Abstract:The tetradecanuclear FeIII pivalate nanocluster [Fe14O10(OH)4(Piv)18], comprising a new type of metal oxide framework, has been solvothermally synthesized from a hexanuclear iron pivalate precursor in dichlormethane/acetonitrile solution. Magnetic measurements indicate the presence of very strong antiferromagnetic interactions in the cluster core.
“…A similar effect was observed for [Fe 14 O 10 (OH) 4 (Piv) 18 ] where the room temperature moment was only about 20% of the spin-only value. 14 …”
Section: Resultsmentioning
confidence: 99%
“…10 Furthermore, when such rings contain magnetic ions, such as manganese, molybdenum or iron, they typically exhibit complex magnetic interactions. 11 Over the years, a number of iron containing molecular ring structures, referred to as ferric wheels, 12,13 have been crystallized via solution routes, including [Fe(OMe) 2 (O 2 CCH 2 Cl)] 10 , 13 [Fe 14 O 10 (OH) 4 (Piv) 18 (HPiv = pivalic acid) 14 and [Fe(OH)(C 30 H 38 N 2 O 8 )Fe 2 (OCH 3 04(O 2 CCH 3 ) 2 ]6. 15 …”
Single crystals of a new iron containing oxide, Ba4KFe3O9, were grown from a hydroxide melt and the crystal structure was determined by single crystal x-ray diffraction. This ferrite represents the first complex oxide containing isolated 6-member rings of corner sharing FeO4 tetrahedra. Mössbauer measurements are indicative of two tetrahedral high-spin Fe3+ coordination environments. The observed magnetic moment (~3.9 BM) at 400 K is significantly lower than the calculated spin-only (~5.2 BM) value indicating the presence of strong antiferromagnetic interactions in the oxide. Our density functional calculations confirm the strong antiferromagnetic coupling between adjacent Fe3+ sites within each 6-member ring and estimate the nearest neighbor spin exchange integral as ~200 K; next nearest neighbor interactions are shown to be negligible. The lower than expected effective moment for Ba4KFe3O9 calculated from χT data is explained as resulting from the occupation of lower lying magnetic states in which more spins are paired. X-band (9.5 GHz) electron paramagnetic resonance (EPR) spectra of powder sample consist of a single line at g~2.01 that is characteristic of Fe3+ ions in a tetrahedral environment, thus, confirming the Mössbauer results. Further analysis of the EPR line shape reveals the presence of two types of Fe6 magnetic species with an intensity ratio of ~1:9. Both species have Lorentzian line shapes and indistinguishable g-factors but differ in the peak-to-peak line widths (δBpp). The line width ratio δBpp(major)/δBpp(minor) ~ 3.6 correlates well with the ratio of the Weiss constants, θminor/θmajor ~ 4.
“…A similar effect was observed for [Fe 14 O 10 (OH) 4 (Piv) 18 ] where the room temperature moment was only about 20% of the spin-only value. 14 …”
Section: Resultsmentioning
confidence: 99%
“…10 Furthermore, when such rings contain magnetic ions, such as manganese, molybdenum or iron, they typically exhibit complex magnetic interactions. 11 Over the years, a number of iron containing molecular ring structures, referred to as ferric wheels, 12,13 have been crystallized via solution routes, including [Fe(OMe) 2 (O 2 CCH 2 Cl)] 10 , 13 [Fe 14 O 10 (OH) 4 (Piv) 18 (HPiv = pivalic acid) 14 and [Fe(OH)(C 30 H 38 N 2 O 8 )Fe 2 (OCH 3 04(O 2 CCH 3 ) 2 ]6. 15 …”
Single crystals of a new iron containing oxide, Ba4KFe3O9, were grown from a hydroxide melt and the crystal structure was determined by single crystal x-ray diffraction. This ferrite represents the first complex oxide containing isolated 6-member rings of corner sharing FeO4 tetrahedra. Mössbauer measurements are indicative of two tetrahedral high-spin Fe3+ coordination environments. The observed magnetic moment (~3.9 BM) at 400 K is significantly lower than the calculated spin-only (~5.2 BM) value indicating the presence of strong antiferromagnetic interactions in the oxide. Our density functional calculations confirm the strong antiferromagnetic coupling between adjacent Fe3+ sites within each 6-member ring and estimate the nearest neighbor spin exchange integral as ~200 K; next nearest neighbor interactions are shown to be negligible. The lower than expected effective moment for Ba4KFe3O9 calculated from χT data is explained as resulting from the occupation of lower lying magnetic states in which more spins are paired. X-band (9.5 GHz) electron paramagnetic resonance (EPR) spectra of powder sample consist of a single line at g~2.01 that is characteristic of Fe3+ ions in a tetrahedral environment, thus, confirming the Mössbauer results. Further analysis of the EPR line shape reveals the presence of two types of Fe6 magnetic species with an intensity ratio of ~1:9. Both species have Lorentzian line shapes and indistinguishable g-factors but differ in the peak-to-peak line widths (δBpp). The line width ratio δBpp(major)/δBpp(minor) ~ 3.6 correlates well with the ratio of the Weiss constants, θminor/θmajor ~ 4.
“…Tables S2 and S3), [33] ATR-FT-IR ( Figures S2-S6), and Mçssbauer studies (Figures S7-S9) did not provide any indication for the presence of Fe II .T hus,o ne oxo or one ethoxo group has to be protonated for charge balance. [34] Moreover,I Rs pectroscopic studies point to as ignificant intramolecular proton transfer between m 3 -oxo groups and ethoxo ligands (Supporting Information, Figures S2-S6). Therefore,t he formula of this new aggregate should be [Fe 19…”
mentioning
confidence: 99%
“…[34] Moreover,I Rs pectroscopic studies point to as ignificant intramolecular proton transfer between m 3 -oxo groups and ethoxo ligands (Supporting Information, Figures S2-S6 Figure 2A) exhibits an approximate O h symmetry.T he aggregate comprises six m 6 -oxo groups that surround the central iron site in anearly perfect octahedral manner ( Figure 2D). Its structure can be considered as a3 De xtract from the rock salt or Wüstite lattice ( Figure 2B,C).…”
The syntheses, crystal structures, and physical properties of [HFe19 O14 (OEt)30 ] and {Fe11 (OEt)24 }∞ are reported. [HFe19 O14 (OEt)30 ] has an octahedral shape. Its core with a central Fe metal ion surrounded by six μ6 -oxo ligands is arranged in the rock salt structure. {Fe11 (OEt)24 }∞ is a mixed-valence coordination polymer in which Fe(III) metal ions form three 3D interpenetrating (10,3)-b nets. The arrangement of the Fe(III) ions can also be compared to that of Si ions in α-ThSi2 . Thus, the described structures are at the interface between molecular and solid-state chemistry.
“…Da Va lenzsummenberechnungen (Tabellen S2 und S3 der SI) [33] sowie ATR-FT-IR-(Abbildungen S2-S6 der SI) und Mçßbauer-spektroskopische Untersuchungen (Abbildungen S7-S9 der SI) das Vorhandensein von Fe II -Ionen ausschließen, muss zum Ausgleichen der Ladungsbilanz eine Oxo-oder eine Ethoxo-Gruppe protoniert sein. [34] Diese Hypothese wird durch IR-spektroskopische Untersuchungen bestätigt, die darüber hinaus auf einen intramolekularen Protonentransfer zwischen den m 3 -Oxo-und den Ethoxo-Gruppen schließen 6 ]-Einheit. [35] So gesehen ist diese interessante ionische Verbindung keine korrekte Erweiterung der Lindqvist-Architektur und muss daher als beispiellose,e igenständige Polyoxometallatstruktura ngesehen werden.…”
[2][3][4] 18, [5,6] 17, [7][8][9] 16, [10,11] 14 [12][13][14] und 13 [15,16] [24][25][26] Bisher wurde nur über sehr wenige molekulare Metall-Sauerstoff-Verbindungen mit mehr als drei m 6 -Oxo-Gruppen berichtet. [27][28][29][30] Ziel dieser Arbeit war die Synthese mehrkerniger EisenSauerstoff-Spezies mit mehr als zwei m 6 -Oxo-Gruppen. Zur Bildung hochaggregierter,k ugelfçrmiger Metall-SauerstoffVerbindungen schienen uns kleine organische Reste einfacher Alkoxo-Gruppen, wie Methoxo-oder Ethoxo-Gruppen, am ehesten geeignet. 24 ]( 1)k onnte durch Einkristallstrukturanalyse charakterisiert werden (Abbildungen 1u nd 2; Tabelle S1 der SI). [46] Komplex 1 enthält ausschließlich Fe III -Ionen. Da Va lenzsummenberechnungen (Tabellen S2 und S3 der SI) [33] sowie ATR-FT-IR-(Abbildungen S2-S6 der SI) und Mçßbauer-spektroskopische Untersuchungen (Abbildungen S7-S9 der SI) das Vorhandensein von Fe II -Ionen ausschließen, muss zum Ausgleichen der Ladungsbilanz eine Oxo-oder eine Ethoxo-Gruppe protoniert sein.[34] Diese Hypothese wird durch IR-spektroskopische Untersuchungen bestätigt, die darüber hinaus auf einen intramolekularen Protonentransfer zwischen den m 3 -Oxo-und den Ethoxo-Gruppen schließen
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