Thermodynamics of electrolytes. VI. Weak electrolytes including H3PO4

Equations previously developed and widely applied to the thermodynamic properties of strong electrolytes are extended to solutions involving a dissociation equilibrium. Excellent agreement is obtained with the data for pure phosphoric acid to 6M and for phosphate buffer solutions. The parameters of the strong electrolyte components of the buffer solutions are taken from other work, and the remaining parameters for H⁺, H₂PO ₄ ^– , and H₃PO₄ are evaluated, including a pK of 2.146. The present method avoids ambiguities which formerly arose in treating weak acids with as small pK as this.     

Interaction model for the volumetric properties of weak electrolytes with application to H3PO4

The Pitzer ion-interaction model for the thermodynamic properties of a weakly dissociating neutral solute is extended to include solution densities and compressibilities. Excellent agreement is obtained with the literature data for pure aqueous phosphoric acid to 8m. The first and second pressure derivatives of the interaction parameters for H⁺, H₂PO ₄ ^? , and H₃PO₄ are evaluated, in addition to the limiting partial molar volumes and adiabatic compressibilities of the ionized and unionized acids. The present method requires no additional data or extraneous assumption regarding the properties of the free electrolyte in extrapolating to infinite dilution. The quantities evaluated are used to estimate the pressure dependence of the ionization constant, activity coefficients, and speciation to 1 kbar. The estimated effect of pressure on aqueous phosphoric acid ionization is in excellent agreement with experimental data.     

Synthese und Kristallstruktur von K2(HSO4)(H2PO4), K4(HSO4)3(H2PO4) und Na(HSO4)(H3PO4)

Synthesis and Crystal Structure of K₂(HSO₄)(H₂PO₄), K₄(HSO₄)₃(H₂PO₄), and Na(HSO₄)(H₃PO₄) Mixed hydrogen sulfate phosphates K₂(HSO₄)(H₂PO₄), K₄(HSO₄)₃(H₂PO₄) and Na(HSO₄)(H₃PO₄) were synthesized and characterized by X‐ray single crystal analysis. In case of K₂(HSO₄)(H₂PO₄) neutron powder diffraction was used additionally. For this compound an unknown supercell was found. According to X‐ray crystal structure analysis, the compounds have the following crystal data: K₂(HSO₄)(H₂PO₄) (T = 298 K), monoclinic, space group P 2₁/c, a = 11.150(4) Å, b = 7.371(2) Å, c = 9.436(3) Å, β = 92.29(3)°, V = 774.9(4) ų, Z = 4, R₁ = 0.039; K₄(HSO₄)₃(H₂PO₄) (T = 298 K), triclinic, space group P 1, a = 7.217(8) Å, b = 7.521(9) Å, c = 7.574(8) Å, α = 71.52(1)°, β = 88.28(1)°, γ = 86.20(1)°, V = 389.1(8)ų, Z = 1, R₁ = 0.031; Na(HSO₄)(H₃PO₄) (T = 298 K), monoclinic, space group P 2₁, a = 5.449(1) Å, b = 6.832(1) Å, c = 8.718(2) Å, β = 95.88(3)°, V = 322.8(1) ų, Z = 2, R₁ = 0,032. The metal atoms are coordinated by 8 or 9 oxygen atoms. The structure of K₂(HSO₄)(H₂PO₄) is characterized by hydrogen bonded chains of mixed H_nS/PO₄^– tetrahedra. In the structure of K₄(HSO₄)₃(H₂PO₄), there are dimers of H_nS/PO₄^– tetrahedra, which are further connected to chains. Additional HSO₄^– tetrahedra are linked to these chains. In the structure of Na(HSO₄)(H₃PO₄) the HSO₄^– tetrahedra and H₃PO₄ molecules form layers by hydrogen bonds.     

Anodic polarization of Al-Sn alloy in H3PO4 solutions

The anodic polarization behaviour of Al-Sn alloy (5.6% Sn) was studied in aerated 1, 1.5 and 2 M H₃PO₄ acid solutions using potentiodynamic and potentiostatic techniques. Anodic behaviour of Al and Sn metals was investigated for comparison. The results show that the alloy exhibits active-passive transition behaviour. The passivation of the examined alloy is due to the formation of oxide film for both Al and Sn incorporated with their phosphates. In general, at constant concentration of PO₄ ³⁻ ion, the passive current density (I _pass) is decreased with increase of pH in the range 2.5–5. Further, the influence of Cl⁻ ions on the passivity of the given alloy was studied. It was found that the aggressive effect of Cl⁻ ions on the passive film is inhibited with increase in phosphate concentration and pH. However, the addition of organic compounds (2- and 3-picoline and 2-aminopyridine) shows that only 2-aminopyridine inhibited the attack of Cl⁻ ions. Received: 24 October 1997 / Accepted: 5 February 1998     

Physicochemical Properties of the H3PO4-Dimethylformamide System

The viscosity, density, and electrical conductivity of H₃PO₄-dimethylformamide solutions and the enthalpies of solution and mixing of the components were measured in the entire composition range in the interval 25-65°C. It was concluded that phosphoric acid dissociates in dimethylformamide and that complexes of the presumed composition 2H₃PO₄·DMF are formed.     

Precipitation of Rare Earth Phosphates from H3PO4 Solutions

Abstract

A study of several factors has been carried out in order to determine their influence on rare earth phosphates precipitation from H₃PO₄ solutions obtained after the treatment of the Kola phosphate rock.     

3-D phase diagram of HPC/H2O/H3PO4 tertiary system

A 3-D phase diagram of the HPC/H₂O/H₃PO₄ tertiary system against various temperatures was established. Four distinct phases—the completely separated phase (S), the cloudy suspension phase (CS), the liquid crystalline miscible phase (LC), and the isotropically miscible phase (I)—were identified. The S phase shrank as the temperature increased, revealing that the HPC solubility increased with temperature, regardless of the LCST (lower critical solution temperature) characteristic. The addition of H₃PO₄ suppressed the formation of LC phase. However, as the temperature was raised sharply from 50 to 70?°C, the LC phase could only be maintained at high H₃PO₄ concentration region; it was a triangular shape, and the top apex of the triangle was the temperature-invariant L* point (HPC/H₂O/H₃PO₄ 38/9/53?wt%). The CS phase expanded considerably into the H₂O-rich but H₃PO₄-poor region when the temperature continued to increase over 48?°C. The LCST points of the CS phase that contained 0 and 15?wt% of H₃PO₄ were 34 and 38?°C, respectively. These CS results demonstrate that H₃PO₄ suppresses the occurrence of LCST behavior. Additionally, the binodal curve exhibits a weak or even zero dependence of binodal temperature on the HPC concentration at HPC concentrations of less than 30?wt% in a pure water system. A hypothesis concerning the sequential desorption of water molecules was proposed to explain such behavior.     

Kinetics of the Kola Apatite Rock Interaction With H3PO4

Abstract

Besides the production of fertilizers, Kola phosphate rock may be used as a source of lanthanides, strontium and fluorine. It implies the necessity to carry out a study of kinetics and mechanisms of the process in order to choose optimal conditions for the realization of the technological scheme [1]. The fluorapatite concentrate used had the following composition: ?Ln₂O₃ - 0.89; Y₂O₃ - 0.04; SrO - 2 80; CaO - 45.40; Fe₂O₃ -0.42; Al₂O₃ - 0.86; MgO - 0 10; F - 2.80; SiO₂ - 1.80; P₂ ^O ₅ - 39.40 weight %; molar ratio CaO : P₂O₅ = 1.5; the content of the apatite - 98.5%. The reaction of H₃PO₄ with fluorapatite was studied using a laboratory reactor with a stationary layer. The following parameters were varied: H₃PO₄ concentration (20, 30 and 50 weight % P₂O₅), temperature (20, 75, 150, 200 and 250°C) and time of contact (1–180 min.). A multimethod approach was used. X-ray diffraction, electron probe microanalysis and paper chromatography were applied to follow the bulk structural aspects of the apatite powders. It was shown that at the first stage of reaction a thin film of calcium monophosphate Ca(H₂PO₄)₂ H₂O is deposited on the apatite particles (avg. diameter 150 nm). The reaction is thought to proceed at the interphase solid/liquid and its kinetics may be described by the equation     

Proton conductivity in TaH(PO4)2 · 2H2O + SiO2 composite electrolytes

The composite electrolytes of composition (1 ? x)TaH(PO₄)₂ · 2H₂O/xSiO₂ (x = 0.2–0.4) are synthesized, and their transport properties are characterized over a wide temperature range. Doping with highly dispersed silica only insignificantly changes the proton conductivity of tantalum hydrogenphosphate below 370 K; above 820 K, the conductivity increases. The evolution of the phase composition of TaH(PO₄)₂ · 2H₂O and its base materials during thermolysis is studied.     

Determination of traces of chloride and fluoride in H2SO4, H3PO4 and H3BO3 by in situ analyte distillation-ion chromatography

A simple dual vessel in situ analyte distillation (IAD) system has been developed for suppressed ion chromatographic determination of chloride and fluoride ions in complex matrices. In IAD system, water vapours generated from the outer vessel reacts with sulfuric acid generating heat, thus favouring the quantitative distillation of chloride and fluoride within 30 min on water bath temperature (approximately 80 degrees C). The distilled analytes, as their respective acids in water, were directly injected into an ion-chromatograph. This newly developed method has been applied for analysis of trace impurities in H2SO4, H3PO4 and H3BO3. The detection limits for chloride is 8, 80 and 70ppb (w/w) for H2SO4, H3PO4 and H3BO3, respectively. For fluoride the detection limits are 6 and 60 ppb (w/w) for H2SO4 and H3PO4, respectively. The recovery of spikes for both the analytes ranged between 87 and 100%.     

过氧化氢和磷酸对以亚磷酸作磷源合成SAPO-41和AIPO-41的影响

考察了以亚磷酸作为磷源合成SAPO-41和AlPO-41时加入过氧化氢或磷酸对生成SAPO-41和AlPO-41的影响.结果表明,向反应体系中加入过氧化氢或者使用磷酸部分替代亚磷酸,都能明显缩短SAPO-41和AlPO-41的晶化时间.此外,使用混合磷源还能够降低模板剂的用量,获得小晶粒晶化产物.     

Muon spin relaxation study of Zr(H2PO4)(PO4).2H2O

Muon spin relaxation has been used to study the muon dynamics in the layered zirconium phosphate Zr(H(2)PO(4))(PO(4)).2H(2)O as a function of temperature. Radiofrequency decoupling was used to establish the origin of the local dipolar field as coupling with (1)H spins. Muons were trapped at two sites, one identified as HMuO and the other consistent with PO-Mu on the basis of their zero-field second moments. Although a small decrease in the local nuclear dipolar field was seen with temperature, the muons remained essentially static over the temperature range 20-300 K.     

Isopiestic Studies of H3PO4(aq) at Elevated Temperatures

Isopiestic molalities of aqueous solutions of phosphoric acid have been measured at 383.15 to 523.15 K. NaCl(aq) served as the isopiestic standard for the calculation of osmotic coefficients. The ion-interaction model gave an excellent fit to the experimental osmotic coefficients by treating H₃PO₄(aq) as a 1–1 weak electrolyte. Activity coefficients, both real and stoichiometric, were also obtained from the analysis of the isopiestic results. As expected, the ionization of H₃PO₄(aq) decreased with increasing temperature. However, at higher molalities, the ionization increased with increasing molality (reionization).