湖北省近500年区域干湿序列重建及其比较分析

在历史旱涝记载资料可靠性检验的基础上,重建了湖北省3个区域近500年来的干湿气候变化序列,并比较分析了各区域干湿气候变化的趋势特征、准周期性及跃变现象。结果表明:在3个区域中,鄂东区1570~1770、1890~1950年两个时段偏湿,1470~1520、1790~1830年则偏干;鄂北区偏湿时期主要在1470~1530、1710~1750、1850~1910年三个时段,1470~1530、1770~1830年则偏干;鄂西南区有1550~1610、1650~1710、1830~1890、1930~1990

Stable isotopic compositions in Australian precipitation

Stable deuterium (delta D) and oxygen-18 (delta O-18) isotopes in 1962 to 2002 precipitation from the seven Australian stations of the Global Network of Isotopes in Precipitation (GNIP) were used to investigate isotope characteristics including temporal and spatial distributions across different regions of Australia. On the basis of 1534 samples, the local meteoric water line (LMWL) was established as delta D = 7.10 delta O-18 + 8.21. delta O-18 showed a depletion trend from north and south to central Australia (a continental effect) and from west to east. Precipitation amount effects were generally greater than temperature effects, with quadratic or logarithmic correlations describing delta/T and delta/P better than linear relationships. Nonlinear stepwise regression was used to determine the significant meteorological control factors for each station, explaining about 50% or more of the delta O-18 variations. Geographical control factors for delta O-18 were given by the relationship delta O-18 (parts per thousand) = -0.005 longitude (degrees) - 0.034 latitude (degrees)-0.003 altitude (m) - 4.753. Four different types of d-excess patterns demonstrated particular precipitation formation conditions for four major seasonal rainfall zones. Finally, wavelet coherence (WTC) between delta O-18 and SOI confirmed that the influence of ENSO decreased from east and north to west Australia.

Design of Fluorescent Assays for Cyanide and Hydrogen Peroxide Based on the Inner Filter Effect of Metal Nanoparticles

We have demonstrated the design of a new type fluorescent assay based on the inner filter effect (IFE) of metal nanoparticles (NPs), which is conceptually different from the previously reported metal NPs-based fluorescent assays. With a high extinction coefficient and tunable plasmon absorption feature, metal NPs are expected to be capable of functioning as a powerful absorber to tune the emission of the fluorophore in the IFE-based fluorescent assays. In this work, we presented two proof-of-concept examples based on the IFE of Au NPs by choosing MDMO-PPV as a model fluorophore, whose fluorescence could be tuned by the absorbance of Au NPs with a much higher sensitivity than the corresponding absorbance approach.

二维分子形状和定量手性程度的研究

以二进制编码描述苯环型化合物分子在二维空间的形状,所得到的编码能够区分二维平面上一对苯环型化合物对映体。由于对映体的二进制编码不同,基于化合物和其镜像的编码计算得到了海明距离,并以其表征1对对映体的定量手性程度。以28对周长为22的手性苯环型化合物对映体为实例,计算苯环型化合物的定量手性程度,其结果仅仅有2个数值,分别为海明距离4和6。具有不同形状的该类化合物很多,为了提高分辨率,分别计算了窗口宽度从1～16时的海明距离,并分别以其来代表定量手性程度。结果显示全部16个窗口的海明距离的加和具有最大的区分能力,共得到17种海明距离。如果将每一窗口的细节引入到计算中,并采用类似的方法计算,则实例中所有的28个苯环型化合物实现了完全的区分,所得到的定量手性程度的区分能力是令人满意的。本研究证明如果用适当的编码来描述二维空间中分子的边界,能够解决分子形状的定量表征。尽管本文的二进制编码衍生于平...

THERMODYNAMICS OF POLY(ETHYLENE OXIDE)-POLY(VINYL ACETATE) BLENDS

Heat-of-mixing data, obtained on blends of poly(ethylene oxide) (PEO) with whole and fractionated poly(vinyl acetate) (PVAc), were used to feed Patterson's theory of polymer-polymer miscibility. Negative values of mixing enthalpy, contact-energy term, interaction'' parameter and excess volume were obtained only for blends with the lowest molecular weight PVAc fraction. These results show that miscibility of PVAc with PEO strongly depends on its molecular weight. The calculated unfavourable excess volume term of the Patterson equation is small in comparison with the absolute value of the interaction term. Therefore, miscibility of PEO and low-molecular-weight PVAc is dictated by the weak specific interactions between different repeat units and by the entropic gain in the mixing process.

海洋剖面测量系统形态模拟及仿真研究

海洋监测是人类认识海洋、研究海洋的有利工具，海洋自动观测仪器又是海洋监测技术最基本的硬件单元。文章介绍了一种具有自主知识产权的新型海洋仪器产品¬――波浪驱动式海洋要素垂直剖面测量系统，并对其工作时的动力特性展开系统的数值模拟与仿真。 该测量系统在水中的受力情况可分解为海面和水下两部分进行系统地分析。本文依照流体力学理论，利用频域和时域的分析方法，给出了非线性条件下海面波浪力对运动系统的影响。 水下工作时，系统在三维方向的流的作用下，呈现不同工作姿态，其姿态又对系统的稳定性影响较大。本文对水下受力情况进行里了详尽的数值分析，建立了数学模型，进而做了仿真开发研究，给出了便于应用的直观仿真模型。利用已获取的深、浅海现场实测海流数据，通过仿真，反演出了该海况下测量系统的虚拟就位状态；得出了较为理想工作运动曲线，并分析了可满足系统高效工作的海流与水深关系。 本文通过一系列理论与实践研究，配合计算机软件编程，以Matlab为仿真模型的开发工具，完成了海洋要素垂直剖面测量系统动力响应的数值模拟和仿真工作，为实现系统最终的下海运行做出了科学的预演。

海藻抗肿瘤抗细菌生物活性物质的研究

该文对近四年来海洋抗肿瘤药物的研究现状和大型海藻天然产物的研究现状进行了简要的综述.概述了近年来世界各国的海藻抗肿瘤筛选方面的工作进展;总结了近年来从蓝藻、甲藻、红藻、褐藻、绿藻中分离的活性化合物,其中包括已经进入临床研究阶段的Scytophycin、Halomon、Cryptophycin、Malyngamide、Tolytoxin等.综述了近四年来从大型海藻中分离的约100个天然化合物,其中大部分具有重要的生物活性.以采自山东沿海的39种海藻的96个样品为材料,进行了较系统的抗肿瘤生物活性的筛选,共发现了8种有选择性抗肿瘤活性的海藻.运用薄层层析方法对10种海藻提取物的抗金黄色葡萄球菌和大肠杆菌活性进行了研究,发现褐藻提取物的抗菌活性最高,红藻的抗菌活性较低,而绿藻门海藻几乎没有活性.红藻门的松节藻、鸭毛藻有一定的活性.褐藻门的酸藻和海黍子活性较高.酸藻和海黍子的3个强抗菌活性带对金黄色葡萄球菌的抑菌圈直径分别为33mm、17mm和17.5mm,酸藻水相的2个活性带还能抑制大肠杆菌,其抑菌圈直径分别为21mm和16mm.对山东沿海分布量较大的两种海藻进行了先导化合物的分离纯化和结构鉴定.对萱藻和松节藻中得到的纯化合物和其它粗提物进行了细胞毒活性的检验.

The behaviors and sources of dissolved arsenic and antimony in Bohai Bay

In this paper, we determined the concentrations of antimony species (antimonite (Sb(III)), antimonate (Sb(V)) and dissolved inorganic antimony (DISb)) and arsenic, in Bohai Bay seawaters, as well as the relationships of the analytes with environmental factors such as seawater characteristics (e.g., suspended particulate material (SPM), salinity and total organic carbon (TOC)), heavy metals, nutrients and phytoplankton species, and evaluated the sources of arsenic and antimony. Dissolved arsenic and antimony concentrations in the surface waters were ranging spatially from 1.03 to 1.26 ng/ml and 0.386 to 1.075 ng/ml, with mean values of 1.18 and 0.562 ng/ml, respectively. Sb(V) as the prominent chemical species constituted about 89%. Regarding arsenic concentrations in the surface waters, there was a tendency for a small variation. However, antimony species concentrations were much variable than arsenic. The highest arsenic and antimony concentrations were found near the Haihe Estuary. These distribution patterns were controlled mainly by environmental factors, biological activities and sources. In this region, DISb and Sb(V) negatively correlated with salinity. Besides, arsenic and antimony correlated well with the nutrients, chlorophyll a and phytoplankton, implying that arsenic and antimony had been involved in biological cycling. In addition, according to our estimate, about 333.5 x 10(8) mg/year of arsenic and 454.2 x 10(8) mg/year of antimony reached Bohai Bay via rivers. (C) 2010 Elsevier Ltd. All rights reserved.

一种鉴定正品藏茵陈川西獐牙菜的分子试剂盒及其鉴定方法

本发明涉及一种鉴定正品藏茵陈川西獐牙菜的分子试剂盒及其应用。该试剂盒反应液主要由DNA片段引物IDl：GGCTTGCCTCTCGACGCTC，ID2：GCAAGCGTCACGAAGACGCG，和DMSO试剂等组成。该试剂盒的应用包括以下步骤：1、对药材进行总DNA提取；2、利用引物对提取的DNA进行PCR扩增，若得到约500bp片段的扩增产物，则为川西獐牙菜；无此扩增片段，则是伪品种类。

电离层参量M(3000)F2和hmF2的经验正交函数方法建模研究

The ionospheric parameter M(3000)F2 (the so-called transmission factor or the propagation factor) is important not only in practical applications such as frequency planning for radio-communication but also in ionospheric modeling. This parameter is strongly anti-correlated with the ionospheric F2-layer peak height hmF2，a parameter often used as a key anchor point in some widely used empirical models of the ionospheric electron density profile (e.g., in IRI and NeQuick models). Since hmF2 is not easy to obtain from measurements and M(3000)F2 can be routinely scaled from ionograms recorded by ionosonde/digisonde stations distributed globally and its data has been accumulated for a long history, usually the value of hmF2 is calculated from M(3000)F2 using the empirical formula connecting them. In practice, CCIR M(3000)F2 model is widely used to obtain M(3000)F2 value. However, recently some authors found that the CCIR M(3000)F2 model has remarkable discrepancies with the measured M(3000)F2, especially in low-latitude and equatorial regions. For this reason, the International Reference Ionosphere (IRI) research community proposes to improve or update the currently used CCIR M(3000)F2 model. Any efforts toward the improvement and updating of the current M(3000)F2 model or newly development of a global hmF2 model are encouraged. In this dissertation, an effort is made to construct the empirical models of M(3000)F2 and hmF2 based on the empirical orthogonal function (EOF) analysis combined with regression analysis method. The main results are as follows: 1. A single station model is constructed using monthly median hourly values of M(3000)F2 data observed at Wuhan Ionospheric Observatory during the years of 1957–1991 and compared with the IRI model. The result shows that EOF method is possible to use only a few orders of EOF components to represent most of the variance of the original data set. It is a powerful method for ionospheric modeling. 2. Using the values of M(3000)F2 observed by ionosondes distributed globally, data at grids uniformly distributed globally were obtained by using the Kriging interpolation method. Then the gridded data were decomposed into EOF components using two different coordinates: (1) geographical longitude and latitude; (2) modified dip (Modip) and local time. Based on the EOF decompositions of the gridded data under these two coordinates systems, two types of the global M(3000)F2 model are constructed. Statistical analysis showed that the two types of the constructed M(3000)F2 model have better agreement with the observational M(3000)F2 than the M(3000)F2 model currently used by IRI. The constructed models can represent the global variations of M(3000)F2 better. 3. The hmF2 data used to construct the hmF2 model were converted from the observed M(3000)F2 based on the empirical formula connecting them. We also constructed two types of the global hmF2 model using the similar method of modeling M(3000)F2. Statistical analysis showed that the prediction of our models is more accurate than the model of IRI. This demonstrated that using EOF analysis method to construct global model of hmF2 directly is feasible. The results in this thesis indicate that the modeling technique based on EOF expansion combined with regression analysis is very promising when used to construct the global models of M(3000)F2 and hmF2. It is worthwhile to investigate further and has the potential to be used to the global modeling of other ionospheric parameters.

印度与欧亚板块强烈相互作用区深部结构特征研究

The central-south Tibet is a part of the products of the continental plate collision between Eurasia and India. To study the deep structure of the study area is significant for understanding the dynamics of the continental-continental collision. A 3-D density model matched well with the observations in the central-south Tibet was proposed in this study. In addition, this study has also used numerical simulation method to prove that Quasi-Love (QL) wave is deduced by anisotropy variation but not by lateral heterogeneity. Meanwhile, anisotropy variation in the upper mantle of the Qiangtang terrane and Lhasa terrane is detected by the QL waves observed in recorded seismograms. Based on the gravity modeling, some results are summarized as follows: 1) Under the constrain of geometrical structure detected by seismic data, a 3-D density model and Moho interface are proposed by gravity inversion of the central-south Tibet. 2) The fact that the lower crustal densities are smaller than 3.2 g/cm3, suggests absence of eclogite or partial eclogitization due to delamination under the central-south Tibet. 3) Seismicity will be strong or weak in the most negative Bouguer gravity anomaly. So there is no a certain relationship between seismicity and Bouguer gravity anomaly. 4) Crustal composition are determined after temperature-pressure calibration of seismic P wave velocity. The composition of lower crust might be one or a mixture of: 1. amphibolite and greenschist facies basalt beneath the Qiangtang terrane; 2. gabbro-norite-troctolite and mafic granulite beneath the Lhasa terrane. Because the composition of the middle crust cannot be well constrained by the above data set, the data set published by Rudnick & Fountain (1995) is used for comparison. It indicated the composition of the middle crust is granulite facies and might be pelitic gneisses.Granulite facies used to be interpreted as residues of partial melting, which coincidences with the previous study on partial melting middle crust. Amphibolite facies are thought to be produced after delamination, when underplating works in the rebound of the lower crust and lithospheric mantle. From the seismology study, I have made several followed conclusions: 1) Through the numerical simulation experiment of surface wave propagating in heterogeneity media, we can find that amplitude and polarization of surface wave only change a little when considering heterogeneity. Furthermore, it is proved that QL waves, generated by surface wave scattering, are caused by lateral variation of anisotropy but not by heterogeneity. 2) QL waves are utilized to determine the variation of uppermost mantle anisotropy of the Tibetan plateau. QL waves are identified from the seismograms of the selected paths recorded by the CAD station. The location of azimuth anisotropy gradient is estimated from the group velocities of Rayleigh wave, Love wave and QL wave. It suggests that south-north lateral variation of azimuthal anisotropy locates in Tanggula mountain, and east-west lateral variation in the north of Gandese mountain with 85°E longitude and near the Jinsha river fault with 85°E longitude.