水溶液中羟脯氨酸稀土配合物的NMR研究

测定了在11种稀土离子(La~(3+)、Pr~(3+)、Nd~(3+)、Eu~(3+)、Tb~(3+)、Dy~(3+)、Ho~(3+)、Er~(3+)、Tm~(3+)、Yb~(3+)和Lu~(3+)存在下羟脯氨酸~(13)C的诱导位移和抗磁性稀土配合物体系的~(1)H化学位移与偶合常数。对配合物构象分析表明,在水溶液中羟脯氨酸以空间位阻小的“外向”构象存在,通过羧基与稀土离子形成双齿配位结构,Ln~(3+)-O键长为2.1。在水溶液中巳配位的与游离的氨基酸和水分子间的快速配位交换平衡导致稀土氨基酸配合物具有有效轴对称性。

RBa_2Cu_3O_(7-δ)的结构和某些性质的变化趋势

本文用X射线衍射、碘量法,扫描电镜等手段系统地研究了RBa_2Cu_3O_7-δ[R=La、Nd、Sm、Gd、Dy、Er、Yb、(DyYb)]化合物的结构和某些性质(如氧含量、Cu~(3+)/Cu~(2+)等)随稀土离子半径的变化规律。发现随着稀土离子半径的减少,晶胞参数(a、b、c、v)几乎线性降低,Cu~(3+)/Cu~(2+)(％)、氧含量(7-δ)、正交畸变(a-b)几乎线性增加,XRD图谱中001峰加强,SEM像中晶形更加完整。

稀土复合氟化物的结构、电学性质及传感性质的研究

本文合成了REF_3(RE=Y、La、Ce、Nd、Gd、Tb、Dy、Er、Yb)及RE_(1-x)B_xF_(3-y)(RE=Y、La、Ce、Gd、Yb、B=Ca、Sr、Ba)。研究了它们的结构与电学性质。La_(0.95Ba_(0.05)F_(3-y),Ce_(0.95)Ca_(0.05)F_(3-y)属固溶体,测定了新化合物Y_(0.71)Ca_(0.29)F_(3-y)和Gd_(0.85)Ca_(0.15)F_(3-y)的晶系。RE_(1-x)B_xF_(3-y)的离子导电性质比REF_3强。本文以RE_(1-x)B_xF_(3-y)为基材制作了固体电解质传感器件,研究了它们对氧的敏感性质,制成了可在150℃使用的氧敏传感器。

磷酸二甲酯稀土配合物的合成与红外光谱研究

本文用稀土氯化物与磷酸三甲酯反应制备了一系列标题配合物RE(DMP)_3(RE=Sm,Eu,Ho,Yb,Lu)。配合物的热分解是一步完成的,由残渣的红外光谱确认其热分解产物为稀土偏磷酸盐。测定了配合物的红外光谱,对其主要吸收谱带进行了归属。红外光谱表明标题配合物与Sm(DMP)_3单晶应具有相同的结构类型,每个稀土原子通过双“O—P—O”桥与邻近的三个稀土原子连接,形成“双桥二十四元环”的环会环的网络结构。RE—O键基本上是离子键。

Ln_xYb_(1-x)Ba_2Cu_3O_(7-δ)(Ln=La 或 Nd)的结构和超导电性的研究

本文系统地研究了轻稀土元素 La、Nd 等部分取代 YbBa_2Cu_3O(7-δ)化合物中的 Yb 对结构和超导电性所产生的影响。少量(约0.1摩尔比)轻稀土元素可有效抑制 YbBa_2Cu_3O(7-δ)化合物中杂相的生成,提高体系中 Cu~(3+)/Cu~(2+)之值。

诱导动力学分光光度法测定钇

α型Y-CPA-PN配合物向β型配合物转化的反应对α型Yb-CPA-PN向β型转化的反应具有诱导作用。利用这一诱导反应可用来测定混合稀土中的钇。在初步研究反应机理的基础上,茯得了不同反应时期反应速率与钇浓度的定量关系,并确定了最佳反应条件。通过求算协同诱导系数、解联立方程的办法可扣除共存轻稀土的干扰。方法可能用于含钇和轻稀土样品中氧化钇的测定。

稀土HEH[EHP]固体配合物的红外光谱

本文制备了La,Ce,Pr,Nd,Sm,Eu,Gd,Tb,Dy,Ho,Er,Tm,Yb,Lu,Y等十五种稀土与2-乙基己基膦酸单(2-乙基己基)酯的固体配合物,测定了4000-100cm~(-1)的FT-IR光谱,对其主要红外光谱吸收带进行了归属。指认150cm~(-1)为Ln-O键的伸缩振动带,250cm~(-1)附近的谱带为COPO,CCPO骨架扭曲振动与Ln-O键的耦合振动带。结果表明配合物为多聚体系,PO_2与稀土离子可能为桥式配位形式。Ln-O键基本上为离子键。

三甲硅基环戊二烯基稀土二氯化物的合成

1978年Lappert等人首先合成了二(三甲硅基环戊二烯基)稀土氯化物[Li(THF)](Me_3SiC_5H_4)_2LnCl] (Ln=Y,Yb)和Yb(C_5H_4SiMe_3)_2。三甲硅基环戊二烯基稀土二氯化物,则未见报导.采用三甲硅基环戊二烯作为合成稀土金属有机化合物的配体,不仅可以增加所合成的稀土化合物在非极性溶剂中的溶解度,而且在反应过程中可以减小歧化反应的发生,得到所要求的产物.我们探索了三甲硅基环戊二烯基稀土二氯化物的合成,并对所得到的产物进行了鉴定.

Ce_(0.9)Yb_(0.1)P_5O_(14)晶体的光电压光谱

前文在研究五磷酸铈晶体中Ln~(3+)对Ce~(3+)发光强度的影响时,发现当加入少量的Eu~(3+)和Yb~(3+)离子到CeP_5O_(14)晶体中能使Ce~(3+)的发射产生严重的猝灭现象,以致于用Ce~(3+)的302nm吸收带激发晶体时,观察不到Ce~(3+)的发射,或者十分微弱。令人费解的是Yb~(3+)离子在紫外和可见区无吸收带,Yb~(3+)离子的加入应该成为一个稀释离子,现却使Ce~(3+)的发射产生严

电感耦合等离子体原子发射光谱法分析稀土元素的研究(Ⅰ)高纯氧化镧中十四种稀土杂质的测定

研究了ICP-AES法测定高纯氧化镧中十四种稀土杂质的方法。利用简单的加热去溶装置成功地测定了99.99％La_2O_3中14种稀土杂质。10mg/ml La_2O_3基体工作曲线下限为(以氧化物百分含量计算)Ce、Pr、Sm_2×10~(-3);Gd、Tb1×10~(-3);Nd,Lu 8×10~(-4),Er,Ho,Dy4×10~(-4); Tm.Eu 2×10~(-4),Yb 8×10~(-5),Y_4×~(-5)。相对标准偏差为2.8—9.7,回收率为85—114％。

Quantitative traits correlative analysis and growth comparison among different populations of bay scallop, Argopecten irradians

The shell traits and weight traits are measured in cultured populations of bay scallop, Argopecten irradians. The results of regression analysis show that the regression relationships for all the traits are significant (P < 0.01). The correlative coefficients between body weight, as well as tissue weight with shell length, shell height and shell width are significant (P < 0.05). But the correlative coefficients between the anterior and posterior auricle length with body weight as well as tissue weight are not significant (P > 0.05). The multiple regression equation is obtained to estimate live body weight and tissue weight. The above traits except anterior and posterior auricle length are used for the growth and production comparison among three cultured populations, Duncan's new multiple range procedure analysis shows that all the traits in the Lingshuiqiao (LSQ) population are much more significant than those of the other two populations (P < 0.01), and there is no significant difference between the Qipanmo (QPM) and Dalijia (DLJ) populations in all traits (P > 0.05). The results indicate that the LSQ population has a higher growth rate and is expected to be more productive than the other two populations.

Rare earth elements in bottom sediments of major rivers around the Yellow Sea: implications for sediment provenance

Rare earth elements (REEs) of 91 fine-grained bottom sediment samples from five major rivers in Korea (the Han, Keum, and Yeongsan) and China (the Changjiang and Huanghe) were studied to investigate their potential as source indicator for Yellow Sea shelf sediments, this being the first synthetic report on REE trends for bottom sediments of these rivers. The results show distinct differences in REE contents and their upper continental crust (UCC)-normalized patterns: compared to heavy rare earth elements (HREEs), light rare earth elements (LREEs) are highly enriched in Korean river sediments, in contrast to Chinese river sediments that have a characteristic positive Eu anomaly. This phenomenon is observed also in primary source rocks within the river catchments. This suggests that source rock composition is the primary control on the REE signatures of these river sediments, due largely to variations in the levels of chlorite and monazite, which are more abundant in Korean bottom river sediments. Systematic variations in I LREE pound/I HREE pound ratios, and in (La/Yb)-(Gd/Yb)(UCC) but also (La/Lu)-(La/Y)(UCC) and (La/Y)-(Gd/Lu)(UCC) relations have the greatest discriminatory power. These findings are consistent with, but considerably expand on the limited datasets available to date for suspended sediments. Evidently, the REE fingerprints of these river sediments can serve as a useful diagnostic tool for tracing the provenance of sediments in the Yellow Sea, and for reconstructing their dispersal patterns and the circulation system of the modern shelf, as well as the paleoenvironmental record of this and adjoining marginal seas.

Preliminary analysis of grain-size populations with environmentally sensitive terrigenous components in marginal sea setting

Terrigenous components were separated from the bulk sediment of Core A7 from the Okinawa Trough and Core A37 from the Ryukru Trench and grain-size distributions of these sub-samples were analyzed. Based upon an analysis of the grain-size data of the two sedimentary sequences, grain-size populations are identified to be sensitive to sedimentary environmental changes. The modal values and size ranges of the two main grain-size populations in Core A7 are evidently different from those of Core A37, indicating the spatial variability of sediment sources and transport processes between the two places. The downcore variations in the content of the environmentally sensitive grain-size populations reveal that during the accumulation of sedimentary material the environment remained relatively stable at the site where Core A7 was collected, except for the apparent events for the formation of two turbidite layers and a volcanic ash layer. However, the sedimentary sequence of Core A37 shows six sedimentary cycles, indicating a highly variable sedimentary environment at this location.

History and variability of Asian interior aridity recorded by eolian flux in the Chinese Loess Plateau during the past 7 Ma

Eolian flux in the Chinese Loess Plateau was reconstructed by measuring the dry bulk density and CaCO3 content of the late Cenozoic loess-paleosol-red clay sequences in the Lingtai profile. Comparison of eolian flux variation between the Lingtai profile and the ODP sites 885/886 in the North Pacific shows a significant wet-dry variability in addition to a gradual drying trend in the dust source regions in interior Asia. Especially, the increase of eolian fluxes from both continental and pelagic eolian sediments indicates a sharp drying of the dust source regions between 3.6 and 2.6 MaBP, which might be attributed to the tectonic uplift of the Tibetan Plateau, which cut down the moisture input to the interior Asia. The average value and variability of eolian flux are higher after 2.6 MaBP than before, which may be related to the Quaternary climatic fluctuations on the glacial-interglacial timescale after the commencement of major Northern Hemisphere Glaciations. The eolian fluxes of the Lingtai profile and Core V21-146 in northwest Pacific show a synchronous variation on the 10(4)-10(5) a timescale, indicating that the flux variations from both continental and marine records are closely correlated to the Quaternary climatic fluctuation forced by the ice volume changes on a global scale.

Geochemical properties of the variolitic andesite from Susong in the Dabie orogenic belt, China

The variolitic andesite from the Susong County in the Dabie Mountains implies that it was erupted in water. The mineralogy of the varioles is primarily radiate plagioclase (albite sind oligoclase), with little pyroxene, hornblende and quartz (derived from alteration). The pyroxene, hornblende and quartz are in the interstices between plagiocalse. The matrix consists of glass, hornblende, chlorite, epidote and zoisite. It is clearly subjected an extensive alteration. The andesite has an uncommon chemical composition. The SiO2 content is about 56.8%, TiO2 = 0.9%, MgO = 6.4%, Fe2O3 (tot) = 6.7%similar to 7.6%, 100Mg/(Mg + Fe) = 64.1 similar to 66.2. Mg-# is significantly high. The andesite has high abundances of large-lithophile trace elements (e.g. K, Ba. Sr, LREE), e.g. La/Nb = 5.56 similar to 6.07, low abundances of high-strength-field elements (HFSE e.g. Ta, Nb, P, Ti), particularly Ta and Nb strongly depleted. These are consistent with the characteristics of subduction-related magmas. In the spider diagram of trace elements, from Ce to right hand, the abundances of elements decrease quickly, showing a character of the continental margins. There has a strong punishment of light-rare-earth elements, with a significant diffraction of REEs (the mean value of (La/Yb)(N) is 32.84). No Eu anomaly, but there are anomaly high (La/Yb)(N) = 28.63 similar to 36.74, (La/Y)(N) = 70.33 similar to 82.4. The elements Y and Yb are depleted greatly, Y<20 g/g, Y-N = 2.74 similar to 2.84, Yb-N = 2.18 similar to 2.35. From the La-(La/Sm) diagram, the andesite is derived from partial melting. But the epsilone value of Nd is - 18.7 similar to -19.2, so that the material source may be the mantle materials affected by the crustal materials. The Nd model age is 1.9 Ga indicating that the variolitic basaltic andesite was resulted from the mantle wedge of North China block, which had the Nd model age of 2.5Ga, when the Yangze block which had the Nd model age of 1.7Ga subducted beneath it. So the variolitic andesite has characteristics of the island-are volconic rocks oil a continental basement in the vicinity of the destructive continental margin.