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1.
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。 相似文献
2.
XIE Xianjian WEI Fangqiang BAI Jingwen LAI Ting 《武汉大学学报:自然科学英文版》2007,12(4):729-736
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. 相似文献
3.
ZHANG BaoMin ZHANG ShuiChang BIAN LiZeng JIN ZhiJun WANG DaRui 《科学通报(英文版)》2007,52(A01):77-91
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. 相似文献
4.
The controlling factors and distribution prediction of H2S formation in marine carbonate gas reservoir, China 总被引:1,自引:0,他引:1
ZHU GuangYou ZHANG ShuiChang LIANG YingBo 《科学通报(英文版)》2007,52(A01):150-163
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. 相似文献
5.
水热合成了钒磷酸盐体系中少有的结构中具有多面体共棱连接的层状孔道结构化合物(pipzH2)2[(VO)3(HPO4)2(PO4)2]·H20的纯相。用ICP、单晶XRD、TG-DTA、粉晶XRD和SEM对产物进行了表征。结果表明,化合物在空气中开始失重的温度为274℃,随着温度的升高,化合物中有机分子分解,同时伴随着重结晶过程,但晶体的外观形貌保持不变直至有机部分分解殆尽。相变过程分析和与模板相同的(pipzH2)0.5[(VO)(PO4)]的热稳定性对比研究表明,有机模板的稳定性及分解过程不但影响化合物的热稳定性和热变化过程,还影响原晶体微形貌的保持;无机骨架结合的牢固程度在很大程度上影响化合物的热稳定性。 相似文献
6.
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… 相似文献
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断裂带中岩石的硅化现象,通常称之为硅化岩或硅化破碎带,即经动力变质作用的断层岩,通过微束技术对其观察,它们显示出下列特征:在扫描电镜(SEM)下,硅化物质表现为细脉状,而在偏光里微镜下则表现为浸染状;对硅化岩进行组构观察,可见压扁 S 面和剪切 S 面;在透射电镜(TEM)下,可进一步区别不同的位错现象;断裂带岩石的硅化现象是受组成岩石的化学元素的构造地球化学作用所制约的,包括动力分异和化学亲和作用,动热变质作用和退化变质作用,氧化和还原作用以及脱水和水解作用。 相似文献