碳纳米管模板对 YBO3：Eu3＋（5％）结构、形貌及光致发光的影响

在前驱体溶液中添加和不添加碳纳米管，采用简单的水热合成法并在1000℃下烧结，获得树枝状和类球状纳米结构的 YBO3：Eu3＋样品．研究表明：对于树枝状结构的样品，其红色和橙色光的强度比更高，且其CIE 坐标为（0．67，0．33），几乎与商业红色荧光粉 Y2 O2 S ：Eu3＋的色坐标相同，可见树枝状结构的红色荧光粉YBO3：Eu3＋在纳米器件和照明器件中具有潜在应用价值．该文还对样品的发光性质和机制做了解释．     

多壁碳纳米管和 pH 值对 YBO3：Eu（5％）的形貌和发光的协同效应

用添加有多壁碳纳米管（MWCNT ）的前驱体溶液，通过水热合成法，在260℃条件下制备了一系列YBO3：Eu3＋样品。当前驱体溶液的pH值从5到10的范围变化时，所制备的样品表现出丰富的形貌，包括鼓状、片状、六面体状、六角状和花状颗粒，这是由碳纳米管表面接枝官能团与前驱体溶液中不同形式 HBO3的协同效应所致。发光测量结果表明p H＝9和10的样品的红／橙（R／O ）比提高了，表现出更好的色纯度，这归因于晶界或颗粒表面的E u3＋具有较低的局部对称性。     

LaP04：Eu3＋^纳米晶的溶剂热合成及下转换荧光性质研究

采用溶剂热法,在乙醇和乙二醇的混合溶剂中,pH=8．5条件,150℃,反应12h,一步合成了LaPO4Eu3＋^晶体．室温下,用x射线衍射对材料的组成进行了表征,XRD数据表明,成功合成了LaPO4Eu^3＋^晶体．荧光光谱分析表明,在352nm紫外光激发下,其发射峰在531nm、640nm,分别对应着Eu^3＋的。Do3＋^→VF^3＋和5^D0→7^F3能级跃迁．并讨论了离子La3＋^：Eu3＋^不同浓度掺杂比对荧光性质的影响,结果表明,Eu3＋^的最佳掺杂浓度比为10％．     

邻菲啰啉衍生物及其铕配合物的合成、表征及光物理性能

为改变铕配合物配体的结构,增强其紫外-可见吸收率,寻找红光效率更高的发光材料,以乙酰丙酮为第一配体,邻菲啰啉及其衍生物为第二配体,合成了5个稀土铕配合物,并进行了1H NMR、MS、IR、元素分析等表征,测定了目标配合物的紫外、荧光光谱和电化学性质.结果表明:随着第二配体共轭结构的变化,铕配合物在紫外区的吸收逐渐增强,荧光发射峰均约为612 nm,发光强度随配体共轭程度的增加而增大;电化学数据与铕配合物的发射波长相匹配,证明强紫外-可见吸收率配体的引入极大地提高了配合物发光效率.     

Eu-Ru共掺NiO-SnO2复合纳米粒子薄膜的阻变特性

通过低温水浴法制备了Eu-Ru共掺杂NiO-SnO2复合纳米粒子，透射电镜图像显示纳米粒子粒径均匀，选区电子衍射表明结晶性差，所测晶面间距与SnO2和NiO相应卡片数据一致，水热机理分析表明纳米粒子由NiO-SnO2微观p-n结组成.原子力显微镜测试薄膜表面平均粗糙度约025nm，由于薄膜太薄及样品结晶性差，XRD分析未见明显衍射峰.电学测试表明纳米粒子薄膜具有可重复双极阻变特性，阈值电压约1V，开关比约500.薄膜高阻态电学输运符合缺陷俘获载流子所致空间电荷限制导电机制，低阻态呈欧姆特性，故阻变机理应为电荷俘获及再释.     

红色荧光粉Ca_3B_2O_6:Eu~(3+)的制备及发光性能

采用高温固相法合成了Ca3B2O6:Eu3+红色荧光粉,并对其发光性质进行了研究.样品的激发光谱由位于220~350 nm的带状谱和350~500 nm的一系列窄带组成,这些窄带是由Eu3+的f-f跃迁引起的,光谱峰值分别为280,396和469 nm.它可以被近紫外光辐射二极管管芯产生的350~410 nm辐射有效激发.用396 nm激发得到样品的发射光谱,峰值位于578,590,610,618和650 nm,分别由Eu3+离子的5D4→7FJ(J=0,1,2,3)跃迁引起的.研究了Eu3+离子浓度和电荷补偿剂对发射光谱的影响.结果显示随着Eu3+浓度增加,发光强度逐渐增强,未发现浓度猝灭现象.掺入Li+,Na+,K+3种离子作为电荷补偿剂,均提高了样品的发光强度,其强度从大到小依次为I(Li+)I(Na+)I(K+),说明Li+是最佳的电荷补偿剂.     

Partial melting of the dry mafic continental crust: Implications for petrogenesis of C-type adakites

C-type adakites have been commonly considered as a result of partial melting of the mafic lower continental crust (LCC) at high pressure, as supported by high P-T experiments on hydrous basalts. However, because the mafic eclogitic LCC is generally dry, experiments on water-bearing materials cannot be used to constrain the melting processes of the dry mafic LCC. Due to the lack of systematic melting experimental studies on dry mafic rocks at crustal pressures, MELTs software was applied to simulating melting of the dry mafic LCC at 1–2 GPa. Comparison of model results with experimental data indicates that, when melting degree is greater than 20%, melts from the dry mafic LCC at 1–3 GPa cannot produce the C-type adakitic melt with high SiO₂ content (~70%). Although the limited experimental results about dry mafic rock melting at 1–2 GPa in the literature suggest that low degree melting (<10%) cannot produce silicic melt either, MELTs software simulation shows that, at pressure >1.8 GPa, low-degree melting can produce dacitic melt with high K₂O/Na₂O (~1) if SiO₂ content of the melt is controlled by residual garnet. Furthermore, the simulation also suggests that, if pressure is <1.8 GPa, abundant plagioclase (plg) in the residual phase may decrease SiO₂ content in the melt to below 62%, much lower than that of the C-type adakites observed in eastern China. Given the high P-T conditions required to produce melts with high SiO₂ and extremely low HREE contents, such melts could easily be contaminated by other crustal-derived melts, implying that the C-type adakites from eclogite melting could be less commonly observed in the outcrops than previously believed. Besides the interpretation that garnet fractionates Sr, Y, and REE, high Sr/Y and La/Yb could be also produced by multiple ways such as inheriting the source features and fractional crystallizing clinopyroxene (cpx). Therefore, it may be problematic using high Sr/Y and La/Yb as criteria to identify adakites. Instead, REE patterns with strong depletion of HREE relative to MREE (e.g. high Gd/Yb) could be a better parameter to identify the role of garnet and thus adakites. Finally, geochemical models based on MELTs simulation indicate that Eu anomaly cannot be simply used to constrain the role of plg in magmatism because Eu anomaly in the melt is a function of source characteristics, oxygen fugacity (fO₂) of magmatic systems, and plg/mafic minerals mode ratio.     

KPb2Cl5晶体中掺杂Er3+和Eu3+离子占据格位倾向性的原子模拟研究

本文采用经验势原子方法模拟研究了稀土Er3+和Eu3+离子掺入KPb2Cl5晶体的格位占据情况,其中经验势参数通过拟合KPb2Cl5、PbCl2、ErCl3、EuCl3晶体结构得到.在此基础上,研究了KPb2Cl5晶体的本征缺陷和替代缺陷,而且通过溶解反应能计算发现,掺杂Er3+/Eu3+离子更倾向于占据Pb2格位,并由最近邻的K空位缺陷提供电荷补偿.这一结论与文献报道的KPb2Cl5:Eu3+光谱分析结果一致,为Er3+掺杂KPb2Cl5占据格位实验假设提供理论支持.     

化学共沉淀法制备Ca_2MgSi_2O_7：Eu~（2＋）荧光粉

以Ca（NO3）2.4H2O、Mg（NO3）2.6H2O、Na2SiO3.9H2O、Eu2O3为原料,采用化学共沉淀法制备了Ca2MgSi2O7：Eu2＋绿色荧光粉.其激发光谱分布在300～480 nm波长范围,谱峰位于310～385 nm,可以被InGaN管芯产生的360～480 nm辐射有效激发;在430 nm激发...     

矿化剂辅助水热法生长Eu掺杂ZnO材料研究

采用温和的水热法、三种不同的矿化剂成功合成了稀土铕(Eu)掺杂的氧化锌(ZnO)样品,并利用XRD、SEM、TEM和XPS对样品的结构和形貌进行了表征和分析.结果表明:稀土Eu离子以+3价成功地掺入到ZnO晶格中.并且采用不同矿化剂可以得到了不同形貌的ZnO材料,三种矿化剂生长的ZnO的形貌分别为纳米棒、纳米针和纳米片.