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使用氯金酸和柠檬酸三钠回流法合成出荧光吸收峰在520 nm的金纳米颗粒,并与罗丹明B修饰合成探针.金纳米颗粒与罗丹明B发生荧光共振能量转移(FRET)作用使罗丹明B的荧光淬灭.在加入毒死蜱之后,毒死蜱及其水解产物能有效取代罗丹明B,使荧光恢复.金纳米颗粒探针对毒死蜱及其水解产物的浓度响应区间为(0~0.1)mm,低至0.1 nm也有响应,且荧光变化迅速,从而能够快速有效地检测超痕量有机磷农药毒死蜱及其水解产物. 相似文献
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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
5.
感应熔敷WC/Ni基复合涂层的组织和性能 总被引:1,自引:0,他引:1
采用高频感应熔敷技术,以Ni60A自熔合金粉末、微纳米碳化钨粉末为原料,在16Mn钢表面制备出以微纳米WC颗粒为增强相的Ni基金属陶瓷涂层,并测试了涂层的显微硬度。利用磨擦磨损试验机,以45#钢为对磨偶件,评价了涂层的滑动干磨擦性能。实验结果表明:涂层的硬度为890~910,磨擦系数为0.3-0.4,耐磨性比16Mn钢提高4倍以上。 相似文献
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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
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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
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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
9.
旋流场中分散相颗粒径向受力及径向速度方程 总被引:3,自引:0,他引:3
从两相流的角度阐释了分散相单颗粒在旋流场中的径向受力,并对各力进行了分析和简化.运用力分析的方法建立了颗粒径向速度对于径向位置分布的径向运动方程,探讨了颗粒径向速度的求解.结果表明,经典的平衡轨道理论所认为的沉降速度只能在某一特定位置出现,并不具有实际应用意义;而径向运动方程则可以求解,并可作为旋流场进一步讨论的基础. 相似文献
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