1Biomimetic synthesis of silica nanospheres depends on the aggregation and phase separation of polyamines in aqueous solution
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Biomimetic synthesis of silica nanospheres depends on the aggregation and phase separation of polyamines in aqueous solution
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Long-chain polyamines extracted from the highly siliceous cell walls of diatoms are known to precipitate silica nanospheres from aqueous, silicic-acid containing solutions at near-neutral pH in vitro.
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The same is true for synthetic polyamines such as polyallylamine.
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In the present contribution we show that the microscopic phase separation of polyallylamine in aqueous solution is strictly correlated with the silica precipitation activity of polyallylamine/silicic acid solutions.
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Multivalent anions such as phosphate or sulfate efficiently induce this microscopic phase separation.
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At higher anion concentrations, macroscopic phase separation occurs.
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In contrast to the multivalent phosphate and sulfate ions, the monovalent chloride ions are much less efficient in polyallylamine aggregate formation.
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Introduction
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Diatom cell walls are outstanding examples for nanoscale structured materials in nature.1
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They consist of an amorphous composite material containing silica as well as certain biomolecules.
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The latter are assumed to play a crucial role in diatom cell wall formation.
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Both these classes of molecules were also shown to precipitate silica from aqueous solutions containing silicic acid in vitro.
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The precipitates formed by the long-chain polyamines from S. turris consist of nanospheres exhibiting a surprisingly narrow size distribution.
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The particle diameter was shown to be strictly controlled by the concentration of phosphate ions added to the solutions.4
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Initial NMR and dynamic light scattering experiments carried out on long-chain polyamines isolated from S. turris have shown that these molecules self-assemble in aqueous solutions.4
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Silaffins from C. fusiformis behave very similarly.5
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It is tempting to speculate that the aggregates (droplets) formed by the biomolecules in solution act as templates during cell wall formation.
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A model based on phase separation processes could be developed which explains the pattern formation in diatom cell walls.6
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Inspired by these observations, a number of synthetic amino acids, peptides, and polyamines were shown to precipitate silica from aqueous solutions as well.7–11
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New opportunities for the so-called biomimetic silica synthesis are likely to arise from these discoveries.
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One particularly interesting example is polyallylamine (PAA), a commercially available compound.
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It exhibits a long-chain structure similar to the polyamines found in diatoms.
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Type: Background |
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The topic of the present paper is the detailed physico-chemical characterisation of PAA in aqueous solution especially with respect to the question whether or not an aggregation of the PAA molecules is a prerequisite for their silica-precipitating function as it is the case for the above-mentioned biomolecules extracted from diatoms.
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Experimental
Materials
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Polyallylamine hydrochloride (PAA) was purchased from Aldrich.
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The PAA molecule exhibits a repeated unit (ru) of the following structure: [–CH2CH(CH2NH2˙HCl)–]n with n ∼ 160 corresponding to a molecular weight of ca. 15 kDa.
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NMR and dynamic light scattering experiments
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NMR spectra were acquired on a DMX-500 spectrometer (Bruker, Karlsruhe, Germany) operating at 500 MHz 1H resonance frequency.
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The calibration of the 31P NMR spectra was performed using H3PO4 (85%) as an external reference.
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Dynamic light scattering (DLS) experiments were carried out on a MALVERN HPPS5001 nanosizer.
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For the NMR and dynamic light scattering analyses, the polyallylamine hydrochloride was dissolved in millipore water.
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A concentration of 1 mM PAA was chosen.
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The desired concentration of orthophosphate ions (Pi) was obtained by the addition of the corresponding amount of sodium dihydrogen phosphate to the samples.
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The final pH value was adjusted to 5.8 by the addition of NaOH.
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Sulfate containing samples were prepared by the addition of sodium sulfate and chloride containing samples by the addition of sodium chloride.
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Before the measurements, all solutions were allowed to equilibrate for at least 2 days.
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In vitro precipitation of silica and SEM analysis
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For the silica precipitation experiments, a freshly prepared solution of 1 M tetramethoxysilane in 1 mM HCl was incubated at 20 °C for 15 min and immediately used as a source of monosilicic/disilicic acid.12
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A typical precipitation assay contained in 50 µl: 0.2 mM polyallylamine and phosphate (5 to 25 mM).
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Silica formation was initiated by the addition of 2 µl silicic acid, prepared as described above.
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After 12 min at 20 °C, precipitated silica was collected by centrifugation (4 min, 12.000 rpm).
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The precipitate was washed twice with water, then suspended in water, applied to an aluminium sample holder, and air dried.
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Silica precipitates were analyzed without sputter-coating with a LEO1530 field-emission scanning electron microscope equipped with energy dispersive X-ray analysis (EDXA, Oxford Instruments).
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Colorimetric determination of silica precipitates was performed by the molybdenum blue method12 after dissolving precipitated silica in 20 µl 2 M NaOH (85 °C, 5 min).
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Results and discussion
The influence of phosphate ions
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Fig. 1 summarizes the results of silica precipitation experiments carried out for samples containing various amounts of phosphate.
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The amount of silica precipitated from the PAA/silicic acid solution is plotted as a function of the phosphate concentration.
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Silica precipitation takes place only above a threshold value of ca. 0.3 [Pi]/[ru].
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Below, no silica precipitates at all indicating a crucial role of the phosphate ions.
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It is interesting to note in this context that the PAA-induced silica precipitation experiments described by Patwardhan et al9. were carried out in a phosphate-containing buffer solution.
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Furthermore, the particle diameter of the silica nanospheres precipitated by PAA is correlated with the phosphate concentration in complete analogy to the observations made for the long-chain polyamines extracted from S. turris.4
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The maximum particle diameter of ca. 3 µm strongly exceeds the maximum value of about 1 µm obtained for the polyamines from S. turris.4
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A possible explanation for this behaviour is the much smaller size of the polyamines from S. turris (1.55 kDa molecular weight).
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On the other hand, the particles precipitated by the synthetic polyallylamine exhibit a much broader size distribution than the nanospheres obtained by using polyamines from S. turris.
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In order to understand this behaviour, we have studied aqueous PAA solutions of various phosphate concentrations by dynamic light scattering (see Fig. 2).
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In the absence of phosphate, aggregates of an average diameter of about 1 nm could be detected.
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For a single PAA molecule, one would expect a diameter of the same order of magnitude.
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This leads to the conclusion that the PAA molecules exist as single molecules (monomers) or small clusters in the absence of phosphate ions.
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Addition of phosphate results in a continuous but slow increase of the aggregate diameter up to about 5 nm at 0.25 [Pi]/[ru].
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Note, that this phosphate concentration is close to to the above-mentioned threshold value of ca. 0.3 [Pi]/[ru] necessary for silica precipitation.
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A rapid increase of the aggregate diameter is observed beyond this threshold value.
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At 0.31 [Pi]/[ru], aggregates of about 120 nm diameter could be detected.
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Visual inspection shows that the samples become cloudy at this concentration which confirms the existence of larger aggregates (see Fig. 3).
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If the phosphate concentration is further increased, the samples remain cloudy up to about 0.5 [Pi]/[ru].
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DLS measurements show that the aggregate diameter increases up to almost 600 nm at 0.44 [Pi]/[ru] while a decreased value could be found at 0.5 [Pi]/[ru].
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Obviously, this amount of polyamine already sediments at the bottom of the sample without forming a visible separate phase.
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The decreased concentration of polyamine in the top part of the sample must be responsible for the decreasing diameter of the aggregates.
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At 0.63 [Pi]/[ru] and higher concentrations, the samples become clear after equilibration but exhibit a macroscopic phase separation: A separate phase containing the polyamine is formed at the bottom of the tube.
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The aqueous phase on top does no longer contain a detectable amount of polyamine aggregates.
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The observed aggregation and phase separation can be explained by the attractive electrostatic interactions between the positively charged polyamine molecules and the negatively charged phosphate ions13 and/or the formation of hydrogen bonds.
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Comparison of Figs. 1 and 2 shows that the formation of the described large polyamine aggregates, i.e., microscopic phase separation is correlated with the capability of the system to precipitate silica from a PAA/silicic acid solution.
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If, however, macroscopic phase separation takes place, i.e. for phosphate concentrations significantly exceeding 0.5 [Pi]/[ru], the solution looses its silica precipitation activity.
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That means, microscopic phase separation is a necessary prerequisite for silica precipitation by the polyamine solution.
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In order to characterize the physico-chemical properties of this microscopically phase separated solution in more detail, extended 31P and 1H NMR spectroscopic studies were carried out.
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For all samples, only one single 31P signal is observed.
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The chemical shift, δ, as well as the linewidth, Δν1/2, (full-width-at-half-maximum) of this signal, however, change.
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The chemical shift is plotted as a function of phosphate concentration in Fig. 4 (top).
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It remains almost constant up to about 0.3 [Pi]/[ru].
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Beyond this phosphate concentration, δ continuously decreases.
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At phosphate concentrations higher than 0.6 [Pi]/[ru], that means in the range of macroscopic phase separation, the chemical shift is again nearly constant and amounts to ca. 1.2 ppm.
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From the observation that only a single signal is observed for all concentrations it is concluded that phosphate ions interacting with the polyamine rapidly exchange with free phosphate ions (on the time scale of NMR spectroscopy).14,15
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The increased and constant chemical shift at low phosphate concentrations indicates that phosphate is preferentially bound to the polyamine molecules up to about 0.3 [Pi]/[ru].
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Above this concentration, an increasing amount of free phosphate exists which results in the described decrease of chemical shift.
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The linewidth of the 31P NMR signals (Fig. 4, bottom) also exhibits an interesting behaviour.
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From an initial value of about 4 Hz it increases up to about 12 Hz for 0.4 [Pi]/[ru].
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At higher concentrations, Δν1/2 decreases until a constant value of 1.6 Hz is found for the aqueous part of the macroscopically phase-separated samples.
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This behaviour can be explained as follows: Due to the rapid exchange between phosphate bound to the polyamine aggregates and free phosphate, an average linewidth is observed.14,15
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It is known from the chemical shift analysis that the phosphate ions are preferentially bound to the polyamine aggregates at low phosphate concentrations.
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The linewidth, therefore, corresponds to the linewidth in the polyamine-bound state for low phosphate concentrations.
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Since an increasing aggregate diameter (see Fig. 2) results in a lower correlation time of rotational diffusion, an increasing linewidth is expected for increasing phosphate concentrations.
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This is in agreement with the experimentally observed behaviour up to 0.4 [Pi]/[ru] (Fig. 4, bottom).
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For concentrations above 0.4 [Pi]/[ru], the influence of the increasing amount of free phosphate is observed.
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Since the linewidth of free phosphate is smaller than that of polyamine-bound phosphate, the measured average linewidth then decreases with increasing phosphate concentration.
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After macroscopic phase separation took place, only free phosphate exists in the NMR samples giving rise to the small and constant linewidth of 1.6 Hz observed for high phosphate concentrations.
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The influence of sulfate and chloride ions
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The influence of sulfate and chloride ions upon aqueous solutions of PAA was also investigated.
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The behaviour of sulfate, another multivalent anion, turned out be very similar compared to phosphate: The solutions become cloudy at about 0.3 [sulfate]/[ru] and exhibit macroscopic phase separation above 0.5 [sulfate]/[ru].
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This behaviour shows that the ability to phase-separate aqueous PAA solutions must not be considered to be a specific property of phosphate ions.
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It is striking that both, phosphate and sulfate are multivalent anions.
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The question arises whether or not monovalent anions such as chloride can also be used to induce the described effects.
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Fig. 5 shows the diameter of the polyamine aggregates determined by dynamic light scattering as a function of chloride ion concentration.
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Obviously, aggregates of increasing diameter are observed at increasing chloride concentrations.
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However, even for the highest chloride concentration (ca. 20 [Cl]/[ru]), the obtained aggregate diameter of ca. 9 nm is almost two orders of magnitude smaller than the maximum aggregate diameter of ca. 600 nm observed for a phosphate concentration of only 0.44 [Pi]/[ru].
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It is furthermore important to note that the macroscopic phase separation found for phosphate and sulfate does not occur for chloride ions even at about 20 [Cl]/[ru].
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That means, the monovalent chloride ions are much less efficient in attracting the PAA molecules compared to the multivalent phosphate and sulfate ions.
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In agreement with these observations, no silica is precipitated at all from the chloride-containing PAA solutions even at chloride concentrations up to ca. 20 [Cl]/[ru] which is far beyond the physiologically relevant level.
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In summary, it can be stated that microscopic phase separation is necessary for the PAA-induced silica precipitation from silicic-acid containing aqueous solutions.
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This microscopic phase separation can be induced by the addition of multivalent anions such as phosphate or sulfate to the aqueous solutions.
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Polysilicic acid molecules may be adsorbed on and/or dissolved in the polyamine microdroplets thereby forming a coacervate which hardens by silica formation.
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