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Anais da Academia Brasileira de Ciências

Print version ISSN 0001-3765On-line version ISSN 1678-2690

An. Acad. Bras. Ciênc. vol.72 n.1 Rio de Janeiro Mar. 2000

http://dx.doi.org/10.1590/S0001-37652000000100006 

Intercalation Compounds involving Inorganic Layered Structures

 

VERA R. L. CONSTANTINO, CÉSAR A. S. BARBOSA, MARCOS A. BIZETO and PATRÍCIA M. DIAS

Departamento de Química Fundamental, Instituto de Química, Universidade de São Paulo
Cx. Postal 26077 - 05513-970 São Paulo, SP, Brazil

Manuscript received on September 8, 1999; accepted for publication on September 15, 1999;
presented by JOSÉ M. RIVEROS

 

 

ABSTRACT

Two-dimensional inorganic networks can shown intracrystalline reactivity, i.e., simple ions, large species as Keggin ions, organic species, coordination compounds or organometallics can be incorporated in the interlayer region. The host-guest interaction usually causes changes in their chemical, catalytic, electronic and optical properties. The isolation of materials with interesting properties and making use of soft chemistry routes have given rise the possibility of industrial and technological applications of these compounds. We have been using several synthetic approaches to intercalate porphyrins and phthalocyanines into inorganic materials: smectite clays, layered double hydroxides and layered niobates. The isolated materials have been characterized by elemental and thermal analysis, X-ray diffraction, surface area measurements, scanning electronic microscopy, electronic and resonance Raman spectroscopies and EPR. The degree of layer stacking and the charge density of the matrices as well their acid-base nature were considered in our studies on the interaction between the macrocycles and inorganic hosts.
Key words: intercalation compounds, layered double hydroxides, smectite clays, layered niobates.

 

 

1 INTRODUCTION

Solid state inclusion chemistry involves almost exclusively inorganic host-guest compounds. Nanoporous inorganic hosts as zeolites and clays can incorporate simple cationic ions, large ionic species as Keggin ions, organic ions or molecules, coordination compounds or organometallics. Considering two-dimensional inorganic networks, graphite and clays were the first layered hosts having the intracrystalline reactivity explored in academic and technological works (Lagaly & Beneke 1991). The interest in the intercalation process increased considerably after 1960 and have included other classes of layered materials as, for example, metal(IV) phosphates and phosphonates, transition metal dichalcogenides, transition metal oxyhalides, alkali-transition metal oxides and hydrotalcite-type anionic clays (Alberti & Costantino 1996).

The attention given to intercalated layered compounds can be attributed mainly to the fact that the host - guest interaction often changes significantly their chemical, catalytic, electronic, optical and mechanical properties. The isolation of materials with interesting properties and use of soft chemistry routes have given rise to the possibility of industrial and technological applications of intercalated compounds as components in electrochemical devices (batteries, sensors etc.) and as heterogeneous catalysts (Alberti & Costantino 1996). Concerning the occurrence of selective chemical reactions in the interlayer region of inorganic hosts containing reactive guest species, transition metal complexes of macrocyclic ligands as porphyrins and phthalocyanines (synthetic models that mimic natural enzymatic systems) have been intercalated and evaluated for catalytic purposes (Rives & Ulibarri 1999, Chibwe et al. 1996, Ukrainczyk et al. 1995, Bedioui 1995). Some studies have shown that the confinement of these reactive species into two-dimensional frameworks can improve their catalytic activity and durability.

We have been using several synthetic approaches to intercalate macrocycle species into inorganic layered materials (cationic clays, layered double hydroxides and layered niobates). The intercalated solids have been characterized by elemental and thermal analysis, X-ray diffraction (XRD), surface area measurements, scanning electronic microscopy, electronic (absorption and emission) spectroscopy, resonance Raman spectroscopy and EPR. The degree of layer stacking and the charge density of the inorganic matrices as well as their acid-base nature were considered in our studies concerning the interaction between macrocyclic species and the inorganic hosts. Some details about the layered structures and some data obtained in our research work are presented as follow.

The clay minerals are a class of lamellar solids that have a remarkable ability to adsorb or intercalate cationic or neutral molecules between the layers. Their structure consists of tetrahedra and octahedra sheets, joined together by sharing oxygen atoms (Mott 1988). The most common structure for cationic clays is based on a octahedral sheet sandwiched between two tetrahedral sheets (TOT layers), as shown in Fig. 1. The substitution of structural cations by others with lower valency leaves a charge deficiency on the layers, neutralized by species adsorbed or located in the interlayer region. The first studies concerning porphyrin adsorption on clays were stimulated by the fact that these macrocycles are the most important biological markers in sediments and sedimentary rocks (Bergaya & Van Damme 1982).

 

\begin{figure}\centerline {\epsfxsize=7.2cm\mbox{\epsfbox{figure1.eps}}} \end{figure}
Fig. 1 - Schematic representation of a 2:1 layered silicate intercalated with a cationic meso-substituted porphyrin (TMPyP).

 

We have studied the interaction between some smectite clays and tetramethylpyridylporphyrins (free base, TMPyP, and the cobalt complex, CoTMPyP). K10, KSF and Swy2 are naturally occurring montmorillonites while Syn1 is a synthetic one. FHT and Laponite are synthetic hectorites (in FHT, the hydroxyl groups are substituted by fluoride). The clay samples investigated show some different structural parameters as the cation exchange capacity (CEC), the occupancy of octahedral sites (di- or trioctahedral minerals) and kind of layer aggregation (face-to-face, edge-to-face). All the clay samples containing porphyrins were prepared by ion exchange reaction in a water suspension.

The basal spacing data obtained for all the clay samples saturated with TMPyP (d001 ~ 14 — 15Å), except for FHT, suggest a flat orientation of the porphyrin ring relative to the host layers, as can be seen in Fig. 1. The higher CEC of FHT compared to the CEC of all the other layered silicates causes the TMPyP intercalation in a tilted orientation (d001 ~ 18Å). K10 and KSF samples saturated with TMPyP are green while the FHT one is brown. Diffuse reflectance spectra of these samples show that the Soret and Q bands are red shifted after interaction with the clays when compared to the free TMPyP or the protonated form (H2TMPyP). The bands at ca. 430 and 468 nm in the clays electronic spectra were assigned to non-protonated and protonated TMPyP, respectively. Resonance Raman data support this attribution and also showed the v2 mode (ca. 1550 cm-1) to be the most sensitive peak to protonation. In the electronic spectra of FHT containing 10, 50 and 100% of CEC balanced by CoTMPyP, the bands are red shifted even when a small amount of porphyrin is used, suggesting that the electronic levels of the macrocycle are more affected by the interaction with the clay than by orientation or possible porphyrin distortions in the gallery region. The resonance Raman spectra obtained for the CoTMPyP samples present only minor shifts in peak positions and band width (Dias et al. 1998).

Layered double hydroxides (LDHs, also named hydrotalcite-type anionic clays) are another class of layered inorganic host that have been used in the intercalation chemistry area. LDHs present the general formula

\begin{displaymath} \hbox{[M{${}^{\hbox{\scriptsize II}}$}(${}_{1-x}$)M{${}^{\h... ...tsize III}}$}${}_x$(OH)${}_2$](A$^{n-}$)${}_{x/n}$.zH${}_2$O} \end{displaymath}

where MII and MIII represent di and trivalent cation octahedrally coordinated to hydroxyl ions and An- is the interlayer anion. These octahedra are connected to each other by edge sharing to form an infinite sheet. LDHs and their calcined products have been used as catalysts and catalyst supports in organic synthesis; environmental adsorbents and/or anionic exchangers; precursors to synthesize advanced ceramics; modified electrodes and in the pharmaceutical and medicine area (Trifirò & Vaccari 1996).

To evaluate the catalytic properties of LDHs intercalated materials, we have intercalated cobalt(II) tetra(4-sulfonatophenyl)porphyrin (CoTPhsP) and cobalt(II) tetrasulfophthalocyanine (CoPcTs) into a LDH of hydrotalcite-type and also supported these macrocycles on the external surface of the LDH (CO2-3 occupies the interlayer region). The intercalated compounds were synthesized through three methods: (i) double hydroxide coprecipitation in the presence of the macrocycle, (ii) structure reconstruction of the mixed oxides obtained by thermal decomposition of LDH phase containing volatile ion; (iii) thermal decomposition of carbonate-containing phase in a polyol media. The effect of the materials textural properties and the macrocycle arrangement in the LDH interlayer region was evaluated by carrying out the hydrogen peroxide decomposition reaction (catalase-like activity) (Barbosa 1999).

The macrocycle intercalation between LDHs layers was confirmed by XRD data: the basal spacing of the carbonate precursor (d003 ~ 8Å) increases to approximately 23Å in the hosts intercalated with phthalocyanine or porphyrin. The surface area data suggested that the macrocycle intercalated solids have no microporous. LDHs samples intercalated with CoPcTs seem to be aggregated in the interlayer space taking into account the diffuse reflectance spectra profile. The characterization data suggest that the plane of macrocycles were perpendicular to the plane of the LDH layers and closely packed into interlamelar space as shown in Fig. 2.

 

\begin{figure}\centerline {\epsfxsize=7.2cm\mbox{\epsfbox{figure2.eps}}} \end{figure}
Fig. 2 - Schematic representation of a layered double hydroxide intercalated with an anionic metallophthalocyanine (MPcTs). Open circles = OH groups; dark circles = metal ions.

 

The confined metallated macrocycle compounds showed catalase-like activity. However, the catalytic activity of the intercalated materials was distinct for each macrocycle system tested. The kinetic curves for molecular oxygen evolution in the hydrogen peroxide dismutation reaction (pH 7.8 and T=30oC) showed that CoTPhsP in homogeneous media was partially deactivated while the immobilized one (heterogeneous condition) was more active during the whole reaction time. It should be pointed out that the porphyrin is stabilized in the presence of hydrogen peroxide when it is immobilized in LDH. Unlike CoTPhsP, the pure phthalocyanine species in homogeneous or heterogeneous media are not degraded by H2O2 (pH 9.6 and T=30oC). The LDH-immobilized phthalocyanine exhibited better catalytic performance than the free macrocycle.

Layered niobates have a semiconducting character that have been explored to achieve the water splitting to H2 by photocatalysis and to promote photoinduced electron transfer process between the host and intercalated guest species (Ogawa & Kuroda 1995). Incorporation of bulky ions into the interlayer space of niobates is not easy to perform due to their high layer charge densities. We have reported for the first time a synthetic procedure to intercalate macrocycle species (TMPyP, in the case) into a KNb3O8 derivative host (Bizeto et al. 1999). The porphyrin intercalation into the layered material containing potassium ions or even in its H+-exchanged form does not occur. The proposed method is based on the expansion of the interlayer region through an acid-base reaction between the proton exchanged form of the matrix and an n-butylamine.

The calculated formula for the porphyrin intercalated compound was

\begin{displaymath} \hbox{[TMPyP]${}_{0.14}$H${}_{0.44}$Nb${}_3$O${}_8$.2.5H${}_2$O} \end{displaymath}

based on elemental and thermogravimetric analysis. The basal spacing variation (Dd020) of 14.3Å is consistent with an inclined orientation of the macrocycle relative to the host lamellar plane. Fig. 3 shows a schematic representation of the porphyrin intercalated compound.

 

\begin{figure}\centerline {\epsfxsize=7.2cm\mbox{\epsfbox{figure3.eps}}} \end{figure}
Fig. 3 - Schematic representation of the layered niobate [Nb3O8]- intercalated with a cationic meso-substituted porphyrin (TMPyP). Squares represent [NbO6] octahedral units (distortions are not shown).

 

XRD pattern of TMPyP confined into the layered niobate shows only the (0k0) peaks which could indicate the occurrence of an exfoliation process when the n-butylamine intercalated material was stirred in water. We can propose that the stirring step provokes the solid delamination and the formation of colloidal particles that upon contact with the TMPyP solution, causes the layer stacking to incorporate the guest species.

The electronic absorption spectrum of the TMPyP intercalated sample showed that the Soret and Q bands practically were not shifted when compared to the spectrum of the macrocycle in water. This result indicates that TMPyP is not protonated in the interlayer region as has been observed in studies with smectite clays. Resonance Raman spectrum also corroborates the assumption of the presence of the non-protonated species in the host structure.

Good results have also been obtained using the synthetic method above described to intercalate TMPyP into the K4Nb6O17 layered host or into the layered perovskite series of general formula

 

ACKNOWLEDGMENTS

We are grateful to Profs. Ana Maria da Costa Ferreira and Dalva Lúcia Araújo de Faria (Instituto de Química - USP) for the fruitful discussions and collaboration. The financial support and fellowships from Fapesp and CNPq are also acknowledged.

 

REFERENCES

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Correspondence to:
Vera R. L. Constantino
E-mail: vrlconst@quim.iq.usp.br

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