# Near-Stoichiometric Adsorption of Phosphate by Silica Gel Supported Nanosized Hematite

Authors: L. I. Gromadskaya; I. V. Romanova; O. A. Vyshnevskyi; S. A. Kirillov
Journal: ISRN Inorganic Chemistry
 (2013)

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## Abstract

Decreasing the size of oxide particles to nanoscale enables one to ensure maximal reaction rates and depths in the solid due to the enhancement of the specific surface area and the increase of the diffusion rate caused by shortening diffusion paths. For that reason, one may suggest that in the case of adsorption onto nanoparticles, the complete conversion of sorbents to stoichiometric compounds would become possible. Adsorption of phosphate ions onto nanosized hematite supported on silica gel surface has been studied. Modification of silica gel surface by hematite in the quantity of 0.62 and 1.25 mass% has been carried out by means of a citric acid aided method. The morphology of the samples obtained has been characterized using DTA, XRD, SEM, and low temperature desorption of nitrogen. It has been found in batch experiments that unlike natural and synthetic hematites, for which the limiting adsorption values do not exceed 14 mg/g, silica gel supported nanosized hematite adsorbs 400–2000 mg of the phosphate ions per gram, thus forming near-stoichiometric iron phosphates on the surface of the support. The degree of conversion of hematite to iron phosphates is greater in acidic media and at a lower surface coverage, when hematite crystallites are small and better accessible by adsorbate.


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## Body

## 1. Introduction

Numerous metal oxides are capable of absorbing inorganic and organic contaminants and due to this ability they are widely used as scavengers of toxic impurities. Advances in nanoscale science and engineering have raised hopes that many of the current problems involving water quality could be resolved or greatly ameliorated using nanosorbents, nanocatalysts, nanostructured catalytic membranes, and nanoparticle-enhanced filtration techniques resulting from the development of nanotechnology [1]. Decreasing the size of oxide particles to nanoscale enables one to ensure maximal reaction rates and depths in the solid due to the enhancement of the specific surface area and the increase of the diffusion rate caused by shortening diffusion paths [1, 2]. For that reason, one may suggest that in the case of adsorption onto nanoparticles, the complete conversion of sorbents to stoichiometric compounds would become possible. However, in spite of these striking benefits, the direct application of nanosized oxides in dynamic sorption is out of question in view of enormous hydraulic resistances of nanopowders. Therefore, studies in the field of nanoadsorptives can be divided into two major areas. The first area includes the works describing potentialities of nanoparticles themselves and the second deals mainly with nanocomposites.In the first area, better understanding of physicochemical aspects of adsorption on oxide nanoparticles, as well as their impact on the fate of environmental pollutants that adsorb onto them in aqueous and biologically relevant media has been achieved in batch studies [3]. In particular, dependences of sorption on grain size have been obtained for a few materials, including iron oxides [4–7], titania [8–12], and clay minerals [13, 14]. With a few exceptions [7, 8, 10], a conclusion has been drawn that the adsorption affinity increases as the particle size decreases.In the second area, significant efforts are directed towards the synthesis of composites where nanosized adsorbents are either incorporated into a polymeric matrix [15, 16] or deposited onto the surface of a support [17]. Such composites are prospective for practical applications in fixed-bed process units or in flow-through systems like permeable barriers [18]. Much works in this field deal with iron oxides especially active towards phosphorus and arsenic compounds containing in aqueous media [19]. These compounds are notorious toxicants, and their presence in drinking water at concentrations exceeding certain (quite low) limits produces numerous diseases [17, 19–21]. As supports for nanosized iron oxides, polymers [22, 23] and inorganic substances, for example, sand [24], concrete [25], or activated carbon [26] are used and high uptakes of phosphates and arsenates are attained.According to batch studies mentioned above, no evidences regarding the complete conversion of sorbents to stoichiometric compounds have been obtained yet. In order to prove the possibility of such phenomenon, a combination of approaches peculiar to both areas of nanoadsorptive studies seems favorable. Potentialities of nanoparticles in adsorption processes are largely obscured by phenomena like aggregation and agglomeration of nanopowders, precipitates, or sediments probed in batch experiments [4–14]. Deposition of small amounts of nanoadsorbents onto the surface of a support could be helpful in avoiding this complication.Silica could be a prospective support for various oxides. Mechanical stability, great specific surface area, and high reaction ability of silanol (≡Si–O–H) groups allowing for surface modification are usually put forward as advantages of this support [28]. Surface modification by organic or inorganic substances as well as by metal complexes enriches silica with high hydrolytic and thermal stability and enhances its adsorption selectivity towards atypical ions [29–31].In this paper, our primary aim was to examine the ability of nanosized iron oxide to the complete conversion to stoichiometric iron phosphates in the course of adsorption from aqueous solutions. To do so, we performed an attempt to deposit a nanolayer of iron oxide onto the surface of a commercial silica gel. Owing to silanol groups, silica demonstrates mainly cation exchange function, and the absence of anion exchange ability of silica is especially advantageous for studies of modifiers demonstrating their anion exchange function (like iron oxides), since concurring adsorption of anions onto the support is of no value in this case. In order to perform surface modification of silica, instead of more common and sometimes more difficult methods (treatment by metal alkoxides in water-free organic solvents and subsequent calcination [32, 33] and impregnation by solutions of metal salts [33]), we used a citric acid aided route already employed in our papers [34–37] for obtaining nanosized metal oxides. We supposed that an acidic citrate compound [35–37] formed by a reaction between an iron salt and citric acid should be bound to silanol groups and after a thermal treatment should produce one of the iron oxides. It was found that in our case, the oxide in question was Fe2O3 (hematite). Modified silica gel samples were tested as sorbents for phosphate ions from solutions of various acidities. It appeared that, as expected, the hematite layer deposited onto the silica gel surface can be almost completely converted to iron phosphates.


## 2. Materials and Methods

Granulated fine-pored technical silica gel (KSMG, GOST 3956-76 [38], Makrokhim, Ukraine) was used as a support. Samples were washed and dried during 2 h at 120°C and 2 h at 210°C; their specific surface area was determined as 480 m2/g. Since according to data sheets [38] fine-pored technical silica gels may contain admixtures of other oxides, first of all, alumina, the chemical analyses of the support for aluminum and iron content were performed according to the existing standards [39–41]. It should be mentioned that procedures described in these standards practically coincide with those recommended by ASTM [42]. In particular, the analysis of the support was made according to [39–41] by means of back complexometric titration after dissolution of samples in a mixture of sulfuric and hydrofluoric acids. It showed the absence of ferric oxide and the presence of 5.0% of aluminum oxide.The initial modifier solution contained equimolar amounts of ferric chloride FeCl3·6H2O and citric acid (p. a., no additional purification). Based on the studies of adsorption of Fe3+ ions on silica gel (see below), the concentrations of Fe3+ in working modifier solutions were set to 1.26 g/L (0.023 mol/L) and 14 g/L (0.25 mol/L) and adjusted by dilution. The impregnation of silica gel was made by means of 4 h shaking and 24 h of static contact; solid : liquid = 1 : 100.In order to find the decomposition temperature of ferric citrate formed in the modifier solution, which determines the conditions of the thermal treatment of impregnated silica gel samples, this salt was synthesized accordingly [35–37]. Specifically, the modifier solution was evaporated at 80−90°C until a viscous dark-brown resin was formed and left overnight. Heating the resin at ca. 120°C gave an acidic citrate (precursor). Its decomposition was studied by means of thermal analysis (Q-1500, MOM, Hungary) and X-ray diffractometry (DRON UM-1, LOMO, Russia, Co-Kα, λ = 1,79283 Å).Specific surface areas and pore size distributions for initial and modified silica gels were obtained from nitrogen adsorption/desorption curves (NOVA 2200e, Quantachrome, USA). A Nova Win 2.0 software was employed for calculations. Specific surface areas and total pore volumes were found using the BET method. To acquire the volume of mesopores and micropores, BJH and DFT methods, respectively, were utilized. The morphology of the modified samples was studied by means of scanning electron microscopy (JSM-6700F, JEOL, Japan).The amount of ferric compound on the surface of silica gel (ferric citrate in the case of impregnation of silica gel or ferric oxide in the case of modified silica gel samples) was determined by means of a colorimetric procedure with o-phenantroline [43] after the alkaline fusion of samples (a KFK-2 colorimeter, UKL, Russia).pH titrations by NaOH and HCl (I-160 M, IT, Belorus) were performed in 0.1 M background solutions of sodium chloride (solid : liquid = 1 : 100) 4 h shaking and one day of static contact. Sorption studies were performed in batch experiments. Sorption of ferric citrate from the modifier solution was examined by the amount of ferric oxide on silica gel. Sorption of phosphate ions was determined using solutions of Na2HPO4·2H2O as a source of phosphate ions. Proper pH values were maintained by means of HCl solutions. In these studies, 1 g of the sorbent was added to 10 mL of solution. This gives the solid : liquid ratio of 1 : 10 and the ratio of the mass of ferric oxide on the surface of the sorbent to the volume of solution of 1 : 161 for sample A and 1 : 80 for sample B (see later). Resulting mixtures were shacked for 4 h, and left for 1 day, after which the sorbents were removed by means of filtration and the phosphate content in filtrates was determined colorimetrically by the vanadium phosphomolybdate (vanadate colorimetry method) [44]. The adsorption capacity values A (mg/g) were calculated as
(1)A=(C0-Ceq.)×V×1000m,
where C0 and Ceq. are the concentrations of the adsorbate in mg/L in initial and equilibrium solutions, respectively, V is the volume of the solution in mL, and m is the mass of the sorbent in g.


## 3. Results and Discussion

In order to deposit a prescribed amount of the modifier onto the surface of the support, the study of adsorption of Fe3+ ions on silica gel from modifying solutions was performed. The data obtained are shown in Figure 1. Respective concentrations of working modifying solutions chosen for further experiments are denoted by arrows. It was expected that using the modifying solutions containing 1.26 and 14 g/L of Fe3+ one should obtain the samples containing such amounts of iron oxide on the surface that differ approximately twice.Figure 1
Dependence of adsorption of Fe3+ onto initial silica gel on its concentration in modifying solution. Arrows show the concentrations of working modifying solution chosen for further experiments.As another preliminary stage of the work, a single iron oxide was obtained by means of the citric acid method mentioned above, and its identification was performed. The minimal temperature required for the thermal decomposition of the precursor was determined by means of the thermal analysis. Precursors of other oxides demonstrate several stages of thermal decomposition including endothermic removal of physisorbed and hydrate water and exothermic crystallization of a citrate salt, both occurring in the region of 100–150°C, and exothermic decomposition (burning up) of the acid radical and formation of a target oxide taking place at 250–400°C [35–37]. In the case of the precursor studied, two first thermal effects are weak and hardly distinguishable resulting in the DTA curve dominated by a strong exothermic effect (250–400°C) corresponding to the burning process. After this effect, formation of an iron oxide is completed and no additional mass losses take place.As the decomposition products, several iron oxides should be considered, namely, magnetite Fe3O4, maghemite γ-Fe2O3, and hematite α-Fe2O3. Furthermore, it should be taken into account that massive samples of maghemite are fully transformed into hematite at ~500°C [45]. On the other hand, hematite is stable if its grain size exceeds 30 nm and transforms to maghemite upon subdivision [46].In order to distinguish between possible varieties of iron oxides formed upon the thermal decomposition of citrate precursors, a sample treated at 400°C for 1 h was analyzed by means of X-ray diffractometry. Its diffraction pattern (Figure2) contains the peaks characteristic of hematite (JCPDS 16-0895). This means that the decomposition reaction leads to the formation of hematite having the grain size of >30 nm. Calculations using the Scherrer equation [47] support this statement leading to the size of crystallites of 50 nm.Figure 2
X-ray diffraction data for iron oxide obtained by the treatment of the citrate precursor at 400°C for 1 h.After these preliminary works, two samples of silica gel impregnated in modifying solutions of different concentrations were obtained, pretreated, and calcined for 1 h at 400°C, as in the case of single iron oxide obtained from the citrate precursor. These samples of modified silica gel were denoted as A and B. Their alkaline fusion and subsequent analysis show the amount of Fe2O3 as 6.2 mg/g for the A sample and 12.5 mg/g for the B sample, respectively.The results of porosity studies of the initial sample and sample B (for samples A and B these are almost the same) are presented in Figure3 as isotherms of nitrogen adsorption/desorption (a) and pore size distributions (b) and summarized in Table 1. These isotherms are characteristic of silica gels and, according to the IUPAC classification [27], belong to the IV type and have H2 type hysteresis loops. For sample B, the isotherms are situated higher than those for the initial sample thus indicating greater pore volume. Specific surface areas for modified samples are greater than those for the initial sample. Upon modification, the total pore volume increases, whereas the mean pore radii are not changing significantly.Table 1
Porosity data for initial and modified silica gels.
Sample
S
sp.
1 m2/g
V
total
1,cm3/g
V
meso
2,cm3/g
V
micro
1,2,cm3/g
Microporefraction,Vmicro/Vtotal,%
r
mean
1,nm
r
BJH
2, nm
Initial
480
0.403
0.380
0.023
5.7
1.68
1.77
A
484
0.393
0.368
0.025
6.36
1.62
1.66
B
536
0.420
0.229
0.190
45.5
1.57
1.72
1By BET.
2By BJH.Figure 3
Nitrogen adsorption/desorption isotherms (a) and pore size distributions obtained in terms of the DFT method for initial(1) and modified (2) silica gels.Analyzing the pore size distributions calculated according to the BET and BJH methods (Table1), it was found that in all samples, mesopores of approx. 1.7 nm radii prevail, and modification decreases their volume (Vmeso). For sample B, such a decrease amounts at ca. 25%. At the same time, both the specific surface area Ssp. and the total pore volumeVtotal found according to the BET procedure either remain almost unchanged (sample A) or increase (sample B). To explain this conflicting result based on calculations in terms of the BET and BJH methods, a hypothesis was put forward regarding the presence of micropores in modified samples (their amount can be estimated as Vtotal-Vmeso=Vmicro) and the data of other pore size calculation methods were applied. In fact, data treatment in terms of microporosity sensitive t, DR, and DFT methods reveals the presence of micropores in the samples studied. A representative pore size distribution curve obtained using the DFT method is given in Figure 3(b) demonstrating that modification leads to a decrease of the number of big pores and appearance of small pores of 0.5 and 1.25 nm radii. Since this feature is more characteristic of the sample B containing a greater amount of iron oxide on the surface, one can suggest that the oxide layer deposited onto the silica gel surface is not uniform and possesses cracks and micropores [48].Knowing the amount of iron oxide deposited onto silica gel and being based on the porosity data, one can speculate regarding the degree of coverage of the surface. Consider sample B for clarity. Hexagonal crystals of hematite belong to theD3d6-R3-c space group, Z=6, a=0.504nm, c=1.377nm [49], and their density is 5.25 g/cm3. If the crystals are set up on their basal planes (the c axis is directed upwards), a monocrystalline layer of hematite of 12.5 mg mass will occupy the area of 1.73 m2. This is clearly insufficient for the complete coverage of the surface of support. Furthermore, covering the surface of the pores of silica gel (rmean≈1.7nm) with a crystalline monolayer of iron oxide of 1.377 nm thickness will lead to their complete filling and disappearance, which does not hold. Therefore, one can consider that iron oxide covers just the apparent surface of the spherical granules of silica gel, whose size is ~5·10-4m2/g, and the thickness of such a solid coverage cannot exceed 4.76 mkm, or 3500 monocrystalline layers of the oxide. It has been mentioned earlier that for such dimensions, the stable phase of iron oxide is hematite. Similar conclusions are applicable for sample A where the mass of hematite and the thickness of the coverage is twice smaller.This conclusion agrees with the literature data regarding the composition of iron oxide phases existing on modified silica. Let us say that  X-ray diffraction patterns of thermally treated samples obtained by sol-gel coprecipitation of mixtures of tetraethoxysilane and ferric chloride (30 mass %) up to 600°C are blank, and only heating at 900°C gives evidence of diffraction peaks corresponding to hematite [50]. Fumed silica impregnated with ferric acetylacetonate and thermally treated at 300°C (the total amount of iron oxides in target products varies from 7 to 70 mass %) contains crystalline phases of maghemite and magnetite. Heating at 600°C reveals the presence of hematite, and its fraction grows on rising temperature [32].In Figure4, SEM micrographs of the support and samples A and B are shown. These manifest clear difference in morphologies of noncoated and coated silica gels. It is well seen at 60000 times magnification that the bare silica gel exhibits a characteristic structure of the surface (Figure 4(a)), whereas in sample A, this structure is not seen due to the presence of coating (Figures 4(b) and 4(c)). Two different kinds of particles forming this coating are discernible. Some of them are of an indefinite shape and the size of approximately 100 nm (Figure 4(b)). In other regions of the surface (Figure 4(c)), aggregates of flat particles are observed.Figure 4
SEM micrographs. Support (a) and sample A at 60000 times magnifications ((b) and (c)) and sample B at various magnifications ((d)–(f)).In the case of sample B, coating becomes even more evident. It is seen at 10000 times magnification that the oxide layer is not homogeneous and contains separated crystals having the hexagonal habit characteristic of hematite [51] (representative examples of clearly hexagonal single crystals are denoted in Figure 4(c) by circles) and the islands of a crystalline crust. Investigations of chippings at 7000 times magnification demonstrate that big crystals can germinate from the thin crust of the iron oxide (Figure 4(d), right upper corner, the light-colored part of image). Upon cracking the sample, some of bigger crystals are falling down and adhere to the chippings (right lower corner, light-colored grains against a dark background). Studies at 60000 times magnification (Figure 4(f), cf. with the micrographs of the support and sample A presented in Figure 4 at the same magnification) enable one to measure the size of the big crystals (up to 800 nm height and 400 nm thickness) and to estimate the width of the crystals forming the crust (ca. 50 nm). Probably, gaps and slits between the crystals in the crust are seen in porosity studies as micropores.pH titration data (Figure5) reveal that initial silica gel samples in alkaline media display cation exchange functions possessing 2.0 mM/g of exchangeable protons. Modified silica gels in alkaline media retain this function. In sample A, the amount of exchangeable protons does not change, whereas in sample B it reaches 9.2 mM/g. In acidic media, initial silica gel samples manifest anion exchange function (2.5 mM/g). According to the literature data [52–54], this is unusual for silica gel and can be explained by the presence of alumina in it. In modified samples, the anion exchange function decreases and becomes equal to 1.0 mM/g, probably reflecting a surface blocking caused by the oxide.Figure 5
pH titrations (a) and dependence of adsorption capacity (b) on pH for initial silica gel and modified samples.Before adsorption studies with modified silica gels, dissolution of the hematite layer in solutions of various acidity was determined and a special examination of the affinity of initial silica gel and hematite for phosphate ions was performed. The solubility of the coating in solutions of pH = 4, 6, and 8 after their contact with samples for 24 h does not depend on pH and is negligible: less than 1% of iron oxide deposited onto the silica gel surface passes into the solution. It was found that initial silica gel samples do not adsorb phosphate ions from alkaline media, and adsorption from acidic media appeared insignificantly small. Hematite obtained by means of the citric acid route forms colloidal solutions, and studies of its affinity towards phosphate ions were unsuccessful. However, the literature data obtained with a number of hematites of different origin reveal that at pH~5-6, limiting adsorption(A∞) of phosphate ions onto natural hematites (14 samples) lies between 0.6 and 11 mg/g with the mean value of A∞=3.5 mg/g [55]. Similar values for 43 samples of synthetic hematites are 0.4–14 mg/g with the mean value of A∞=5.1 mg/g [56].The dependence of phosphate sorption by modified sorbents on the acidity of solutions evidences (Figure6) that in acidic media sorption is small and the maximum of the phosphate uptake is situated in the pH region where the initial silica gel shows up no anion exchange properties or behaves as a cation exchanger. At pH from 2 to 9, for sample A, the quantity of phosphate adsorbed equals 6–13.5 mg per 1 g of the sorbent, which amounts at 950–2150 mg of PO43- per 1 g of hematite. For sample B, these values are 5–8 mg/g and 400–650 mg/g.Figure 6
Dependence of adsorption capacity on pH for modified silica gel samples. Sample A (a):C0=5.6 g/L and sample B (b):C0=5.99 g/L.Based on these data, adsorption isotherms were obtained at pH = 4 and 8 (Figure7). Their treatment was performed using the Langmuir equation
(2)A=A∞KCeq.1+KCeq.,
where A is the adsorption value in mg/g obtained at the equilibrium concentration of the sorbate Ceq., g/L, A∞ is the limiting adsorption value in mg/g, and K is a constant measured in L/g. Respective values of A∞ and K for samples A and B are summarized in Table 2. As expected, limiting values of the phosphate ion adsorption onto hematite supported on silica gel are at least two orders of magnitude greater than those for natural and synthetic hematites [55, 56]. It should be mentioned, however, that saturation of the sorbent takes place much faster than the Langmuir equation predicts, being especially pronounced in the case of sample A, for which the calculated Langmuir dependencies do not completely match the experimental points (Figure 7). On the one hand, this makes the Langmuir fits tentative; on the other hand, fast saturation of the sorbent may be indicative for mechanisms other than adsorption, namely, for precipitation of ferric phosphates.Table 2
Parameters of the Langmuir equations and Fe3+ : PO43- molar ratio for adsorbates.
Sample
A
∞, mg/g
K, L/g
A
max
., mg/g
Fe
3
+ : PO43- molar ratio on the surface
Per 1 gof the sorbent
Per 1 gof hematite
Per 1 gof the sorbent
Per 1 gof hematite
pH= 4
A
14.57
±
1.03
2345
±
166
3.57
±
1.28
12.2
1964
1 : 1.66
B
9.28
±
0.46
742
±
37
0.59
±
0.14
8.4
672
1 : 0.56
pH= 8
A
5.57
±
0.37
897
±
60
4.13
±
1.53
5.2
837
1 : 0.70
B
6.51
±
0.28
521
±
22
0.19
±
0.02
5.2
416
1 : 0.35Figure 7
Phosphate adsorption isotherms at pH = 4 and 8 for samples A and B.Knowing the adsorption values attained at the maximal concentrations of solutions and expressed in mg ofPO43- per 1 g of hematite, one can find the maximal Fe3+ : PO43- molar ratios on the surface of modified samples (Table 2). They are quite close to the Fe3+ : PO43- ratios in stoichiometric compounds; therefore, it is reasonable to claim the complete conversion of hematite and the formation of single ferric phosphates (or their mixtures) on the surface of silica gel. It is noticeable that the degree of conversion of hematite to iron phosphates is greater in acidic media and at a lower surface coverage, when hematite crystallites are small and better accessible by adsorbate.There are two possible explanations of such a behavior of the samples studied. Firstly, some authors have already drawn attention to the existence of common (competitive) and specific (selective) adsorption sites on the surface of hematite crystals [57]. As follows from recent studies [58], such selective sites may be associated with low coordinated Fe atoms on the {104} facets of hematite (reflections from planes parallel to this facet are the most intense in XRD data, Figure 2). Flat hematite crystals forming the developed {104} facets, like those discernible for sample A, Figure 4(c), are especially active towards the oxygen atoms of phosphoryl groups [58] and significantly differ from ordinary hematite particles, sample B, Figures 4(d)–4(f), formed by (001) basal planes and (012) side planes [51]. Based on this observation, different affinities of samples A and B towards phosphate ions are due to differences in the morphology of deposited hematite particles.Secondly, the degree of conversion of Fe2O3 to a respective phosphate is determined by the rate of diffusion of the PO43- ions into the bulk of the oxide crystal. In its turn, the diffusion rate depends on the charge of the crystal surface. The point of zero charge of hematite lies at pH = 7.85±1.34 [52–54]. This means that the formation of Fe2(HPO4)3 in acidic media proceeds easily since the surface of hematite at pH = 4 is charged positively. On the other hand, the formation of basic phosphates is difficult since at pH = 8, the surface of hematite is charged negatively, thus preventing from diffusion of both phosphate and hydroxyl ions. These circumstances may explain the greater degree of conversion of hematite to phosphate at lower pH of solutions.Speaking about the dependence of the degree of conversion on acidity, one should bear in mind that in solutions of different pH, different anionic forms of phosphate dominate:H2PO4- at pH = 4-5 and HPO42- at pH = 8.5–9.5 [59]. However, in systems containing Fe3+ anions, precipitation of salts of different phosphate anions takes place at pH values much lower (i.e., in more acidic media) than the region of existence of respective anionic forms: for instance, Fe2(HPO4)3 (Fe3+:PO43-=1:1.5) precipitates at pH~2 [60] and FePO4 (Fe3+:PO43-=1:1) at pH~6.5 [61] (Figure 8). Therefore, one can consider that compounds formed on the silica gel surface contain a less acidic anion than that existing in an equilibrium solution. Guidelines for determining the composition of such compounds, in addition to Fe2(HPO4)3 and FePO4, can be found in mineralogy.Figure 8
pH influence on dominance of anionic forms of phosphate in solutions, precipitation of ferric phosphates, and Fe3+ :  PO43- ratio in phosphates formed on the silica gel surface.Among ferric phosphate minerals, in the order of decreasing theFe3+:PO43- ratio and simultaneous increasing the Fe3+:OH- ratio, various basic phosphates are known [62] (Table 3). One can guess that for sample A, where the size of hematite particles is small and their inner parts are more accessible, hematite deposited onto the silica gel surface at pH = 4 converts mainly to Fe2(HPO4)3 and at pH = 8 to tinticite Fe4(HPO4)3(OH)3·5H2O, ferristrunzite Fe3(PO4)2(OH)3·5H2O, or their mixture. For sample B with greater hematite particles, the composition of compounds formed is probably the same, and the lowering of the Fe3+:PO43- ratio is caused by the presence of some excess hematite remaining due to low accessibility of its bulk.Table 3
Natural ferric phosphates [27] ordered according to Fe3+ : PO43- : OH− ratio.
Fe3+ : PO43- : OH− ratio
Chemical formula
Name
1 : 0.75 : 0.75
F
e
4
(
P
O
4
)
3
(
OH
)
3
·
5
H
2
O
Tinticite
1 : 0.66 : 1
F
e
3
(
P
O
4
)
2
(
OH
)
3
·
5
H
2
O
Ferristrunzite  (or allanpringite)
1 : 0.66 : 1.33
NaF
e
3
(
P
O
4
)
2
(
OH
)
4
·
2
H
2
O
Cyrilovite
1 : 0.5 : 1.5
F
e
4
(
P
O
4
)
2
(
OH
)
6
·
4
–
6
H
2
O
Delvauxite


## 4. Conclusions

In this paper, an attempt to deposit a nanolayer of iron oxide onto the surface of silica gel has been performed, and the ability of this deposit to complete conversion to stoichiometric iron phosphates in the course of adsorption from aqueous solutions has been examined. Modification of silica gel surface by iron oxide in the quantity of 0.62 and 1.25 mass % has been carried out by means of a citric acid aided method. It has been found that the covering layer consists of hematite.The morphology of the samples obtained has been studied using low temperature desorption of nitrogen and scanning electron microscopy. As follows from micrographs, hematite covers just the apparent surface of silica gel and does not penetrate its pores. At a low coverage, the coating is represented by flat particles of an indefinite shape and the size of approximately 100 nm. At a high coverage, big crystals of 800 nm height and 400 nm thickness are growing on the surface of silica gel.These differences in morphology determine the ability of hematite layer to adsorb phosphates from aqueous solutions. As expected, all samples studied are able to be almost completely converted to iron phosphates. On the other hand, the degree of conversion of hematite to iron phosphate appears greater (i) in acidic media than in neutral solutions and (ii) at a lower coverage than at a higher one, and these circumstances require explanations. The pH dependence of the degree of conversion can be described in terms of electrostatics. The role of coverage can be understood accounting for the shape and size of hematite crystals. Different habit of the crystals leads to different affinity of their facets towards phosphate ions. The bulk of bigger crystals formed at a high coverage is less accessible to phosphate ions.In acidic media (pH = 4), hematite deposited onto the silica gel surface converts mainly toFe2(PO4)3 and in almost neutral solutions (pH = 8), to basic phosphates, like tinticite Fe4(PO4)3(OH)3·5H2O, ferristrunzite Fe3(PO4)2(OH)3·5H2O, or their mixture. However, this conclusion should be considered tentative, and its confirmation will require some additional investigations of adsorbents and adsorbates by means of vibrational spectroscopy [63, 64] that are now in progress.To summarize we conclude that, in line with [4–6, 9, 11–14], the adsorption affinity nanosized adsorbents increases as the particle size decreases; furthermore, the adsorption of phosphate ion onto hematite deposited onto the silica gel surface leads to the complete conversion to stoichiometric iron phosphates.



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