内蒙古呼伦贝尔市饮茶型氟铝联合中毒研究

目的探讨饮茶型氟中毒是否为砖茶型氟铝联合中毒。方法对饮茶型氟中毒病区进行饮水、砖茶、奶茶、主食、副食及牧民发、血、尿氟铝水平检测,对饮茶型氟中毒病区儿童和成人进行临床检查和拍摄X线片,同时对成人进行血液生物化学检查,以饮水型病区及非病区居民为对照组。结果呼伦贝尔市饮茶型病区饮水、主食、副食氟铝水平均在正常范围,砖茶氟铝水平分别为(541.3±48.8)、(4351±724)mg/kg,奶茶氟铝水平分别为(3.83±0.73)、(4.28±1.56)mg/L。饮水型病区饮水氟铝水平分别为(3.68±1.05)、(0.45±0.25)mg/L。饮茶型病区牧民氟总摄入量96.15%、铝总摄入量89.60%来源于砖茶。儿童氟斑牙检出率饮茶型病区为25.24%,饮水型病区为63.17%,饮茶型病区非常显著低于饮水型病区(P<0.01);成人氟中毒检出率饮茶型病区为42.61%,饮水型病区为28.83%,饮茶型病区显著高于饮水型病区(P<0.01)。结论呼伦贝尔市饮茶型氟中毒发病机理较为复杂,可能是砖茶型氟铝联合中毒。

The rheological behavior and dynamic mechanical properties of syndiotactic 1,2-polybutadiene

The rheological behavior and the dynamic mechanical properties of syndiotactic 1,2-polybutadiene (sPB) were investigated by a rotational rheometer (MCR-300) and a dynamic mechanical analyzer (DMA-242C). Rheological behavior of sPB-830, a sPB with crystalline degree of 20.1% and syndiotactic content of 65.1%, showed that storage modulus (G ') and loss modulus (G '') decreased, and the zero shear viscosity (eta(0)) decreased slightly with increasing temperature when measuring temperatures were lower than 160 degrees C. However, G ' and G '' increased at the end region of relaxation curves with increasing temperature and)10 increased with increasing temperature as the measuring temperatures were higher than 160 degrees C. Furthermore, critical crosslinked reaction temperature was detected at about 160 degrees C for sPB-830. The crosslinked reaction was not detected when test temperature was lower than 150 degrees C for measuring the dynamic mechanical properties of sample. The relationship between processing temperature and crosslinked reaction was proposed for the sPB-830 sample.

Polypropylene as a carbon source for the synthesis of multi-walled carbon nanotubes via catalytic combustion

Multi-walled carbon nanotubes (MWCNTs) were efficiently synthesized by catalytic combustion of polypropylene (PP) using nickel compounds (such as Ni2O3, NiO, Ni(OH)(2) and NiCO3 (.) 2Ni(OH)(2)) as catalysts in the presence of organic-modified montmorillonite (OMMT) at 630-830 degrees C. Morphologies of the sample undergoing different combustion times were observed to investigate actual process producing MWCNTs by this method. The obtained MWCNTs were characterized by X-ray diffraction (XRD), transmission electron microscope and Raman spectroscopy. The yield of MWCNTs was affected by the composition of PP mixtures with OMMT and nickel compounds and the combustion temperature. The proton acidic sites from the degraded OMMT layers due to the Hoffman reaction of the modifiers at high temperature played an important role in the catalytic degradation of PP to supply carbon sources that are easy to be catalyzed by nickel catalyst for the growth of MWCNTs. The XRD measurements demonstrated that the nickel compounds were in situ reduced into the Ni(0) state with the aid of hydrogen gas and/or hydrocarbons in the degradation products of PP, and the Ni(O) was really the active site for the growth of MWCNTs. The combination of nickel compounds with OMMT was a key factor to efficiently synthesize MWCNTs via catalytic combustion of PP.

Heterojunction ambipolar organic transistors fabricated by a two-step vacuum-deposition process

Ambipolar organic field-effect transistors (OFETs) are produced, based on organic heterojunctions fabricated by a two-step vacuum-deposition process. Copper phthalocyanine (CuPc) deposited at a high temperature (250 degrees C) acts as the first (p-type component) layer, and hexadecafluorophthalocyaninatocopper (F16CuPc) deposited at room temperature (25 degrees C) acts as the second (n-type component) layer. A heterojunction with an interpenetrating network is obtained as the active layer for the OFETs. These heterojunction devices display significant ambipolar charge transport with symmetric electron and hole mobilities of the order of 10(-4) cm(2) V-1 s(-1) in air. Conductive channels are at the interface between the F16CuPc and CuPc domains in the interpenetrating networks. Electrons are transported in the F16CuPc regions, and holes in the CuPc regions. The molecular arrangement in the heterojunction is well ordered, resulting in a balance of the two carrier densities responsible for the ambipolar electrical characteristics. The thin-film morphology of the organic heterojunction with its interpenetrating network structure can be controlled well by the vacuum-deposition process.

Polydispersity of ethylene sequence length in metallocene ethylene/alpha-olefin copolymers. II. Influence on crystallization and melting behavior

In this work, crystallization and melting behavior of metallocene ethylene/alpha-olefin copolymers were investigated by differential scanning calorimetry (DSC) and atomic force microscopy (AFM). The results indicated that the crystallization and melting temperatures for all the samples were directly related to the long ethylene sequences instead of the average sequence length (ASL), whereas the crystallization enthalpy and crystallinity were directly related to ASL, that is, both parameters decreased with a decreasing ASL. Multiple melting peaks were analyzed by thermal analysis. Three phenomena contributed to the multiple melting behaviors after isothermal crystallization, that is, the melting of crystals formed during quenching, the melting-recrystallization process, and the coexistence of different crystal morphologies. Two types of crystal morphologies could coexist in samples having a high comonomer content after isothermal crystallization. They were the chain-folded lamellae formed by long ethylene sequences and the bundlelike crystals formed by short ethylene sequences. The coexistence phenomenon was further proved by the AFM morphological observation.

Isothermal and nonisothermal melt-crystallization kinetics of syndiotactic polystyrene

Analyses of the isothermal and nonisothermal melt kinetics for syndiotactic polystyrene have been performed with differential scanning calorimetry, and several kinetic analyses have been used to describe the crystallization process. The regime II-->III transition, at a crystallization temperature of 239degrees, is found. The values of the nucleation parameter K-g for regimes II and III are estimated. The lateral-surface free energy, sigma = 3.24 erg cm(-2), the fold-surface free energy, sigma(e) = 52.3 +/- 4.2 erg cm(-2), and the average work of chain folding, q = 4.49 +/- 0.38 kcal/mol, are determined with the (040) plane assumed to be the growth plane. The observed crystallization characteristics of syndiotactic polystyrene are compared with those of isotactic polystyrene. The activation energies of isothermal and nonisothermal melt crystallization are determined to be DeltaE = -830.7 kJ/mol and DeltaE = -315.9 kJ/mol, respectively.

Synthesis, structure characterization of the complexes of beta-alkoxycarbonylethyltin trichlorides with Schiff base ligands

Thirty - two title complexes (ROCOCHRCH2SnCl3)-C-1 . (2 - HOC6H4CH = NC6H4 - X) (R = Me, Et, n - Bu; R-1 = H, Me; X = H,4' - Cl, 3' - Pr, 3' - OH, 3', 4' - Cl-2, 4' - OMe) were synthesized and characterized by elemental analysis,UV - vis, IR, H-1 NMR. The crystal structure of n - BuOCOCH2CH2SnCl3 . (2 - HOC6H4CH - NC6H4OMe - 4') were determined by the X - ray diffraction analysis, The crystal belongs to monoclinic system, with a = 1.4661 (3)nm, b = 0.9307 (2)nm, c = 1.7888 (4)nm, beta = 94.04 (3)degrees, V = 2.4348nm(3), D-c = 1.581mg/m(3), Z = 4, F(000) = 1160, mu = 1.405mm(-1), R = 0.0354, R-w = 0,0486, space group: P2(1)/c. The complexes exist as a discrete monomer. The tin atom has a distorted octahedral geometry due to intramolecular coordination of the carbonyl oxygen and the phenolic oxygen of the Schiff base ligands, The coordination number of tin atom is 6.

β-烷氧羰乙基三氯化锡与Schiff碱配合物的合成、表征与结构

合成表征了32个标题化合物ROCOCHR~1CH_2SnCl_3·(2-HOC_6H_4CH=NC_6H_4-X)(R=Me,Et,n-Bu;R~1=H,Me;X=H,4’-Cl,3’-Br,3’-OH,3’,4’-Cl_2,4’-OMe),通过元素分析,UV-vis,IR和~1H NMR进行了表征n-BuOCOCH_2CH_2SnCl_3·(2-HOC_6H_4CH=NC_6H_4OMe-4’)的晶体结构分析表明,该晶体属单斜晶系,a=1.4661(3)nm,b=0.9307(2)nm,c=1.7888(4)nm,β=94.04(3)°;v=2.4348nm~3,Z=4;空间群P2_1/c.该化合物为含有分子内碳基氧配位,Schiff碱以酚羟基上的氧原子配位,中心锡原子为六配位,空间构型为畸变八面体构型的单分子有机锡化合物.

细胞色素P-450模拟体系的活性中间体——第三类型氧合铬(Ⅴ)——四苯基卟啉配合物的分离、表征和氧化反应

氧合过渡金属卟啉配合物是细胞色素P-450模拟体系的可能活性中间体。已分离和表征的钛(Ⅳ)、钒(Ⅳ)、钼(Ⅳ,Ⅴ)和铬(Ⅳ)等氧合过渡金属卟啉配合物,因其不是有效的氧化剂,所以不是细胞色素P-450模拟体系的可能活性中间体。氧合锰(Ⅳ)卟啉虽能氧化碳氢化合物,但至今还未能分离出。我们曾分离出并表征的氧合铬(Ⅳ)卟啉以及

1,5,9-环十二碳三烯的阳离子型跨环齐聚合反应

本文研究1,5,9-环十二碳三烯在阳离子型引发剂AlCl_3和BF_3·OEt_2催化下进行的跨环聚合反应,考察各种反应条件对跨环聚合反应的影响。产物为白色粉末,分子量均在1096—1431之间。对其溶解性、核磁共振和红外光谱的分析,确认了它的结构。

海洋生物膜的电活性及其在微生物燃料电池中的应用基础研究

海洋电活性微生物（又称电活性生物膜，electroactive biofilms, EABs）是自然界存在的一类功能性微生物，能够将代谢有机物产生的电子直接或间接传递给电极，人们对其在环境中的广泛性及其在生物防腐、生物能源和生物修复中的应用正在开展广泛的研究。 本论文着眼于海洋天然生物膜的电活性，从微生物腐蚀和微生物燃料电池的角度，考察研究了海洋天然生物膜对316L SS腐蚀行为的影响，发现海洋天然生物膜能抑制316L SS腐蚀，系统研究了海洋生物膜与石墨等电极的电子传递过程，提出了电活性生物膜（EABs）与电极间的电子传递机制，并初步研究了海洋电活性生物膜在微生物燃料电池(MFCs)中的应用。 对附着天然海洋生物膜的316L SS研究发现，生物膜使316L SS电位正移了500mV （vs. Ag/AgCl）。316L SS表面附着海洋生物膜后，其孔蚀电位由原来的50mV增加到540mV，孔蚀敏感性降低；同时，海洋生物膜的附着导致316L SS的阻抗增加，由此，我们明确提出海洋生物膜能够抑制316L SS腐蚀的发生。进一步研究了生物膜抑制腐蚀发生的可能机理。循环伏安实验表明，海洋生物膜与不锈钢电极之间存在电子传递过程。扫描电镜（SEM）及能谱（EDS）分析发现有钙盐的沉积生成。通过以上结果我们提出了生物膜对腐蚀的抑制机制假设，即在电极与电活性海洋生物膜间发生了电子传递，海洋生物膜能够将电子传递给不锈钢，316L SS作为电子接受体受到保护。 为进一步研究天然海洋生物膜的这种电活性，我们选择不会发生腐蚀的惰性电极材料石墨，玻碳，碳纸电极验证生物膜的电活性。 首次考察了天然海洋生物膜对石墨电极和玻碳电极的开路电位变化的影响，结果显示随电极在天然海水中浸泡时间，石墨电极正移50mV vs. Ag/AgCl，玻碳电极正移了300 mV （vs. Ag/AgCl）。与316L SS相似，三种电极的变正趋势相同，都经历了三个阶段，即初始缓慢变正期，随后的指数变正期和以后的稳定期，此与生物膜在固体表面形成的趋势相似。伏安曲线及阻抗实验结果表明，在石墨，玻碳和碳纸电极材料表面附着海洋生物膜后，电流密度增加，电荷转移电阻减小，说明生物膜与电极间存在电子传递，并能加速电子传递过程，不同材料表面生物膜的电活性能力由大到小为石墨＞316L SS＞碳纸＞玻碳。 进一步研究了海洋沉积物-海水生物膜微生物燃料电池，初步建立了相应的电极材料和微生物燃料电池结构。我们选择石墨阳极和石墨阴极或316L SS阴极组装海泥沉积物(阳极区)和海水（阴极区）MFC，316L SS代替石墨做阴极最大输出电量达9mW.m-2，约为后者的2倍。两种MFC输出电流和功率密度随时间的延长而增加的趋势相同，都可以分为三个阶段，即初期的缓慢增加阶段，中期的指数增长阶段，后期的平台稳定期阶段。这也与生物膜在固体表面形成的趋势相似。此研究也说明优化316L SS表面性质筛选活性海洋生物膜用于MFC有其潜在的应用价值。

柴达木盆地弃耕地水盐动态分析

对柴达木盆地盐碱化弃耕地水盐动态进行了监测，结果表明，该示范区地下水位年变幅为3.12～3.46 m，处于临界水位以上。示范区土壤水盐季节动态受当地自然气候条件的影响强烈，在5月和8月间皆出现有高峰期。

碎屑锆石年龄和Nd-Hf同位素组成对扬子基底演化的制约

The South China craton was formed by the collision of the Yangtze and Cathaysia blocks during the Neoproterozoic Jiangnan orogeny (also termed as the Jingnin or Sibao orogeny in Chinese literature). Basement rocks within the Yangtze block consist mainly of Proterozoic sediments of the Lengjiaxi and Banxi Groups. U-Pb ages of detrital zircons obtained by the LA-ICP-MS dating technique imply that the deposition of the Lengjiaxi Group continued until the Neoproterozoic. The youngest detrital zircons suggest a maximum deposition age of ~830 Ma for the Lengjiaxi Group, consistent with the initiation time of the deposition of the overlying Banxi Group, likely indicating continuous deposition of these two groups and a short temporal hiatus (~10 Ma) between the Neoproterozoic sedimentary rocks distributed in the South China craton. Detrital zircons from both the Lengjiaxi and Banxi Groups have a wide range of εHf(t) values from -12 to 14.2 and a continuous Nd and Hf model age spectrum from ~820 Ma to 2200 Ma. Some grains have model ages ranging up to ca. 2.9-3.5 Ga, indicating that both juvenile mantle material and ancient crust provided sedimentary detritus. This is also consistent with the Nd isotopic signature of sedimentary rocks recorded in the Lengjiaxi Group, suggesting a back-arc tectonic setting. The Banxi Group has slightly enriched Nd isotopic signatures relative to the Lengjiaxi Group, implying a higher percentage of old continental material in the sedimentary source. Combined with previously published data, new results can help us to reconstruct the Neoproterozoic tectonic evolution of the South China craton. The age spectrum of detrital zircons and Nd-Hf isotopic composition suggests a two-stage collision: Between 1000 Ma to 870 Ma, a continental magmatic arc was build up along the eastern margin of the Yangtze block. Convergence led to continent-based back-arc extension, subsidence and formation of a back-arc basin. Detritus originating from arc-related magmatic and old basement rocks was transported into this back-arc basin resulting in formation of the Lengjiaxi Group and its equivalents. At around 870 Ma, a second (oceanic) arc was formed by extension of an inter-arc basin, subduction subsequently led to the first collision and the emplacement of the blueschist mélange. Accretion of the magmatic arc lasted until the closure of an oceanic basin between the Yangtze and Cathaysia blocks at about 830 Ma. Shortly after the collision, subsequent uplift, further extension of the former back-arc basin and post-collisional granitoid magmatism caused a tilting of the Lengjiaxi sediments. Between 830 Ma and 820 Ma, subsequent closure of the oceanic back-arc basin and formation of the Jiangnan orogen took place, leaving a regional unconformity above the Lengjiaxi Group. Above this unconformity the Banxi Group was immediately deposited during the post-tectonic stage.