南雄县紫色土砂页岩流失区银合欢引种栽培

紫色砂页岩沟状重水土流失区，土层十分干旱，常见绿化造林树种极难生长。根据这种情况，1983年始，应用多年来对银合欢属树种具有耐高温、耐干旱，适宜碱性土壤生长的观察研究结果，在南雄县13个自然村，500公顷低丘陵荒坡地、应用银合欢属树种营造水保林，综合治理水土流失试验。经三年试验，从26个银合欢引种材料中，选出适宜当地生长的三个优良品种，提出了一套树种栽培营林和水保工程措施相结合的治理技术。经治理三年的营林地段，水土流失年冲刷模数（固体迳流）从未治理的每平方公里对照区流失量19.057吨下降到每平方公里流失量5.372吨每公里长林带（林带宽1.5米）生产造纸用材9.8吨，供饲料生产的干嫩叶2.8吨。该项研究，在国内率先提出了控制紫色砂页岩地区水土流失的先进技术，具有在我国同类型地区推广应用价值。

斑纹薄鳅(Leptobotia zebra)应该为斑纹沙鳅(Sinibotia zebra)

斑纹薄鳅(Leptobotia zebra)最初是由Wu(1939)描述的一个新种,当时定名为斑纹沙鳅(Botia zebra),后来Chen(1980)根据眼下刺不分叉将其改归为薄鳅属的物种。本研究通过对线粒体DNA细胞色素b基因序列的测定和分析,发现斑纹薄鳅和薄鳅属(除斑纹薄鳅)物种间的平均遗传距离为0.177,和中华沙鳅属物种美丽沙鳅(Sinibotia pulcher)的平均遗传距离仅为0.057。系统发育分析发现斑纹薄鳅并未和薄鳅属的物种聚在一起,而是和中华沙鳅属物种美丽沙鳅聚在一起形成姐妹群。

The youngest split in sympatric schizothoracine fish (Cyprinidae) is shaped by ecological adaptations in a Tibetan Plateau glacier lake

Although new empirical evidence shows that sympatric speciation has occurred in some species, there are few indisputable model organisms for this process of speciation. The two subspecies (Gymnocypris eckloni eckloni and G. e. scoliostomus) of the schizothoracine Gymnocypris fish species complex from a small glacier lake in the Tibetan Plateau, Lake Sunmcuo, fit several of the key characteristics of the sympatric speciation model. We used combined mitochondrial control region sequences and the cytochrome b gene (1894 bp) to address the phylogenetics and population genetics of 232 specimens of G. e. eckloni and G. e. scoliostomus, as well as all of its closely related sister species. We found that: (i) a total of four old lineages were uncovered in the widespread G. e. eckloni, of which only one was shown to be shared with all G. e. scoliostomus individuals and (ii) the new subspecies (G. e. scoliostomus) evolved in Lake Sunmcuo from the ancestral G. e. eckloni population within approximately 0.057 Ma. These two taxa of the species complex are morphologically distinct, and reproductive isolation is further suggested. Ecological disruptive selection based on morphological traits (e.g. mouth cleft characters) and food utilization may be a mechanism of incipient speciation of two sympatric populations within Lake Sunmcuo. This study provides the first genetic evidence for sympatric speciation in the schizothoracine fish.

24-二甲基戊二稀土化合物的合成

本文叙述了2.4-二甲基戊二烯基稀土金属有机化合物的合成并通过元素分析，红外光谱、核磁共振谱及质谱的鉴定。测定了Gd(2.4-GH_(11))_3的单晶结构，此外还合成了（2.4-GH_(11)K.TMEDA及K_2C_8H_8·3THF并也测定了它们的晶体结构。在所合成化合物的红外光谱中，没有属于C=C双键的吸收峰，表明分子中配位体以η~5形式的大π键体系与稀土金属离子结合，在Ln(2.4-GH_(11))_2Cl·TMF和Ln(2.4-GH_(11))Cl_2·GH_THF的红外光谱中，于1060波数附近出现一强而宽的吸收峰，即化合物中有四氢呋喃分子络合。化合物的室温NMR谱有四个吸收峰，2.4-二甲基戊二烯配位体可能为η~5平面∪或W构型。化合物的水解'H-NMR谱与质谱都证实水解产物为2.4－二甲基－1.3－戊二烯。它是－2.4二甲基戊二烯阴离子水解所得的唯一产物，它表明化合物中的配位体确为2.4－二甲基戊二烯阴离子。(2.4-GH_(11))_2Cl·TMDA配合物晶体结构是应用低温X－射线衍射技术用Nicolet R_3 M/E型四园衍射仪LT－1低温装置并利用重原子法测定的最小二乘法精修至收敛时的一致性因子R=0.055. Rw=0.057。晶体属单斜晶系P21/n空间群。晶胞参数a=11.322(4)A, b=9.242(3)A, c=15.956(5)A. β=106.70(3)分子中2.4－二甲基戊二烯阴离子呈平面∪构型。钾离子与四甲基乙二胺二啮体结合形成的络合阳离子和2.4-二甲基戊二烯阴离子相间排列形成无限链状结构分子。2.4－二甲基戊二烯阴离子的C－C键长明显分为中间与外端C－C键两组。外端组C－C键双性质较强键长较短。表明C3具有负电荷的共振杂化体贡献较大。分子中K－C键最短的是K-C(1.5)。而不是具有较多负电荷的C3－K键。这可能是由于几何因素造成的。K_2C_8H_8·3THF的晶体结构是采用与前者相同的方法测定的。它属三斜晶系，PT空间群，晶胞参数a=10.263(3)A, b=13.157(4)A, c=9.443A, α=87.51(2)°, β=114.93(2)°, γ=76.81(2)°. V=1111.6A, R=0.051. 晶体中负二价的环辛四烯阴离呈平面构型，具有中心对称性，两侧与两中心对称相关的钾离子连接，相邻的非等效的钾离子间通过两四氢呋喃分子的氧原子相连接，从而形成了无限链状结构的分子。环辛四烯反映了Huckel的4n+2芳香性规则。该结构的特别之处在于四氢呋喃分子的氧原子以桥键形式与两个钾离子同时连接。而这种形式的桥键在其它化合物中似还未发现。Go(2.4-GH_(11))_3的晶体结构亦是采用与前述相同的方法测定的。其晶体为三斜晶系，PT空间群，晶胞参数a=12.541A, b=12.853A, c=8.432A, α=91.44°, β=108.61°, γ=117.97°, V=112.54A~3. 结构测定表明，Gd(2.4-GH_(11))_3分子具有C_3h对称性。三个配位体阴离了的九个带负电荷的碳原子近似以三帽三角棱柱形式与钆离子配位。分子中2.4－二甲基戊二烯阴离子的C－C键长－亦分为而组。外端C－C键较中间C－C键强，键长较短，亦表明C3具有较多的负电荷。2.4－二甲基戊二烯阴离子本身近似呈平面∪构型。C2,C4偏离由C1 C3 C5三碳原子构成的平面0.067A。方向上远离中心钆离子。可能在此以离子性为主的化合物中，钆离子与不带电荷的C2 C4间的相互作用有些排斥性质。与Nd(2.4-GH_(11))_3不同的是，在Gd(2.4-GH_(11))_3分子中，Gd-(C(1,5）键最短，而不是Gd-C(3)键。这可能是由于钆离子的半径较小，化合物的空间位阻效应较大所致。

泽兰实蝇的生态学特性及对紫茎泽兰的控制作用

紫茎泽兰(Eupatorium adenophorum Spreng)是一种原产于墨西哥的恶性杂草。近年来已严重妨碍了云南省甚至整个西南地区、林、牧业的发展。自1984年8月引进泽兰实蝇(procecidochares utilis Stone)开展了生物防治研究。已在云南境内七个地州（市）定殖扩散。为了解泽兰实蝇的控制作用，本文从研究泽从实蝇生态学特性入手。分析了泽兰实蝇生态学特性与紫茎泽兰生物防治的关系。定量地评价了泽兰实蝇的控制作用。并且应用灰色系统中局势决策方法比较了不同环境条件下的生防效果。其主要结果如下：1、泽兰实蝇雌性与雄性成虫的存活曲线均近于Deevery I型；雌雄一并来看。则成虫存活曲线为Deevery II型；雌性成虫的寿命比雄性长。产卵峰期多在产卵开始后的第二到第四天。2、泽兰实蝇幼虫与成虫均存在密度制约。在平均每雌占有两枝供试产卵枝条时产卵量最大。同时孕育虫的后代也最多。3、泽兰实蝇的净增殖率R. = 24.365。内禀增长率r_m = 0.055。周限增长值λ = 1.057。种群加倍时间t = 12.603天，世代周期T = 58.371天。4、泽兰实蝇幼虫种群的空间分布呈聚集型且接近于负二项分布。一般来说平均拥挤度大的地区，对紫茎泽兰的控制效果也好。5、利用计算机模拟术对泽兰实蝇的控制作用进行拟合。较之以寄生率来评价生防效果更为科学，也更为符合客观实际。6、对不同环境下的控制作用进行局势决策可知，温度较高。湿度偏低的地区。生防效果优于那些温度较低或温、温度均较高的地区。在本文所进行调查的几个样地中，泽兰实蝇控制效果大小的次序依次为：元江＞宜良＞双柏＞思茅。

黄河上游青海沙蜥种组的系统地理学研究

沙蜥属（Phrynocephalus）的卵胎生类群主要分布在我国青藏高原，包括南疆沙蜥（P. forsythii）、西藏沙蜥（P. theobaldi）、红尾沙蜥（P. erythrurus）、贵德沙蜥（P. putjatia）和青海沙蜥（P. vlangalii）。其卵胎生生殖方式适应了高寒生境，与青藏高原隆升有关。纵观前人的研究，上述几种卵胎生沙蜥的分类、系统发育关系以及生物地理都还存在疑问。本文研究了分布在若尔盖湿地的青海沙蜥红原亚种（P. v hongyuanensis）以及分布在黄河上游其它地区青海沙蜥种组的地理分布格局，并探讨了其形成机制。 青海沙蜥在黄河上游主要分布于若尔盖湿地以及青海湖周边地区。若尔盖湿地青海沙蜥红原亚种的生境由于沼泽的形成被切割成不连续的斑块，通过遗传分析可以推测这种特殊生境对它们遗传结构的影响。其次，贵德沙蜥、青海沙蜥的青海湖周边各居群以及若尔盖湿地居群之间的系统地理格局还未见报道。因此本文以居群为单位，将它们作为一个复合体，通过系统地理研究，可以了解其种群遗传结构，据此分析相关的地质历史事件对其分布的影响。主要结果如下： 1. 若尔盖湿地青海沙蜥红原亚种的种群遗传结构： 共研究了三个地理单元（红原（HY）、辖曼（XM）、玛曲（MQ））的7个采集点的72个个体。所有ND4-tRNALeu序列比对得到785 bp的片断，定义了9种单倍型。结果显示总的核苷酸多样性较低，单倍型多样性较高。分子变异分析（AMOVA）显示3个单元间差异显著（P<0.01），遗传变异主要存在于地理单元间，占62.61%。除MQ单元，XM各居群与HY居群混杂在一起，单倍型网络图没有显示出单倍型和地理位置的对应关系。XM单元单倍型的不配对分布（Mismatch distribution）为明显左移的单峰，且Fu’s Fs test为负值，表明XM单元可能经历了近期种群扩张，有足够的时间积累单倍型的多态性，还不足以大幅提高核苷酸多样性，这是其单倍型多样性较高和核苷酸多样性较低的原因。MQ单元遗传多样性低而与其他单元显著分化，推测这与3万年前黄河在若尔盖玛曲之间贯通有关。近期沼泽的形成对XMb居群的隔离时间短，使得其遗传多样性低但还不足以形成大的遗传差异。无论黄河的贯通还是沼泽的形成其隔离形成的时间都不长，其作用改变了单倍型出现的频率，也出现了一些特有单倍型，但共享单倍型还广泛存在，还不足以使得不同居群之间形成较大的遗传距离。 2. 黄河上游青海沙蜥种组的分布格局与地史过程的关系： 黄河上游青海沙蜥种组包括贵德沙蜥、青海沙蜥指名亚种的青海湖周边各居群、青海沙蜥红原亚种若尔盖湿地居群、以及青海湖以西的部分居群（序列由Genbank下载获得），总计22个居群189个样品。所有ND4-tRNALeu序列比对得到703个位点，定义了39种单倍型。以南疆沙蜥为外群构建的贝叶斯树以及MP法构建的无根树，都分为A、B两大组。其中A包括若尔盖湿地居群以及玛多居群（A1）、青海湖以西的居群和兴海居群（A2）、西藏沙蜥；B包括青海湖以南的居群和天祝居群（B1）、青海湖以东北的居群（B2）。单倍型网络图分别对应了系统发育树上的各支。按照系统发育结果分组进行分子变异分析，得到组间变异占88.63％，各组间差异显著（P=0.000）。种群遗传结构分析得到，A1和B2可能经历了近期的种群扩张，前者扩张时间约为0.105－0.189 Ma B.P.（million years before present），后者为0.057－0.102 Ma B.P.，可能与末次间冰期的气候变暖有关。A2和B1对应的两个地理单元都具有较强的种群遗传结构，较为稳定。 青海沙蜥种组A、B两大支之间遗传距离大，分化明显，分化大约发生在4.29－2.38 Ma B.P.，推测青藏运动的A幕运动后复杂的地形变化可能是它们产生分化的原因。B1和B2分化大约发生在1.73－0.96 Ma B.P.，这与湟水流域构造运动发生的时间相符。在早、中更新世时期，B1支内部各居群可能有交流，中更新世末共和盆地出现的抬升以及河流溯源改道等事件可能是引起这支内部多个单倍型丢失的原因。A1、A2支的分化可能与倒数第三次冰期降临之后气候变冷、阿尼玛卿山的大冰帽有关。 The viviparous group of genus Phrynocephalus is mainly distributed in the Qinghai –Tibetan Plateau, including P. forsythii、P. theobaldi、P. erythrurus、P. putjatia and P. vlangalii. These species are adapted well to the cold clime there, and the origin of this group was the result of a vicariance event associated with the uplifting of the Qinghai -Tibetan Plateau. Although many works have been done, there are still several questions about classification、phylogenetic relationships and the biogeography of this group. The phylogeographic pattern of the P. vlangalii complex on the upper reaches of the Yellow River and the P. v. hongyuanensis in Zoige Wetland were studied in this thesis. On the upper reaches of the Yellow River, P. vlangalii complex are distributed in Zoige Wetland and the southeast and northeast region of Kuku-noor Lake. Because of the forming of the wetland in Zoige, the habitats for sand lizards are divided into many discontinuous ones, and it is necessary to analyze genetic structure in these unique habitats. The phylogeographic patter among P. putjatia、populations of P. vlangalii in the southeast region of Kuku-noor Lake and populations of P. vlangalii in Zoige Wetland hasn’t been studied yet, and the complicated geological events of the Plateau may play an important role in the populations’ diversity and species forming there. So these populations were gathered as a complex, and phylogeographic analysis were used to clarify these doubts. According to the two topics above, this thesis has two parts of results as follows: 1. Three geographic units of P. vlangalii hongyuanensis in Zoige Wetland were defined, and they were Xiaman （XM）、Hongyuan （HY） and Maqu （MQ）. 785bp fragments of the mtDNA ND4-tRNAleu were determined from 72 samples and nine haplotypes were identified. As a whole, the nucleotide diversity was low，but the haplotype diversity was high. Analysis of molecular variance （AMOVA） showed that the three units were distinctly different（P<0.01），and 62.61% of the total genetic diversity was attributable to variation among units. There were 3 haplotypes shared among XM and HY，and no geographic clustering was observed except MQ from the TCS network. The results from the mismatch distribution analysis and Fu’s Fs test implied that there might be a recent population expansion in the XM unit, and this may be the reason why XM had a high haplotype diversity but a low nucleotide diversity. We estimate that the MQ and XMb have lower diversities because of some very recent geographic events, such as the formation of the Yellow river’s upriver and the Zoige Wetland. Although they are distinctly different, not enough time has passed for them to have diverged a great genetic distance. 2. 189 samples in 22 populations of P. vlangalii complex were collected, including P. putjatia、populations of P. vlangalii in the southeast and northeast region of Kuku-noor Lake、 populations of P. vlangalii in Zoige Wetland and the data from Genbank. 703bp ND4-tRNALeu sequences identified 39 haplotypes. P. forsythii was selected as outgroup, and both the Bayesian tree and the MP unrooted tree were divided into two groups（A、B）. A included populations in Zoige Wetland and Xinghai（A1）、populations in the west of Kuku-noor Lake（A2）、P. theobaldi, and B included populations in the southeast of Kuku-noor Lake and Tianzhu（B1）、populations in the northeast of Kuku-noor Lake（B2）. The haplotype network agreed with these groups. AMOVA showed that these five groups were distinctly different（P<0.01）, and 88.63% of the total genetic diversity was attributable to variation among groups. There might be recent population expansion in A1 and A2, which corresponded to the dry climate of the last interglacial period. The expansion times were 0.189-0.105 Ma B.P. and 0.102-0.057 Ma B.P., respectively. A2 and B1 had strong genetic structure. The large genetic distance between A and B showed that they had been separated from each other for a long time（about 4.29-2.38 Ma B.P.）, and it corresponded to the A phase of Qingzang Movement. The diversity between B1 and B2 at 1.73-0.96 Ma B.P. may be caused by the geological event in Huangshui valley. In early Pleistocene, populations in B1 may have gene flow because of geographic linkage, and later the uplift of the Plateau and the change of river route there made a few haplotypes lost. A1 and A2 were divided into two parts by A’nyemaqen Mountains at 0.66-0.37 Ma B.P., which maybe corresponded to glaciations at about 0.7 Ma B.P.

Multi-armed poly(L-glutamic acid)-graft-oligoethylenimine copolymers as efficient nonviral gene delivery vectors

Background The application of polyethylenimine (PEI) in gene delivery has been severely limited by significant cytotoxicity that results from a nondegradable methylene backbone and high cationic charge density. It is therefore necessary to develop novel biodegradable PEI derivates for low-toxic, highly efficient gene delivery.Methods A series of novel cationic copolymers with various charge density were designed and synthesized by grafting different kinds of oligoethylenimine (OEI) onto a determinate multi-armed poly(L-glutamic acid) backbone. The molecular structures of multi-armed poly(L-glutamic acid)-graft-OEI (MP-g-OEI) copolymers were characterized using nuclear magnetic resonance, viscosimetry and gel permeation chromatography. Moreover, the MP-g-OEI/DNA complexes were measured by a gel retardation assay, dynamic light scattering and atomic force microscopy to determine DNA binding ability, particle size, zeta potential, complex formation and shape, respectively. MP-g-OEI copolymers were also evaluated in Chinese hamster ovary and human embryonic kidney-293 cells for their cytotoxicity and transfection efficiency.

Hydrothermal synthesis and characterization of a new compound [Ni(en)(3)](2)[Ni(en)(2)(H2O)(2)][As6V15O42] center dot 4H(2)O

A new compound, [Ni(en)(3)](2)[Ni(en)(2)(H2O)(2)][As6V15O42] . 4H(2)O, was first prepared by hydrothermal synthesis and characterized by elemental analysis, IR, TGA-DSC, ESR and single crystal X-ray diffraction. Crystal data: monoclinic, space group C-c, a = 1. 523 6(3) nm, b = 2. 051 8(4) nm, c = 2.395 9(5) nm, beta = 97. 41(3)degrees, V = 7.427(3) nm(3), Z = 4, R = 0. 057 0, wR(2) = 0.135 7. The polyanion consists of six AsO3 pyramids and fifteen VO5 pyramids. Counterions are complex ions with octahedral structure, which consist of NH2CH2CH2NH2 and Ni2+.

Electrochemical behavior and electrocatalytic properties of ultrathin films containing silicotungstic heteropolyanion SiW12O404-

We describe here a controlled fabrication of ultrathin monolayer and multilayer films consisting of silicotungstic heteropolyanion SiW12O404- and a cationic polymer of quaternized poly(4-vinylpyridine) partially complexed with osmium bis(2,2'-bipyridine) on Au electrodes previously self-assembled with cysteamine monolayers based on layer-by-layer electrostatic interaction. The thus-forming monolayer and multilayer chemically modified electrodes are investigated by cyclic voltammetry on their electrochemical behavior and electrocatalytic properties. The composite ultrathin films exhibit remarkable electrocatalytic effects on the reduction of BrO3-, H2O2, and HNO2. The electrocatalytic effects on HNO2 reduction are enhanced with increasing layer number from 1 to 3 but level off with much thicker multilayers. The stability of the monolayer and multilayer films is also examined. (C) 2000 The Electrochemical Society. S0013-4651(99)04-057-4. All rights reserved.

Synthesis, structure and properties of alpha-Keggin-type of K6H3[ZnW11O40Al]center dot 9.5H(2)O

A new heteropolycomplex, K6H3[ZnW11O40Al] . 9.5H(2)O was prepared and characterized by means of elemental analysis, IR, UV spectroscopy, Al-27 NMR, electrochemistry and X-ray crystallography. The crystal of K6H3[ZnW11O40Al] . 9.5H(2)O is cubic, space group Fm-3m, with lattice constants a=b=c=2. 144 8(2) nm, V = 9.866(2) nm(3), Mo radiation, R = 0.057 8 for 497 independent data with [I>2 delta(I)]. The anion is of alpha-type Keggin structure with C-s symmetry.

Studies on the two class glass transition and the typical VTF behaviour of an amorphous comb polymer electrolyte

A comb polymer (CP350) with oligo-oxyethylene side chains of the type -(CH2CH2O)(7)CH3 was prepared from methyl vinyl ether/maleic anhydride copolymer and poly(ethylene glycol) methyl ether. The polymer can dissolve LiNO3 salt to form homogeneous amorphous polymer electrolyte. This electrolyte system was first found to have two class glass transitions, and the two T(g)s were observed to increase with increasing salt content. The ionic conduction was measured by using the complex impedance method, and conductivities were investigated as functions of temperature and salt concentration. At 25 degrees C, the ionic conductivity maximum of this system can get to 3.72 X 10(-5) S/cm at the [Li]/ [EO] ratio of 0.057. The appearance of the conductivity maximum has been interpreted as being due to the effect of T-g and the so called physical crosslinks. The temperature dependence of the ionic conductivity displaying non-Arrhenius behaviour can be analyzed using the Vogel-Tammann-Fulcher equation and interpreted on the basis of the configurational entropy model.

Synthesis and molecular structures of di- and trinuclear molybdenum complexes containing pyridine-2-thiolato (pyS) ligand

Dinuclear complexes [Mo-2(mu-pyS)(2)(CO)(4)(PPh(3))(2)] (1), [Mo-2(mu-pyS)(2)(CO)(5)(PPh(3))] (2) and a trace quality of trinuclear complex [Mo-3(mu-pyS)(2)(mu(3)-pyS)(2)(CO)(6)] (3) were obtained from the reaction of [Mo(CO)(3)(MeCN)(3)] with pyridine-2-thione (pySH) and PPh(3) in THF. The crystal structures of 1.2C(7)H(8) and 3.7 C7H8 have been determined by X-ray diffraction studies. Crystals of 1.2C(7)H(8) are monoclinic, space group C2/c and Z = 4, with a = 18.797(3), b = 11.143(4), c = 28.157(7) Angstrom, beta = 101.23(2)degrees. The structure was refined to R = 0.050 and Rw = 0.057 for 3146 observed reflections, Crystals of 3.7 C7H8 are monoclinic, space group P2(1)/a and Z = 4, with a = 13.912(2), b = 17.161(2), c = 15.577(3) Angstrom, beta = 101.17(1)degrees. The structure was refined to R = 0.046 and Rw = 0.051 for 4357 observed reflections. The molecule of 1 consists of two Mo(CO)(2)(PPh(3)) fragments linked by an Mo-Mo bond (2.974(2)Angstrom) and by two doubly-bridging pyS ligands. The compound 3 contains a bent open geometry of three molybdenum atoms (Mo(1)-Mo(2)-Mo(3) angle 122.99(3)degrees) linked by two Mo-Mo bonds (2.943(1) and 2.950(1) Angstrom) and by two doubly- and two triply-bridging pyS ligands.

轻稀土配合物[Li·(DME)_3ⅡCH_3C_5H_4Ln(NPh_2)_3l(Ln=La、Pr、Nd)的合成和镧配合物的晶体结构

CH_3C_5H_4LnCl_2·2LiCl·nTHF与2mol的LiNPh_2在THF、已烷和甲苯混合液中反应,经DME萃取,得到[Li·(DME)_3][(η~5-CH_3C_5H_4)Ln(NPh_2)_3](Ln=La,Pr,Nd)。对其进行了元素分析、IR和NMR表征。镧配合物单晶结构测定表明,属单斜晶系,P2_1/a空间群,晶胞参数为α=1.7461(6)nm,b=1.6576(5)nm,c=1.8335(6)nm,β=96.04°,V=5.277um~3,Z=4,D_c=1.26g/cm_3,R=0.057,R_w=0.048。该配合物是一个离子对,La-N和La-C(环)键的平均距离分别为0.2459(8)和 0.2843(11)nm。稀土离子形成一个六配位的扭曲四面体。

SYNTHESES OF METHYLCYCLOPENTADIENYL DERIVATIVES OF LANTHANIDES (LN = LA-ND) AND CRYSTAL-STRUCTURES OF [(THF)2LI(MU-CL)2]2[MECPND(THF)] AND [LI(DME)3][MECPLA(NPH2)3]

The reaction of LnCl3.2LiCl with 1 equiv of MeCpNa in THF gives the complexes [(THF)2Li(mu-Cl)2]2[MeCpLn(THF)] (Ln = Nd (1), La (2)) in good yield. These precursors react further with 2 equiv of LiNPh2 to produce the new complexes [Li(DME)3][MeCpLn(NPh2)3] (Ln = La (3), Pr (4), Nd (5)). They have been characterized by elemental analyses and IR and NMR spectra, as well as by structural analyses of 1 and 3. The chloride 1 crystallizes in the monoclinic space group P2(1)/n (No. 14) with a = 12.130 (5) angstrom, b = 17.343 (5) angstrom, c = 17.016 (5) angstrom, beta = 108.54 (3)-degrees, V = 3393.87 angstrom3, Z = 4, and D(c) = 1.45 g/cm3. Least-squares refinement led to a final R value of 0.051 (I greater-than-or-equal-to 3-sigma(I(o))) for 2004 independent reflections. Complex 3 crystallizes in the monoclinic space group P2(1)/c (No. 14) with a = 18.335 (6) angstrom, b = 16.576 (5) angstrom, c = 17.461 (6) angstrom, beta = 96.04 (3)-degrees, V = 5277.17 angstrom3, D(c) = 1.26 g/cm3, Z = 4, and R = 0.057 (I greater-than-or-equal-to 2.5-sigma(I(o))) for 3378 reflections. The structure of 3 consists of discrete ion pairs [Li(DME)3]+ and [MeCpLa(NPh2)3]- with average La-N and La-C(ring) distances of 2.459 (8) and 2.84 (1) angstrom, respectively.