Specific features of absorption of Cu<Superscript>2+</Superscript>, Zn<Superscript>2+</Superscript>, Co<Superscript>2+</Superscript>, and Pb<Superscript>2+</Superscript> cations from aqueous solutions by calcium phosphates

Kinetic characteristics of the interaction of trisubstituted calcium phosphate Ca₃(PO₄)₂ · xH₂O with Cu²⁺, Zn²⁺, Co²⁺, and Pb²⁺ ions in aqueous solutions were studied.     

Phosphoryl transfer from phenyl and 4-nitrophenyl phosphates in aprotic and protic solvents : Amine catalysis and formation of oxyphosphorane and metaphosphate intermediates

The behavior of 4-nitrophenyl dihydrogen phosphate, ArOPO₃H₂, and of its tetra-n-butylammonium and tetramethylammonium salts, ArOPO₃H^?R₄N⁺, ArOPO₃^2?2(R₄N⁺), was studied in aprotic solvents, in the absence and in the presence of increasing amounts of alcohols or water. The reactions were investigated in the absence of amines, and in the presence of hindered and unhindered amines, diisopropylethylamine and quinuclidine. The course of the reactions was followed at 35° or at 70° by ³¹P and ¹H NMR spectrometry. Values for the approximate half-times of the reactions were estimated (± 25 %) from the times at which reactant signal intensity becomes equal to product signal intensity. The mononitrophenyl ester transfers its phosphoryl group to alcohols and water from the diprotonated acid by the addition-elimination mechanism via oxyphosphorane intermediates, and from the monoanion and dianion by the elimination-addition mechanism via the monomeric metaphosphate intermediate, PO₃^?. Formation of PO₃^? is faster from dianion than from monoanion in acetonitrile and in alcohol solutions. Conversely, PO₃^? is generated at a faster rate from monoanion than from dianion in aqueous solution. This effect results from a decrease in the rate of formation of PO₃^? in the solvent series: acetonitrile > alcohols > water. The rate depression as a function of the medium is greater for the dianion than for the monoanion, and is attributed to greater solvation of the more polar phosphate ground state than of the less polar transition state in the more polar protic solvents. Unhindered amines add to 4-nitrophenyl phosphate monoanion, but not to the dianion. The oxyphosphorane intermediate thus formed collapses to aroxide ion and a protonated dipolar phosphoramide which is rapidly deprotonated by the relatively basic 4-nitrophenoxide: ArOPO₃H^? + CH(CH₂CH₂)₃N(acetonitrile ? CH(CH₂CH₂)₃N⁺P(O)(OH)O^? + ArO^?? CH(CH₂ CH₂)₃N⁺PO₃^2?+ ArOH → CH(CH₂CH₂)₃N + PO₃^?. The postulated formation of PO₃^? by this route explains why the addition of quinuclidine to an acetonitrile solution containing the monoanion salt, ArOPO₃H^?R₄N⁺, and t?BuOH produces t-butyl phosphate at a faster rate than the addition of diisopropylethylamine to the same solution. 2,4-Dinitrophenyl phosphate, which was previously studied by the same techniques, reacts via oxyphosphorane intermediates from the diprotonated and the monoanion forms, and via monomeric metaphosphate, from the dianion form.     

Na2Co(H2PO4)4·4H2O

In the title compound, disodium cobalt tetrakis­(dihydrogen­phosphate) tetrahydrate, the Co^II ion lies on an inversion centre and is octahedrally surrounded by two water molecules and four H₂PO₄ groups to give a cobalt complex anion of the form [Co(H₂PO₄)₄(OH₂)]^2?. The three‐dimensional framework results from hydrogen bonding between the anions. The relationship with the structures of Co(H₂PO₄)₂·2H₂O and K₂CoP₄O₁₂·5H₂O is discussed.     

Kinetics of H+/Na+ Ion Exchange on H1 ± xZr2 − xMx(PO4)3 (M = Y or Nb) NASICON Materials

The thermodynamic parameters of ion exchange have been estimated for HZr₂(PO₄)₃ · H₂O and the products of its aliovalent doping. Ion exchange occurs via formation of the (H₃O_{1 ? x}Na_x)Zr₂(PO₄)₃ solid-solution series. As in the case of ion exchange on layered zirconium phosphate (Zr(HPO₄)₂ · H₂O), the interdiffusion coefficient and the major interfacial defect generation processes are considerably affected by the contact-solution pH.     

Beiträge zum thermischen Verhalten und zur Kristallchemie von wasserfreien Phosphaten XXXII [1] Neue Orthophosphate des zweiwertigen Chroms — Mg3Cr3(PO4)4, Mg3, 75Cr2, 25(PO4)4, Ca3Cr3(PO4)4 und Ca2, 00Cr4, 00(PO4)4

Contributions on Crystal Chemistry and Thermal Behaviour of Anhydrous Phosphates. XXXII. New Orthophosphates of Divalent Chromium — Mg₃Cr₃(PO₄)₄, Mg_{3, 75}Cr_{2, 25}(PO₄)₄, Ca₃Cr₃(PO₄)₄ and Ca_{2, 00}Cr_{4, 00}(PO₄)₄ Solid state reactions via the gas phase led in the systems A₃(PO₄)₂ / Cr₃(PO₄)₂ (A = Mg, Ca) to the four new compounds Mg₃Cr₃(PO₄)₄ ( A ), Mg_3.75Cr_2.25(PO₄)₄ ( B ), Ca₃Cr₃(PO₄)₄ ( C ), and Ca_2.00Cr_4.00(PO₄)₄ ( D ). These were characterized by single crystal structure investigations [( A ): P2₁/n, Z = 1, a = 4.863(2) Å, b = 9.507(4) Å, c = 6.439(2) Å, β = 91.13(6)°, 1855 independend reflections, 63 parameters, R1 = 0.035, wR2 = 0.083; ( B ): P2₁/a, Z = 2, a = 6.427(2) Å, b = 9.363(2) Å, c = 10.051(3) Å, β = 106.16(3)°, 1687 indep. refl., 121 param., R1 = 0.032, wR2 = 0.085; ( C ): P‐1, Z = 2, a = 8.961(1) Å, b = 8.994(1) Å, c = 9.881(1) Å, α = 104.96(2)°, β = 106.03(2)°, γ = 110.19(2)°, 2908 indep. refl., 235 param., R1 = 0.036, wR2 = 0.111; ( D ): C2/c, Z = 4, a = 17.511(2) Å, b = 4.9933(6) Å, c = 16.825(2) Å, β = 117.95(1)°, 1506 indep. refl., 121 param., R1 = 0.034, wR2 = 0.098]. The crystal structures contain divalent chromium on various crystallographic sites, each showing a (4+n)‐coordination (n = 1, 2, 3). For the magnesium compounds and Ca_2.00Cr_4.00(PO₄)₄ a disorder of the divalent cations Mg²⁺/Cr²⁺ or Ca²⁺/Cr²⁺ is observed. Mg_3.75Cr_2.25(PO₄)₄ adopts a new structure type, while Mg₃Cr₃(PO₄)₄ is isotypic to Mg₃(PO₄)₂. Ca₃Cr₃(PO₄)₄ and Ca_2.00Cr_4.00(PO₄) ₄ are structurally very closely related and belong to the Ca₃Cu₃(PO₄)₄‐structure family. The orthophosphate Ca₉Cr(PO₄)₇, containing trivalent chromium, has been obtained besides C and D .     

Cation Distribution Studies in Double Orthophosphates with Whitlockite Structure

Abstract

The structure of β-Ca₃ (PO₄)₂ is known to be similar to that of whitlockite (R3c, Z =21). The cations are distributed in five different positions, the position Ca(4) being only half occupied. The whitlockite network is stable while the filling of the Ca(4) position changes from 0 to 1. The presence of vacancies allows to provide heterovalent substitutions 3Ca²⁺ = 2M³⁺ + and Ca²⁺ + 0 = 2Me⁺ with limits of compositions Ca₉M (PO₄)₇ and Ca_loMe(PO₄)₇ respectively. The possible cation size can be changed from 0.55 Å (Fe³⁺) to 1.51 Å (K⁺). In order to check these suggestions we have synthesized Ca₉M(PO₄)₇ (M = rare earth element, Y, Bi, Fe, Al, In, Sc) compounds, The double phosphates were studied by luminescence, infrared spectroscopy and X-ray diffraction. All these compounds are isostructural to β-Ca₃(PO₄)₂. The cell parameters gradually decrease for M = La-Ho, Y and remain constant for M = Er-Lu. This divergence can be attributed to the change of the coordination number of the rare earth element. A considerable decrease of parameters is observed for the compounds of small-size trivalent elements, their IR spectra show more bands. By luminescence it was found that rare earth elements and Y, Bi occupy Ca(1), Ca(2), Ca(3) positions. The study of Ca_9.18 Fe_0.88 (PO₄)₇ structure shows that Fe³⁺ occupies octa-hedral Ca(5) site. The considerable decrease of lattice parameters and changes in IR spectra of compounds with M = Fe, Al, In, Sc result from the occupation of Ca(5) Site with trivalent cations and from redistribution of charges in the cation sublattice of the β-Ca₃(PO₄)₂ type structure.     

Thermal behavior and phase transformations of nanosized carbonate apatite (Syria)

The phase transformations of Syrian phosphorite upon mechanochemical activation are examined in the present work. The latter is carried out in planetary mill equipped with 20 mm steel milling bodies and duration from 30 to 300 min. The established by means of DTA, DTG, TG analyses transformation of non-activated carbonate fluorine apatite type B into the carbonate hydroxyl fluorine apatite (COHFAp) mixed type A2-B leads to substantial changes in the properties of the activated samples expressed in lowering the degree of crystallinity, strong defectiveness of the structure, and increase of the citric solubility. The thermal analysis gives evidence for the decomposition of the carbonate-containing component within the phosphorite, as from the positions placed in the vicinity of the hexagonal 6₃ axis (type A2), as well as from the positions of the phosphate ion (type B), and from the free carbonates. The data from the thermal analysis, the powder X-ray analysis and the infrared spectroscopy give also evidence for phase transformations of the activated apatite (with admixtures of quartz and calcite) into Ca₁₀FOH(PO₄)₆, β-Ca₃(PO₄)₂, Ca₄P₂O₉, Ca₃(PO₄)₂ · Ca₂SiO₄ and for that one of the quartz—into larnite and wollastonite. The influence of the α-quartz as a concomitant mineral is considered to be positive. The α-quartz forms Si–O–Si–OH bonds retaining humidity in the solid phase thus facilitating the isomorphous substitution OH^? → F^? with the subsequent formation of partially substituted COHFAp. Calcium silicophosphate and Ca₄P₂O₉ are obtained upon its further heating. The presented here results settle a perspective route for processing of low-grade phosphate raw materials by means of tribothermal treatment aiming at preparation of condensed phosphates suitable for application as slowly acting fertilizer components.     

Organic radicals in natural apatites according to EPR data: Potential genetic and paleoclimatic indicators

In a group of natural marine apatites Ca₅(PO₄)₃(F, OH), organic ?H₃, ?H₂—R, HO?HR, (CH₃)₂—?R, and —?_org radicals are identified by EPR. The relation between the EPR spectra of the observed organic radicals, the valence form, and the structural location of impurity vanadium ions (V⁴⁺ (VO²⁺) on the Ca²⁺ II site or V⁵⁺ (VO₄)^3- → (PO₄)^3-) is established. The structure of organic radicals correlates with the type of organic matter in the sample under analysis: sapropelic or humic, depending on the climatic conditions of mineral genesis.     

Hydrothermal Synthesis,Crystal Structures and Characterization of Two Hydrogen Phosphates Templated by 4-Amino-2,2,6,6-tetramethylpiperidine

Abstract

Chemical preparations, crystal structures, thermal analyses, and IR spectroscopic studies are given for two new hydrogen phosphates templated by 4-amino-2,2,6,6-tetramethylpiperidine: (C₉H₂₂N₂)₂·(H₂PO₄)·(HPO₄)·(F)·H₂O (I) and (C₉H₂₂N₂)·(H₂PO₄)₂(II). The structures are determined by single crystal X-ray diffraction. Both compounds crystallize in the P2₁/c (N°14) monoclinic space group with the unit cell parameters: a = 14.856 (1) Å, b = 14.092 (2) Å, c = 14.7166 (9) Å, β = 118.434 (7)°, V = 2709.2 (4) Å ³, and Z = 4 for (I) and a = 9.803 (2) Å, c = 0.466 (2) Å, c = 15.640 (8) Å, β = 94.990 (4), V = 1598.68 (7) ų, and Z = 4 for (II).

The structure of I, refined to R = 0.042 and R_w = 0.067 for 6009 reflections (I ≥ 2σ (I)), exhibits infinite inorganic chains _∞((H₂PO₄)·(HPO₄)·(F)·H₂O)^4? linked together through weak hydrogen bonds to form layers onto which the diprotonated [C₉H₂₂N₂]^{2 +} amine molecules are anchored.

The structure of II, refined to R = 0.060 and R_w = 0.086 for 1435 reflections (I ≥ 2σ (I)), consists of _∞(H₂PO₄)^? (100) layers between which [C₉H₂₂N₂]²⁺ cations are inserted. A network of hydrogen bonds connects the different components. IR spectra of I and II show the characteristic bands of amine groups and phosphate anions.     

Kinetics and mechanism of protection of thymine from phosphate radical anion under anoxic conditions

The rates of photooxidation of thymine in the presence of peroxydiphosphate (PDP) have been determined by measuring the absorbance of thymine at 264 nm spectrophotometrically. The rates and the quantum yields (φ) of oxidation of thymine by phosphate radical anion have been determined in the presence of different concentrations of dithiothreitol (DTT). An increase in DTT is found to decrease the rate of oxidation of thymine, suggesting that DTT acts as an efficient scavenger of PO₄^·2? and protects thymine from it. Phosphate radical anion competes for thymine as well as DTT; the rate constant for the phosphate radical anion with DTT has been calculated to be 2.21 × 10⁹ dm³ mol^?1 s^?1, assuming the rate constant of phosphate radical anion reaction with thymine as 9.6 × 10⁷ dm³ mol^?1 s^?1. The quantum yields of photooxidation of thymine have been calculated from the rates of oxidation of thymine and the light intensity absorbed by PDP at 254 nm, the wavelength at which PDP is activated to phosphate radical anion. From the results of experimentally determined quantum yields (φ_exptl) and the quantum yields calculated (φ_cl), assuming DTT acts only as a scavenger of PO₄^·2? radicals, show that φ_exptl values are lower than φ_cl values. The φ′ values, which are experimentally found quantum yield values at each DTT concentration and corrected for PO₄^·2? scavenging by DTT, are also found to be greater than φ_exptl values. These observations suggest that the thymine radicals are repaired by DTT in addition to scavenging of phosphate radical anions. © 2001 John Wiley & Sons, Inc. Int J Chem Kinet 33: 271–275, 2001     

Dissolution De L'hydroxyapatite et Du Phosphate Tricalcique β Dans Les Solutions D'acide Nitrique

Using an isoperibol calorimeter for rapid reactions and a Calsol type microcalorimeter for slow processes, are applied to determine the enthalpies of solution of two synthetic phosphate products in nitric acid. Namely, β tricalcium phosphate Ca₃(PO₄)₂ and the calcium hydroxyapatite Ca₁₀ (PO₄)₆ (OH)₂ are measured by varying pH value of the solvent. Some dissolution mechanisms are proposed for various pH values. They are ensured by complementary reactions of solution of Ca(NO₃)₂, Ca(H₂ PO₄)₂ and H₃ PO₄ in the same solvents. An extrapolation of solution enthalpies to pH=7 leads to the enthalpy of solution of these products in the pure water. These values are Δ_sol H °=–138.3 kJ mol^–1 for Ca₃ (PO₄)₂ and –393.6 kJ mol^–1 for Ca₁₀ (PO₄)₆ (OH)₂ . This revised version was published online in August 2006 with corrections to the Cover Date.     

Vibrational spectroscopic characterization of the phosphate mineral series eosphorite–childrenite–(Mn,Fe)Al(PO4)(OH)2·(H2O)

The phosphate mineral series eosphorite–childrenite–(Mn,Fe)Al(PO₄)(OH)₂·(H₂O) has been studied using a combination of electron probe analysis and vibrational spectroscopy. Eosphorite is the manganese rich mineral with lower iron content in comparison with the childrenite which has higher iron and lower manganese content. The determined formulae of the two studied minerals are: (Mn_0.72,Fe_0.13,Ca_0.01)(Al)_1.04(PO₄, OHPO₃)_1.07(OH_1.89,F_0.02)·0.94(H₂O) for SAA-090 and (Fe_0.49,Mn_0.35,Mg_0.06,Ca_0.04)(Al)_1.03(PO₄, OHPO₃)_1.05(OH)_1.90·0.95(H₂O) for SAA-072. Raman spectroscopy enabled the observation of bands at 970 cm⁻¹ and 1011 cm⁻¹ assigned to monohydrogen phosphate, phosphate and dihydrogen phosphate units. Differences are observed in the area of the peaks between the two eosphorite minerals. Raman bands at 562 cm⁻¹, 595 cm⁻¹, and 608 cm⁻¹ are assigned to the ν₄ bending modes of the PO₄, HPO₄ and H₂PO₄ units; Raman bands at 405 cm⁻¹, 427 cm⁻¹ and 466 cm⁻¹ are attributed to the ν₂ modes of these units. Raman bands of the hydroxyl and water stretching modes are observed. Vibrational spectroscopy enabled details of the molecular structure of the eosphorite mineral series to be determined.     

Phase formation along sections of the HfO(NO3)2-H3PO4-RbF-H2O system

The phase formation in the system HfO(NO₃)₂-H₃PO₄-RbF-H₂O was studied along the sections at the molar ratios PO ₄ ^3? /Hf = 0.5, 1.0, 1.5, 2.0, and 3.0 and RbF: Hf = 1?5. The initial solutions contained 2–10 wt % HfO₂. The synthesis was performed at room temperature. The following substances were obtained for the first time: crystalline fluorophosphatehafnate RbHfF₂PO₄ · 0.5H₂O, crystalline triple salt HfF₄ · Rb(PO₄)_0.33 · RbNO₃, crystalline solvate Rb₃Hf₃(PO₄)₅ · 3HF, and amorphous fluorophosphate Hf₃O₂F₂(PO₄)₂ · 8H₂O (formula is conditional). The compounds were studied by crystal-optical, elemental, X-ray diffraction, thermogravimetric, IR spectroscopic, and electron microscopic analyses.     

Alendronate zwitterions bind to calcium cations arranged in columns

Alendronate is used clinically in the treatment of skeletal disorders, the mode of action depending on the adsorption to calcium hydroxy­apatite crystals (bone). In the title compound, calcium 4‐ammonium‐1‐hydroxy­butyl­idene‐1,1‐bis­phospho­n­ate, Ca²⁺·2C₄H₁₂NO₇P₂⁻, alendronate is a zwitterion, possessing one negative charge on each PO₃ group and a protonated N atom. The zwitterion is disposed with its negative end facing the Ca²⁺ ion, while its positive end is stretched in the opposite direction. The geometry of the carbon chain is all‐trans, while the hydroxy group is approximately gauche. The Ca²⁺ ion lies on a twofold axis parallel to b. The coordination sphere around the metal cation is octahedral and is determined by monodentate‐ and bidentate‐coordinated alendronate zwitterions. The O⋯O bite distance is 3.080 (2) Å. Coordinated Ca²⁺ metal cations are arranged at the centre of a column running along c.     

Structure cristalline de (NH4)2PO3H,H2O: Stereochimie de l'Ion PO3H2− et ses relations avec PO3F2− et SO32−

(NH₄)₂PO₃H, H₂O crystallizes in the monoclinic system, space group P2₁/c, with a = 6.322(1) Å, b = 8.323(1) Å, c = 12.676(1) Å, β = 98.84(1) and Z = 4. The structure was refined to R = 0.022 based on 853 independent X-Rays intensities. Improved dimensions of the tetrahedral PO₃H^2? ion have been obtained: P?H = 1.34(2) and P?O = 1.514(2) Å. The geometry of this ion is compared with that of PO₃F^2? and SO₃^2? ions and we find a decrease of the volume: V_F? > V_H+ > V_{lone pair}.     

Ir spectroscopic and crystal morphology studies of the structure of alakli metal fluorophosphatozirconates (hafnates)

Potassium, rhubidium, and caesium fluorophosphatozirconates (hafnates) and oxo(hydroxo)fluorophosphatonitratometalates with PO ₄ ^3? /Zr molar ratios of 2.0, 1.5, 1.0, 0.66, 0.5, and 0.33 are synthesized for the first time. Most of them form either fine crystalline or X-ray amorphous particles. In order to characterize them IR spectroscopy and SEM are used. For the crystalline compounds the types of PO₄ groups and the character of bonds between fluorine and water are revealed. The occurrence of triple MeF₄·Rb(PO₄)_0.33·RbNO₃ (Me = Zr, Hf) salts and also M₃Me₃(PO₄)₅·3HF crystalline solvates is found. The layered habit of K₃Hf₃(PO₄)₅·3HF, RbHfF₂PO₄·0.5H₂O, Rb₃Hf₃(PO₄)₅·3HF, CsHfF₂PO₄·0.5H₂O, CsHf₂F₆PO₄·4H₂O, and CsH₂Hf₂F₂(PO₄)₃·2H₂O crystals gives grounds to suppose that the structure of these compounds is layered unlike the structure of triple MeF₄·Rb(PO₄)_0.33·RbNO₃ salts.     

Quantum chemical and spectroscopic analysis of calcium hydroxyapatite and related materials

Amorphous calcium hydroxyapatite was examined by vibrational spectroscopy (Raman and infra-red (IR)) and quantum chemical simulation techniques. The structures and vibrational (IR, Raman and inelastic neutron scattering) spectra of PO₄³⁻ ion, Ca₃(PO₄)₂, [Ca₃(PO₄)₂]₃, Ca₅(PO₄)₃OH, CaHPO₄, [CaHPO₄]₂, Ca₃(PO₄)₂·H₂O, Ca₃(PO₄)₂·2H₂O and Ca₃(PO₄)₂·3H₂O clusters were quantum chemically simulated at ab initio and semiempirical levels of approximation. A complete coordinate analysis of the vibrational spectra was performed. The comparison of the theoretically simulated spectra with the experimental ones allows to identify correctly the phase composition of the amorphous calcium hydroxyapatite and related materials. The shape of the bands in the IR spectra of the hydroxoapatite can be used in order to characterize the structural properties of the material, e.g., the PO₄³⁻ ion status, the degree of hydrolysis of the material and the presence of hydrolysis products.     

Peroxo derivatives of hydroxyapatite and calcium hydrophosphate

Hydroxyapatite and calcium hydrophosphate peroxo solvates were synthesized and characterized by IR spectroscopy, powder X-ray diffraction, and TGA to be used as biocompatible and antibacterial medicaments in manufacturing calcium phosphate bioceramics for implantations in orthopedics and dentistry. A wide range of hydrogen peroxide percentages in stable mixtures of mCa₅(PO₄)₃(OH) + nCaHPO₄ · H₂O₂ · H₂O (ranging from 0.5 to 18%) allows composites to be prepared with a tailored active oxygen content.     

Sur le dosage argentométrique de l'anion phosphorique

1. In aqueous solutions of phosphoric acid or alcali phosphates, the PO₄^-3can be determined by potentiometric titraition with silver nitrate PO₄^-3 + 3 Ag⁺ ár unAg₃PO₄↓The pH value of the solution is maintained about 9 by using borax-buffer 2 The determination of phosphate ion is also possible by precipitation of Ag₃PO₄ with an excess of silver nitrate, the pH of the solution is adjusted between 7 and 8 by using a new buffer mixture containing NH₄⁺, NHXXX, and Ag⁺. After diluting the solution up to a known volume and filtering through dry filter paper, the excess of silver is determined by potentiometric titration with potassium bromide. This method gives very good results, it is applicable in the presence of Mg⁺² and Ca⁺². The presence of Fe⁺³ and Al⁺³ hinders the determination of the phosphate ion. 3. The properties of the ,,ammonium-silverdiamme” buffer system are described. This buffer contains NH₄⁺, NH₃ and Ag⁺ (the latter in excess with regard to NH₃)     

Anion Coordination of Bis‐bisurea Ligands: Aggregation of Dihydrogen Phosphate Anion into Oligomers and Infinite Chains

A series of alkanediyl‐spaced bis‐bisurea ligands ( L² – L⁴ ) were synthesized and their anion coordination behavior studied. These ligands form interesting complexes with polymeric and oligomeric dihydrogen phosphate aggregates in the solid state. The ligands L² and L³ coordinate with H₂PO₄^– anions to form a unique molecular “necklace” with an infinite (H₂PO₄^–)_n chain and surrounding ligand molecules. Meanwhile, two different dihydrogen phosphate‐water oligomers, (H₂PO₄)₆ · (H₂O)₄ and (H₂PO₄)₄ · (H₂O)₂, were observed in the complexes with the ligands L³ and L⁴ . In addition, solution anion binding properties of the ligands were studied by ¹H NMR and UV/Vis spectroscopy.