Measurement of the galactic cosmic ray antiproton flux from 0.25 gev to 3.11 gev with the isotope matter antimatter experiment (imax)

The intensities and relative abundances of galactic cosmic ray protons and antiprotons have been measured with the Isotope Matter Antimatter Experiment (IMAX), a balloon-borne magnet spectrometer. The IMAX payload had a successful flight from Lynn Lake, Manitoba, Canada on July 16, 1992. Particles detected by IMAX were identified by mass and charge via the Cherenkov-Rigidity and TOP-Rigidity techniques, with measured rms mass resolution ≤0.2 amu for Z=1 particles.

Cosmic ray antiprotons are of interest because they can be produced by the interactions of high energy protons and heavier nuclei with the interstellar medium as well as by more exotic sources. Previous cosmic ray antiproton experiments have reported an excess of antiprotons over that expected solely from cosmic ray interactions.

Analysis of the flight data has yielded 124405 protons and 3 antiprotons in the energy range 0.19-0.97 GeV at the instrument, 140617 protons and 8 antiprotons in the energy range 0.97-2.58 GeV, and 22524 protons and 5 antiprotons in the energy range 2.58-3.08 GeV. These measurements are a statistical improvement over previous antiproton measurements, and they demonstrate improved separation of antiprotons from the more abundant fluxes of protons, electrons, and other cosmic ray species.

When these results are corrected for instrumental and atmospheric background and losses, the ratios at the top of the atmosphere are p/p=3.21(+3.49, -1.97)x10^(-5) in the energy range 0.25-1.00 GeV, p/p=5.38(+3.48, -2.45) x10^(-5) in the energy range 1.00-2.61 GeV, and p/p=2.05(+1.79, -1.15) x10^(-4) in the energy range 2.61-3.11 GeV. The corresponding antiproton intensities, also corrected to the top of the atmosphere, are 2.3(+2.5, -1.4) x10^(-2) (m^2 s sr GeV)^(-1), 2.1(+1.4, -1.0) x10^(-2) (m^2 s sr GeV)^(-1), and 4.3(+3.7, -2.4) x10^(-2) (m^2 s sr GeV)^(-1) for the same energy ranges.

The IMAX antiproton fluxes and antiproton/proton ratios are compared with recent Standard Leaky Box Model (SLBM) calculations of the cosmic ray antiproton abundance. According to this model, cosmic ray antiprotons are secondary cosmic rays arising solely from the interaction of high energy cosmic rays with the interstellar medium. The effects of solar modulation of protons and antiprotons are also calculated, showing that the antiproton/proton ratio can vary by as much as an order of magnitude over the solar cycle. When solar modulation is taken into account, the IMAX antiproton measurements are found to be consistent with the most recent calculations of the SLBM. No evidence is found in the IMAX data for excess antiprotons arising from the decay of galactic dark matter, which had been suggested as an interpretation of earlier measurements. Furthermore, the consistency of the current results with the SLBM calculations suggests that the mean antiproton lifetime is at least as large as the cosmic ray storage time in the galaxy (~10^7 yr, based on measurements of cosmic ray ^(10)Be). Recent measurements by two other experiments are consistent with this interpretation of the IMAX antiproton results.

双菱体λ/4消色差相位延迟器的设计

根据菲涅尔全内反射相变理论,给出了双菱体λ/4消色差器的结构设计、性能分析和测量方法.由有效通光孔径和光线追迹设计出BK7玻璃在波长532 nm时相位延迟λ/4的双菱体的结构,用作532 nm至1 064 nm波长范围的标准λ/4相位延迟器.理论分析了入射角变化和波长变化对双菱体相位延迟的影响,当入射角变化限制在±4.3°以内时,其影响得到补偿；波长从532 nm到1 064 nm产生的误差为－0.65°.采用椭偏法中的消光技术,分别实测了双菱体在532 nm和1 064 nm波长下的相位延迟为：90.08±0.14°和88.99±0.1°,可知两不同波长产生的相位延迟误差为－1.09°.

六六六在水环境中转移、积累和归趋研究——3.六六六在鱼体的积累释放

鳃是六六六进入鱼体的主要通道,鱼体的残留水平决定于水与体脂间的分配平衡。要使背肌六六六残留低于0.5毫克/公斤,则水中六六六含量要低于0.024毫克/升。鱼体六六六残留向水体释放的速度与温度有关,温度低,释放慢;当温度低于10℃时,释放的速度极慢以至难以检出。建议采用清水寄养的方法,让鱼体释放六六六,降低残毒,提高商品质量。这种方法估计也适用于其它脂溶性的与水分配系数不是太大的污染物。

EFFECTS OF IRON ON PHYSIOLOGICAL AND BIOCHEMICAL CHARACTERISTICS OF Microcystis wesenbergii (Kom.) Kom. (Cyanobacterium)

Iron is an essential trace element for biological requirements of phytoplankton. Effects of iron on physiological and biochemical characteristics of Microcystis wesenbergii were conducted in this study. Results showed that 0.01 mu M [Fe3+] seriously inhibited growth and chlorophyll synthesis of M. wesenbergii, and induced temporary increase of ATPase activities, however, NR. ACP and ALP activities were restrained by iron limitation. Interestingly, iron addition on day 8 resulted in the gradual restoration of structures and functions of above enzymes and resisted a variety of stresses from iron limitation. M. wesenbergii in 10 mu M [Fe3+] treatment group grew normally. enzymes maintained normal levels, and residual phosphate contents in cultures first sharply decreased, then smoothly as M. wesenbergii has a characteristic of luxury consumption of phosphorus. Above parameters in 100 mu M [Fe3+] treatment group were almost same with those in 10 mu M [Fe3+] treatment group except for NR, ACP and ALP activities. In 100 mu M [Fe3+] treatment group, activities of ACP and ALP had temporary increase because phosphate and ferric iron could form insoluble compound - ferric phosphate (Fe3PO4) through adsorption effect. resulting in lack of bioavailable phosphate in culture media. The experiment suggested that too low or too high iron can affect obviously physiological and biochemical characteristics of M. wesenbergii.

Mode coupling and vertical radiation loss for whispering-gallery modes in 3-D microcavities

The characteristics of whispering-gallery modes (WGMs) in 3-D cylindrical, square, and triangular microcavities with vertical optical confinement of semiconductors are numerically investigated by the finite-difference time-domain (FDTD) technique. For a microcylinder with a vertical refractive index 3.17/3.4/3.17 and a center layer thickness 0.2 mu m, Q-factors of transverse electric (TE) WGMs around wavelength 1550 nm are smaller than 10(3), as the radius R < 4 mu m and reach the orders of 10(4) and 10(6) as R = 5 and 6 mu m, respectively. However, the Q-factor of transverse magnetic (TM) WGMs at wavelength 1.659 mu m reaches 7.5 x 10(5) as R = 1 mu m. The mode coupling between the WGMs and vertical radiation modes in the cladding layer results in vertical radiation loss for the WGMs. In the microcylinder, the mode wavelength of TM WGM is larger than the cutoff wavelength of the vertical radiation mode with the same mode numbers, so TM WGMs cannot couple with the vertical radiation mode and have high Q-factor. In contrast, TE WGMs can couple with the corresponding vertical radiation mode in the 3-D microcylinder as R < 5 mu m. However, the mode wavelength of the TE WGM approaches (is larger than) the cutoff wavelength of the corresponding radiation modes at R = 5 mu m (6 mu m), so TE WGMs have high Q-factors in such microcylinders too. The results show that a critical lateral size is required for obtaining high, Q-factor TE WGMs in the 3-D microcylinder. For 3-D square and triangular microcavities, we also find that the Q-factor of TM WGM is larger than that of TE WGM.

Comparison of Q-factors between TE and TM modes in 3-D microsquares by FDTD simulation

Mode characteristics of three-dimensional (3-D) microsquare resonators are investigated by finite-difference time-domain (FDTD) simulation for the transverse electric (TE)-like and the transverse magnetic (TM)-like modes. For a pillar microsquare with a side length of 2 pin in air, we have Q-factors about 5 X. 103 for TM-like modes at the wavelength of 1550 run, which are one order larger than those of TE-like modes, as vertical refractive index distribution is 3.17/3.4/3.17 and the cororresponding center layer thickness is 0.2 mu m. The mode field patterns show that TM-like modes have much weaker vertical radiation coupling loss than TE-like modes. TM-like modes can have high Q-factors in a microsquare with weak vertical field confinement.

铬系催化剂聚合1,3-双烯烃的研究

铬系催化剂是合成1,2-聚丁二烯和3,4-聚异戊二烯的一种主要催化剂体系，1,2-聚丁二烯和3,4-聚异戊二烯是制造高性能轮胎的重要原料。本论文研究了以含氮化合物和含磷化合物为配体的铬催化剂合成1,2-聚丁二烯和3,4-聚异戊二烯的反应规律。 1. 以邻菲咯啉为配体的铬催化剂在己烷中50℃下可获得1,2-结构、顺-1,4-结构和反-1,4-结构单元含量分别约为50%、30%和20%，分子量呈双峰分布的聚丁二烯。改变聚合温度，可有效控制聚合物的1,2-结构含量和分子量及分布。催化剂通过预陈化方式，可有效抑制低聚物的生成。 2. 以亚磷酸二烷基酯为配体的铬催化剂是合成1,2-聚丁二烯的高效催化剂，所得聚合物具有高的1,2-结构含量（> 78%）。改变烷基铝和亚磷酸二烷基酯的结构，可以得到高熔点或低熔点间同1,2-聚丁二烯和无规1,2-聚丁二烯。催化剂以现配方式的活性最高。 3. 以磷酸三苯酯为配体的铬催化剂可获得间同1,2-聚丁二烯，而聚合物中含有低聚物。催化剂以现配方式的活性最高。聚合物的熔点，低聚物的含量与磷酸三苯酯的结构有一定的关系。 4. 以邻菲咯啉为配体的铬催化剂在50℃下聚合异戊二烯，具有高的催化活性，可获得3,4-结构含量约67%的高分子量无规3,4-聚异戊二烯。催化剂的组成对聚合物的微观结构无明显影响。改变聚合温度，可有效控制聚合物的3,4-结构含量和分子量及分布。

稀土离子在硼铝酸盐及相关基质中的VUV-Vis范围发光性质

PDP(等离子平板显示器)是一种最有前途的大屏幕壁挂式彩电,而它需要VUV激发下的高效荧光粉,同时由于VUV荧光粉也是无汞荧光灯的需求,所以研究VUV激发的稀土激活的荧光粉是实际应用的需要.对于光谱分析该工作采用了理论计算与光谱数据分析相结合的方法,对所测光谱各个谱峰进行了详细的指认.得到了以下的结论和成果:1.得到了大量的含氧酸盐中稀土离子的VUV光谱数据.2.首次系统地应用两种方法预测了三价稀土离子的f-d跃迁位置,并首次系统地通过计算预测了三价稀土离子在含氧酸盐中的电荷迁移带的位置.3.首次实验观察到Ce<'3+>的电荷迁移带,观察到了Tb<'3+>的电荷迁移带.4.在所有含Dy<'3+>的样品中都观察到Dy<'3+>的f-d跃迁.5.LaPO<,4>和ABLa(PO<,4>)<,2>(A=K,Na;B=Mg,Zn)基质中,观察到了Ce<'3+>的5个f-d跃迁,指认了Tb<'3+>的5个f-d跃迁,指认了掺杂Ce、Tb的VUV光谱中的所有谱峰.6.对所研究基质中的稀土离子的f-d跃迁和电荷迁移带进行了系统地预测和指认.7.通过总结不同稀土离子在相同基质中的VUV光谱,并参考文献的相关报导,总结了所研究基质的基质吸收位置.8.通过Eu<'3+>的灾光探针作用和ce<'3+>的发射光谱等,确证三价稀土离子在La<,2>CaB<,10>O<,19>基质中同时取代了八配位的Ca<'2+>和十配位的La<'3+>,占据了两种格位.9.合成了一种新型绿色长余辉材料,具有亮度高,余辉时间长,可用日光激发等优点.10.合成了一种UV激发下性能优异的掺Eu<'3+>的红色荧光粉,亮度可以跟商业红粉Y<,2>O<,3>:Eu相比拟,而基质材料与Y<,2>O<,3>相比降低了成本.

稀土发光材料M_2O_3:RE~(3+)（M＝Y，Gd:RE＝Eu，Tb）体系的AAO模板组装

AAO模板具有高度有序的纳米孔阵列，其孔径可以在5一200nm范围内调节，利用AAO模板进行纳米组装已成为纳米结构材料组装的重要技术之一。目前，采用该技术已经制备出了金属、半导体、碳、导电高分子以及其它材料构成的纳米管、纳米线、纳米纤维、电缆等纳米结构单元和有序纳米阵列材料，同时，研究了它们的光、电、磁和催化等特性及其在光学材料、铿电池的电极材料、垂直磁性记录材料和光催化剂等方面的潜在应用。然而，有关稀土发光材料的AAO模板合成及其性质还鲜见报道。本论文采用二次阳极氧化技术制备出了具有高度有序纳米阵列孔的AAO模板。采用溶胶一凝胶法和水热法对稀土发光材料M2O3:RE3+（M＝Y,Gd; RE＝Eu，Tb）体系进行了AAO组装，得到了纳米线、纳米管及其纳米线阵列。对AAO模板和组装样品的形貌、结构和光谱性质进行了表征，得到了一些令人感兴趣的研究结果，其主要的结果和结论总结如下：（1）采用二次阳极氧化法制备出了孔径约为5Onm、35nm和2Onm等系列高度有序纳米阵列孔的基体铝支持的AAO模板和独立支撑的AAO模板。（2）XRD测试结果表明：退火后的基体铝片，其331晶面优先结晶生长，这有利于高度有序纳米阵列孔AAO模板的制备。使用这些退火后的铝片，通过二次阳极氧化法制备的高度有序纳米阵列孔AAO膜为非晶态，并且在退火后转变为γ-Al2O3。（3）未退火的基体铝支持的AAO模板，在350一600nm范围内发出较强的蓝光，其峰值波长位于435nm。该蓝光发射带经过程序控温慢慢退火后完全消失，这说明它产生于缺陷发光中心。（4）采用溶胶一凝胶法，利用AAO模板首次合成出了（YO.96RE0.05）O3（RE＝Eu，Tb）纳米线及其阵列，并通过SEM、EDX、TEM、SAED、XRD和PL分析测试加以确认。x-射线衍射（XRD）和选区电子衍射（SAED）的结果证明，这些纳米线主要是由立方相的RE2O3（RE＝Y或Gd）多晶材料组成的。光谱测试结果表明，同体相材料相比，Eu3＋的，D0一7F2跃迁发射峰和Tb3＋的5D4一7FJ（J=6，5，4，3）跃迁发射峰出现了宽化，这种现象可能是纳米颗粒的表面界面效应所引起的非均匀宽化造成的。（5）首次观察到利用溶胶一凝胶法组装的一部分M2O3:RE3＋（M＝Y，Gd；RE＝Eu，Tb）样品，沿着AAO模板阵列孔壁的边沿所形成的网状结构，并初步地探讨了其形成的机理。（6）对于M2O3:RE3＋（M=Y，Gd；RE＝Eu，Tb）体系，仅仅依靠毛细作用是难以充分地将溶胶前驱液组装进从O模板的阵列孔中。（7）首次利用水热合成法，在中性条件介质下，将（Y，Gd）2O3:Eu3+样品充分地组装进了AAO模板的纳米孔道中，这说明水热产生的高压可以作为AAO模板组 装样品的驱动力。（8）以M2O3: RE3+（M＝Y，Gd；RE＝Eu，Tb）溶胶或氢氧化物沉淀作为前驱物，分别在酸性和碱性条件下，进行了从0模板水热合成组装。实验结果表明，AAO模板被部分地损坏。但在碱性条件下的高压釜中，却得到了单晶纳米管、纳米片和纳米棒。

两种端乙炔基芳醚砜单体的核磁研究双端乙炔基芳醚砜溶液聚合反应和催化剂的研究非等温DSC法测双[4－（4－乙炔基苯氧基）苯基]砜（酮）的本体聚合反应动力学

本工作对下面两种端乙炔基芳醚砜单体的核磁共振谱进行了研究。通过加入位移试剂Eu（fod）_3引起共振吸收峰化学位移值的变化趋热及同核去偶，'H选择质子去偶的方法分别对其'H谱和~(13)C谱（COM）做了归属。在确认对化合物＜I＞'H谱和~(13)C谱（COM）归属的基础上，演绎出三种苯环上取代基团的'H和~(13)C化学位移取代参数。这些基团的取代参数目前在文献中尚未见报导，用这些参数来计算化的＜II＞的'H和~(13)C谱（COM）化学位移值时，与观测值有较好的吻合。本工作对双[4－（4－乙炔基苯氧基）苯基]砜的溶液聚合反就（DMSO）作溶剂、PdCl_2·2DMSO作催化剂）进行了研究。采用高压液体色谱和旋转薄层色谱分离反应的各种中间产物，通过中间产物的红外和'HNMR谱变化，演绎聚合反应的历程，还在'H核磁谱仪样品管内做了短时间反应，跟踪记录反应信息。聚合产物自始至终可分为溶于二氯甲烷和不溶于二氯甲烷两部分。在整个反应过程中，可溶性产物逐渐转变成不溶性产物，色谱分析表明可溶性产物是由未反应的单体、线型及环状低聚物、聚合度在9－10的齐聚物和少量聚合度更高的组分构成的。从称重测量不溶性产物所占比重和可溶性产物的高压液体色谱诸吸收峰峰高的变化，推算出聚合反应过程中单体、主要中间产物的变化趋势。可溶性产物的红外光谱中2920、1665－25、960－930、890，760－730 cm~(-1)吸收峰和'HNMR谱中的5.3, 3.5ppm吸收表明产物具有共轭多烯结构。'HNMR谱在芳核质子区出现7.7ppm吸收峰表明反应初期已有环化现象，这点与本体聚合反应是不同的。不溶性产物除聚合度或交联度高以外，与可溶性产物在结构上也有差异，其芳化程度高很多。从不同反应时间中间产物的红外和'HNMR谱（可溶部分）变化，显示了溶液聚合反应历程十分复杂，同时存在着几种反应。主反应是氯化钯络合物引发的配位络合聚合反应，钯络合物与单体的端乙炔基络合生成活性中心，三键在顺式位打开，生成共轭多烯增长链。链增长过程中伴随着热引起的多烯链顺－反异构化，部分反式多烯分子内环化，继而脱质于芳化生成三取代苯形式的环交联，芳化过程中可发生链的局部断裂。最终产物是共轭多烯链间通过芳环，炔烯桥交联成的体型聚合物。多烯和端乙炔基之间，多烯－多烯之间可发生Diels-Alder反应，因此溶液聚合产物再经短时间热处理，芳化程度增高，玻璃化温度大幅度提高。另外还研究了反应的溶剂效应和增加因含量对反应产率的影响，发现用氯仿和二氯甲烷作溶剂有利于共轭多烯链的顺－反异构化，固含量在2.25－11.25％范围，聚合产率变化不大。本文还对适用于双端炔基聚合反应的催化剂作了广泛的试探，首先考察了若干钯络合物，发现除PdCl_2·2DMSO外，PdCl_2·2MeCN、PdCl_2·2PhCN络合物也可作为双端炔基芳醚砜溶液聚合的催化剂。钴、镍的膦络合物[Co(PPh_3)_2]Cl_2、[Ni(PPh_3)_2]Cl_2可使双端炔基芳醚砜环化生成环状低聚物。极性溶剂四氢呋，二氧六环。氯仿和三氯甲烷可以用作Ziegler-Natta催化剂聚合双端炔基芳醚砜的溶剂。用AlEt_3-Ti(OBu)_4催化得到的聚合物以顺式多烯为主，玻璃化浊度高于250℃，热形变稳定性好。Al/Ti比在6－8时催化活性较高。用稀土体系的Ziegler-Natta催化剂AlEt_3-NdCl_3·2THF、AlEt_3－（CF_3COO）_3Nd也可得到类似的催化效果。制备了以双氰为配位基的高分子－钯络合物，在催化双端炔基单体聚合时具有与类似的低分子钯络合物PdCl_2·2MeCN相近的效果。改变高分子催化剂的N／Pd比未出现明显的活性高峰。这部分工作还有待深入，予期在进一步深入研究之后，该高分子催化剂可用于制备双端乙炔基芒醚砜增强复合材料的连续化浸渍工序，让单体的氯仿溶液流经高分子－钯络合物填充的柱子形成齐聚物后，再浸渍涂层，可缩短成型的热固化时间，具有较大的经济意义。用非等温DSC法测定了双[4-(4-乙炔基苯氧（基)苯基]砜和双[4-(4-乙炔基苯氧基)苯基]酮的本体热聚合及有PdCl_2·2DMSO存在下的催化聚合的反劝力学参数，并与文献报导的（3－乙炔基苯氧基）苯模型物和双[4－（3－乙炔基苯氧基）苯基]砜的本体热聚合反应动力学参数进行比较。经电子计算机最小二乘曲线拟合程序汞得的结果表明表现反就活化能Eap，指数前因子A均与DSC的升温速率和转化率无关。讨论了模型物端乙炔基的位置和链上砜基，羰基的存在对聚合反应的影响，还通过对DSC升温过程中试样的红外光谱跟踪，解释了DSC峰表征的化学反应。

离子注入选育维生素C高产菌

维生素C二步发酵混菌生产中，第一步由单菌发酵将D-山梨醇转化为L-山梨糖，第二步由产酸菌氧化葡萄糖酸杆菌与伴生菌巨大牙孢杆菌混菌发酵将L-山梨糖转化为2-酮基-L-古龙酸（维生素C的前体物）.利用离子注入技术，采用N<'+>离子束为诱变源，诱变维生素C二步混菌发酵中的产酸菌氧化葡萄糖酸杆菌.通过建立的维生素C高产菌筛选方法，以2-酮基-L古龙酸为筛选标记，获得一株维生素C高产菌株D14，其与生产用伴生菌巨大牙孢杆菌组成维生素C新混合菌系ND14，平均醇酸转化率比生产用混菌提高3.3个百分点.维生素C高产菌株D14及维生素C新混合菌系ND14生长特性及发酵特性为：维生素C高产菌株D14生长能力明显增强;维生素C新混合菌系D14于种子培养基中稳定期延长8-12小时，总生物量增加;在发酵过程中ND14生长明显快于CK，菌体总生物量增加.利用均匀设计的方法对新混合菌系ND14发酵培养基进行了优化，其结果为：最适玉米浆浓度为1.6%、最适尿素浓度为1.6%、最适MgSO<,4>浓度为0.03%、最适KH<,2>PO<,4>浓度为0.06%.

若尔盖湿地3种两栖类的种间竞争及畜牧业对其食性的影响

从空间、时间、食物3个方面研究了若尔盖湿地3种两栖类的种间竞争，运用生态位理论探讨了3种两栖类利用环境资源的能力以及它们之间的共存模式，研究了3种两栖类年周期食性，并考察了畜牧业对3种两栖类食性及食物竞争格局的影响；此外，还通过实验室研究对2种两栖类幼体的种间竞争策略进行了考察。主要结果如下： 1、两栖类的空间资源利用状况：在3种两栖类成体生态位宽度的比较中，岷山蟾蜍（Bufo minshanicus）成体在牧场性质(0.41)、牛粪数量(0.42)、植被盖度(0.20)、地表温度(0.50)、地表湿度(0.51) 5个维度上的生态位宽度最窄；而倭蛙（Nanorana pleskei）成体在牛粪数量(0.81)、植被高度(0.63)、植被盖度(0.47)、小水体距离(0.68) 4个维度上的生态位宽度最宽。在3种两栖类亚成体生态位宽度的比较中，岷山蟾蜍亚成体在牧场性质(0.66)、牛粪数量(0.58)、植被高度(0.64)、小水体距离(0.51)、地表湿度(0.79) 5个维度的上生态位宽度最宽；倭蛙亚成体在牧场性质(0.39)、牛粪数量(0.30)、地表温度(0.18)、地表湿度(0.33) 4个维度上的生态位宽度最窄。高原林蛙（Rana kukunoris）在地表温度（成体：0.62；亚成体：0.56）、地表湿度（成体：0.84；亚成体：0.60）两个维度上具有较大的生态位宽度值，而在小水体距离维度上（成体：0.27；亚成体：0.14）的生态位宽度值则很小。比较3种无尾两栖类在不同生长阶段（成体、亚成体）的生态位宽度，发现高原林蛙和倭蛙的亚成体对栖息环境的要求更高。3种两栖类空间资源利用的相似程度很高，高原林蛙与倭蛙之间的生态重叠度(0.87)较之它与岷山蟾蜍(0.81)的生态位重叠度更大。 2、两栖类的日活动节律：高原林蛙成体、亚成体、岷山蟾蜍亚成体活动的最低气温为0℃、2℃、8℃；岷山蟾蜍和高原林蛙亚成体出现的数量与气温成极显著的正相关（r=0.797, p<0.001；r=0.794, p<0.001），高原林蛙成体出现的数量与气温有一定相关性（r=0.456, p<0.05）；晴天时两栖类的活动性明显高于阴天（p<0.001）；多云转晴天气，高原林蛙和岷山蟾蜍亚成体出现两次日活动高峰，分别为中午12:30左右和下午15:30～16:30之间；多云天气，高原林蛙和岷山蟾蜍亚成体出现两次日活动高峰，分别为9:30～10:30之间和15:30～16:30之间。 3、两栖类的食物资源利用状况：春、秋两季，高原林蛙最主要的食物是蜉金龟科(Aphodiidae)昆虫，相对重要性指数(IRI)最高（春季：35.28%，秋季：28.57%），其次为昆虫的幼虫，以及双翅目的毛蚊科(Bibionidae)、蝇科(Muscidae)、丽蝇科(Calliphoridae)昆虫，秋季，蝗虫是高原林蛙食物组成中的重要部分；岷山蟾蜍最主要的食物是蚂蚁(IRI，春季：85.54%，秋季：49.70%)，其次为蜉金龟科、象甲科(Curculionidae)、步甲科(Carabidae)、粪金龟科(Geotrupidae) 等鞘翅目昆虫；倭蛙春季的最主要食物也是蜉金龟科昆虫(IRI，春季：13.41%)，其次为蚂蚁、毛蚊科昆虫、昆虫的幼虫以及狼蛛科(Lycosidae)。3种两栖类中，倭蛙的食性生态位宽度相对较宽（0.43），而岷山蟾蜍（0.09）和高原林蛙（0.22）的生态位宽度较窄，与春季相比，两栖类在秋季的食谱更宽。以利用食物种类为标准，春季高原林蛙与倭蛙的生态位重叠度(0.40)比它与岷山蟾蜍的生态位重叠度（0.33）更大。 4、畜牧业对两栖类食性及食物竞争格局的影响：以藏牦牛粪为食物或寄居场所的昆虫，如蜉金龟科、粪金龟科、毛蚊科、蝇科、丽蝇科昆虫和某些昆虫幼虫，是3种两栖类食物谱中最主要的组成部分，蜉金龟科昆虫在高原林蛙食谱中的比例更高，高原林蛙可能从畜牧业发展中获得更多的好处，使之在食物竞争方面处于优势地位。与无放牧样地相比，在有放牧样地的中，两栖类食谱中的蜉金龟科昆虫数量更多(有放牧：31.94%；无放牧：21.32%)、出现频率更高(有放牧：76.38%；无放牧：44%)。然而在不同样地上（有放牧/无放牧），两栖类的食物组成无显著性差异(P=0.188)，两栖类的数量(P=0.075)、肥满度(P=0.537)均没有显著差别。 5、两栖类幼体的竞争策略：实验室条件下，通过活动性水平，变态时的体重、增长率和完成变态所需时间考察自然条件下常同水塘分布的中华蟾蜍（Bufo gargarizans）和高原林蛙蝌蚪的竞争策略。结果表明：中华蟾蜍蝌蚪在不同食物资源条件下，所选择的生存策略可能不同，即食物资源充足时，增加活动性获取更多食物，食物资源有限时，降低活动性且提前完成变态；与中华蟾蜍蝌蚪相比，在食物资源有限时高原林蛙蝌蚪获取食物能力可能更强。 This paper presented the study of competition of three amphibians (Rana kukunoris, Nanorana pleskei, Bufo minshanicus) based on spatial, temporal and dietary scales in Zoige wetland. We measured coexistence patterns of three amphibians and analyzed their ability of exploiting resource. Effects of grazing on the diet composition and diet competition of amphibians were analyzed by their diet composition during spring and autumn. Furthermore, we examined the competitive ability of larval common frogs (Rana kukunoris)and common toads(Bufo gargarizans) in a laboratory experiment, and analyzed their competitive strategies respectively. The results were as follows: 1 .The status of using spatial resource Niche breadths of B. minshanicus adults on 5 dimensional axes including character of pasture(0.41), number of yaks dung(0.42), vegetation coverage(0.20), temperature (0.50)and humidity(0.51) of ground surface were narrower than adults of R. kukunoris and N. pleskei. Niche breadths of B. minshanicus subadults were broader than R.kukunoris subadults and N.pleskei subadults on 5 dimensional axes including character of pasture (0.66), number of yaks dung (0.58), vegetation height (0.64), distance to small waterbodies (0.51), humidity of ground surface (0.79). Niche breadths of N. pleskei subadults were the narrowest in three anurans subadults on 4 dimensional axes including character of pasture (0.39), number of yaks dung (0.30), temperature (0.18) and humidity (0.33) of ground surface, niche breadths of N. pleskei adults were the broadest in three anurans adults on 4 dimensional axes including number of yaks dung (0.81), vegetation height (0.63) and coverage(0.47), distance to small waterbodies(0.68).Comparatively, niche breadths of R. kukunoris were broader on the two microclimate factors including temperature(adults：0.62；subadults：0.56) and humidity (adults：0.84；subadults：0.60)of ground surface, but was narrow on distance to small waterbodies(adults：0.27；subadults：0.14). Strategies for using habitat resource of adults and subadults of the three species anuran were different. Generally, subadults of R. kukunoris and N. pleskei needs better habitat condition. It was quite similar that three anurans exploited spatial resource, Niche overlap between R. kukunoris and N. pleskei (0.87) was greater than that between R. kukunoris and B.minshanicus(0.81). 2.Daily activity rhythm R. kukunoris audlts were active when air temperatures were as low as 0℃, R. kukunoris subadults were active at 2℃, B.minshanicus subaudlts were active at 8℃. Positive correlation was found between activities of amphibians and air temperature, Subadults of R.kukunoris, (r=0.797, p<0.001), Subadults,of,B.minshanicus, (r=0.794, p<0.001), andbadults,of,R.kukunoris(r=0.456, p<0.05).Amphibians were more active during sunny days than cloudy days. In cloudy turning into sunny, R. kukunoris and B.minshanicus subadults had two active peak: at noon about 12:30 and 15:30～16:30 pm; in cloudy, R. kukunoris and B.minshanicus subadult had two active peak too : 9:30～10:30am,15:30～16:30pm. 3.Diet analysis Aphodiidae was the most commonly consumed food item by R. kukunoris based on index of relative importance (IRI) during spring (35.28%) and autumn (28.57%) in Zogie wetland. Besides Aphodiidae, larval insect, dipterans such as Bibionidae, Muscidae, Calliphoridae also were important food item for R. kukunoris, in autumn, locust was one of important food item for R. kukunoris. The most important food item for B.minshanicus during spring (IRI:85.54%) and autumn (IRI:49.70%) was ants, following, was coleopterans, such as Aphodiidae, dung beetle. Aphodiidae (IRI:13.41%) were the most important consumed food item by N. pleskei during spring too, following, was ants and Bibionidae. Dietary breadth of N. pleskei (0.43) were greater than R. kukunoris (0.22) and B. minshanicus (0.09). As a whole, Dietary breadth of amphibians during aurumn were greater than spring. Based on prey item, dietary overlap between R. kukunoris and N. pleskei (0.40) was greater than that between R. kukunoris and B.minshanicus (0.33) during spring. 4.Effects of grazing on the diet composition and diet competition of amphibians Amphibians are an important part of the pasture ecosystems as prey and predator. In Zogie wetland, major diet of amphibians was closely associated with dung of yaks, for example, Aphodiidae, Bibionidae, Muscidae, dung beetle. Dung of yaks was major diet and habitat of these insects. Proportion of Aphodiidae was higher in diet composition of R. kukunoris than N. pleskei and B.minshanicus, with development of pasturage, R. kukunoris may have a diet competitive advantage over N. pleskei and B.minshanicus. Number of Aphodiidae in diet composition of amphibians was higher in samples with grazing (31.94%) than in those without grazing (21.32%). Occurrence Frequency of Aphodiidae in diet composition of amphibians was higher in samples with grazing (76.38%) than in those without grazing (44%). However, There was not significantly different on diet composition (P=0.188), and number (P=0.075) and the relative fatness (P=0.537) of amphibians between grazing samples and without grazing. 5.Competitive strategies of amphibian larvae I examined the competitive ability of larval toads (Bufo gargarizans) and frogs (Rana kukunoris) which co-occur in the nature pond by activity level, the growth rate and mass at metamorphosis and larval period in a laboratory experiment. The results suggest: In laborary, B.gargarizans adapted himself to different food level by changing activity. At high food level, B. gargarizans increased activity to gain more diet. At low food level, B. gargarizans decreased activity and achieved early metamorphosis. When food resource was limit, R. kukunoris could gain more food than B. gargarizans.

Polyimides derived from 3,3 '-bis(N-aminophthalimide)

A novel diamine, 3,3'-bis(N-aminophthalimide) (BAPI), was prepared from 3,3'-bis(N-phenylphthalimide). Its structure was determined via IR, H-1 NMR, N-15 NMR, elemental analysis, and single-crystal X-ray diffraction analysis. A series of homo- and copolyimides were synthesized by a conventional one-step method in p-chlorophenol. The characteristic IR absorption bands of hydrazine-based imide groups were near 1780, 1750, 1350, 1100, and 730 cm(-1). The polymers showed good solubility in polar aprotic solvents and phenols at room temperature. The temperatures of 5% weight loss (T-5%) of the polyimides ranged from 495 to 530 degrees C in air. DMTA analyses indicated that the glass-transition temperatures (Tgs) of the polyimides were in the range 371-432 degrees C. These polymers had cutoff wavelengths between 350 and 400 nm. The polyimide films of 6FDA/BAPI and 4,4'-HQPDA/BAPI were colorless; other films were pale yellow or yellow.

冲绳海槽黑潮流域近4万年以来的古海洋环境演化

本文采用取自冲绳海槽的91个站位的表层样品和2个柱状岩芯，通过微体古生物有孔虫分析、氧碳同位素测试、AMS~(14)C测年、沉积物粒度和地球化学分析，探讨了现代生物群落、表层沉积物氧同位素与现代海洋环境之间的关系，进而对冲绳海槽区域近4万年来的古海洋环境和古黑潮演化进行了详细的研究。表层沉积物中的浮游有孔虫氧同位素与现代海洋环境之间的关系密切，浮游有孔虫从G.ruber到G.sacculifer到N.dutertrei其δ~(18)O值由轻变重，表明三种有孔虫其生活水层依次由浅到深。在横穿海槽的剖面上浮游有孔虫δ~(18)O在近陆端因受冲淡小影响较强而变轻，而在东侧站位，受黑潮暖流或其支流的影响氧同位素同样有变轻的趋势。N. dutertrei和G.ruber的氧同位素差值表明了冲绳海槽北部区域黑潮支流对表层水体的影响要大于次表层水体，而在冲绳海槽南部区域，黑潮暖流对次表层水体有相对较强的影响。冲绳海槽南部表层沉积物中的浮游有孔虫整体上属于赤道区组合，溶解作用对该区的浮游有孔虫群落有显的影响，冲绳海槽北部区浮游有孔虫组合对具有温带群落的特征。浮游有孔虫分布与海洋环境密切相关，南北区的浮游有孔虫分布都明显受暖流的影响，在暖流的主流轴处浮游有孔虫丰度通常较高。冲绳海槽具有相对较浅的碳酸盐溶跃面，浮游有孔虫丰度和底栖有孔虫深水胶结壳的含量都进一步表明了该区碳酸钙溶跃面大约在1700 m水深左右，比开放大洋明显要浅得多。表层沉积物中的底栖有孔虫主要受水深和水团等因素的制约。水深制约着有孔虫属种的分带，也影响底栖有孔虫的组合。根据Q型因子分析，冲绳海槽南部表层沉积物中的底栖有孔虫从陆架连缘到海槽底部可以划分为5个特定的组合，分别对应黑潮表层水和次层水影响环境、黑潮中层水影响环境、溶跃面以上的黑潮深层水影响环境、黑潮底层水团影响环境和溶解作用较强的槽底环境；北部区的底栖有孔虫群落反映了四个组合，分别代表了陆架混合水团影响环境、黑潮暖流中层水影响环境、冷涡沉积和上升流区影响环境以及对马暖流水团影响下的环境。以氧同位素曲线为基础，结合AMS~(14)C测年和生物地层学对柱状岩芯进行了地层划分和对比，E107孔记录了冰消期以来大约15,000 a来的古环境演化记录，具有较高的沉积速率，DOC－42孔保存在主要是末冰期中40－10ka BP期间的古环境沉积记录，沉积物记录的分辨率相对较低。浮游有孔虫有碎壳比和底栖有孔虫深海胶结壳含量表明了现代冲绳海槽的浅溶跃面是大约最近2000 a BP才开始突然变浅形成的，碳酸盐的溶解作用从冰消期到现在逐增强。冲绳海槽南部E107孔的底栖有孔虫组合把映了15,000 a来的底层水团具有两种完全不同的营养状况，约6500 a BP以前有机质通量较高，6500 a BP以后有机质通量则明显降低。DOC－42孔的底栖有孔虫组合反映该区约4万年以来的底部水团演化主要受有机质通量和氧含量的共同制约，氧同位素3期主要为高有机质通量的沉积环境，伴随有氧含量水平的较大波动；氧同位素2期有机质通量有所降低，氧含量整体为中等水平；氧同位素1期早期义部水体则较高氧含量为主。浮游有孔虫温跃层转换函数反映了冲绳海槽中部的温跃层在约13100 a BP有一个明显的变化，在这之前产温跃层深度较浅，平均89 m，而在该时间以后，温跃层平均深度变为166 m。此外在160 cm处和100 cm的温跃层深度的两次明显的降低，分别对应于新仙女木事件和黑潮暖流的重新入侵，表明这两个事件导致了海洋上层水体结构的突然变化。冲绳海槽北部浮游有孔虫转换函数古温度和浮游有孔虫的低温、低盐特征种反映了在氧同位素3期早期约40000a BP和氧同位素2期间存在两个明显的低温、低盐阶段，可能与沿岸水在该期间加强有关。其中氧同位素3期早期的表层海水古水温比末次冰期还要低，反映了区域海洋环境的重大变化。冲绳海槽南部E107孔的沉积物粒度、地球化学特征、黑潮特征指示种、表层古水温以及底层水团的性质在6500 a BP左右发生了重大的改变，与冲绳海槽南部的其他岩芯反映的古环境化基本一致，表明了南部海槽在6500 a BP前后古黑潮流径发生了重大变化。而冲绳海槽北部区域2万年以来的古环境则与南部有明显差异，总结前人对冲绳海槽古黑潮流径的研究，笔者对未次冰盛期古黑潮流径提出了新的推测。