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。     

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.     

中微子物理若干前沿问题

 在过去的几年间,大量的实验结果已经表明中微子有非零质量以及轻子味混合。这一进展为我们打开了一个全新的值得探索的基本粒子世界。关于中微子我们已经知道了多少,我们想要发现什么?本文将从理论与唯象的观点进行阐述。目前中微子物理的前沿问题主要包括:中微子真的发生味转化吗?有几代中微子?存在惰性中微子吗?中微子的质量是多少?中微子是马约拉纳粒子还是狄拉克粒子?轻子味混合矩阵的混合角有多大?轻子味混合矩阵包含CP破坏位相吗?如果包含,那么在中微子振荡和无中微子双β衰变中,这些位相会导致可探测的CP破坏效应吗?     

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…     

制备介孔复合环境材料的酸洗刻蚀工艺

探索了一种制备介孔复合环境材料的方法--破坏式造孔与有机复合相结合,使最终产品可大量吸附污染水体中的各种污染物并具有一定的杀菌功能.该方法通过酸洗刻蚀,达到了去除原材料中的杂质和刻蚀孔径的目的,所制备的中间产品24h吸湿率为原材料的2倍,染料吸附量为原材料的1.6倍.     

斜坡变形破坏的预测及防护

通过对斜坡变形破坏和影响因素的研究，探讨工程建设中斜坡变形破坏的预测及防护。     

半刚性基层沥青路面水损破坏的结构分析

从设计方面对半刚性基层沥青路面的水损破坏进行理论分析,得出水的渗入对材料设计参数的影响以及唧浆现象使结构层层间接触条件的改变是产生水损破坏的根本原因。合理设置水泥稳定碎石排水基层有利于减缓或者防止唧装现象的出现,从而有利于使沥青面层和基层之间的层间接触状态维持连续状态,延缓沥青路面出现水损玻坏,延长沥青路面的使用寿命。     

稀土的发射光谱分析

本文介绍了稀土分析的发射光谱法，包括（1）痕量稀土镧和钆的粉末筛选电极法，镧、钆、铕、镨、钕和钐的载体分馏法。（2）岩石和矿物中稀土分析的直接法（Pyc-aHOB法）和化学光谱法（ЛaКTИOHOBa法）。（3）氧化铕中稀土元素及杂质的光谱分析的全能量法和分馏法，稀土元素氧化物混合物的光谱全分析法。（4）钢中铈、镧和钡的测定（CopoКИHa法），钢、金属和合金中稀土元素的化学光谱测定，纯金属、钢及镍合金中铈、镧、钕、镨、铒、铥、钐和钇的测定等。