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Properties of UO2C2O4

Properties of UO2C2O4 (Uranyl oxalate):

Compound NameUranyl oxalate
Chemical FormulaUO2C2O4
Molar Mass358.04671 g/mol

Chemical structure
UO2C2O4 (Uranyl oxalate) - Chemical structure
Lewis structure
3D molecular structure
Physical properties
AppearancePale yellow powder
Solubilitysoluble

Elemental composition of UO2C2O4
ElementSymbolAtomic weightAtomsMass percent
UraniumU238.02891166.4798
OxygenO15.9994626.8111
CarbonC12.010726.7090
Mass Percent CompositionAtomic Percent Composition
U: 66.48%O: 26.81%C: 6.71%
U Uranium (66.48%)
O Oxygen (26.81%)
C Carbon (6.71%)
U: 11.11%O: 66.67%C: 22.22%
U Uranium (11.11%)
O Oxygen (66.67%)
C Carbon (22.22%)
Mass Percent Composition
U: 66.48%O: 26.81%C: 6.71%
U Uranium (66.48%)
O Oxygen (26.81%)
C Carbon (6.71%)
Atomic Percent Composition
U: 11.11%O: 66.67%C: 22.22%
U Uranium (11.11%)
O Oxygen (66.67%)
C Carbon (22.22%)
Identifiers
CAS Number2031-89-2
SMILESC(=O)(C(=O)[O-])[O-].O=[U+2]=O
Hill formulaC2O6U

Related compounds
FormulaCompound name
UO2CO3Uranyl carbonate

Related
Molecular weight calculator
Oxidation state calculator

Uranyl oxalate (UO2C2O4): Chemical Compound

Scientific Review Article | Chemistry Reference Series

Abstract

Uranyl oxalate (UO2C2O4) is an inorganic coordination compound consisting of the uranyl cation (UO22+) complexed with oxalate anions (C2O42-). This pale yellow crystalline solid typically exists as a trihydrate (UO2C2O4·3H2O) under ambient conditions due to its hygroscopic nature. The compound crystallizes in the monoclinic system with space group P21/c. Uranyl oxalate exhibits limited solubility in aqueous media and demonstrates significant thermal stability, decomposing above 300°C. Its principal applications include use as an actinometer in photochemical studies and as an intermediate in nuclear fuel processing operations. The compound's distinctive photochemical properties and coordination chemistry make it valuable for both industrial and research applications.

Introduction

Uranyl oxalate represents an important class of uranyl carboxylate compounds with significant applications in nuclear chemistry and photochemical research. As an inorganic coordination compound, it bridges the chemistry of uranium(VI) oxo complexes with organic dicarboxylate ligands. The compound's discovery dates to early investigations of uranium chemistry in the late 19th century, with systematic characterization occurring throughout the 20th century alongside developments in coordination chemistry and nuclear technology. Uranyl oxalate's photochemical reactivity was recognized early in its history, leading to its application as a chemical actinometer for quantifying light intensity in photochemical experiments. In industrial contexts, the compound appears as an intermediate in nuclear fuel reprocessing operations, particularly in precipitation processes designed to separate uranium from other actinides and fission products. The compound's structural features, combining the linear uranyl cation with the planar oxalate anion, create distinctive coordination geometries that continue to interest researchers in materials science and coordination chemistry.

Molecular Structure and Bonding

Molecular Geometry and Electronic Structure

The molecular structure of uranyl oxalate centers on the uranyl ion (UO22+), which exhibits linear geometry with uranium-oxygen bond lengths of approximately 1.76 Å. This linear configuration results from the strong covalent bonding between uranium and oxygen atoms, with the uranium atom in the +6 oxidation state (electron configuration [Rn]). The oxalate anion (C2O42-) adopts a planar configuration with typical carbon-carbon bond lengths of 1.54 Å and carbon-oxygen bond lengths of 1.26 Å for carbonyl groups and 1.31 Å for coordinating oxygen atoms. In the solid state, uranyl oxalate trihydrate crystallizes in the monoclinic system with space group P21/c and unit cell parameters a = 8.92 Å, b = 10.37 Å, c = 7.65 Å, and β = 111.5°. The uranium atom achieves pentagonal bipyramidal coordination geometry, with the two uranyl oxygen atoms occupying axial positions and five oxygen atoms from oxalate ligands and water molecules forming the equatorial plane. The equatorial U-O bond distances range from 2.32 to 2.48 Å, significantly longer than the axial U-O bonds due to the trans influence of the strong uranyl bonds.

Chemical Bonding and Intermolecular Forces

The bonding in uranyl oxalate involves both covalent and ionic character. The uranium-oxygen bonds in the uranyl ion demonstrate substantial covalent character with bond dissociation energies estimated at 700-800 kJ/mol, while the coordination bonds between uranium and oxalate oxygen atoms are primarily ionic with bond energies of approximately 200-300 kJ/mol. The oxalate ligand functions as a bidentate chelating agent, forming five-membered rings with the uranium center that enhance complex stability through the chelate effect. Intermolecular forces in the crystal structure include hydrogen bonding between coordinated water molecules and oxalate oxygen atoms, with O···O distances of 2.65-2.85 Å and typical hydrogen bond energies of 15-25 kJ/mol. Van der Waals interactions between hydrocarbon portions of adjacent molecules contribute additional stabilization to the crystal lattice. The compound exhibits a calculated dipole moment of approximately 4.5 D in the gas phase, though this is substantially reduced in the solid state due to crystal packing effects. The overall lattice energy is estimated at 2500-3000 kJ/mol, contributing to the compound's thermal stability and limited solubility.

Physical Properties

Phase Behavior and Thermodynamic Properties

Uranyl oxalate trihydrate appears as pale yellow crystalline powder with density of 3.28 g/cm³ at 25°C. The compound demonstrates limited solubility in water, with a solubility product constant (Ksp) of 1.6 × 10-8 at 25°C. Thermal analysis reveals dehydration processes beginning at 80°C with complete loss of water of hydration by 150°C. The anhydrous compound remains stable to approximately 300°C, above which decomposition occurs through reduction to uranium(IV) species and ultimately to uranium dioxide (UO2) around 600°C. The enthalpy of formation for the trihydrate is -2450 kJ/mol, with Gibbs free energy of formation of -2250 kJ/mol at 298 K. The compound exhibits a heat capacity of 350 J/mol·K at room temperature, increasing gradually with temperature until decomposition. The refractive index measures 1.62-1.65 across visible wavelengths, with birefringence of 0.03-0.05 characteristic of its monoclinic crystal structure. The molar volume is 125.3 cm³/mol for the trihydrate form, with a coefficient of thermal expansion of 4.7 × 10-5 K-1 along the a-axis and 5.2 × 10-5 K-1 along the c-axis.

Spectroscopic Characteristics

Infrared spectroscopy of uranyl oxalate trihydrate reveals characteristic vibrations including the asymmetric UO22+ stretch at 925 cm-1, symmetric UO22+ stretch at 855 cm-1, and carbonyl stretches of the oxalate ligand at 1650 cm-1 and 1380 cm-1. The U-O coordination bonds produce vibrations between 450-550 cm-1, while water of hydration exhibits O-H stretching at 3400 cm-1 and bending at 1620 cm-1. Raman spectroscopy shows the uranyl symmetric stretch at 870 cm-1 with a linewidth of 12 cm-1, along with oxalate ring vibrations at 580 cm-1 and 910 cm-1. Electronic absorption spectra display the characteristic charge-transfer bands of the uranyl ion with maxima at 420 nm (ε = 12,000 M-1cm-1) and 340 nm (ε = 8,500 M-1cm-1), along with weaker f-f transitions in the visible region. Photoluminescence spectroscopy exhibits the typical uranyl emission at 515 nm, 535 nm, and 560 nm with lifetime of 180 μs at room temperature. Mass spectrometric analysis shows fragmentation patterns dominated by loss of water molecules followed by decarboxylation of the oxalate ligand.

Chemical Properties and Reactivity

Reaction Mechanisms and Kinetics

Uranyl oxalate demonstrates moderate thermal stability but undergoes photochemical decomposition under ultraviolet irradiation. The photodecomposition follows first-order kinetics with quantum yield of 0.57 at 254 nm, making it useful as a chemical actinometer. The decomposition mechanism involves electron transfer from the oxalate ligand to the uranyl ion, resulting in reduction of uranium(VI) to uranium(IV) and oxidation of oxalate to carbon dioxide. Thermal decomposition proceeds through intermediate uranium(IV) oxalate formation, with activation energy of 120 kJ/mol for the dehydration step and 180 kJ/mol for the decarboxylation process. The compound exhibits limited reactivity with acids, dissolving slowly in concentrated mineral acids with formation of uranyl salts and oxalic acid. With bases, uranyl oxalate undergoes hydrolysis, particularly at elevated temperatures, producing uranium trioxide hydrates. Reaction with hydrogen peroxide yields uranyl peroxide precipitates, while reduction with hydrazine or other reducing agents produces uranium(IV) species. The compound demonstrates stability in dry air but gradually absorbs moisture to reform the trihydrate, with hydration kinetics following diffusion-controlled mechanisms.

Acid-Base and Redox Properties

The uranyl ion in uranyl oxalate exhibits weak acidic character with estimated pKa values of 4.2 and 6.8 for hydrolysis reactions, though these are largely suppressed by coordination to the oxalate ligand. The oxalate ligand itself can undergo protonation with pKa1 = 1.2 and pKa2 = 4.2 for free oxalic acid, though these values shift upon coordination to uranium. The compound demonstrates buffering capacity in the pH range 3-5 due to the equilibrium between protonated and deprotonated forms of the coordinated oxalate. Redox properties are dominated by the uranium center, with standard reduction potential UO22+/U4+ of +0.38 V vs. SHE, modified by coordination to oxalate. The compound is stable in oxidizing environments but susceptible to reduction by strong reducing agents. Electrochemical studies show irreversible reduction waves at -0.45 V and -0.85 V vs. SCE, corresponding to successive one-electron transfers. The compound maintains stability across a pH range of 2-7, outside of which hydrolysis or precipitation of other uranium species occurs.

Synthesis and Preparation Methods

Laboratory Synthesis Routes

The most common laboratory synthesis involves precipitation from aqueous solutions of uranyl nitrate and oxalic acid. Typically, 0.1 M uranyl nitrate hexahydrate solution is added dropwise to 0.1 M oxalic acid solution maintained at 60°C with constant stirring. The molar ratio of uranium to oxalate is maintained at 1:1.05 to ensure complete precipitation of uranium. The pale yellow precipitate forms immediately and is digested at 60°C for one hour to improve crystallinity. The product is collected by filtration, washed with cold water and ethanol, and dried under vacuum at room temperature. This method yields uranyl oxalate trihydrate with typical yields of 95-98% and purity exceeding 99%. Alternative synthesis routes include metathesis reactions between uranyl chloride and sodium oxalate, though these may introduce sodium contamination. Crystallization from aqueous solution produces well-formed prismatic crystals suitable for single-crystal X-ray diffraction studies. The compound can be dehydrated by heating under vacuum at 150°C for 24 hours, producing the anhydrous form which is hygroscopic and must be handled under inert atmosphere.

Analytical Methods and Characterization

Identification and Quantification

Uranyl oxalate is identified primarily through its characteristic X-ray diffraction pattern, with strongest reflections at d-spacings of 8.12 Å (100%), 4.06 Å (85%), 3.45 Å (60%), and 2.87 Å (45%). Quantitative analysis of uranium content is performed by dissolving the compound in nitric acid and employing inductively coupled plasma mass spectrometry (ICP-MS) or spectrophotometric methods using arsenazo III reagent with detection limit of 0.1 μg/mL. Oxalate content is determined by oxidation with potassium permanganate in sulfuric acid solution at 60°C, with titration endpoint detection potentiometrically. Thermogravimetric analysis provides quantitative measurement of water content through mass loss between 80-150°C and oxalate content through decomposition above 300°C. Infrared spectroscopy serves as a rapid identification method, with the ratio of uranyl stretch intensities (925 cm-1/855 cm-1) providing a characteristic fingerprint. Chromatographic methods including ion chromatography with conductivity detection can separate and quantify oxalate ions with detection limits of 0.5 mg/L.

Purity Assessment and Quality Control

Pharmaceutical-grade specifications for uranyl oxalate (when used as an actinometer) require uranium content of 66.2-66.8% and oxalate content of 32.8-33.2% for the anhydrous compound, with loss on drying not exceeding 0.5% when dried at 150°C. Common impurities include uranyl nitrate, uranium tetrafluoride, and ammonium diuranate, all detectable by X-ray diffraction and infrared spectroscopy. Heavy metal contaminants are limited to less than 50 ppm as determined by atomic absorption spectroscopy. The compound exhibits good storage stability when kept in sealed containers protected from light, with shelf life exceeding five years. Accelerated stability testing at 40°C and 75% relative humidity shows no significant decomposition over six months. Quality control protocols include measurement of specific rotation (in solution), absorbance ratios at characteristic wavelengths, and testing of actinometric properties against standard light sources.

Applications and Uses

Industrial and Commercial Applications

Uranyl oxalate serves primarily as a chemical actinometer in photochemical research, particularly for ultraviolet radiation measurements in the range 254-435 nm. Its well-characterized quantum yield and photochemical stability make it valuable for calibrating light sources and measuring photon fluxes in photochemical reactors. In nuclear technology, the compound appears as an intermediate in fuel reprocessing operations, where its low solubility facilitates uranium precipitation from nitric acid solutions containing fission products. The compound has historical significance in early uranium purification processes, though modern methods often employ different precipitation agents. Additional applications include use as a catalyst in oxidation reactions, where the uranyl ion acts as a photochemical oxidant, and as a precursor for the synthesis of other uranium compounds including uranium dioxide and uranium carbide. The compound's distinctive yellow color and stability led to limited use as a pigment in specialized ceramics and glass formulations, though these applications have declined due to radioactivity concerns.

Historical Development and Discovery

Uranyl oxalate first appeared in chemical literature during the late 19th century as chemists systematically investigated uranium compounds following the element's discovery in 1789. Early studies by Peligot and other uranium chemists documented the compound's formation and basic properties. The compound's photochemical reactivity was recognized in the early 20th century, with detailed quantum yield measurements published by Leighton and Forbes in 1929, establishing its utility as a chemical actinometer. Throughout the mid-20th century, research focused on the compound's role in nuclear fuel cycle chemistry, particularly its precipitation behavior in the presence of other actinides and fission products. Structural characterization advanced significantly with the application of X-ray crystallography in the 1950s-1960s, revealing the pentagonal bipyramidal coordination geometry around uranium. Recent research has explored the compound's potential in materials science applications, including synthesis of uranium-containing nanomaterials and development of uranium-based metal-organic frameworks. The compound continues to serve as a model system for understanding uranyl carboxylate chemistry and photochemical processes in actinide compounds.

Conclusion

Uranyl oxalate represents a chemically significant uranyl compound with well-characterized structural, thermal, and photochemical properties. Its coordination geometry, featuring uranium in pentagonal bipyramidal arrangement with oxalate and water ligands, provides insight into uranyl carboxylate chemistry more broadly. The compound's photochemical reactivity, with well-defined quantum yield, ensures its continued utility as a chemical actinometer despite the development of electronic measurement techniques. In industrial contexts, the compound's precipitation behavior remains relevant to nuclear fuel cycle operations. Future research directions may explore the compound's potential in materials synthesis, particularly as a precursor for uranium-containing nanomaterials, and further investigation of its photophysical properties using advanced spectroscopic techniques. The fundamental chemistry of uranyl oxalate continues to provide valuable insights into actinide coordination chemistry and photochemical processes.

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