拜登上任后,美国—巴西关系向何处去

几经波折,2020年美国大选终于落下帷幕,民主党候选人拜登当选下一任美国总统。有"南美特朗普"之称的巴西总统博索纳罗纵有万般不情愿,也只能接受现实。大幅度向美国靠近是博索纳罗上任两年多来巴西外交政策的突出特点,博索纳罗与特朗普在意识形态上的高度一致为美巴关系迅速走近提供了难得契机。拜登上任后巴西和美国的意识形态联盟能否持续?美巴关系将如何调整?     

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。     

煤与瓦斯突出过程中温度变化的实验研究

介绍了通过实验方法测定在煤与瓦斯突出过程中的温度变化，测定结果证实了在煤与瓦斯突出过程中，瓦斯的膨胀做功过程并非绝热过程，而是一个接近于等温过程的多变过程。     

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.     

叠砖平衡的一种简单解法

 叠砖的平衡问题(见图1)是一个有趣的力学平衡问题,本文利用质点系质心的定义,介绍一种较为简单的解法。为保持本文的完整性,不妨重述叠砖的平衡问题:N块完全相同的砖块以图1所示方式叠放在一起并保持平衡,每个砖块的长度为l,质量为m,求砖块突出部分的最大长度Lmax。图1考察平衡时,前i-1块砖、第i块砖和第i+1块砖之间的关系。设第i块砖相对于第i+1块砖探出的长度为di。     

月球的形成

天文学家认为 ,月球是由一个像火星般大小的物体撞入地球 ,将物质溅射到围绕地球的轨道上形成的 .这一撞击还把地球上一天的时间延长到现今的 2 4小时 .月球中的物质一部分来自地球 ,其余部分来自撞击体 .科学家们对撞击体的物质在月球中所占的比例做了估计 ,结果分歧很大 .进行地球化学研究得到的估计值从小于 1%到大于 5 0 % ,而大多数地球物理模型则预言这一比例在 5 0 %到 90 %的范围 .在德国的天文学家通过将月球与地球岩石样品的成分进行比较 ,计算出月球上来自碰撞物体的物质不超过月球的三分之一 .此外 ,他们还估计 ,月球至少是在 4…