黄河三角洲湿地生态系统的形成及其保护

通过对黄河三角洲新生湿地的野外调查,利用TM陆地卫星影像图的判读,结合黄河尾闾变动的历史资料分析,结果表明,黄河三角洲新生湿地是多泥沙的黄河淤积和海岸蚀退所形成.受区域气候、地貌、地质沉积、土壤、植被的相互作用和互相影响,形成4.5×105hm2的湿地,其中有6.84×104hm2的人工湿地.湿地生态类型随着黄河尾闾摆动和海退陆进程度而变化,自海洋向陆地依次为潮下带水生生态系统潮间带湿地生态系统潮上带盐生生态系统芦苇獐茅湿地生态系统草甸湿地生态系统陆上农田生态系统.该系统资源丰富,共有野生动物1524种,鸟类300种,鱼类1040种.石油开发和近年来黄河断流对湿地产生一定影响,应在开发利用中加强管理和保护

沈阳市苏家屯区耕层土壤养分空间变异性研究

利用地统计学和地理信息系统相结合的方法,研究了沈阳市苏家屯区耕地土壤(0～20 cm)有机质、速效氮、速效磷、速效钾含量的空间变异性特征.结果表明,各变量符合正态分布或经对数转换后符合正态分布,最佳的变异函数理论模型均为球状模型.有机质具有较强的空间相关性(C0与C0+C比值为24.11％),速效氮、速效磷、速效钾具有中度的空间相关性(C0与C0+C比值分别为29.53％、60.77％、58.82％).各变量的空间自相关距离分别为26.051、28.293、15.132和23.813 km.有机质和速效氮的空间变异主要受结构性因子(如成土因子)的影响,速效磷和速效钾主要受随机性因子(如施肥)的影响.Kriging插值绘制出的养分含量空问分布图显示了养分的空间分布格局,它将有助于进一步监测养分动态,为农业和环境管理提供数字地图支持.

基于随机背包的公钥密码

该文构造了一个背包型公钥密码算法。该背包公钥密码具有如下优点:加解密只需要加法和模减法运算,因此加解密速度快;该算法是基于随机背包问题而不是易解背包问题而构造的;证明了在攻击者不掌握私钥信息情况下该密码算法能抵抗直接求解背包问题的攻击,包括低密度攻击和联立丢番图逼近攻击等;证明了攻击者能够恢复私钥信息与攻击者能够分解一个大整数是等价的。分析表明,该算法是一个安全高效的公钥加密算法。

Sensing H2O2 with layer-by-layer assembled Fe3O4-PDDA nanocomposite film

It was found that Fe3O4 nanoparticles (Fe3O4 NPs) possess intrinsic enzyme mimetic activity similar to that found in natural peroxidase. Here, we applied Fe3O4 NPs to the construction of efficient electrochemical sensor to detect the concentration of hydrogen peroxide. The sensor was fabricated with layer-by-layer assembly of Fe3O4 NPs and poly(diallyldimethylammonium chloride) (PDDA) through the electrostatic interaction, and the multilayer film was characterized with UV-vis absorption spectra, atomic force microscopy, and cyclic voltammetry.

Synthesis and Characterization of Coil-Rod-Coil Triblock Copolymers Comprising Fluorene-Based Mesogenic Monodisperse Conjugated Rod and Poly(ethylene oxide) Coil

A series of coil-rod-coil triblock copolymers (i.e., F3T8EO8, F3T8EO17, F3T8EO45, and F3T8EO125) with a mesogenic monodisperse conjugated oligomer comprising 3 fluorene, 8 thiophene, and 2 phenyl units as the rod and poly(ethylene oxide) (PEO) as the coil were synthesized. A reference compound, that is F3T8ME2, with the identical rod but without PEO was also prepared for comparison. The volume fraction of PEO (f(PEO)) was 0, 0.16, 0.28, 0.50, and 0.73 for F3T8ME2, F3T8EO8, F3T8EO17, F3T8EO45, and F3T8EO125, respectively. It was found that the introduction of PEO into the triblock copolymers encouraged the formation of H-type aggregation and f(PEO)-dependent highly ordered mesophases while f(PEO) < 0.73. For F3T8ME2, only nematic mesophase was observed. In contrast, F3T8EO8 and F3T8EO17, with f(PEO) of 0.16 and 0.28, respectively, are smectic A (SA) mesomorphism.

Structural and Bluish-White Luminescent Properties of Li+-Doped BPO4 as a Potential Environmentally Friendly Phosphor Material

Many efforts have been devoted to exploring novel luminescent materials that not contain expensive or toxic elements, or do not need a mercury vapor plasma source. In this paper, BPO4 and Li+-doped BPO4 powder samples were prepared by the Pechini-type sol-gel (PSG) process. The structure and optical properties of the resulting samples were characterized by X-ray diffraction (XRD), Fourier transform infrared (FT-IR) spectroscopy, field emission scanning electron microscopy (FESEM), photoluminescence (PL) excitation and emission spectra, kinetic decay, and X-ray photoelectron spectra (XPS), respectively. It was found that PSG -derived Li+-doped BPO4 annealed at 960 degrees C exhibited bright bluish-white emission centered at 416 nm. The luminescence decay curves analysis indicates that each sample has two kinds of lifetimes (5.9 ns and 0.529 ms) and two types of kinetic decay behaviors which can be fitted into a single-exponential function and a double-exponential function, respectively.

Luminescence properties of rare earth ions in cadmium metasilicate

The luminescence properties of CdSio(3):RE3+ phosphors doped with various rare earth ions are reported. The series of rare earth ions doped CdSiO3 phosphors are prepared by the conventional high-temperature solid-state method, and characterized by XRD and photoluminescence (PL) spectra. The results of XRD measurement indicate that the products fired under 1050 degreesC for 3 h have a good crystallization without any detectable amount of impure phase. The PL spectra measurement results show that CdSiO3 is a novel self-activated luminescent matrix. When rare earth ions such as Y3+, La3+, Gds(3+), Lus(3+), Ce3+, Nd3+, Ho3+, Era(3+), Tm3+ and Yb3+ are introduced into the CdSi03 host, one broadband centered at about 420 nm resulted from traps can be observed. In the case of other earth ions which show emissions at the visible spectrum region, such as Pr3+, Sm3+, Eu3+, Tb3+ and Dy3+, the mixture of their characteristic line emissions with the similar to 420 nm strong broadband luminescence results in various emitting colors. As a consequence, different emitting colors can be attairied via introducing certain appropriate active ions into the CdSiO3 matrix. In additional, this kind of phosphors shows good long-lasting properties when excited by UV light. All the results show that CdSiO3 is a potential luminance matrix.

An eta(6)-toluene complex of neodymium: [Nd(eta(6)-C6H5CH3)(AlCl4)(3)]

The Nd-III ion in hexa-mu-chloro-1:2 kappa(2)Cl;1:3 kappa(2)Cl;1:4 kappa(2)Cl-hexachloro-2 kappa(2)Cl,3 kappa(2)Cl,4 kappa(2)Cl- [1 (eta(6))- toluene] trialuminiumneodymium has distorted pentagonal bipyramidal coordination geometry. Five Cl atoms form the equatorial plane, and the toluene ring and the sixth Cl atom occupy the apical sites. The average Nd-C(eta(6)) and Nd-Cl distances are 2.926 (5) and 2.857 (1) Angstrom, respectively.

Isolation and characterization of microsatellites in yellow perch (Perca flavescens)

A total of 45 microsatellite loci from yellow perch, Perca flavescens, were isolated and characterized. Among the 45 microsatellite loci, 32 had more than two alleles. A wild population of P. flavescens (n = 48) was used to examine the allele range of the microsatellite loci. Mendelian inheritance of alleles was confirmed by examining the amplified products in pair-mated families. The number of alleles for the 32 polymorphic loci varied from two to 16, and observed heterozygosity ranged between 0.024 (YP79) and 0.979 (YP60). Cross-species polymorphic amplification in four other Percidae species was successful for 22 loci.

The preparation and stability of the inclusion complex of astaxanthin with beta-cyclodextrin

Inclusion complex of astaxanthin with beta-cyclodextrin was prepared. The water solubility of the inclusion complex was < 0.5 mg/ml, which is better than that of astaxanthin. Large aggregates were observed in the aqueous solution of the inclusion complex. Furthermore, the stability of the inclusion complex against temperature and light was greatly enhanced compared to that of astaxanthin. (c) 2006 Elsevier Ltd. All rights reserved.

胶州湾生态系统数学模型与计算机模拟及优化管理对策

六十年代产生的系统生态学，在生态系统研究中使得数学模型至今都是一个必不可少的有效工具，建立数学模型已成为生态学中研究的热点。文章运用概率统计、时序分析手段及灰色系统理论，对胶州湾生态系统调查的历史资料进行初步分析，取得如下成果。1. 建立了非生物环境因子的八个静态统计模型，并分析了它们之间的相关关系，从定性、定量的角度对胶州湾非生物环境因子相互关系进行了研究，并结合实际情况对数学模型进行了解释。2. 根据历史资料及前人研究成果，把胶州湾生态系统划分为：浮游动物、浮游动物食性鱼类、植食性鱼类、底栖生物、底栖生物食性鱼类、肉食性鱼类六个子系统，并把有机质及浮游植物（初级生产力）作为系统的输入，运用灰关联度方法对子系统与生物及非生物环境因子的关系进行定量分析，排列出影响各子系统生物量变化的非生物环境因素的主次顺序，建立了相应的GM（1，N）模型，并对模型进行了残差检验，模型能较好的反映实际情况。预测了各子系统的发展特性，并结合实际情况提出了各类渔业资源管理的具体指标值，对优化子系统提供了具体参数。3. 根据胶州湾的实际情况，提出了新的数学模型 - 差分摆动模型及其建立方法。模型的意义在于可量化任意几个有关因子的数量关系，并对未能考虑到的因子，甚至一直未能被人们认识到的所有因子对这种生物作用的信息量进行量化，把生态系统中生物与非生物环境因子相互作用通过方程联系起来，并在论文中得到了验证。4. 根据灰色系统分析方法，对胶州湾生态系统进行了动态分析，建立了生态系统的量化动态模型，利用劳斯判断准则及根平面法，分析了系统的发展稳定状态，发现胶州湾生态系统周年内处于不稳定的发展状态。总之，论文运用各种数学手段从系统的角度来分析生态系统中各环境因子之间关系，并用数学模型把这种关系定量地表示出来，利用胶州湾生态系统现有资料，对胶州湾生态系统从系统的角度进行综合分析，为科学管理与合理开发胶州湾生物资源、优化胶州湾生态系统提供了意义的参考意见。

白垩纪超静磁带地球磁场古强度测定

The long-term variations in the strength of the geomagnetic field provide important constraints on the chemical-physical processes of the Earth’s interior. Especially, the intensity of the geomagnetic field during the Cretaceous normal superchron (CNS) is crucial to understand the geodynamo. But a paucity of paleointensity further limits to obtain essential knowledge interior process in the deep earth. In order to improve the experimental efficiency, this study tried to apply two new rock magnetic methods (FORC diagram and low-temperature demagnetization technique) to determine the paleointensity. First, some problems in the theory and technique in paleointensity experiments were introduced. A combined palaeomagnetic and geochronologic study was further conducted on a basaltic lava sequence at Jianchang in Liaoning Province, northeastern China. Radiometric 40Ar/39Ar dating indicates that the volcanism occurred at about 119 Ma within the marine anomaly C34n in Cretaceous normal superchron (CNS). Rock magnetic investigations show that pseudo-single domain (PSD) titanium-poor titanomagnetite is dominant in the studied lava flows. Both stepwise thermal and alternating field demagnetizations isolate the well-defined normal characteristic remanent magnetization (ChRM) in three independent lava flows with a mean direction of D/I = 6.0/51.9 degree(a95 = 12.3degree). Palaeointensity was determined using the modified Thellier method with systematic partial thermoremanent magnetization (pTRM) checks on total 72 samples, but only 10 samples exhibit ideal linear behavior on the Arai-plot in the temperature interval of 300-560 C and yield an average paleointensity of (25.8+/-1.4)uT. In addition, slopes of the line defined by the initial and the final points on the Arai-plot for the other 18 samples with characteristic PSD features give an average paleointensity estimation value of (24.8+/-1.9)uT. The consistency of these two approaches confidently demonstrates the fidelity of our results. The overall mean field strength determined using both approaches are thus estimated to be (25.2+/-0.7 )uT. This value corresponds to the virtual dipole magnetic moments (VDM) of (4.5+/-0.1)E22 Am^2, which is about half of the value of present field. This finding suggests that palaeointensity just at the onset of the CNS is characterized by a weak magnetic field.