含粗骨料超高性能混凝土高温性能的研究进展

与高性能混凝土类似,含粗骨料超高性能混凝土(Ultra High Performance Concrete with Coarse Aggregate,UHPC-CA)经历高温后残余力学性能会发生变化,甚至出现高温爆裂行为.为了推进UHPC-CA的实际应用进程,结合现有文献分析了含湿量、纤维、加热速率、骨料、加载应力和混凝土强度等因素对U HPC-CA高温爆裂的影响;分析了高温后U HPC-CA的残余抗压强度、残余劈拉强度和残余断裂能等残余力学性能的变化;分析了U HPC-CA高温性能的改善措施.结果表明:随着含湿量、加热速率、加载应力和混凝土强度的增加,U HPC-CA的高温爆裂程度均呈现加重趋势,加入粗骨料与纤维后可减轻U HPC-CA的高温爆裂;随目标温度的升高,U H PC-C A的残余抗压强度与残余劈拉强度均呈现先增大后减小的趋势,残余断裂能逐渐下降;热水—干热组合养护可避免U HPC-CA的高温爆裂,显著改善其高温性能.     

基于专利的难溶性含钾岩石生产钾肥技术分析

难溶性含钾岩石的开发和利用对提高我国钾肥产能，保障粮食生产安全有重要意义。该文围绕难溶性含钾岩石生产钾肥技术，通过专利数据库和专利分析系统，统计了本行业相关的专利数据，并对其进行了各种指标的分析，从而揭示了该技术领域中一些非常有价值的情报信息，为科研立项、课题选择、产品攻关、建立知识产权预警制度等提供一定参考。     

凯瑟硬蜱—中国蜱种新记录

目的基于形态学与分子生物学鉴定方法对我国新发现的疑似硬蜱进行鉴定。方法从新疆亚洲獾和长尾黄鼠体表共采集到硬蜱57只,对其中的8只代表蜱首先进行体视显微镜观察,描绘蜱的形态学特点,随后进行线粒体16S rDNA和cox1基因片段扩增和测序。结果结果显示,采集的硬蜱经形态学观察符合凯瑟硬蜱的形态特点,16S rDNA遗传进化树分析表明8只代表蜱其序列与欧洲凯瑟硬蜱聚为一簇,与六角硬蜱为近源种; cox1基因遗传进化树分析表明我国分布的凯瑟硬蜱较为古老,并且发现来源于亚洲獾和长尾黄鼠凯瑟硬蜱在16S rDNA和cox1基因上不存在宿主差异性。结论新疆凯瑟硬蜱的发现扩大了我国已有蜱种的种类。关注野生动物体表寄生蜱的种类有望进一步在我国发现新的蜱种。     

含PM-映射的变分不等式

文章在自反Banach空间中，利用锐角原理讨论了含PM-映射的变分不等式解的存在性问题。     

硬线控制冷却工艺

研究了影响硬线性能的主要工艺参数，这些参数是决定线材最终产品质量的关键，并初步讨论了其影响规律。     

Comparison of Drought-Resistance about Three Wild Rocky-Grasses

In this experiment, using the methods of drought-stress in the pot and PEG simulative drought-stress, three native rocky-slope grasses Pogonatherum panideum（Lam.） Hack, Erioophorum comosum nees and Cynodon dactylon cultivated in the pots were selected as materials to study their drought-resistance by analyzing the indexes such as the leaf area index, the drying roots accumulation, the holding water ability of leaf, the relative conductance of leaf, the soluble protein, chlorophyll. At the same time, by comparing with membership function value of each index, the order of each grass drought-resistance was decided. The results showed that the drought-resistance of Erioophorum comosum nees was stronger than Cynodon dactylon and drought-resistance of Cynodon dactylon was stronger than Pogonatherum panideum （Lam.） Hack. The purpose of the experimental results was to find theoretical foundations for selecting and cultivating native protecting-slope vegetations to adapt to rocky slopes.     

Developmental modes of the Neoproterozoic-Lower Paleozoic marine hydrocarbon source rocks in China

Based on the researches on rock type, the mode of occurrence, diagnostic minerals and creatures, the sedimentary geochemistry and organic facies of Chinese marine source rocks from wells and outcrops, and on the research findings of developmental modes of foreign marine source rock, the authors consider that it is impossible to objectively make clear the formation mechanism of hydrocarbon source rock with high organic matter abundance by either single mode of preservation or high organic matter productivity. According to the Chinese geological features, the formation mechanism of the Neoproterozoic-Lower Paleozoic marine source rock is generalized into four modes, namely, thermal water activity-upwelling flow-anoxic; carbonate gentle slope-upwelling flow; xerothermic climate-brine euxinic milieu; and humid climate-retained euxinic milieu; as the Lower Cambrian undercompensation basin organic facies （the Tarim Basin, South China and southwestern margin of North China）, carbonate gentle lime mud bound organic facies （the Upper Ordovician in Tazhong region of the Tarim Basin and the Lower Silurian in the Upper Yangtze Platform）, the Middle Cambrian evaporation laggon organic facies （the Tarim Basin and the Upper Yangtze Platform）, enclosed undercompensation terrigenous bay organic facies （the Middle-Upper Ordovician in the west of the Tarim Basin, the Lower Silurian Long- maxi Formation in the Upper Yangtze platform）. Chinese marine sedimentations with lower organic matter abundance are generalized into two modes of consumption-dilution mode of open epicontinental sea and depletion-dilution mode of supercompensation basin.     

The controlling factors and distribution prediction of H2S formation in marine carbonate gas reservoir, China

Generally, there are some anhydrites in carbonate reservoir, as H2S is also familiar in carbonate oil and gas reservoirs. Nowadays, natural gas with high H2S concentration is usually considered as TSR origin, so there is close relationship between H2S and anhydrite. On the contrary, some carbonate rocks with anhydrite do not contain H2S. Recently, researches show that H2S is only a necessary condition of H2S formation. The reservoir porosity, sulfate ion content within formation water, reservoir temperature, oil/gas and water interface, hydrocarbon and some elements of reservoir rock have great controlling effects on the TSR occurrence. TSR deoxidizes hydrocarbon into the acidic gas such as H2S and CO2, and the H2S formation is controlled by TSR occurrence, so the relationship among reaction room, the contact chance of sulfate ion and hydrocarbon, the reservoir temperature has great influence on the TSR reaction. H2S has relatively active chemical quality, so it is still controlled by the content of heavy metal ion. Good conditions of TSR reaction and H2S preservation are the prerequisite of H2S distribu- tion prediction. This paper builds a predictive model based on the characteristic of natural gas reservoir with high H2S-bearing. In the porosity reservoir with anhydrite, the formation water is rich in sulfate and poor in heavy metal ion. Oil and gas fill and accumulate in the gas reservoir with good preservation conditions, and they suffered high temperature later, which indicates the profitable area of natural gas with high H2S-bearing.     

含参数λ微分方程类型的可积判据

提出几类含参数λ微分方程,借助变量替换法、线性化法、降阶法、交换变量位置法,论证其可积性,给出可积的判据及通解的表达式.扩大微分方程的可积范围,提供其求解的方法及通解公式.