Abstract

Iron(II)oxalate dihydrate FeC2O4 × 2 H2O—humboldtine is not only an important synthetic intermediate, but also a key building block for the preparation of various advanced materials. Interestingly, FeC2O4 × 2 H2O can be transformed readily into phase-pure siderite FeCO3. The importance of siderite for earth sciences, in particular for the understanding of the deep carbon cycle of our planet, is paramount. The availability of high-quality single crystals of FeC2O4 × 2 H2O is crucial for diffraction or spectroscopic studies at high pressure. The present article describes a versatile synthetic approach to single crystals of FeC2O4 × 2 H2O and its deuterated analogue starting from metallic iron together with a complete characterization of the products obtained. The same protocol has been employed successfully for the preparation of 57FeC2O4 × 2 H2O, as required for Möβbauer spectroscopy. In addition, the pressure-dependence of the crystal and molecular structure of the title compound was investigated up to p ≥ 20 GPa.

Highlights

  • Iron(II)oxalate dihydrate FeC2 O4 × 2 H2 O—humboldtine is an important synthetic intermediate, and a key building block for the preparation of various advanced materials

  • FeC2 O4 × 2 H2 O has emerged as an important building block for the preparation of new, functional advanced materials

  • The pressure dependence of the crystal and molecular structure of the title compound is reported for applied hydrostatic pressures up to p ≥ 20 GPa

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Summary

Introduction

Iron(II)oxalate dihydrate FeC2 O4 × 2 H2 O is the ferrous salt of ethandicarboxylic acid (oxalic acid). FeC2 O4 × 2 H2 O has emerged as an important building block for the preparation of new, functional advanced materials In this context, high, thermally activated proton conductivity of synthetic humboldtine has been reported [8]. While an impressive body of information is available on the thermal, spectroscopic, magnetic, and structural properties of iron(II)oxalate dihydrate at ambient conditions, little if anything is known about the pressure-dependence of the molecular and crystal structure [3,4,5,6,7,8,9,10,11,12,13,14,15,16,17,18,19]. The pressure dependence of the crystal and molecular structure of the title compound is reported for applied hydrostatic pressures up to p ≥ 20 GPa

Chemicals and Instrumentation
High Pressure Studies
Synthesis
Structural Properties
GPa mains almost constant up to around p
Lattice parameters of2Oα-FeC
O-Fe-OH
Oblique
Full Text
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