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Synthesis and magnetic properties of centennialite: a new S=1/2 Kagome antiferromagnet and comparison with herbertsmithite and kapellasite

机译:百年长石的合成和磁性:一种新的S = 1/2 Kagome反铁磁体,并与赫氏铁矿和针叶石进行比较

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Minerals of the atacamite group such as herbertsmithite and kapellasite have recently attracted enormous attention as the S = A1/2 Kagom, antiferromagnets for achieving the quantum spin liquid (QSL) state with diverse technological applications. Herein we report on the synthesis of the newly discovered mineral centennialite by using an unconventional "solid-state" reaction method at 463 K. Synthetic centennialite, Ca1.06Cu2.94Cl2.01(OH)(5.99)center dot 0.73H(2)O, has been characterized by scanning electron microscopy, electron microprobe analyses, Fourier-transform infrared spectroscopy, thermogravimetric and differential scanning calorimetric analyses, single-crystal X-ray diffraction structure refinements, and magnetic susceptibility measurements. The crystal structure of centennialite is characterized by a perfect (threefold symmetry) Kagom, layer with < 5 % substitution between Ca and Cu and therefore differs from those of herbertsmithite and kapellasite, in which 15-25 % mixing between similar Zn and Cu atoms dramatically affects the QSL state. Centennialite remains antiferromagnetic down to similar to 7 K with a moderate spin frustration (i.e., a Weiss temperature theta = -56 K and a spin frustration parameter f = 8), but exhibits a canted antiferromagnetic ordering with a ferromagnetic component at lower temperatures.
机译:随着S = A1 / 2 Kagom(反铁磁体,用于通过多种技术应用实现量子自旋液体(QSL)状态)的合成,塔卡蒙铁矿的矿物(如铁矾石和钾铝矾石)最近受到了极大的关注。在这里,我们通过在463 K上使用非常规的“固态”反应方法报告了新发现的矿物百年长石的合成。合成百年长石,Ca1.06Cu2.94Cl2.01(OH)(5.99)中心点0.73H(2) O通过扫描电子显微镜,电子显微探针分析,傅立叶变换红外光谱,热重和差示扫描量热分析,单晶X射线衍射结构细化以及磁化率测量来表征。百年长石的晶体结构具有完美的(三对称性)Kagom层,Ca和Cu之间的取代度小于5%,因此不同于赫伯铁矿和kapellasite的层,在后者中,相似的Zn和Cu原子之间的混合比例高达15-25%影响QSL状态。百年长石在具有适度的自旋失意度(即Weiss温度theta = -56 K和自旋失意度参数f = 8)的情况下仍可降低至约7 K的反铁磁性,但在较低温度下表现出倾斜的反铁磁有序性。

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