LnGa_(1-x)Fe_xO_3(Ln=La,Pr,Nd)的磁化率研究

钙钛矿型含镓的稀土复合氧化物的发光及光谱性质已有研究和报道.进一步在稀土镓复合氧化物体系中掺进过渡元素Fe~(3+)离子,用XRD,XPS和IR方法研究了LaGa_(1-x)Fe_xO_3体系中磁性铁离子的自旋态及其对化合物结构,红外光谱等性质的影响.在此基础上,本文首次对LnGa_(1-x)Fe_xO_3(Ln=La,Pr,Nd)体系化合物的磁化率等磁性质进行初步探讨,以揭

SYNTHESES AND X-RAY STRUCTURES OF BIS(T-BUTYLCYCLOPENTADIENYL)LANTHANIDE CHLORIDE COMPLEXES [(BU(T)CP)2LNCL]2 (LN = PR, GD, ER)

Reaction of lanthanide trichlorides with two equivalents of sodium t-butylcyclopentadienide in THF gave rise to the bis(t-butylcyclopentadienyl)lanthanide chloride complexes [(Bu(t)Cp)2LnCl]2 (Ln = Pr, Gd, Er), which were characterized by elemental analysis, IR and H-1 NMR spectroscopy. In addition, the crystal structures of [(ButCp)2PrCl]2 (1) and [(ButCp)2GdCl]2 (2) were determined by single crystal X-ray diffraction at room temperature. The coordination number for Pr3+ and Gd3+ is 8 and the bond lengths Pr-Cl and Gd-Cl are 2.864(2) and 2.771(3) angstrom, respectively. The structural studies showed the complexes to have C2h symmetry.

(η~5-C_5H_5)Ln(η~8-C_8H_8)(THF)_n(Ln=Pr,Nd,Gd)的合成及(η~5-C_5H_5)Pr(η~8-C_8H_8)(THF)_2的晶体结构

自1969年首次报道稀土环辛四烯基化合物Eu(C_8H_8)和Yb(C_8H_8)的合成以来,相继合成K[Ln(C_8H_8)_2],[Ln(C_8H_8)Cl·2THF]_2和[Ln(C_8H_8)·2THF]等,还报

LnBa_2C_3O_(7-δ)(Ln=Pr、Y)体系的XPS研究

该文研究了YBa_2Cu_3O_(7-δ)和PrBa_2Cu_3O_(7-δ)两体系的XPS谱图,结果表明从XPS图中难以判断三价铜的存在,与YBa_2Cu_3O_(7-δ)体系相比,PrBa_2Cu_3O_(7-δ)体系中Ba的结合能低,O_(18)的两个状态变得模糊不清。讨论了空穴浓度对高T_c超导电性的影响。

SYNTHESIS AND CRYSTAL-STRUCTURE OF HETEROPOLY MOLYBDOSILICIC LANTHANIDE K10H3[PR(SIMO11O39)2].18H2O

The intensity data of the title complex were collected at a low temperature of -90-degrees-C. The compound crystallizes in the monoclinic space group P2(1)/n, a = 17.504(2), b = 27.323 (5), c = 21.616(4) angstrom, beta = 104.49 (2)degrees, Z = 4. The structure was solved by Patterson and Fourier techniques and refined by least-squares to an R = 0.088 for 8320 independent reflections. The central Pr ion is bonded to eight oxygen atoms from two molybdosilicic heteropoly ligands to form a square antiprism. The Pr-O average distance is 2.44 (2) angstrom. Both molybdosilicic heteropoly ligands are of a defective alpha-Keggin structure.

THE SYNTHESES OF THE COMPLEXES (ETA-5-C5H5)LN(ETA-8-C8H8).NTHF AND (ETA-5-C9H7)LN(ETA-8-C8H8).2THF AND THE CRYSTAL-STRUCTURE DETERMINATION OF (ETA-5-C5H5)PR(ETA-8-C8H8).2THF AND (ETA-5-C9H7)PR(ETA-8-C8H8).2THF

LnCL3 reacts with NaC5H5 and K2C8H8 to yield the complexes (eta-5-C5H5)Ln(eta-8-C8H8).nTHF (Ln = Pr, Nd, n = 2; Ln = Gd, n = 1) and LnCl3 reacts with KC9H7 and K2C8H8 to yield the complexes (eta-5-C9H7)Ln(eta-8-C8H8).2THF (Ln = Pr, Nd; eta-5-C9H7 = indenyl); crystallography reveals (eta-5-C5H5)Pr(eta-8-C8H8).2THF and (eta-5-C9H7)Pr(eta-8-C8H8).2THF not to possess the parallel ring sandwich structure.

钙钛矿型LnGaO_3(Ln=La、Pr、Nd)晶体的光谱性质

本文报导了室温下钙钛矿型LnGaO_3(Ln=La、Pr、Nb)晶体的紫外、可见和红外吸收光谱的测定,对主要谱带进行了归属。从理论上计算出点阵振动数目和对称类型,并与实验结果进行了对比。晶体的色心及退火对吸收光谱的影响也做了研究。首次得到LaGaO_3和PrGaO_3晶体室温下的激发光谱和荧光光谱,观察到由于晶场环境不同引起荧光谱线窄化的现象。发现LaGaO_3晶体能够产主峰值为540nm的可见荧光,有成为色心发光晶体的可能性。

稀土钼硅杂多酸根配合物K_(10)H_3[Pr(SiMo_(11)·O_(39))_2]·18H_2O的合成及晶体结构

本文采用低温技术,在—90℃的干燥氮气保护下,收集标题化合物晶体的衍射数据,用重原子法解出结构。P2_1/n空间群,a=17.504(2),b=27.323(5),c=21.616(4),β=104.49(2)°,z=4.8320个衍射参与精修,最后的R值为0.088。中心离子Pr(Ⅲ)同2个钼硅杂多酸根中的8个氧原子键合,形成正方反棱柱配位多面体。Pr—O的平均键长为2.44(2)。钼硅杂多酸根配体具有缺位的α型Keggin结构。

NaLn(WO_4)_2晶体的研究(Ln=La,Pr,Nd)

用助熔剂缓冷法从Na_2WO_4—LiCl熔体中生长出NaLn(WO_4)_2(Ln=La,Pr,Nd)晶体。化学组成分析证明了所得晶体是NaLa(WO_4)_2、NaPr(WO_4)_2和NaNd(WO_4)_2。测定表明该类晶体属白钨矿型结构,四方晶系,空间群I4_1/a。计算了它们的晶胞参数,发现随着稀土元素(La、Pr、Nd)原子序数的增加,Ln~(3+)离子半径减小,Ln—O键长呈规律地递减,NaLn(WO_4)_2晶体的晶胞体积减小。测定了晶体的红外光谱和NaPr(WO_4)_2的激发光谱和荧光光谱。

Pr的部分取代对LnBa_2Cu_3O_(7-δ)超导电性的影响

本文合成了 Pr_xLn_(1-x)Ba_2Cu_3O(7-δ)系列化合物,讨论了稀土离子的价态、半径对超导电性及结构正交性的影响。

RE_(0.06)La_(0.94)Nb_2O_6Cl的制备与光谱性质(RE=Pr、Eu、Tb、Dy)

本文采用真空下气体输运技术制备RE_(0.06)La_(0.94)Nb_2O_6Cl(RE=Pr、Eu、Tb、Dy)小单晶和多晶粉末样品。测定其晶体结构与LaNb_2O_6Cl的晶体结构相同,为正交晶系;Eu_(0.06)La_(0.94)Nb_2O_6Cl小单晶的晶胞参数为:a=9.751,b=7.321,c=8.364。观察RE_(0.06)La_(0.94)Nb_2O_6Cl(RE=Pr、Eu、Tb、Dy)的特征激发光谱和发射光谱及其能量传递现象。

A unified criterion for initiation of sediment motion and inception of sheet flow under water waves

A unified criterion is developed for initiation of non-cohesive sediment motion and inception of sheet flow under water waves over a horizontal bed of sediment based on presently available experimental data. The unified threshold criterion is of the single form, U-o = 2 pi C[1 + 5(T-R/T)(2)](-1/4), where U-o is the onset velocity of sediment motion or sheet flow, T is wave period, and C and T-R are the coefficients. It is found that for a given sediment, U-o initially increases sharply with wave period, then gradually approaches the maximum onset velocity U-o = 2 pi C and becomes independent of T when T is larger. The unified criterion can also be extended to define sediment initial motion and sheet flow under irregular waves provided the significant wave orbital velocity and period of irregular waves are introduced in this unified criterion.