2006年3月11日南京“泥雨”降尘特征及其粉尘来源

对２００６年春季南京地区一次“泥雨”形式的湿降尘特征进行了系统分析，并在此基础上对泥雨粉尘来源及泥雨降尘形成机制进行了探讨.

Microcalorimetric and IR spectroscopic studies of CO adsorption on molybdenum nitride catalysts

The adsorption of CO on both nitrided and reduced passivated Mo(2)N catalysts in either alumina supported or unsupported forms was studied by adsorption microcalorimetry and infrared (IR) spectroscopy. The CO is adsorbed on nitrided Mo(2)N catalysts on three different surface sites: 4-fold vacancies, Mo(delta+) ( 0 < delta < 2) and N sites, with differential heats of CO adsorption decreasing in the same order. The presence of the alumina-support affects the energetic distribution of the adsorption sites on the nitrided Mo(2)N, i.e. weakens the CO adsorption strength on the different sites and changes the fraction of sites adsorbing CO in a specific form, revealing that the alumina supported Mo(2)N phase shows lower electron density than pure Mo(2)N. On reduced passivated Mo(2)N catalysts the CO was found to adsorb mainly on Mo(4+) sites, although some slightly different surface Mo(delta+) d (0 < delta < 2) sites are also detected. The nature, density and distribution of surface sites of reduced passivated Mo(2)N/gAl(2)O(3) were similar to those on reduced MoO(3)/gamma-Al(2)O(3).

对改善环境的经济动力的探讨

对改善环境的经济动力的探讨李法云，范志平中科院沈阳应用生态研究所由于人口的增加、工业生产的发展，资源消耗在加快，我们正面临着环境污染蔓延和生态环境恶化这一环境问题的挑战。我国目前的环境状况不容乐观，森林面积仍在减少，水土流失面积也在增大，河流污染现状...

汾河景区垂柳主要虫害的生态防治对策

在研究汾河景区垂柳柳厚壁叶蜂生物学特征的基础上,通过对柳厚壁叶蜂种群数量的调查,分析了该虫在羽化产卵阶段与垂柳生长期的耦合过程、新老树种虫害程度的差异及其与环境的关系.结果表明:柳厚壁叶蜂对垂柳最大危害的枝条是从第1叶片到第6叶片的生长期;柳厚壁叶蜂种群在草地覆盖条件下密度较大.最后对汾河景区防治柳厚壁叶蜂的危害,提出了生态防治对策.

中国东北植被生态学研究中的焦点问题

中国东北植被经过半个多世纪的系统研究 ,但有关植被生态学一些争论性问题尚未统一 .本文仅就作者近年来研究工作涉及到的内容和关注的问题 ,提出一些看法 :1)中国东北植被地带性分布规律可用Kira的温暖指数 (WI)、寒冷指数 (CI)和作者的湿度指数 (HI)进行定量解释 .2 )大兴安岭北部山地 ,在海拔14 0 0m以上存在冻原植被 ,是作者于 196 3年首次发现的我国第三块冻原植被 ,其WI <15℃·月 .3)大小兴安岭植被分界线是我国植被区划中第一级分区界线 ,其位置在爱辉 -果松沟 -嫩江以南附近 ,WI为 4 5℃·月 .4 )大兴安岭植被地带性分异显著 ,南段、中段为典型草原地带和森林草原地带 ,北段为针叶林地带 ,HI值分别为 3 5～ 5 5、5 5～ 7 5、>7 5mm/℃·月 .大兴安岭东麓阔叶林是森林草原带上的森林植被类型 .5 )东北东部山地岳桦林是山地植被垂直带谱重要组成部分之一 ,是山地森林垂直分布林线 ,WI为 2 0～ 15℃·月为地带性植被类型 ,而WI>2 0℃·月为非地带性植被类型 .6 )内蒙古浑善达克沙地云杉林是陆地上非常罕见的森林生态系统类型 ,但这种云杉林究竟是哪一树种组成 ,在中国植物分类上一直是个争论性问题 ,作者通过核型分析和同工酶实验进一步证明是一个新种即沙地云杉Piceamongolica(H .Q .Wu)W .D .

Preparation and characterization of a novel solid solution of aluminum in tungsten carbide by mechanically activated high-temperature reaction

In this work, a novel substitutional solid solution (W0.8Al0.2)C was synthesized by mechanically activated high-temperature reaction. X-ray diffraction was used for phase identification during the whole reaction process. Environment scanning electronic microscopy-field emission gun and energy dispersive x-ray were used to investigate the microstructure and the quantitative material composition of the specimen. (W(0.8)A(10.2))C was found to crystallize in the WC-type, and the cell parameters were a = 2.907(1) angstrom and c = 2.837(1) angstrom. The hardness of (W0.8Al0.2)C was tested to be 19.3 +/- 1 GPa, and the density was 13.19 +/- 0.05 g cm(-3).

Identification of a silicatein(-related) protease in the giant spicules of the deep-sea hexactinellid Monorhaphis chuni

Silicateins, members of the cathepsin L family, are enzymes that have been shown to be involved in the biosynthesis/condensation of biosilica in spicules from Demospongiae (phylum Porifera), e. g. Tethya aurantium and Suberites domuncula. The class Hexactinellida also forms spicules from this inorganic material. This class of sponges includes species that form the largest biogenic silica structures on earth. The giant basal spicules from the hexactinellids Monorhaphis chuni and Monorhaphis intermedia can reach lengths of up to 3 m and diameters of 10 mm. The giant spicules as well as the tauactines consist of a biosilica shell that surrounds the axial canal, which harbours the axial filament, in regular concentric, lamellar layers, suggesting an appositional growth of the spicules. The lamellae contain 27 kDa proteins, which undergo post-translational modification (phosphorylation), while total spicule extracts contain additional 70 kDa proteins. The 27 kDa proteins cross-reacted with anti-silicatein antibodies. The extracts of spicules from the hexactinellid Monorhaphis displayed proteolytic activity like the silicateins from the demosponge S. domuncula. Since the proteolytic activity in spicule extracts from both classes of sponge could be sensitively inhibited by E-64 (a specific cysteine proteinase inhibitor), we used a labelled E-64 sample as a probe to identify the protein that bound to this inhibitor on a blot. The experiments revealed that the labelled E-64 selectively recognized the 27 kDa protein. Our data strongly suggest that silicatein(-related) molecules are also present in Hexactinellida. These new results are considered to also be of impact for applied biotechnological studies.

一种基于工艺特征的制造单元划分方法

在现代生产中,单元化生产是提高制造系统生产效率的一个重要手段。对于一个给定的制造系统,其中制造单元的划分并不是唯一的,人们提出了各种制造单元划分方法。这些方法的不足是只采用0和1两值来表示系统中的相似关系。本文提出了相似系数和隶属度的概念,进一步发展了一种完善的制造单元划分方法,最后以一个数值例子进行了验证。

藏东及滇东南新生代钾质岩浆作用及其深部制约

The dissertation focuses on the petrology, geochemistry of the volcanic rocks in east Tibet and southeast Yunnan. It lucubrates the Magmatic process, forming mechanism and the possible tectonic settings of the volcanic rocks. The volcanic rocks of Nangqen basin in east Tibet, Qinghai province are mainly Cenozoic intermediate-acid shoshonites. The rocks are LREE enriched and the LREE/HREE = 3～34; (La/Yb)_N = 18.17-53.59, and ΣREE 222～1260μg/g. There are no Eu anomaly, and Nb, Ta, Zr, Hf, Ti are markedly depleted. The isotopic composition is ~(87)Sr/~(86)Sr = 0.70497～0.70614, ~(206)Pb/~(204)Pb = 18.622～18.974, ~(208)Pb/~(204)Pb = 38.431～38.996, ~(207)Pb/~(204)Pb = 15.511～15.613, respectively. K-Ar age of the whole rocks and the single mineral are between 32.0-36.5Ma. Based on the trace elements and isotopic elements, we get the conclusion that the partial melting is one of the dominated forming mechanisms for the volcanic rocks in Naneqen basin. The magma did not experience the crustal contamination en route to the surface; however, the complex mixture took place in the upper mantle before the melt was formed. There are at least two kinds of mixed sources that can be identified. The basalt in southeast Yunnan province is studied. They are distributed in Maguan, Tongguan, and Pingbian County, which is located on the both sides of the Red River belt, and the ultrabasic xenolith are cursory introduced. The volcanic rocks belongs to the alkali series, which can be subdivided into trachybasalt and basanite(Ol normal molecule >5). The volcanic rocks are characteristics by high Ti and low Mg#. According to the magma calculation model, the original rocks of the basalt in southeast Yunnan province are Spinel Lherzolite in Tongguan, Garnet Lherzolite in Pingbian and Maguan, while Togguan undergoes 2-5 percent and percent of partial melting, whereas volcanism in Maguan and Pingbian was so complex to calculate. The fractional crystallization took place during the magma evoltion in southeast Yunnan. The basalt is enriched in LREE with LREE/HREE=9.23-20.19. All of the trace elements display weak Nb, Ta peak, and the depletion of Zr, Hf and Ti in Maguan and pingbian represent the presence of Garnet in the source. The composition of the isotope ratio are ~(87)Sr/~(86)Sr = 0.70333-0.70427, ~(143)Nd/~(144)Nd = 0.512769-0.512940, ~(206)Pb/~(204)Pb = 18.104-18.424, ~(207)Pb/~(204)Pb = 15.483 -15.527; ~(208)Pb/~(204)Pb = 37.938-38.560, respectively, which shows the characteristics of the HIMU type OIB. The volcanic rocks of the southwest Yunnan are derived from the enriched, OIB type mantle sources by synthesizing all the data from trace and isotope elements. It is similar to that of the volcanic rocks in Hawaii, a typical kind of the mixtures of the recycled oceanic crust plume and depleted asthenosphere. To sum up, the volcanic rocks in southeast Yunnan are formed by the intraplate hotpot volcanism.

中东亚地区土地退化早期阶段关键营养元素C、N的差异流失作用

土地退化是导致土地生产力下降的过程之一,也是造成土地资源日益减少的主要原因.在气候变化的大背景下,人类对土地资源的过度利用正使得土地退化成为世界性难题.