Molecular Mechanics Studies of Montmorillonite Intercalated with Tetramethylammonium and Trimethylphenylammonium

The intercalation of organoammonium cations into smectite structure is the important step in the technology of non-linear optical materials. In this study we investigated the structure of montmorillonite (MMT), intercalated with two organoammonium cations : tetramethylammonium (TMA) and trimethylphenylammonium (TMPA) using molecular mechanics simulations. The studies were focused to following aspects: arrangement of organoammonium cations in the interlayer, their positions and orientation with respect to silicate layers and their anchoring to the layers. The calculated (basal) d-spacings for MMT with TMA 14.29 Å and 15.36 Å for MMT with TMPA are in good agreement with X-ray diffraction data.     

Adsorption of phenol and aniline on natural and organically modified montmorillonite: experiment and molecular modelling

Natural and intercalated Wyoming montmorillonite (MMT) with the tetramethylammonium (TMA) cations were used for the adsorption of phenol and aniline. Laboratory experiments characterised by adsorption isotherms were compared with the results of molecular modelling simulations. Aniline adsorbed itself strongly on MMT; while using the TMA intercalates (TMA-MMT), its adsorption decreased. On the contrary, the adsorption of phenol on TMA-MMT was moderately higher than on the MMT surface. The MMT surface models were described by empirical force field used in molecular mechanics and dynamics. The Burchart–Universal force field was used in the Cerius² modelling environment. The modelling results revealed the important role of water forming a moderately concentrated layer on the pure MMT surface. Water molecules enable the adsorption of aniline on MMT and, on the contrary, repel phenol molecules from MMT. In the case of TMA-MMT, lower amount of water near a silicate layer caused decrease in the aniline adsorption and, on the contrary, increase in the phenol adsorption.     

Interlayer Porosity in Montmorillonite Intercalated with Keggin-like Cation Studied by Molecular Mechanics Simulation

Molecular mechanics simulation using Cerius² modeling environment have been used to investigate the structure of montmorillonite, intercalated with Keggin-like cation⁷⁺. Present work is focused to the strategy of modelling in case of intercalated layered structures and to investigation of structure parameters characterizing the interlayer porosity, that means: the interlayer distance, the position, orientation and distribution of Keggin cations in the interlayer space and the stacking of layers. Molecular simulations revealed the structure of the interlayer and led to the following conclusions: In the most stable configuration the 3-fold axis of Keggin cation is perpendicular to the silicate layer. This orientation of Keggin cations leads to the basal spacing 19.51 (10^-10 m). Energy minimization during the translation of Keggin cation along the silicate layer gives only small fluctuations of basal spacing and no correlation has been found between the shift of cation along the layers and the value of basal spacing. No systematic relationship has been found between the shift of cation and crystal energy and no systematic relationship exists between the mutual shift of two successive layers and the values of basal spacing and crystal energy. Consequently, no two-dimensional ordering of Keggin cations in the interlayer and no regular stacking of layers can be expected. X-ray diffraction diagrams obtained for montmorillonites, intercalated with Keggin cation, confirm present conclusions.     

Surface and interlayer structure of vermiculite intercalated with methyl viologen

Molecular modeling using empirical force field revealed the differences between the surface and interlayer arrangement of the dye guest molecules in vermiculite intercalated with the divalent methyl viologen cation (MV²⁺). Conformation and anchoring of MV²⁺ cations on the silicate layer in the interlayer space of vermiculite host structure is different from that on the crystal surface. A preferential position has been found for the anchoring of guests on the silicate layer. Anyway the arrangement of guests in the interlayer space as well as on the crystal surface exhibits a high degree of disorder due to a certain flexibility in guest molecules arrangement and first of all due to the presence of water molecules in the interlayer space. The presence of water disturbs not only the regularity in guest positions and orientations but also in conformation of guest molecules in the interlayer space of the host structure.     

Molecular Mechanics Simulations in Structure Analysis of Intercalate VOPO4·2CH3CH2OH

Molecular mechanics simulations using Cerius² combined with X-ray diffraction and supported with vibrational spectroscopy have been used to investigate the layered structure of vanadyl phosphate VOPO₄ intercalated with ethanol. This intercalated structure exhibits certain degree of disorder, which affects the diffraction diagram and obstructs the conventional structure analysis based on diffraction methods only. Present structure analysis is focused to the crystal packing in the interlayer space and layer stacking in the intercalate. The bilayer arrangement of ethanol molecules in the interlayer has been found, giving the basal spacing d = 13.21 Å, experimental d-value obtained from X-ray diffraction is 13.17 Å. One half from the total number of CH₃CH₂OH molecules is anchored with their oxygens to VOPO₄ layers to complete vanadium octahedra and their orientation is not very strictly defined. The second half of ethanoles is linked with hydrogen bridges to the anchored etahanoles and sometimes also to the layer oxygens. Positions and orientations of these unachored ethanoles with respect to VOPO₄ layers exhibit certain degree of disorder, resulting in the disorder in layer stacking. Molecular mechanics simulations revealed the character of this displacement disorder in layer stacking and enabled to determine the components of the displacement vector.     

Permeation and inhibition of polycystin-l channel by monovalent organic cations

Polycystin-L (PCL), homologous to polycystin-2 (71% similarity in protein sequence), is the third member of the polycystin family of proteins. Polycystin-1 and -2 are mutated in autosomal dominant polycystic kidney disease, but the physiological role of PCL has not been determined. PCL acts as a Ca-regulated non-selective cation channel permeable to mono- and divalent cations. To further understand the biophysical and pharmacological properties of PCL, we examined a series of organic cations for permeation and inhibition, using single-channel patch clamp and whole-cell two-microelectrode voltage clamp techniques in conjunction with Xenopus oocyte expression. We found that PCL is permeable to organic amines, methlyamine (MA, 3.8 Å), dimethylamine (DMA, 4.6 Å) and triethylamine (TriEA, 6 Å), and to tetra-alkylammonium cation (TAA) tetra-methylammonium (TMA, 5.5-6.4 Å). TAA compounds tetra-ethylammonium (TEA, 6.1-8.2 Å) and tetra-propylammonium (TPA, 9.8 Å) were impermeable through PCL and exhibited weak inhibition on PCL (IC₅₀ values>13 mM). Larger TAA cations tetra-butylammonium (TBA, 11.6 Å) and tetra-pentylammonium (TPeA, 13.2 Å) were impermeable through PCL as well and showed strong inhibition (IC₅₀ values of 2.7 mM and 1.3 μM, respectively). Inhibition by TBA was on decreasing the single-channel current amplitude and exhibited no effect on open probability (NP_o) or mean open time (MOT), suggesting that it blocks the PCL permeation pathway. In contract, TEA, TPA and TPeA reduced NP_o and MOT values but had no effect on the amplitude, suggesting their binding to a different site in PCL, which affects the channel gating. Taken together, our studies revealed that PCL is permeable to organic amines and TAA cation TMA, and that inhibition of PCL by large TAA cations exhibits two different mechanisms, presumably through binding either to the pore pathway to reduce permeant flux or to another site to regulate the channel gating. These data allow to estimate a channel pore size of ∼7 Å for PCL.     

Hydrothermal synthesis and structural investigation of silver magnesium complex of benzenehexacarboxylic acid (mellitic acid), Ag2Mg2[C6(COO)6] · 8H2O with two-dimensional layered structure

Crystal and molecular structure of silver magnesium mellitate, Ag₂Mg₂[C₆(COO)₆] · 8H₂O, was synthesized hydrothermally and characterized by X-ray structure analysis. The complex crystallizes in the monoclinic system, space group P2/n, with unit cell dimensions of a=7.4347(2), b=9.9858(2), c=14.4248(3) Å, β=99.2429(5)°, V=1055.01(4) ų, and Z=2. The structure was solved and refined to R=0.036 (R_w=0.045) for 1707 independent reflections [I_o>2σ(I_o)]. The Ag cations are coordinated by six carboxylic oxygen atoms of mellitate anions with composition of [C₆(COO)₆]⁶⁻ on the (1 0 1) plane; each mellitate anion linking three neighboring Ag distorted trigonal prisms produces a two-dimensional layered structure parallel to (1 0 1). The Mg cations, which are coordinated by four water molecules and two carboxylic oxygen atoms, are intercalated between the two-dimensional layer stacks. The carboxylate group coordinated to Mg and Ag cations serve as a tridentate ligand in that structure. The number of water molecules incorporated into the mellitate compound is controlled mainly by ionic radii of metal cation in the structure. Furthermore, the ionic radii of metal cations in the mellitate compound play an essential role in arrangement of mellitate anions in the structure, whether as a one-dimensional infinite chain, a two-dimensional layered structure, or a three-dimensional framework structure.     

On the mechanism of anion uptake by plant roots

Summary The effect of the valence of the associated cation on Cl^–-uptake by excised barley roots grown in CaSO₄ has been studied at 26°, 6° and 2°C. The uptake of Cl^– relative to that of the associated cation was found to increase in the order: trivalent > divalent > monovalent. This was explained on the expected effect of the cation on the negative charge and potential of root surfaces. A lyotropic order was observed in case of monovalent cations, whereas divalent cations showed no such order. The order observed in Cl^–-uptake from chloride solutions of monovalent cations is associated with the ability of the absorbed cation to remove Ca and Mg from the roots. Li⁺ behaved similar to divalent cations in affecting the relative Cl^–-uptake from LiCl.As to the effect of temperature on the uptake of Cl^– and associated cation, it appears that Cl^– is not taken up to any great extent at 2°C whereas cations are still adsorbed at this low temperature. This has been explained on the assumption of the presence of negative adsorption spots on the root surface which can hold cations but not anions. It appears that Cl^–-uptake by roots requires the expenditure of energy to overcome repulsion arising from the negative surface.This work is supported by AEC contract AT (11-1) — 34 project 55.     

Structure analysis of montmorillonite intercalated with rhodamine B: modeling and experiment

The intercalation process and the structure of montmorillonite intercalated with [rhodamine B]+ cations have been investigated using molecular modeling (molecular mechanics and molecular dynamics simulations), X-ray powder diffraction and IR spectroscopy. The structure of the intercalate depends strongly on the concentration of rhodamine B in the intercalation solution. The presence of two phases in the intercalated structure was revealed by modeling and X-ray powder diffraction: (i) phase with basal spacing 18 A and with bilayer arrangement of guests and (ii) phase with average basal spacing 23 A and with monolayer arrangement of guests. In both phases the monomeric and dimeric arrangement can coexist in the interlayer space. Three types of dimers in the interlayer structure have been found by modeling: (i) H-dimer (head-to-head arrangement) present in the 18 A phase, (ii) sandwich type of the head-to-tail arrangement (present in the 23 A phase) and (iii) J-dimer (head-to-tail arrangement) present in the 23 A phase. Figure Montmorillonite intercalated with rhodamine B cations. On the left: phase 18 A, bilayer dimeric arrangement of guests (H-dimers). On the right: phase 23 A, monolayer arrangement of guests prepared using intercalation solution with a low concentration of rhodamine B     

Saturation transfer electron paramagnetic resonance detection of sickle hemoglobin aggregation during deoxygenation.

In Myxicola axons, substitution of tetramethylammonium (TMA+) for Cs+ alters intramembrane charge movements (gating currents). Although the total charge moved during and following a depolarizing step remains constant, with TMA+ the ON response has additional slower component(s), and the OFF response is retarded. Concommitantly, TMA+ produces the same voltage-dependent block of Na+ inactivation in Myxicola as has been observed in other preparations. At large positive potentials as many as 70% of the Na+ channels fail to inactivate in the steady state. In addition, TMA+ slows Na+ activation, retards the inactivation of those Na+ channels that remain able to inactivate, and decreases the maximum Na+ conductance. The steady-state Na+ conductance induced by internal TMA+ or Na+ is consistent with a scheme in which these internal cations simply modify Na+ channels in an all-or-none fashion so that a fraction become incapable of inactivating.     

Cation diffusion in cartilage measured by pulsed field gradient NMR

In this study, the pulsed field gradient (PFG) nuclear magnetic resonance (NMR) technique was used for the investigation of (1) concentration and compression effects on cation self-diffusion, and (2) restricted diffusion of cations in cartilage. Since physiologically relevant cations like Na+ are difficult to investigate owing to their very short relaxation times, the cations tetramethylammonium (TMA) and tetraethylammonium (TEA) were employed for diffusion studies in samples of explanted cartilage. Results indicated that the diffusion of monovalent cations shows strong similarities to observations already made in studies of the diffusion of water in cartilage: with increasing compression, i.e. decreasing water content, the diffusion coefficient of the cation decreases concomitantly. The diffusion coefficients also showed a decrease with increasing cation concentrations, basically reflecting the corresponding decrease in the water content. Both results could be explained by the well-established model of Mackie and Meares. This, together with the similarity of the diffusion coefficient D in cartilage relative to free solution (about 50%) for both cations, is consistent with the view that the water content and not the charge is the most important determinant of the intratissue diffusivity of monovalent cations. Diffusion studies with increasing observation times showed strong evidence of restricted diffusion, allowing the estimation of the geometry of barriers within cartilage.     

Non-covalent interactions between cations in the crystal structure of [Pt{4′-(p-tolyl)trpy}Cl]SbF6, where trpy is 2,2′:6′,2″-terpyridine, underpin the salt’s complex solid-state luminescence spectrum

The synthesis and characterization of [Pt{4′-(p-tolyl)trpy}Cl]SbF₆ is described where trpy is 2,2′:6′,2″-terpyridine. A single crystal X-ray structure determination at 100 K shows that the cations are stacked in columns that comprise cations arranged in a staircase motif. Successive cations within a column are linked by π(trpy)-π(phenyl) stabilizing interactions; and each cation in one column is linked to a cation in an adjacent column by a weakly stabilizing Pt···Pt interaction. The Pt···Pt distance is 3.434(1) Å. The metrics governing non-covalent interactions between [Pt{4′-(aryl)trpy}Cl]⁺ cations have been analyzed for the present structure and related structures in the CSD (Cambridge Structural Database). Cation dimers cluster into three distinct groups based on their lateral shifts and, to a lesser extent, the angular parameters governing their relative displacements; the dominant grouping exhibits Pt···Pt and π(trpy)-π(trpy) stabilizing interactions. An emission spectrum recorded at 77 K on a solid sample of the compound is best interpreted as arising from the decay of three photoexcited states: a ³MLCT (MLCT = metal-to-ligand charge transfer) state; a ³MMLCT (MMLCT = metal-metal-to-ligand charge transfer) state, and an excimeric ³π-π^∗ state.     

Monovalent cation size and DNA conformational stability

The effect of monovalent cations on the thermal stability of a small model DNA hairpin has been measured by capillary electrophoresis, using an oligomer with 16 thymine residues as an unstructured control. The melting temperature of the model hairpin increases approximately linearly with the logarithm of increasing cation concentration in solutions containing Na(+), K(+), Li(+), NH(4)(+), Tris(+), tetramethylammonium (TMA(+)), or tetraethylammonium (TEA(+)) ions, is approximately independent of cation concentration in solutions containing tetrapropylammonium (TPA(+)) ions, and decreases with the logarithm of increasing cation concentration in solutions containing tetrabutylammonium (TBA(+)) ions. At constant cation concentration, the melting temperature of the DNA model hairpin decreases in the order Li(+) ～ Na(+) ～ K(+) > NH(4)(+) > TMA(+) > Tris(+) > TEA(+) > TPA(+) > TBA(+). Isothermal studies indicate that the decrease in the hairpin melting temperature with increasing cation hydrophobicity is not due to saturable, site-specific binding of the cation to the random coil conformation, but to the concomitant increase in cation size with increasing hydrophobicity. Larger cations are less effective at shielding the charged phosphate residues in B-form DNA because they cannot approach the DNA backbone as closely as smaller cations. By contrast, larger cations are relatively more effective at shielding the phosphate charges in the random coil conformation, where the phosphate-phosphate distance more closely matches cation size. Hydrophobic interactions between alkylammonium ions interacting electrostatically with the phosphate residues in the coil may amplify the effect of cation size on DNA thermal stability.     

Cation distribution,cycling, and removal from mineral soil in Douglas-fir and red alder forests

Overstory species influence the distribution and dynamics of nutrients in forest ecosystems. Ecosystem-level estimates of Ca, Mg, and K pools and cycles in 50-year old Douglas-fir and red alder stands were used to determine the effect of overstory composition on net cation removal from the mineral soil, i.e. cation export from the soil in excess of additions. Net cation removal from Douglas-fir soil was 8 kg Ca ha^–1 yr^–1, 1 kg Mg ha^–1 yr^–1, and 0.3 kg K ha^–1 yr^–1. Annual cation export from soil by uptake and accumulation in live woody tissue and O horizon was of similar magnitude to leaching in soil solution. Atmospheric deposition partially off-set export by adding cations equivalent to 28–88% of cation export. Net cation removal from red alder soil was 58 kg Ca ha^–1 yr^–1, 9 kg Mg ha^–1 yr^–1, and 11 kg K ha^–1 yr^–1. Annual cation accumulation in live woody tissue and O horizon was three times greater than in Douglas-fir, while cation leaching in soil solution was five to eight times greater. The lack of excessive depletion of exchangeable cations in the red alder soil suggests that mineral weathering, rather than exchangeable cations, was the source of most of the removed cations. Nitric acid generated during nitrification in red alder soil led to high rates of weathering and NO₃-driven cation leaching.     

Similarities and differences between organic cation inhibition of the Na,K-ATPase and PMCA

The effects of three classes of organic cations on the inhibition of the plasma membrane Ca pump (PMCA) were determined and compared to inhibition of the Na pump. Quaternary amines (tetramethylammonium, tetraethylammonium, and tetrapropylammonium, TMA, TEA, and TPA, respectively) did not inhibit PMCA. This is not to imply that PMCA is inherently selective against monovalent cations because guanidine and tetramethylguanidine inhibited PMCA by competing with Ca(2+). The divalent organic cation, ethyl diamine, inhibited PMCA but was not competitive with Ca(2+). In contrast, propyl diamine did compete with Ca(2+) and was about 10-fold more potent than butyl diamine in inhibiting PMCA. For the Na pump, both TEA and TPA inhibited, but TMA did not. TEA, guanidine, and tetramethylguanidine inhibition was competitive with Na(+) for ATPase activation and with K(+) for pNPPase activation, both of which are cytoplasmic substrate cation effects. Thus, these findings are consistent with TEA, guanidine, and tetramethylguanidine inhibiting from the cytoplasmic side of the Na pump; in contrast, we have previously shown that TPA did not inhibit from the cytoplasmic side. The divalent alkane diamines ethyl, propyl, and butyl diamine all inhibited the Na pump and all competed at the intracellular surface. The order of potency was ED > PD > BD consistent with an optimal size for binding; similarly, for the quaternary amines TMA is apparently too small to make appropriate contacts, and TPA is too large. Homology models based upon the high-resolution SERCA structure are included to contextualize the kinetic observations.     

Surface charge near the cardiac inward-rectifier channel measured from single-channel conductance

Summary The conductance of a channel to permeable ions depends on the number of ions near the mouth of the pore. Surface charge controls the local concentration, and impermeable cations can modify this charge. Correlating channel conductance with the concentration of impermeable cations therefore determines the local charge near the open pore. This paper presents data from cell-attached patches on embryonic chick ventricle cells, and it uses the conductance of inward-rectifier channels in the patch (in 100mm K, with various concentrations of Na, Ca, Ba, and Mg) to estimate the local surface potential. The results indicate the presence of ionized residues near the mouth of the channel. Using the Boltzmann equation and the Gouy-Chapman relation, the surface potential due to these residues (in 100K/33Na/0Ca/0Ba/0Mg) is –40 mV, and the charge density is –0.25e/nm².     

Divalent Cation Effects on the Shaker K Channel Suggest a Pentapeptide Sequence as Determinant of Functional Surface Charge Density

The effects of the divalent cations strontium and magnesium on Shaker K channels expressed in Xenopus oocytes were investigated with a two-electrode voltage-clamp technique. 20 mm of the divalent cation shifted activation (conductance vs. potential), steady-state inactivation and inactivation time constant vs. potential curves 10–11 mV along the potential axis. The results were interpreted in terms of the surface charge theory, and the surface charge density was estimated to be −0.27 e nm⁻². A comparison of primary structure data and experimental data from the present and previous studies suggests that the first five residues on the extracellular loop between transmembrane segment 5 and the pore region constitutes the functional surface charges. The results further suggest that the surface charge density plays an important role in controlling the activation voltage range. Received: 12 November 1997/Revised: 1 June 1998     

Interaction of alginate single-chain polyguluronate segments with mono- and divalent metal cations: a comparative molecular dynamics study

The interaction of a set of monovalent (Na⁺, K⁺) and divalent (Mg²⁺, Ca²⁺) metal cations with single-chain polyguluronate (periodic chain based on a dodecameric repeat unit, 2₁-helical conformation) is investigated using explicit-solvent molecular dynamics simulations (at 300 K and 1 bar). A total of 14 (neutralising) combinations of the different ions are considered (single type of cation or simultaneous presence of two types of cation, either in the presence or absence of chloride anions). The main observations are: (1) the chain conformation and intramolecular hydrogen bonding is insensitive to the counter-ion environment; (2) the binding of the cations is essentially non-specific for all ions considered (counter-ion atmosphere confined within a cylinder of high ionic density, but no well-defined binding sites); (3) the density and tightness of the distributions of the different cations within the counter-ion atmosphere follow the approximate sequence Ca²⁺>Mg²⁺>K⁺～Na⁺; (4) the solvent-separated binding of the cations to the carboxylate groups of the chain is frequent, and its occurrence follows the approximate sequence K⁺>Na⁺>Ca²⁺>Mg²⁺ (contact-binding events as well as the binding of a cation to multiple carboxylate groups are very infrequent); and (5) the counter-ion atmosphere typically leads to a complete screening of the chain charge within 1.0–1.2 nm of the chain axis and, for most systems, to a charge reversal at about 1.5 nm (i.e. the effective chain charge becomes positive at this distance and as high in magnitude as one-quarter of the bare chain charge, before slowly decreasing to zero). These findings agree well (in a qualitative sense) with available experimental data and predictions from simple analytical models, and provide further insight concerning the nature of alginate–cation interactions in aqueous solution.     

Cation-selective Pathway of OmpF Porin Revealed by Anomalous X-ray Diffraction

The OmpF porin from the Escherichia coli outer membrane folds into a trimer of β-barrels, each forming a wide aqueous pore allowing the passage of ions and small solutes. A long loop (L3) carrying multiple acidic residues folds into the β-barrel pore to form a narrow “constriction zone”. A strong and highly conserved charge asymmetry is observed at the constriction zone, with multiple basic residues attached to the wall of the β-barrel (Lys16, Arg42, Arg82 and Arg132) on one side, and multiple acidic residues of L3 (Asp107, Asp113, Glu117, Asp121, Asp126, Asp127) on the other side. Several computational studies have suggested that a strong transverse electric field could exist at the constriction zone as a result of such charge asymmetry, giving rise to separate permeation pathways for cations and anions. To examine this question, OmpF was expressed, purified and crystallized in the P6₃ space group and two different data sets were obtained at 2.6 Å and 3.0 Å resolution with K⁺ and Rb⁺, respectively. The Rb⁺-soaked crystals were collected at the rubidium anomalous wavelength of 0.8149 Å and cation positions were determined. A PEG molecule was observed in the pore region for both the K⁺ and Rb⁺-soaked crystals, where it interacts with loop L3. The results reveal the separate pathways of anions and cations across the constriction zone of the OmpF pore.     

Modelling of Aniline-Vermiculite and Tetramethylammonium-Vermiculite; Test of Force Fields

Molecular mechanics simulations in Cerius² have been used for modelling vermiculite intercalated with tetramethylammonium and aniline cations. The published structure data obtained for these intercalated structures from X-ray single crystal diffraction have been used to test the force fields and modelling strategy for organo-clays. The strategy of modelling was based on the nonbond host-guest interactions and on rigid silicate layers and rigid guest species. The rigidity of silicate layers requires that the cell parameters a, b and % are kept fixed during the energy minimisation. The energy term was set up using the nonbond interaction terms only and the Crystal Packer module in Cerius² has been used for the energy minimisation. In Crystal Packer the rigid units, i.e. the silicate layers and guest species can be translated and rotated during energy minimisation and the cell parameters c, !, and # have been varied. Three sets of Van derWaals (VDW) parameters available in Crystal Packer: Tripos, Universal and Dreiding have been used in present molecular simulations. Ab initio MP2 calculations were performed to justify the application of the force field. The best agreement of molecular mechanics simulations with both: experimental and ab initio data was obtained with the Tripos VDW parameters for both intercalates. The results of modelling are in good agreement with the experimental data as to the cell parameters and the interlayer packing. The cell parameters reported by Vahedi-Faridi and Guggenheim (1997) for tetramethylammonium-vermiculite are: c = 13.616 Å, ! = 90°, # = 97.68° ; from the present modelling we obtained: c = 13.609 Å, ! = 90.19°, # = 97.56°. Tetramethylammonium-cations are arranged in one layer in the interlayer space. One C-C edge of NC₄ tetrahedra is perpendicular to the silicate layers. The deep immersion of the methyl groups into the ditrigonal cavities suggested by Vahedi-Faridi and Guggenheim was not confirmed by modelling. Slade and Stone (1984) presented the measured cell parameters for aniline vermiculite: c = 14.89 Å, ! = 90°, # = 97°; present result is: c = 14.81 Å, ! = 90.72°, # = 96.70° for partially exchanged vermiculite and c = 14.84 Å, ! = 90.53°, # = 97.17° for fully exchanged vermiculite. The aniline cations are positioned over the ditrigonal cavities alternating in their anchoring to lower and upper silicate layer. The C-N bonds are perpendicular to layers.