Co-Precipitation of Fe—Cu Bimetal Oxalates in an Aqueous Solution and Their Thermally Induced Decomposition
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F21%3A73607917" target="_blank" >RIV/61989592:15310/21:73607917 - isvavai.cz</a>
Výsledek na webu
<a href="https://chemistry-europe.onlinelibrary.wiley.com/doi/epdf/10.1002/ejic.202100581" target="_blank" >https://chemistry-europe.onlinelibrary.wiley.com/doi/epdf/10.1002/ejic.202100581</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1002/ejic.202100581" target="_blank" >10.1002/ejic.202100581</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Co-Precipitation of Fe—Cu Bimetal Oxalates in an Aqueous Solution and Their Thermally Induced Decomposition
Popis výsledku v původním jazyce
This work focuses on the preparation of bimetal Fe−Cu oxalates by a co-precipitation reaction in an aqueous solution and subsequently on their thermally induced decomposition. The formation of solid solutions of Fe−Cu oxalates with various Fe/Cu ratios was studied by energy dispersive X-ray analysis, X-ray powder diffraction, transmission 57Fe Mössbauer spectroscopy, and scanning electron microscopy. The results suggest that the bimetal Fe−Cu oxalate precipitated in a structure similar to β-FeC2O4 ⋅ 2H2O. The maximum relative amount of Cu obtained within the bimetal oxalate was approximately 40 %. However, the single bimetal phase composition was obtained only for a limited range of Fe/Cu ratios. The Fe-rich samples contained also β-FeC2O4 ⋅ 2H2O, while the Cu-rich samples were predominantly composed of CuC2O4 ⋅ nH2O and contained much lower amounts of Fe than expected. The thermal decomposition of the prepared oxalate with the nominal Fe/Cu ratio of 65/35 was studied by in-situ X-ray powder diffraction in combination with ex-situ Mössbauer spectroscopy. The mixing of both metals at the molecular level allowed the preparation of copper ferrite particles at a relatively low temperature of 470 °C.
Název v anglickém jazyce
Co-Precipitation of Fe—Cu Bimetal Oxalates in an Aqueous Solution and Their Thermally Induced Decomposition
Popis výsledku anglicky
This work focuses on the preparation of bimetal Fe−Cu oxalates by a co-precipitation reaction in an aqueous solution and subsequently on their thermally induced decomposition. The formation of solid solutions of Fe−Cu oxalates with various Fe/Cu ratios was studied by energy dispersive X-ray analysis, X-ray powder diffraction, transmission 57Fe Mössbauer spectroscopy, and scanning electron microscopy. The results suggest that the bimetal Fe−Cu oxalate precipitated in a structure similar to β-FeC2O4 ⋅ 2H2O. The maximum relative amount of Cu obtained within the bimetal oxalate was approximately 40 %. However, the single bimetal phase composition was obtained only for a limited range of Fe/Cu ratios. The Fe-rich samples contained also β-FeC2O4 ⋅ 2H2O, while the Cu-rich samples were predominantly composed of CuC2O4 ⋅ nH2O and contained much lower amounts of Fe than expected. The thermal decomposition of the prepared oxalate with the nominal Fe/Cu ratio of 65/35 was studied by in-situ X-ray powder diffraction in combination with ex-situ Mössbauer spectroscopy. The mixing of both metals at the molecular level allowed the preparation of copper ferrite particles at a relatively low temperature of 470 °C.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
21001 - Nano-materials (production and properties)
Návaznosti výsledku
Projekt
—
Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2021
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
EUROPEAN JOURNAL OF INORGANIC CHEMISTRY
ISSN
1434-1948
e-ISSN
—
Svazek periodika
2021
Číslo periodika v rámci svazku
37
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
10
Strana od-do
3886-3895
Kód UT WoS článku
000693316600001
EID výsledku v databázi Scopus
2-s2.0-85114159322