首页> 外文期刊>European journal of inorganic chemistry >Anomalous Difference in Magnetic Behavior between Highly Saddled Iron(III) Porphyrin Complexes in the Solid State
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Anomalous Difference in Magnetic Behavior between Highly Saddled Iron(III) Porphyrin Complexes in the Solid State

机译:固态高度鞍化的铁(III)卟啉配合物之间的磁行为异常差异

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The spin states of microcrystalline samples of [Fe(OMTPP)L_2]~+ (L=DMAP or Py) have been examined and interpreted using Mossbauer spectroscopy,SQUID magnetometry and X-ray crystallography.The Mossbauer spectra of [Fe(OMTPP)(DMAP)_2]~+ and [Fe(OMTPP)Py_2]~+ showed that both of these complexes maintain the low-spin (S=1/2) state over the 77-300 K temperature range.The spin states of these complexes were further confirmed by SQUID magnetometry.Thus,the magnetic behavior of [Fe(OMTPP)Py_2]~+ is quite different from that of the structurally related species [Fe(OETPP)Py_2]~+.The latter complex exhibits a novel spin crossover between the S=3/2 and S=1/2 states as revealed by the spectroscopic and magnetic measurements.In order to understand the reasons for the absence of the spin crossover process of [Fe(OMTPP)Py_2]~+,we have comopared the crystal and molecular structures of [Fe(OMTPP)Py_2]~+ with those of the recently reported species [Fe(OETPP)Py_2]~+.In the case of [Fe(OMTPP)Py_2]~+,the Fe-N_(axial) bond lengths hardly change with temperature and are 2.058(6) and 2.024(4) A at 298 and 80K,respectively.These results are in sharp contrast to those of the spin crossover complex [Fe(OETPP)Py_2]~+,in which the Fe-N_(axial) bonds contract from 2.201(3) A at 298 K to 1.993(3) A at 80 K.We have ascribed the difference in magnetic behavior between [Fe(OMTPP)Py_2]~+ and [Fe(OETPP)Py_2]~+ to the difference in molecular packing;the former adopts a densely packed cubic crystal system while the latter shows a less condensed monoclinic system.A cavity calculation has further confirmed the above mentioned assumption.While the cavity sizes around the pyridine ligands in [Fe(OETPP)Py_2]~+ are 32.08 and 28.88 A~3 at 298 K,that in [Fe(OMTPP)Py_2]~+ is only 19.81 A~3.Furthermore,the cavities contract by 17.7% in [Fe(OETPP)Py_2]~+ when the temperature is lowered from 298 to 80 K whereas the contraction is only 5.3% in the case of [Fe(OMTPP)Py_2]~+.On the basis of these results,we have concluded that the loosely packed crystal system and the wide cavities around the axial ligands are the important requirements for the occurrence of the spin crossover process in the solid state.
机译:[Fe(OMTPP)L_2]〜+(L = DMAP或Py)微晶样品的自旋态已通过Mossbauer光谱,SQUID磁力分析和X射线晶体学检查和解释。[Fe(OMTPP)( DMAP)_2]〜+和[Fe(OMTPP)Py_2]〜+表明这两种配合物在77-300 K的温度范围内均保持低自旋(S = 1/2)状态。因此,[Fe(OMTPP)Py_2]〜+的磁行为与结构相关物种[Fe(OETPP)Py_2]〜+的磁行为完全不同。后者的复合物表现出新颖的自旋交叉通过光谱和磁学测量揭示了在S = 3/2和S = 1/2之间的关系。为了理解[Fe(OMTPP)Py_2]〜+没有自旋交叉过程的原因,我们有使[Fe(OMTPP)Py_2]〜+的晶体和分子结构与最近报道的物种[Fe(OETPP)Py_2]〜+的晶体和分子结构相比更难。在[Fe(OMTPP)Py_2]〜+的情况下,Fe -N_(轴向)键长几乎不随温度变化,在298和80K时分别为2.058(6)和2.024(4)A。这些结果与自旋交联复合物[Fe(OETPP)Py_2]形成鲜明对比。 〜+,其中Fe-N_(轴向)键从298 K时的2.201(3)A收缩到80 K时的1.993(3)A收缩。我们已将[Fe(OMTPP)Py_2]之间的磁行为差异归因于+和[Fe(OETPP)Py_2]〜+表示分子堆积的差异;前者采用密集堆积的立方晶体系统,而后者则表现出较不凝结的单斜晶系统。型腔计算进一步证实了上述假设。 [Fe(OETPP)Py_2]〜+吡啶配体周围的空穴尺寸为298 K时分别为32.08和28.88 A〜3,而[Fe(OMTPP)Py_2]〜+的吡啶配体周围的空穴尺寸仅为19.81 A〜3。此外,空穴收缩当温度从298 K降低到80 K时,[Fe(OETPP)Py_2]〜+的收缩率为17.7%,而[Fe(OMTPP)Py_2]〜+的收缩仅为5.3%。 ,我们有总结认为松散堆积的晶体系统和轴向配体周围的宽腔是固态发生自旋交叉过程的重要要求。

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