La_4(P_2O_7)_3:Ce,Gd,Tb磷光体的合成与光谱性质

本文首次采用溶液沉淀法合成了一系列La_4(P_2O_7)_3;Ce,Gd,Tb磷光体.经X射线分析表明,它们属于纯的La_4(P_2O_7)_3相。测定了这些化合物的激发和发射光谱、相对亮度及Ce~(3+)的发光寿命,观察到在此基质中Ce~(3+)与Gd~(3+)的光谱重叠,它们之间存在着一定的相互作用,使(La_(0.64)Ce_(0.3)Gd_(0.06)_4(P_2O_7)_3的亮度比(La_(0.7)Ce_(0.3)_4(P_2O_7)3和(La_(0.94)Gd_(0.06)_4(P_2O_7)_3有少许增加.此外,Ce~(3+)能有效地敏化Tb~(3+)~9,从而大大增强Tb~(3+)的发射.然而,Gd~(3+)与Tb~(3+)共存时存在着竞争吸收和独自发射,使(La_(0.80)Gd_(0.06)Tb_(0.14)_4(P_2O_7)_3的亮度与单掺的(La_(0.86)Tb_(0.14)_4(P_2O_7)3相比有少许降低.相应地在Ce,Gd和Tb共掺时,由于Gd~(3+)的影响,使Tb~(3+)的发射减弱,从而总的发光相对亮度有所降低。

WATER-SOLUBLE AND AMPHIPHILIC POLYMERS .11. GRAFT-POLYMERIZATION OF ACRYLIC-ACID ON POLY(VINYL ALCOHOL)

The graft polymerization of acrylic acid(AA) on poly(vinyl alcohol) (PVAL) has been investigated by using either potassium persulfate (KPS) or ceric ammonium nitrate(CAN) as an initiator. In the case of KPS initiation, the formation of the graft polymer always lags behind the homopolymer formation. The graft polymer is separated by acetone, and the increase of reaction temperature favors the homopolymer formation at the early stage. In the case of CAN initiation, graft polymers with a high PAA content can hardly be obtained when the polymerization is performed under nitrogen and at < 0.06 mol/L HNO3 concentration. It has been found that incorporation of a small amount of oxygen in a protective nitrogen gas accelerates markedly the graft polymerization, and that the resulting graft polymers can not be separated by acetone precipitation technique in most cases. The Dalian nitrogen(containing 0.7% oxygen) is a good protective gas for CAN-initiated PVAL-AA graft polymerization.

四-4-(2-正丁氧基乙氧基-羰基)酞菁铜(Ⅱ)在四氢呋喃和氯仿中的二聚物

本文通过对四-4-(2-正丁氧基乙氧基-羰基)酞菁铜(Ⅱ)在THF和CHCl_3溶液可见光谱的分析表征了它在一定的浓度范围(10~(-7)～10~(-5)mol/L)存在单分子和双分子聚集态之间的动态平衡。在THF和CHCl_3溶液中,双分子二聚物的离解常数K_d=C~2m/C_D分别是2.08(±0.05)×10~(-6)mol/L和1.10(±0.06)×10~(-6)mol/L。利用作图法,绘制出纯单分子和纯二聚物的可见光谱图。最后,对两种溶液可见光谱的区别进行了讨论。

菲律宾蛤仔（Ruditapes philippinarum）对胶州湾生态环境影响的现场研究

本文对我国胶州湾养殖的主要滤食性贝类菲律宾蛤仔的生理生态学进行了系统研究，通过资料收集、现场调查、定点连续观测、现场模拟实验等综合性方法探讨了菲律宾蛤仔养殖对胶州湾生态环境的影响。主要系统调查了不同季节胶州湾自然沉积物中C、N和P的变化；研究了菲律宾蛤仔生物沉积作用的周年变化；同时还研究了不同月份菲律宾蛤仔的耗氧率，排泄率的变化。结果如下: 1、综述了滤食性贝类通过滤食、生物沉积和呼吸排泄等作用对海区环境的影响,系统评述了埋栖性贝类生物沉积的测定方法及其生态效应。国际上已有不少研究专门报道了贝类在海区现场的生物沉积作用，而在我国，关于埋栖性贝类生物沉积特征的研究较少。 2、在胶州湾红岛附近养殖海区，从2003年10月到2004年7月以及2005年8月到2005年12月对菲律宾蛤仔生物沉积进行了现场测定。大、中和小规格菲律宾蛤仔生物沉积速率范围分别为121.6～1527.4mg/ind·d，49.5～902.1mg/ind·d，14.2～653.9mg/ind·d。海底自然沉积物OM分别为3.1％和5.7±1.1％。而大、中和小规格菲律宾蛤仔生物沉积物的OM分别为6.2±1.2％、5.9±1.3％和6.1±1.4％。大、中和小菲律宾蛤仔生物沉积物TP含量分别为399±26ppm，372±16ppm，345±15ppm。大、中和小规格蛤子生物沉积物中的OP分别为80±17ppm，92±12ppm和102±10ppm，明显高于对照沉积物的OP。生物沉积物中的OP/TP要明显高于对照沉积物，前者为23～25％，而后者仅为20％。菲律宾蛤仔生物沉积速率呈明显季节性变化，其与软体干重呈异速方程关系，a值的变化范围为0.85～4.50（平均为2.32）。菲律宾蛤仔贝肉的OC和ON含量分别为40.80±7.59％和的10.26±2.19％。贝壳的OM、TP、OP、OC和ON含量分别为3.28±0.47%、109.2±16.6ppm、64±22.9ppm、12.21±0.30％和0.19±0.05％。 3、不同规格菲律宾蛤仔的代谢率呈明显季节变化。7月份，单位个体菲律宾蛤仔耗氧率最高为1.72 g/ind•h；8月份，排氨率和排磷率达到最高，分别为2.44μmol/ind•h、0.58μmol/ind•h。菲律宾蛤仔的O:N在10.7~31.9范围内，O:N和N:P具有明显的季节变化，8月份最大。 4、研究了本湾底质环境特征，测定了自然沉积物的OM、OC、ON、TP和OP的含量。胶州湾站位沉积物的有机质和C、N、P含量季节变化不大，有机质含量大约为3.5％，OC和ON含量大约为0.7％和0.06％。TP含量为285ppm左右，OP含量大约为50ppm。养殖海区沉积物有机质和C、N、P的含量明显高于非养殖海区沉积物含量，其C/N、C/OP和OP/TP一般也比非养殖海区站位高。 夏季，胶州湾菲律宾蛤仔养殖区（平均密度按600ind/m2计算）单位面积（m2）的生物沉积速率平均为176g/m2•d，对于整个海湾，将有1.2万吨的悬浮颗粒物通过贝类排粪作用沉积到海底。通过菲律宾蛤仔的呼吸作用，单位面积（m2）的耗氧量为6.67gO2/m2•d；同时从海底向水体释放大约为16.7μmolN /m2•d和3.3μmolP/m2•d的溶解态N和P；对于整个海湾，菲律宾蛤仔将耗掉水体中的467T/d氧气，同时向水体中释放16.4T/d氨氮和7.2T/d无机磷。对于半封闭的胶州湾，大规模菲律宾蛤仔的滩涂养殖其产生的生物沉积物聚集于海底可能会对海区底部的物理化学和生物环境产生很大影响；而氧的消耗、氨和无机磷的排泄，会对水层中的物理化学环境和营养盐循环产生很大影响。从而由此推测，菲律宾蛤仔高密度大规模的养殖，在整个胶州湾水层－底栖系统耦合作用中可能起着很重要的作用。

八株海洋微生物次级代谢产物的研究

本论文选取4株胶州湾海洋放线菌和4株条斑紫菜丝状体相关丝状真菌，进行了次级代谢产物的分离纯化与鉴定，共得到78个单体化合物，其中10个为新颖结构。对部分纯化合物进行了抑菌，抗肿瘤活性测试，并对菌株进行了菌种鉴定。具体结果如下： 从胶州湾放线菌M491，M097，M361和M353得到40个单体化合物，其中6个为新颖结构化合物。从M491分离到14个单体化合物，包括2个新结构倍半萜15-hydroxy-T-muurolol (1a)和11,15-dihydroxy-T-muurolol (1b)，2个首次报道的微生物来源的倍半萜T-muurolol (2b)和3α-hydroxy-T-muurolol (2c)，2个新颖结构大环内酯chalcomycin C (7)和chalcomycin D (8)。制备了3-oxo-T-muurolol (2a)单晶体，纠正了前人发表的错误结构。从M353分离得到10个化合物，包括2个新颖倍半萜5-hydroxy-epi-isozizaene (28)和5,14-dihydroxy-isozizaene (30)。自M097和M361分别分离得到12个，4个已知结构化合物。 从健康条斑紫菜丝状体分离得到了12株真菌。从优势附生菌N5分离得到了12个化合物，包括phenylacetic acid (42)，p-hydroxyphenylethyl alcohol (43)和L-β-phenyllactic acid (49)等广谱抗生素和紫菜生长调节剂。 对分离自白斑病条斑紫菜丝状体真菌N27，EF8，GA4进行了次级代谢产物研究，分离得到38个单体化合物。从GA4分离得到了16个化合物，4个为新结构化合物，包括1个酰脲类化合物hualyzin (62)和3个phenalenone族新化合物7-methyl isonorherqueinone (69)，7,8-dimethyl atrovenetin (70)和8-methyl-deoxyherqueinone (73)。从真菌N27和EF8分别分离得到12个和2个已知结构化合物。 采用MTT法，对37株人体肿瘤细胞株活性表明：chalcomycin C (7)和chalcomycin D (8)具有非常强的细胞毒活性，其平均IC50分别为0.027 μg/mL和0.007 μg/mL。7,8-Dimethyl atrovenetin (71)和8-methyl deoxyherqueinone (73)具有中等细胞毒活性，其平均IC50分别为5.1 μg/mL和0.7 μg/mL。 此外，本文首次报道了几个已知化合物的细胞毒活性，分别是chalcomycin （0.015 μg/mL），kalamycin (0.06 µg/mL)，(+)-homononactic acid（1.9 µg/mL），(+)-nonactic acid（2.3 µg/mL），griseoviridin（3.9 µg/mL），cyclo（L-Trp-L-Phe）（3.3 µg/mL），WIN 64821（5.8 µg/mL）和3,5-dihydroxy-2-methyl-4-pyrone（3.3 µg/mL）。 菌种鉴定结果表明：M353归属链霉菌，GA4，N27归属青霉属，EF8归属曲霉属，N5为枝孢霉属。

Nutrient structure of seawater and ecological responses in Jiaozhou Bay, China

Nutrient concentrations in seawater, and C, N, P, Si and chlorophyll a content in different-sized particulates were measured in Jiaozhou Bay, and C, N, P, Si composition in different-sized fractions of phytoplankton and their ecological responses to nutrient structure of the seawater were studied. Microphytoplankton and nanophytoplankton were dominant in Jiaozhou Bay. High C (16.50-20.97 unol L-1), N (2.46-2.99 mu mol L-1) and low P (0.06-0.12 mu mol L-1), Si (0.18-0.57 mu mol L-1) content, and high N/P (24.7-64.6) and low SUP (4.4-10.8), Si/N (0.06-0.20) ratios were found in all sized groups of particulates. These values reflected the elemental compositions of different-sized fractions of phytoplankton as being an ecological response to the nutrients in the seawater. The ratios deviated significantly from the Redfield values. The nutrient composition of seawater and particulates and their relationship to chlorophyll a showed that phytoplankton growth was possibly limited by Si. Si limitation appears favorable for controlling the ecological equilibrium of Jiaozhou Bay. Different-sized fractions of phytoplankton had different suitability to nutrient structures of the seawater. Among phytoplankton size groups, nanophytoplankton and microphytoplankton growths were more adaptable in eutrophic Jiaozhou Bay, and more competitive for assimilation of Si. This is consistent with their diatom-dominated composition, controlling the biomass and productivity of phytoplankton in Jiaozhou Bay. (c) 2006 Elsevier Ltd. All rights reserved.

青藏高原主要植被类型生物生产量的比较研究

以18种群落类型的实测数据和1013块森林测树样地的估算数据为基础，首次系统地分析和比较了青藏高原主要植被类型生物生产量的构成规律及分布格局。亚高山暗针叶林的生物量一般在300t/hm2以上，最高可达约1600 t/hm2，叶生物量8～39 t/hm2，根茎比0.1～0.2，生产量8～13 t/hm2．a-；高山灌丛类型生物量20～40t/hm2，叶生物量3～6t/hm2，根茎比0.4～0.8，生产量4～7 t/hm2．a-；高寒草甸生物量一般为20～60 t/hm2，沼泽草甸高达100 t/hm2以上，叶生物量2.5～5.5 t/hm2，根茎比8～20，生产量4～9 t/hm2．a-；高原冬小麦和春小麦年生物产量高达26～30 t/hm2，叶生物量12～16t/hm2，根茎比约0.06。在垂直分异方面，随着海拔升高，生物量呈递增, 在一定海拔高度达最大, 海拔继续升高生物量则迅速下降;而生产量随海拔升高一般呈递减趋势, 反映出热量条件随海拔升高而递减的限制作用。与全国相比, 青藏高原同一森林植被类型的生物量均高于全国的平均水平, 而其生产量基本持平。

高温实验中重金属钼在硅酸盐熔体中的含量研究

This dissertation discusses current status of high temperature and high pressure and focuses on analyzing systematically the solubility of heavy metals in the silicate magma in HTHP experiments. The high temperature study on the content of heavy metal molybdenum in the silicate melts in this dissertation, which is granted, based on the geology mineralization model and the theory of HTHP experiments and combined with mineralization grade and geochemical nature of Mo, discusses the difference of mineralization between mantle plume and aqueous fluids and comes to the conclusions, which are as follows: (1) The content of Mo in the silicate melts is much greater than Mo mineralization grade. The molybdenum ore has the exploitation value when the industrial grade is higher than 0.06%. Mo content in different silicate melts varies because of the concentration of SiO2, that is, Mo content in the granodiorite is greater. (2) The content of Mo, which varies with reaction time, arises first and drops down in the alkali basalt melts, while variation is not too obvious in the granodiorite melts on the whole. (3) According to the picture of sample, the conclusion is not reached very well on some issues, such as the volatility and characteristic of molybdenum oxide and dependence on the geology environment.

铂族元素分析方法研究及其在有关地质问题中的应用

Characterization of Platinum Group Elements (PGE) has been applied to earth, space and environmental sciences. However, all these applications are based on a basic prerequisite, i.e. their concentration or ratio in the research objects can be accurately and precisely determined. In fact, development in these related studies is a great challenge to the analytical chemistry of the PGE because their content in the geological sample (non-mineralized) is often extremely low, range from ppt (10~(-12)g/g) to ppt (10~(-9)g/g). Their distribution is highly heterogeneous, usually concentrating in single particle or phase. Therefore, the accurate determination of these elements remains a problem in analytical chemistry and it obstructs the research on geochemistry of PGE. A great effort has been made in scientific community to reliable determining of very low amounts of PGE, which has been focused on to reduce the level of background in used reagents and to solve probable heterogeneity of PGE in samples. Undoubtedly, the fire-assay method is one of the best ways for solving the heterogeneity, as a large amount of sample weight (10-50g) can be hold. This page is mainly aimed at development of the methodology on separation, concentration and determination of the ultra-trace PGE in the rock and peat samples, and then they are applied to study the trace of PGE in ophiolite suite, in Kudi, West Kunlun and Tunguska explosion in 1908. The achievements of the study are summarized as follows: 1. A PGE lab is established in the Laboratory of Lithosphere Tectonic Evolution, IGG, CAS. 2. A modified method of determination of PGE in geological samples using NiS Fire-Assay with inductively coupled plasma-mass spectrometry (ICP-MS) is set up. The technical improvements are made as following: (1) investigating the level of background in used reagents, and finding the contents of Au, Pt and Pd in carbonyl nickel powder are 30, 0.6 and 0.6ng/g, respectively and 0.35, 7.5 and 6.4ng, respectively in other flux, and the contents of Ru, Rh, Os in whole reagents used are very low (below or near the detection limits of ICP-MS); (2) measuring the recoveries of PGE using different collector (Ni+S) and finding 1.5g of carbonyl nickel is effective for recovering the PGE for 15g samples (recoveries are more than 90%), reducing the inherent blank value due to impurities reagents; (3) direct dissolving nickel button in Teflon bomb and using Te-precipitation, so reducing the loss of PGE during preconcentration process and improving the recoveries of PGE (above 60% for Os and 93.6-106.3% for other PGE, using 2g carbonyl nickel); (4) simplifying the procedure of analyzing Osmium; (5)method detection limits are 8.6, 4.8, 43, 2.4, 82pg/g for 15g sample size ofRu, Rh, Pd, Ir, Pt, respectively. 3. An analytical method is set up to determine the content of ultra-trace PGE in peat samples. The method detection limits are 0.06, 0.1, 0.001, 0.001 and 0.002ng/mL for Ru, Rh, Pd, Ir and Pt, respectively. 4. Distinct anomaly of Pd and Os are firstly found in the peat sampling near the Tunguska explosion site, using the analytical method. 5. Applying the method to the study on the origin of Tunguska explosion and making the following conclusions: (1) these excess elements were likely resulted from the Tunguska Cosmic Body (TCB) explosion of 1908. (2) The Tunguska explosive body was composed of materials (solid components) similar to C1 chondrite, and, most probably, a cometary object, which weighed more than 10~7 tons and had a radius of more than 126 m. 6. The analysis method about ultra-trace PGE in rock samples is successfully used in the study on the characteristic of PGE in Kudi ophiolite suite and the following conclusions are made: (1) The difference of the mantle normalization of PGE patterns between dunite, harzburgite and lherzolite in Kudi indicates that they are residual of multi-stage partial melt of the mantle. Their depletion of Ir at a similar degree probably indicates the existence of an upper mantle depleted Ir. (2) With the evolution of the magma produced by the partial melt of the mantle, strong differentiation has been shown between IPGE and PPGE; and the differentiation from pyroxenite to basalt would have been more and more distinct. (3) The magma forming ophiolite in Kudi probably suffered S-saturation process.

城市生活垃圾填埋场释放汞的形态初步研究

大气的人为汞释放源研究已经较为广泛,但国内外对垃圾填埋场这一潜在的大气汞释放源还没有重视,尤其是垃圾填埋场释放汞的形态研究较为缺乏。2003 年11 月下旬,对贵阳市一新建的生活垃圾填埋场排放气体中的总汞( TGM) 、单甲基汞(MMHg) 、二甲基汞(DMHg) 进行了初步的研究。结果显示填埋半年、填埋一年与填埋两年的垃圾填埋场排气筒气体中总汞浓度分别为665. 52 ±291. 25 ng/ m3 ( n = 305) 、25. 6 ±3. 2 ng / m3 ( n = 13) 、14. 5±1. 8 ng/ m3 ( n = 28) ;填埋半年与填埋两年的垃圾填埋场排气筒气体中单甲基汞浓度分别为2. 06 ±1. 82 ng/ m3( n = 11) 、0. 18 ±0. 06 ng/ m3 ( n = 2) ,二甲基汞浓度为9. 45 ±5. 18 ng/ m3 ( n = 12) 。这一结果初步说明垃圾填埋场不仅是大气总汞的释放源类型之一,也是大气中毒性更强的单甲基汞与二甲基汞的释放源之一。

Heat capacity and thermodynamic properties of myclobutanil

The low-temperature heat capacities of myclobutanil (C15H17CIN4) were precisely measured with an automated adiabatic calorimeter over the temperature range from 78 to 368 K. The sample was observed to melt at (348.800 +/- 0.06) K. The molar enthalpy and entropy of the melting as well as the chemical purity of the substance were determined to be Delta(fus)H(m) = (30931 +/- 11) J.mol(-1), Delta(fus)S(m) = (88.47 +/- 0.02) J.mol(-1).K-1 and 99.41%, respectively. Further research of the melting process for this compound was carried out by means of DSC technique. The result was in agreement with that obtained from the measurements of heat capacities.

Heat capacity and enthalpy of fusion of fenoxycarb

Fenoxycarb was synthesized and its heat capacities were precisely measured with an automated adiabatic calorimeter over the temperature range from 79 to 360 K. The sample was observed to melt at (326.31 +/- 0.14) K. The molar enthalpy and entropy of fusion as well as the chemical purity of the compound were determined to be (26.98 +/- 0.04) kJ-mol(-1), (82.69 +/- 0.09) J-K-1-mol(-1) and 99.53% +/- 0.01%, respectively. The thermodynamic functions relative to the reference temperature (298.15 K) were calculated based on the heat capacity measurements in the temperature range between 80 and 360 K. The extrapolated melting temperature for the absolutely pure compound obtained from fractional melting experiments was (326.62 +/- 0.06) K. Further research on the melting process of this compound was carried out by means of differential scanning calorimetry technique. The result was in agreement with that obtained from the measurements of heat capacities.