MeBeF_4(Me=Ca,Sr,Ba)中钐的价态及光谱

讨论了MeBeF_4基质中钐离子的光谱及价态.还原气氛中仅在SrBeF_4和BaBeF_4中观察到了Sm~(2+)的发射.

INVESTIGATION ON THE LUMINESCENCE PROPERTIES OF DY3+ AND EU3+ IN M3LN2(BO3)4 (M=CA, SR, BA, LN= LA, GD, Y)

In this paper, the luminescence properties of Dy3+ and Eu3+ in M3Ln2 (BO3)4 (M = Ca,Sr,Ba; Ln = La, Gd, Y) were systematically studied. The hypersensitive transitions of Dy3+ and Eu3+ were investigated in relation to the host compositions; the relationship between the energy of Eu3+ charge-transfer band and M2+ ion was discussed, and the concentration quenching of Dy3+ luminescence was reported.

THE COMPOSITIONS AND STRUCTURES OF SOME COMPOUNDS IN THE SYSTEM CA-SR-CU-O

The system of Ca-Sr-Cu-O have been investigated. Two new compounds with compositions Sr3Cu5O8+alpha and CaSrCu3O5+alpha have been discovered. Both are orthorhombic with a = 6.489, b = 11.280, c = 12.240 angstrom for CaSrCu3O5+alpha and a = 3.950, b = 11.479, c = 13.420 angstrom for Sr3Cu5O8+alpha. The X-ray powder data for CaSrCu3O5+alpha, Sr3Cu5O8+alpha, Sr2CuO3 and SrCuO2 are presented. The oxidation state of Cu ion and oxygen contents are analyzed by iodometric titration. Sr0.5Ca0.5CuO2 that has a similar structure with SrCuO2 has been found and its X-ray data are presented also.

高Jc Ag-Bi-Pb-Sr-Ca-Cu-O超导材料

Bi_2Sr_2Ca_2Cu_3O_y-Ag_x、Bi_(1.7)Pb_(0.3)Sr_2Ca_2Cu_3O_y-Ag_x和Bi_(1.7)Pb_(0.3)Sr_2Ca_2Cu_(3.2)O_y-Ag_x系列的超导材料是用固相反应的方法合成的。原料为分析纯AgNO_3、PbO、Bi_2O_3、CaCO_3、SrCO~3和CuO。把试剂按所需配比混和研磨后,在800℃烧12h,研磨压片,片子在850℃烧结200h,破碎、研磨后,按配比加入AgNO_3·800℃灼烧12h,再次研磨、压片,850℃再烧结200h,炉冷至室温。

Ca-Sr-Cu-O系中若干化合物的组成和结构的研究

研究了Ca-Sr-Cu-O三元金属复合氧化物体系,发现了两个新化合物Sr_3Cu_5O_(8+x)和CaSrCu_3·O_(5+x),两者都属正交晶系,前者a=3.950,b=11479,c=13.420 A.后者a=6.489,b=11.280,c=12.240A.文中给出了这两个化合物和SrCuO_2、Sr_2CuO_3的XRD谱.用碘量法测定了化合物中的氧含量.此外还发现了结构与SrCuO_2相似的固溶体Sr_(0.5)Ca_(0.5)CuO_2,也测定了它的XRD谱.

组成和制备条件对Bi-Pb-Sr-Ca-Cu-O材料超导电性的影响

制备了一系列 Bi—Pb—Sr���Ca—Cu—O 超导材料。在一定范围内,不同组分的 Bi—Pb—Sr���Ca—Cu—O 样品都能得到接近单110K 相的材料,但样品性能差别极大.性能的好坏极大地依赖着组成条件。烧结温度过高或过低都不利于提高样品的临界电流密度,850℃的烧结温度是较合适的,长时间烧结有利于110K 相的形成。样品烧结完成后,应缓慢降温退火,以保证材料充分吸氧。

Bi-Sr-Ca-Cu-O体系中可能存在一个新的高T_c超导相

最近,Pb能加强BiSrCaCuO超导体中高T_c相(即2223相,其c(?)37,T_c(?)110K)的出现和掺入sb形成BiPbSbSrCaCuO的T_c可以达到132 K已见报道,我们希望通过其它元素的掺杂取代也出现类似的结果。我们做了大量掺Sb、Ba、In的实验,通过改变

Dy~(3+),Sm~(3+)和Ce~(3+)离子在M_3La_2(BO_3)_4(M=Ca,Sr,Ba)中光谱性质的研究

本文报导了Dy~(3+),Sm~(3+)和Ce~(3+)离子在M_3La_2(BO_3)_4(M=Ca,Sr,Ba)基质中的激发与发射光谱;研究了Dy~(3+)离子黄蓝发射的相强度随基质化合物的组成和结构的不同而呈现的变化规律;讨论了Sm~(3+)离子电荷迁移激发带的能量与基质中近邻阳离子的关系并分析了Sm~(3+)和Eu~(3+)离子4f电子构型对电荷迁移带能量的影响。本文还给出了Dy~(3+),Sm~(3+)和Ce~(3+)离子发光的浓度淬灭值。

Major element, trace element, and Sr, Nd and Pb isotope studies of Cenozoic basalts from the South China Sea

The whole rock K-Ar ages of basalts from the South China Sea basin vary from 3.8 to 7.9 Ma, which suggest that intra-plate volcanism after the cessation of spreading of the South China Sea (SCS) is comparable to that in adjacent regions around the SCS, i.e., Leiqiong Peninsula, northern margin of the SCS, Indochina block, and so on. Based on detailed petrographic studies, we selected many fresh basaltic rocks and measured their major element, trace element, and Sr-Nd-Pb isotope compositions. Geochemical characteristics of major element and trace element show that these basaltic rocks belong to alkali basalt magma series, and are similar to OIB-type basalt. The extent of partial melting of mantle rock in source region is very low, and magma may experience crystallization differentiation and cumulation during the ascent to or storing in the high-level magma chamber. Sr-Nd-Pb isotopic data of these basaltic rocks imply an inhomogeneous mantle below the South China Sea. The nature of magma origin has a two end-member mixing model, one is EM2 (Enriched Mantle 2) which may be originated from mantle plume, the other is DMM (Depleted MORB Mantle). Pb isotopic characteristics show the Dupal anomaly in the South China Sea, and combined with newly found Dupal anomaly at Gakkel ridge in Arctic Ocean, this implies that Dupal anomaly is not only limited to South Hemisphere. In variation diagrams among Sr, Nd and Pb, the origin nature of mantle below the SCS is similar to those below Leiqiong peninsula, northern margin of the SCS and Indochina peninsula, and is different from those below north and northeast China. This study provides geochemical constraints on Hainan mantle plume.

7.0Ma以来中国黄土粉尘源区的化学风化历史研究-Sr���位素比值的证据

To investigate the changes in the chemical weathering intensity of dust source region in Asia continent, ~(87)Sr/~(86)Sr ratios of acid-washed residues from the loess deposits in China and Tajikistan were analyzed, respectively. The results and conclusions are listed as below. 1. The oscillation of ~(87)Sr/~(86)Sr ratios of acid-insoluble residues in the Chinese Loess Plateau was mainly attributed to the chemical weathering intensity of the source region and the grain size. Counteracted the effect of particle size, the calibrated 87Sr/S6Sr ratio can be used as a proxy for the chemical weathering intensity of the source region. 2. The Sr/ Sr ratios of red clay-loess sequence from the Loess Plateau indicate that the chemical weathering intensity of the dust source region between 7.0 and 2.6 Ma is stronger than that in the Quaternary period. This also suggests a general decline in chemical weathering intensity of the source region from 2.6 Ma to the present. Such pattern is more remarkable since 1.0 Ma BP. 3. The ~(87)Sr/~(86)Sr ratios of the Tajik loess during 0.8-1.8 Ma is much more higher than those from 0.8 Ma to the present. This implies that the chemical weathering intensity of the source region in Central Asia is much stronger during 0.8-1.8 Ma than the period since 0.8 Ma. 4. The record of Sr isotope ratios from both sections shows an accelerating course of aridity of the Asian dust source region over the Quaternary period.

生物壳体Sr���Ca、Mg／Ca、^87Sr���^86Sr���值在恢复古气候、古环境中的应用—以小渡口剖面为例

生物壳体的Sr/Ca、Mg/Ca比值能反映其沉积水体的Sr/Ca、Mg/Ca比值，在一定条件下反映水体的盐度、温度，并分别与宿生水体的盐度、温度呈正比关系。生物壳体的^87Sr/^86Sr���值是恢复盆地古水文条件的一种重要手段。本文以著名的泥河湾盆地小渡口剖面的第28层为实例，力图通过对有孔虫、介形虫、腹足类生物壳体Sr/Ca、Mg/Ca比值与^87Sr/^86Sr���值的对比研究，并结合前人所作的中更新世古地理特征研究，来恢复生物壳体沉积时泥河古湖水的温度、盐度，进而进行古气候、古环境的恢复。研究结果表明：在0.97-0.94Ma间，古泥河湾湖为一陆相湖泊，湖水的温度、盐度变化趋势相吻合，均呈低－高－低的演化特征，可能对应着盆地水体的扩展－退缩－扩展变化。其中，在0.96-0.95Ma间，古泥河湾湖具有较高的温度、盐度特征。生物壳体的Sr/Ca、Mg/Ca比值能反映其沉积水体的Sr/Ca、Mg/Ca比值，在一定条件下反映水体的盐度、温度，并分别与宿生水体的盐度、温度呈正比关系。生物壳体的^87Sr/^86Sr���值是恢复盆地古水文条件的一种重要手段。本文以著名的泥河湾盆地小渡口剖面的第28层为实例，力图通过对有孔虫、介形虫、腹足类生物壳体Sr/Ca、Mg/Ca比值与^87Sr/^86Sr���值的对比研究，并结合前人所作的中更新世古地理特征研究，来恢复生物壳体沉积时泥河古湖水的温度、盐度，进而进行古气候、古环境的恢复。研究结果表明：在0.97-0.94Ma间，古泥河湾湖为一陆相湖泊，湖水的温度、盐度变化趋势相吻合，均呈低－高－低的演化特征，可能对应着盆地水体的扩展－退缩－扩展变化。其中，在0.96-0.95Ma间，古泥河湾湖具有较高的温度、盐度特征。

贵州黄壤地区植物营养元素来源的Sr���位素示踪

为研究植物营养元素来源，对贵州龙里地区黄壤上生长的12种主要植物的部分营养元素含量及Sr���位素特征进行了分析。结果表明：喀斯特地区黄壤上的植物具有高钙含量，营养元素含量由高到低排序为Ca〉K〉Mg；研究区植物的Ca、K、Sr���均含量均高出报道的陆生植物的平均含量，但比贵州地区同样以灰岩为母质发育而来的石灰土上生长的植物低；植物样品的^87Sr���^86Sr���位素比值变化范围在0．70856～0．71145之间。基于锶同位素组成的端员模式计算结果表明，除了苔藓、石松的营养元素主要来源于大气输入外，其他植物的营养元素主要来源于土壤风化.