Santos Hellen S, Laihinen Tero, Rodrigues Lucas C V, Sinkkonen Jari, Mäkilä Ermei, Damlin Pia, Nakamura Liana K O, Brito Hermi F, Hölsä Jorma, Lastusaari Mika
Department of Chemistry, University of Turku, Turku, Finland.
Doctoral Programme in Physical and Chemical Sciences, University of Turku Graduate School (UTUGS), Turku, Finland.
Luminescence. 2019 Feb;34(1):23-38. doi: 10.1002/bio.3561. Epub 2018 Nov 13.
Trivalent europium (Eu ) and terbium (Tb ) ions are important activator centers used in different host lattices to produce red and green emitting materials. The current work shows the design of new clay minerals to act as host lattices for rare earth (RE) ions. Based on the hectorite structure, nano-chlorohectorites and nano-fluorohectorites were developed by replacing the OH present in the hectorite structure with Cl or F , thus avoiding the luminescence quenching expected due to the OH groups. The produced matrices were characterized through X-ray powder diffraction (XPD), transmission electron microscopy (TEM), FT-IR, Si MAS (magic angle spinning) NMR, nitrogen sorption, thermogravimetry-differential scanning calorimetry (TGA-DSC) and luminescence measurements, indicating all good features expected from a host lattice for RE ions. The nano-clay materials were successfully doped with Eu and/or Tb to yield materials preserving the hectorite crystal structure and showing the related luminescence emissions. Thus, the present work shows that efficient RE luminescence can be obtained from clays without the use of organic 'antenna' molecules.
三价铕(Eu)离子和铽(Tb)离子是用于不同基质晶格中以产生红色和绿色发光材料的重要激活中心。当前的工作展示了新型粘土矿物作为稀土(RE)离子基质晶格的设计。基于锂蒙脱石结构,通过用Cl或F取代锂蒙脱石结构中存在的OH,开发出了纳米氯代锂蒙脱石和纳米氟代锂蒙脱石,从而避免了因OH基团导致的发光猝灭。通过X射线粉末衍射(XPD)、透射电子显微镜(TEM)、傅里叶变换红外光谱(FT-IR)、29Si魔角旋转(MAS)核磁共振(NMR)、氮气吸附、热重-差示扫描量热法(TGA-DSC)和发光测量对所制备的基质进行了表征,结果表明其具有作为RE离子基质晶格所期望的所有良好特性。纳米粘土材料成功地掺杂了Eu和/或Tb,得到了保留锂蒙脱石晶体结构并显示出相关发光发射的材料。因此,当前的工作表明无需使用有机“天线”分子就能从粘土中获得高效的稀土发光。