第十三届亚洲女排锦标赛中国女排发球效果分析

通过对第十三届亚洲女排锦标赛中国女排与韩国女排半决赛、与哈萨克斯坦女排决赛中发球站位、发球类型、发球落点、发球速度、发球效果进行统计分析和研究,发现中国女排发球环节上在亚洲处于明显的优势,中国女排发球的得分、破攻率高于哈、韩女排,发球一般率低于哈、韩女排,失误率高于哈、韩女排.提高发球速度、力量和控制发球路线落点的变化是当今世界女排发球技、战术的趋势.     

SHRIMP U-Pb zircon age of tuff from the Kunyang Group in central Yunnan： Evidence for Grenvillian orogeny in South China

Whether or not Grenvillian orogeny occurred in South China still remains highly controversial because high-quality,discriminating data are lacking,and therefore,the key to resolve this matter is to find datable volcanic and/or sedimentary rocks related to Grenvillian orogeny. Such rocks are apparently present in the Fuliangpeng Member from the lower-middle part of Kunyang Group in central Yunnan; here the unit is more than 100 m thick and consists of andesitic ignimbrite,tuffite,terrigeous clastic rocks and carbonates. These volcanic rocks,developed south of the Sibao fold-thrust belts,represent the earliest calc-alkaline volcanic activity in late Precambrian time from central Yunnan and are coeval with both a change in sedimentary facies from detritus to carbonates and the beginning of seismite development elsewhere. Two samples for SHRIMP analysis were collected from this volcanic unit. Sample G3-29-2,from the bottom of Fuliangpeng Member,is an ignimbrite,and about 100 zircon crys-tals recovered from it have euhedral shapes and display relatively simple sector zonation under cathodoluminescent (CL) imaging,suggesting a magmatogenic origin. Twenty-five of the zircons were analyzed and a weighed-mean U-Pb age of 1032±9 Ma was obtained. Sample G3-29-3 from uppermost part of Fuliangpeng Member is a tuffite,and many rounded,evidently detrital zircons were recovered. Nine of these zircons were analyzed,and the oldest single-grain U-Pb zircon age is 1938±26 Ma,im-plying that Paleoproterozoic basement developed in Cathaysia. The dating result,combined with the geotectonic research on the Fuliangpeng Member,leads us to conclude that late Mesoproterozoic orogenic volcanic activity occurred in the western part of South China,and that the related collision of Yangtze and Cathaysian cratons was an integral part of the assembly of Rodinia.     

甲烷卤代物热力学性质的拓朴指数计算

定义化学键特征值为iδj=|xi-xj|/(ni nj)0.85,分子化学键电负性连接指数nmY=∑(iδ.jδ…)。用0Y、(10Y)0.5和(33Y)0.25回归计算了70个甲烷卤代物的标准生成焓和生成自由能;单参数相关系数为0.997 6和0.998 2,三参数相关系数为0.999 0和0.998 6。     

滩间山群火山岩特征及其成岩构造背景

滩间山群火山岩分为下部火山碎屑岩组(O1-2h)和上部熔岩次火山岩组(O3y)。从岩石组合、岩石化学、地球化学等方面进行了研究,指出下部火山岩总体体现大陆裂谷环境特征,上部火山岩总体显现类岛弧环境特征,由下至上,由双峰式火山岩向类岛弧钙碱性火山岩演变,揭示其成岩构造背景是经历了大陆裂谷、逐渐稳定、俯冲到类岛弧火山岩形成的几个阶段。     

社会语言学视阈中的网络语词

文章以近年来出现的网络语词为例证,从语用功能、构词理据、语言与社会发展关系三方面分析论证了网络语词产生和传播的社会语言学意义及其对语言自身与社会发展所产生的影响。虽然网络语词具有明显的非规范特征,但其交际的有效性却充分证明了其存在的合理性,网络语词的广泛使用既是社会发展影响语言的必然,也是语言顺应社会发展的必然。     

团星系和场星系的恒星形成性质

通过对团星系和场星系的聚度参数、特征恒星形成率、星系中包含的恒星质量、金属丰度等物理参量的比较,研究了处在不同引力环境中星系的恒星形成性质.研究表明,聚度高的星系主要居于星系团中,大部分低质量星系是场星系,星系的特征恒星形成率与恒星质量和金属丰度之间存在着显著的相关.另外,团星系和场星系在红移小于0.1的范围内仍表现出了明显的宇宙学演化效应.     

区域高新技术产业发展的集群网络化模式

在对集群网络概念界定的基础上，通过对硅谷等几个具有代表性的高新技术产业集聚区成功经验的分析，认为成功的高新技术产业集聚区的成功并非区域内生产要素的简单叠加，而是区域内各种生产要素的有效组合及其形成的紧密集群网络．本文运用社会网络理论探讨了区域高新技术产业集群网络的层次结构及网络作用机制，基于集合论、拓扑学、分形几何构建了区域高新技术产业集群网络形成演化模型，并结合大连市高新技术产业发展实际，探讨了针对城市高新技术产业发展的集群网络化模式．     

Effects of nitrogen sources and glucose on the consumption of ethylene and methane by temperate volcanic forest surface soils

There is limited knowledge with regard to the consumption of ethylene (C2H4) and methane (CH4) in volcanic forest soils containing low microbial carbon-to-organic carbon ratio, and to the responses of both consumptions to nitrogen and carbon additions. Temperate volcanic forest surface soils under three forest stands (e.g. Pinus sylvestris L., Cryptomeria japonica and Quercus serrata) were used to compare CH4 and C2H4 consumption by forest soils, and to study the effects of nitrogen sources and glucose on both consumptions. There was a good parallel between CH4 and C2H4 consumption by for- est soils, but mineralization reduced CH4 consumption rather than C2H4 consumption in forest soils, particularly in a Pinus forest soil. The stimulatory effect of glucose addition on both CH4 and C2H4 consumption by forest soils was increased by increasing the pre-incubation period after glucose addi- tion, and a largest stimulation occurred in the Pinus forest soil. The addition of KNO3-N at the rate of 100 μg·g1 significantly reduced the consumptions of both C2H4 and CH4 by forest soils (P≤0.05). In the presence of urea plus dicyandiamide, the consumption rates of C2H4 and CH4 by forest soils were higher than those in the KNO3-N and urea-N treated soils at the same N rate (P≤0.05), but were similar to those of the control. Hence, under experimental conditions, there was a strong inhibitory effect of NO3 rather than NH4 addition on the CH4 and C2H4 consumption in these forest soils. When amount of the added NO3-N increased up to more than 2―3 times the soil initial NO3-N concentrations, both C2H4 and CH4 consumption rates were reduced to 10%―20% of the rates in soils without nitrate addition. By comparing the three forest stands, it was shown that there was a smallest effective concentration of the added nitrate that could inhibit C2H4 and CH4 consumption in the Pinus forest soil, which indicated that C2H4 and CH4 consumption of the soil was more sensitive to NO3-N addition.     

酸雨对环境的危害及防治对策

简述了酸雨特性及酸雨成因，描述了酸雨对自然生态环境和人类造成的种种危害，指出迄今我国酸雨发生和发展的严峻状况，针对性的提出了依靠政策措施、经济手段和先进环保技术防治酸雨的对策建议。     

Chronological record of the Early Mesozoic underplating in the northern margin of North China─U-Pb chronometry of zircons in the Late Mesozoic andesite from Western Liaoning

Cathodoluminescence spectroscopic analysis of zircons in the uppermost sanukites of the early Cretaceous Yixian Formation in Western Liaoning reveals zoning structures of the zircons in the volcanic rocks. LA-ICP-MS chronometry shows that the central part of the zircons is remnant zircon with a U-Pb dating of 254 Ma, which is consistent with the age of the Early Mesozoic underplating granulites, and that the periphery is zircon crystallizing out of the host magma with a U-Pb dating of 116 Ma, which is highly consistent with the Ar-Ar dating of the host volcanic rocks. Compositions of the clinopyroxenes xenocrystals in the sanukites are similar to those of the clinopyroxenes in the underplating granulites, indicating that the granulites accreted to the lower crust in the Early Mesozoic have been reformed and disrupted by the upwelling diapers of the asthenosphere and taken part in formation of the sanukites in the Late Mesozoic.