Nd:YIG中Nd3+基态多重态耦合对磁矩及磁光效应的影响

应用量子理论计算了Nd：YIG中Nd^3 离子基态多重态耦合对磁矩与磁光效应的影响。计算结果显示，当较高能级的多重态被考虑进来后，离子基态的能级分布与状态波函数要发生改变，从而对离子磁矩与Faraday偏转产生影响；多重态耦合对磁矩的影响不大，但对Faraday偏转的影响较大，计算过程中不可忽略。．     

K-rich lamellar exsolution in clinopyroxene： Constraint on the depth of peridotite source at Zhimafang

The oriented lamellar K-rich exsolutions within clinopyroxene host were recognized in garnet peridotite massif at Zhimafang in the Sulu ultrahigh pressure metamorphic terrane, eastern China. EMP and TEM analyses revealed that the composition and the index of electron diffraction for this exsolution are corresponding with phlogopite, and the shape is the lamellae with 1 μm in width and 5 to 30 μm in length. Moreover, the topotaxy is that the (001) of K-rich exsolution parallels to (I00) of the clinopyroxene host. The electron diffraction analyzing shows the exsolution is of a 1M polymorphism. The high-resolution lattice fringe image displays the stack features along [001], which only a layer mineral shows. We conclude that the clinopyroxene with IM and K-rich exsolution was probably derived from mantle depths over 240 km, thus resulting from decompressional exsolution in the initial stage of slab exhumation.     

Coupled isomorphic substitution and exsolution of pyroxene,rutile, apatite and quartz in supersilicic garnet

Dissolution of pyroxene in garnet at ultrahigh pressures produces supersilicie garnet with the coupled substitutions of Si^Ⅵ M^Ⅵ= A^Ⅵ A^Ⅵ and Si^Ⅵ Na^Ⅷ=A^Ⅵ M^Ⅷ,which are enhanced by rising pressure. The supersilicic garnet and exsolution of pyroxene, rutile, apatite and quartz in garnet during decompression were found in natural rocks,pointing to the importance in studying mantle-derived rocks and ultrahigh pressure metamorphism related to plate deep subduction. Ti, P, K and H2O enters garnet via the substitutions of Ti = Si, P^Ⅵ Na^Ⅷ = Si^Ⅵ CaⅧ, Si^Ⅵ K^Ⅷ = AI^Ⅵ M^Ⅷ, and [(OH)4]^4- = [SiO4]^4- or [4H]^4 = Si^4 respectively. The possible entering of Eskola pyroxene component M0.5AlSi2O6 in clinopyroxene, together with the common pyroxene component M2Si2O6, into garnet can lead to the presence of the substitution of Si^Ⅵ 0.5□^Ⅷ= A^Ⅵ 0.5M^Ⅷ in garnet structure, which plays a key role in the exsolution of rntile, apatite and quartz in garnet. Two new breakdown reactions are thus proposed on the basis of the new coupled substitution, which can be regarded as a theoretical model for the exsolntion of the 3 minerals in garnet. The real exsolution may be a combination of several breakdown reactions.     

Nd:YIG磁和磁光性质理论研究

应用量子力学理论计算了Ｎｄ：ＹＩＧ和Ｎｄ＾３＋在ＯＫ～３００Ｋ热力学温度范围内的磁矩及它对Ｆａｒａｄａｙ偏转的贡献，结果表明Ｎｄ：ＹＩＧ稀土次点阵的磁光疚主要来源于离子内４ｆ＾３→４ｆ＾２５ｄ电偶极跃迁，晶场和交换作用是决定磁矩和磁光效应的两具重要因素。在计算基组态的晶场劈裂时，必须考虑＾４Ｉ谱项的４个多重态间的混合，否则会引起较大误差，计算结果与实验符合良好。     

Y3Al5O12基质中Dy3+的浓度猝灭机制

采用溶胶-凝胶/燃烧合成法制备不同掺杂浓度的Dy:Y3Al5O12(YAG)发光粉体。分析基质晶体结构、Dy3+掺量对Dy3+光致发光性能的影响,并探讨Dy3+在Y3Al5O12基质中的自身浓度猝灭机制。根据激发光谱,Dy:YAG的主激发峰位置在353 nm,对应Dy3+的6H15/2→6P7/2跃迁。在Dy:YAG晶体结构中,Dy3+取代Y3+的位置具有D2对称性,故Dy:YAG的蓝光发射强度要高于黄光发射强度,且Dy3+最佳摩尔分数为0.02;Dy3+的4F9/2→6H15/2、6H13/2跃迁发射的浓度猝灭机制均为相邻中心的电偶极-电偶极相互作用引起的交叉弛豫(4F9/2+6H15/2→6H9/2+6F3/2)所造成的。     

明溪石榴石的宝石学特征

产于福建明溪的石榴石有两种类型 .一种为紫红色 ,具有主波长 5 85～ 5 88nm ,饱和度 0 .5 6 9～ 0 .6 2 9,折射率 1.74,密度 3.6 5～ 3.78g/cm3;另一种为褐红色 ,主波长 5 95～ 6 0 0nm ,饱和度 0 .86 6～ 0 .939,折射率1.75～ 1.76 ,密度 >3.8g/cm3.在RI -D图上 ,前者属镁铝榴石 ,而褐红色的石榴石落在铁铝榴石—镁铝榴石区域内 .明溪石榴石含有特征的钉状包裹体 .电子探针分析表明 ,紫红色的石榴石中含有较高的Cr,而褐红色的石榴石中则富含Fe和Ti.文章还探讨了明溪石榴石的吸收光谱特点及颜色成因 .     

Age of granulite from Huangtuling, Dabie Mountain: Pb-Pb dating of garnet by a stepwise dissolution technique

A new stepwise dissolution scheme, involving acids with different properties, enables the selective recovery of radiogenic and common Pb from a mineral, and makes single-mineral Pb-Pb dating possible. Garnet from a granulite sample from Huangtuling, northern Dabie Mountain yields a Pb-Pb isochron age of (1998 ±35) Ma, which is interpreted as the timing of peak metamorphism of granulite facies.     

Garnet granulite facies xenoliths from Yingfengling Cenozoic basalt in Leizhou, Guangdong Province

The granulite xenoliths are first found in Yingfengling pyroclastic rocks of Leizhou region, Guangdong Province. Of them high_pressure garnet granulite xenolith found is very sparse in China. Garnet granulite is different from pyroxene granulite in mineral assemblage and composition. \%P_T\% calculation shows that garnet granulite was formed at 1 130-1 160℃and 1.4-1.7 GPa, and pyriclasite at about 800℃and 0.65-0.80 GPa. High xenolith_derived paleogeotherm indicates Cenozoic rifting in Leizhou area. Granulites with varied mineral assemblages were formed at different depths by the metamorphism of the underplated basaltic melt.     

含钕石榴石磁光效应的量子理论

应用量子理论分析了含钕石榴石中Nd^3 离子的磁光效应；计算了50～300K温度范围内离子的Faraday偏转及300K时Faraday偏转与光子能量的函数关系．计算结果表明，Nd：YIG中Nd^3 离子的磁光效应主要源于离子内4f^3→4f^25d的电偶极跃迁；离子能级由于旋轨耦合、晶场作用及超交换作用而劈裂；实验观察到的Faraday偏转为顺磁性的．计算结果与实验符合良好．     

Yttrium zoning in garnet from the Xihuashan granitic complex and its petrological implications

The Xihuashan granitic complex is characterized by enrichment in rare-earth elements (REE). In particular, the second-stage granite (G-b) is markedly enriched in yttrium, and therefore contains complex associations of Y-bearing minerals. In this granite, garnet displays specific yttrium zoning with an Y-rich core and a “clean“ rim. Besides minute inclusions of Y-bearing minerals, garnet involves a striking amount of Y and HREE in its central area.It is suggested that enrichment in Y in the garnet core accords with that in the melt as a result of REE magmatic fractionation. However, the “clean“ rim may be the direct result of accumulation of fluid phases in the magma, which is virtually unfavorable for the entrance of REE in the garnet structure.