm Fe-mTA
1.5 ± 0.08
In microcapillaries, the crystal growth kinetics after
precipitation
show exactly the same behavior as for the evaporating droplets: the
precipitated crystal grows with a cubic shape at the early stages
and after a certain time roughness starts to appear on the faces of
the crystal followed by the development of branched patterns at a
later stage of growth; the higher the additive concentration, the
more branched crystals are formed (Figure ). The fact that the roughness emerges after
a certain time and not at the onset of precipitation at high supersaturation
confirms that the interaction of Fe-mTA with the crystalline faces
occurs at low saturations. This conclusion has practical implications
as it shows that for the additive to be effective, a high level of
purity is not needed, i.e., impurities that could induce heterogeneous
nucleation at low saturation would even induce a faster interaction
of the additives with the crystalline faces.
Figure 5
Snapshots of evaporation-induced
nucleation and growth of sodium
chloride crystals in microcapillaries at RH ∼ 55% and T = 21 °C. Top: pure NaCl solution (5.95 m); bottom:
NaCl solution (5.95 m) + 160 ppm Fe-mTA.
Snapshots of evaporation-induced
nucleation and growth of sodium
chloride crystals in microcapillaries at RH ∼ 55% and T = 21 °C. Top: pure NaCl solution (5.95 m); bottom:
NaCl solution (5.95 m) + 160 ppm Fe-mTA.Because both concentrations of mTA show similar results, in the
rest of the discussion of this manuscript, we have chosen to show
the case of 160 ppm as a clear example of growth behavior in the presence
of mTA. In the microcapillaries, we have studied the growth of cubic
crystals before the emergence of any roughness as a function of time
for all solutions at the same T, RH, and S. The measurements are done along one side of the crystal
in contact with the solution. As seen in Figures and 6, growth is
slowed down by the presence of Fe-mTA. This behavior underlines the
growth inhibitor role of Fe-mTA. Generally, three growth regimes can
be distinguished: first (Regime 1), crystal growth is limited by the
integration of the ions into the crystal face and appears linear in
time; with the consumption of ions and the decrease of supersaturation
(Regime 2), growth becomes diffusion-limited; it is the speed of the
ion diffusion in the solution to reach the crystal surface that limits
the growth in this regime. As would be expected for a diffusion-controlled
growth, a linear relation between the crystal size and the square
root of time is obtained (see the inset of Figure ). However, because the additive impact occurs
at low supersaturation, the growth rate (slope of the curve) in this
regime is larger for the pure salt than for solutions containing Fe-mTA,
confirming again the growth inhibitor role of the additive. Finally
(Regime 3), the crystal growth rate decreases slowly and almost stagnates.
This could be due to anisotropic growth caused by confinement once
the crystal reaches the walls of the capillary.
Figure 6
Growth of cubic crystals
in the unconfined direction as a function
of time for (a) pure salt solutions (two, experiments; red symbols)
and (b) salt solutions with 160 ppm Fe-mTA (two experiments; green
symbols). Data are shown up to the moment that the crystal faces start
to display roughness (after about 120 min). The inset zooms in on
Regime 2, showing crystal growth as a function of the square root
of time; the dashed lines are linear fits, indicative of diffusion-limited
growth.
Growth of cubic crystals
in the unconfined direction as a function
of time for (a) pure salt solutions (two, experiments; red symbols)
and (b) salt solutions with 160 ppm Fe-mTA (two experiments; green
symbols). Data are shown up to the moment that the crystal faces start
to display roughness (after about 120 min). The inset zooms in on
Regime 2, showing crystal growth as a function of the square root
of time; the dashed lines are linear fits, indicative of diffusion-limited
growth.
Deliquescence-Recrystallization
Cycles
To study the
impact of repeated deliquescence-recrystallization cycles, we allow
droplets to dry completely and placed the glass slides with salt crystals
inside a mini-climatic chamber at RH = 90% and T =
21 °C under a microscope. NaCl crystals start to take up water
because they are in an environment above its equilibrium relative
humidity RHeq = 75%, i.e., the deliquescence relative humidity
(DRH). The deliquescence of the precipitated crystals from the previously
dried droplet is allowed to continue until the last crystal is completely
dissolved. The volume of the “new” droplets is found
to be approximately the same as that of the initially deposited droplets.We consider three variables to describe the impact of deliquescence-recrystallization
cycling (Figure ):
(1) The time needed to precipitate the first crystal after a droplet
is deposited on the glass slide in the first cycle or when the mini-climatic
chamber is removed after complete deliquescence in the subsequent
cycles; (2) the number of crystals (nuclei) emerging inside the droplet
during evaporation; (3) the time needed to observe the morphology
transition from cubic to roughened shape in the presence of Fe-mTA.
Figure 7
Crystals
formed after three subsequent crystallization-deliquescence
cycles for a salt solution with Fe-mTA (160 ppm). The number of crystals
and the magnitude of the roughness increase with the number of cycles.
Bars are 250 μm.
Crystals
formed after three subsequent crystallization-deliquescence
cycles for a salt solution with Fe-mTA (160 ppm). The number of crystals
and the magnitude of the roughness increase with the number of cycles.
Bars are 250 μm.The first parameter,
the crystallization time, shows no measurable
dependence on the presence or absence of the anticaking agent. It
depends essentially on the solution, substrate, and environment (temperature
and relative humidity). It is known that with recrystallization, the
number of emerging crystals decreases, as it increases the crystal
purity by rejecting impurities.[19] This
trend is indeed observed in our experiments with pure salt. However,
in the presence of Fe-mTA and independent of the amount of additive,
more crystals appear with deliquescence-recrystallization cycling.
This shows that Fe-mTA acts more as a nucleation promoter with cycling.The role of the Fe-mTA additive as a nucleation promoter is confirmed
by analyzing the time needed to change the morphology of growth. For
the first cycle of drying, this time is significantly longer than
for the following cycles; the average time goes from ∼200 s
in the first cycle to ∼50 s in the third cycle. This can be
explained by the fact that if more crystals precipitate with cycling,
the supersaturation will drop quicker, and consequently, the interaction
of the Fe-mTA leading to rough crystalline faces will be seen earlier.Our results show that cycling will lead to multiple nucleations
with more roughened crystals; consequently, the effect of Fe-mTA is
to make the system evolve toward smaller and rougher crystals with
the number of cycles of deliquescence and drying. This outcome is
important for harnessing the anticaking effect in practice; smaller
crystals are less strongly bonded together since the bridges are smaller,
and salt in practice may undergo many deliquescence-drying cycles.
C-Macroscale Effect of Fe-mTA
To relate our
microscale results with evaporating droplets to the macroscale behavior
of the anticaking effect of Fe-mTA, we perform macroscale capillary
bridge experiments on sets of two macroscopic NaCl crystals in a configuration
as explained in Figure . Figure shows the
drying of the liquid capillary bridges of the pure salt solution and
a salt solution with 160 ppm Fe-mTA. With the evaporation of the pure
salt solution, a solid crystalline bridge is observed to form between
the two grains: this is direct visualization of the caking phenomenon.
The two crystals are linked by a continuous and smooth line in which
further salt crystallization takes the shape of the concave menisci.
In contrast, when the Fe-mTA is added to the salt solution, no crystalline
bridge is formed after the water evaporates from the liquid bridge:
the two crystals do not stick together. However, a clear roughness
starts to form on the crystal surfaces. Quantification of the contact
line as extracted from these snapshots (Figure c) as well as profilometry of the interface
between the crystals (Figure ) confirm the role of the Fe-mTA in preventing crystallization
from solution and in inducing surface roughness instead. Scanning-electron
microscopy (SEM) of the crystal interfaces after repeated application
and evaporation of liquid capillary bridges (Figure ) reveals the roughness in the case of Fe-mTA
to be of a snake scale-like morphology.
Figure 8
(a, b) Photographs
of the capillary bridges at the contact point
of two adjacent crystals after the consecutive deposition of 5 droplets
of pure salt solution (a) and of salt solution with 160 ppm Fe-mTA
(b). Variation of the contact length after consecutive application
of 0–5 droplets of the pure salt solution (two experiments;
yellow symbols) and of a salt solution with 160 ppm Fe-mTA (two experiments;
green). The lengths were determined from photographs such as shown
in (a) and (b), where the red lines indicate the contact lengths.
The different curves show the reproducibility of the experiments.
Figure 9
Microscope image and height profile (along the blue line)
for the
contact between two salt crystals after application of (a) a droplet
of the pure salt solution and (b) salt solution plus 160 ppm Fe-mTA.
Red circles indicate surface roughness not encountered in the case
of the pure salt solution (bar scale = 500 μm).
Figure 10
SEM images of the contact point between two salt crystals after
liquid capillary bridge experiments: (a) droplet of the pure salt
solution results in a solid bridge; (b) droplet of a salt solution
with 160 ppm Fe-mTA does not result in a solid bridge, instead gives
rise to a snake scale-like crystalline surface.
(a, b) Photographs
of the capillary bridges at the contact point
of two adjacent crystals after the consecutive deposition of 5 droplets
of pure salt solution (a) and of salt solution with 160 ppm Fe-mTA
(b). Variation of the contact length after consecutive application
of 0–5 droplets of the pure salt solution (two experiments;
yellow symbols) and of a salt solution with 160 ppm Fe-mTA (two experiments;
green). The lengths were determined from photographs such as shown
in (a) and (b), where the red lines indicate the contact lengths.
The different curves show the reproducibility of the experiments.Microscope image and height profile (along the blue line)
for the
contact between two salt crystals after application of (a) a droplet
of the pure salt solution and (b) salt solution plus 160 ppm Fe-mTA.
Red circles indicate surface roughness not encountered in the case
of the pure salt solution (bar scale = 500 μm).SEM images of the contact point between two salt crystals after
liquid capillary bridge experiments: (a) droplet of the pure salt
solution results in a solid bridge; (b) droplet of a salt solution
with 160 ppm Fe-mTA does not result in a solid bridge, instead gives
rise to a snake scale-like crystalline surface.Our experiments show that the application of Fe-mTA induces a micron-scale
roughness on the crystal surface, which appears as whitening of the
crystalline surface. Such roughness has several consequences: at the
macro scale : first, it helps to spread the liquid over a larger surface
of the crystal and hence reduce the formation of capillary bridges.[20] Second, the formation of such roughness reduces
the contact area between the two macrocrystals, which further suppresses
the caking phenomenon in the subsequent deliquescence-drying experiments.
Moreover, the precipitation of such small crystals makes the surface
mechanically weaker than that of the smooth surface of the pure salt
crystal, causing them to break more easily. All these factors together,
i.e., roughness appearance, smaller contact area, and more brittle
surface, explain the anticaking mechanism of Fe-mTA at the macroscopic
scale. In addition, such roughness not only avoids the caking phenomenon
but also confers antiadhesive properties with respect to other solid
substrates such as glass slides or lab plastic Petri dishes in our
case.
Conclusions
Understanding the mechanism by which the
caking of salt occurs
is critical to devising strategies aimed at preventing it. Crystalline
solids often cake by the formation of liquid bridges by deliquescence
(during periods of high relative humidity) and subsequent recrystallization
of microcrystals from solutions (during dry periods). The formation
of such solid bridges depends on the material’s particle size
and shape and can be influenced by adding anticaking agents. While
some anticaking agents act by absorbing excess moisture or by coating
particles and making them water-repellent, others interact at the
atomic scale with the crystalline grains.Here, we have investigated
the functionality of Fe-mTA, a bio-based
anticaking agent originating from the wine industry, which has previously
been shown to be quite effective even at very low concentrations (ppm)
by weight.Our results show that, at the microscale, Fe-mTA
acts as a nucleation
promoter and growth inhibitor by inducing roughness on the surface
of crystals; this leads to a snake scale-like morphology at the edges
and corners of the crystalline grains at the macroscale. The appearance
of roughness, on the one hand, decreases the effective contact area
between crystals and, on the other hand, improves the spreading ability
of the liquid bridge over the crystalline surfaces. Consequently,
the formation of a macroscopic solid crystalline bridge between grains
as water evaporates is avoided. In this way, a small amount of Fe-mTA
additives not only suppress the caking phenomenon but also gives an
antiadhesive quality to the grains with respect to other solid substrates.We also show that the efficiency of the Fe-mTA anticaking agent
does not require a very clean environment; impurities that induce
heterogeneous nucleation at low supersaturation will induce an even
faster interaction of the additives with the crystalline faces.These findings open new routes on the use of this additive in other
applications such as the food industry, where other types of crystals
are used and can have such caking problems. Also, in the field of
conservation of cultural heritage, salt crystallization in pores of
stones can induce severe damage to artworks due to the development
of the crystallization pressure during the growth in the presence
of thin films of solution,[21,22] the surface roughening
and antiadhesive properties elucidated here could be an alternative
to avoid the development of the crystallization pressure and consequently
reduce damage with salt crystallization in confinement.
Authors: Arno A C Bode; Sanne J C Granneman; Martin C Feiters; Paul Verwer; Shanfeng Jiang; Jan A M Meijer; Willem J P van Enckevort; Elias Vlieg Journal: Dalton Trans Date: 2016-04-21 Impact factor: 4.390