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71.
The improvement on the calculation of anti-Stokes energy transfer rate is studied in the present work. The additional proportion coefficient between Stokes and anti-Stokes light intensities of quantum Raman scattering theory as compared with the classical Raman theory is introduced to successfully describe the anti-Stokes energy transfer. The theoretical formula for the improvement on the calculation of anti-Stokes energy transfer rate is derived for the first time in this study. The correctness of introducing coefficient exp{ΔE / kT} from well-known Raman scatter theory is demonstrated also. Moreover, the experimental lifetime measurement in Er0.01YbxY1 - 0.01 - xVO4 crystal is performed to justify the validity of our important improvement in the original phonon-assisted energy transfer theory for the first time. 相似文献
72.
Adam P. Piotrowski Maciej J. Napiorkowski Jaroslaw J. Napiorkowski Marzena Osuch Zbigniew W. Kundzewicz 《水文科学杂志》2017,62(4):606-625
In recent years sampling approaches have been used more widely than optimization algorithms to find parameters of conceptual rainfall–runoff models, but the difficulty of calibration of such models remains in dispute. The problem of finding a set of optimal parameters for conceptual rainfall–runoff models is interpreted differently in various studies, ranging from simple to relatively complex and difficult. In many papers, it is claimed that novel calibration approaches, so-called metaheuristics, outperform the older ones when applied to this task, but contradictory opinions are also plentiful. The present study aims at calibration of two simple lumped conceptual hydrological models, HBV and GR4J, by means of a large number of metaheuristic algorithms. The tests are performed on four catchments located in regions with relatively similar climatic conditions, but on different continents. The comparison shows that, although parameters found may somehow differ, the performance criteria achieved with simple lumped models calibrated by various metaheuristics are very similar and differences are insignificant from the hydrological point of view. However, occasionally some algorithms find slightly better solutions than those found by the vast majority of methods. This means that the problem of calibration of simple lumped HBV or GR4J models may be deceptive from the optimization perspective, as the vast majority of algorithms that follow a common evolutionary principle of survival of the fittest lead to sub-optimal solutions. 相似文献
73.
本研究以PNIPAM(聚N-异丙基丙烯酰胺)为单体,先制备出来Fe3O4@SiO2纳米颗粒,再与DMP(十二烷基三硫代碳酸酯)链转移剂进行酯化反应,制备的产物作为新的链转移剂,在偶氮二异丁腈为引发剂的条件下,利用可逆加成-断裂链转移自由基聚合(RAFT)活性聚合法制备温度响应性磁纳米粒子。通过红外光谱法、核磁共振法对聚合物的结构进行表征,谱图表明成功地合成出所需的产物。通过扫描电镜对其进行分析,所得到的Fe3O4@SiO2-PNIPAM聚合物纳米颗粒分布比较均匀。 相似文献
74.
不同年龄杉木人工林土壤无机氮比较研究 总被引:1,自引:0,他引:1
在福建南平杉木林中心产区,选取11、21、28、40、88年生杉木人工林以及采伐迹地、杂木林为研究对象,研究不同年龄杉木林土壤无机氮的差异.结果表明:不同年龄杉木林土壤NH4^+-N含量差异显著,以21年生的杉木人工林最高(11.91±0.43mg·kg^-1),其他的为88年生的(8.33±0.38mg·kg^-1)〉28年生的(8.19±0.25mg·kg^-1)〉11年生的(5.65±0.17mg·kg^-1)〉40年生的(5.63±0.38mg·kg^-1);NO3^--N含量较低(3.15~4.11mg·kg^-1),且没有显著差异,这与杉木林所处的生长阶段、土壤理化性质有关.杉木林取代杂木林后,NH4^+-N和NO3^--N含量都有所下降;采伐迹地土壤NH4^+-N(19.74±1.44mg·kg^-1)和NO3^--N(18.05±0.72mg·kg^-1)含量远高于88年生的杉木林,分别是88年生的2.37和4.60倍.本地区无机氮含量较低,NH4^+-N占无机氮的比例为60.0%~74.3%,NH4^+-N为无机氮的主要形态. 相似文献
75.
Future temperature distributions of the marginal Chinese seas are studied by dynamic downscaling of global CCSM3 IPCC_AR4 scenario runs.Different forcing fields from 2080-2099 Special Report on Emissions Scenarios(SRES) B1,A1,and A2 to 1980-1999 20C3M are averaged and superimposed on CORE2 and SODA2.2.4 data to force high-resolution regional future simulations using the Regional Ocean Modeling System(ROMS).Volume transport increments in downscaling simulation support the CCSM3 result that with a weakening subtropical gyre circulation,the Kuroshio Current in the East China Sea(ECS) is possibly strengthened under the global warming scheme.This mostly relates to local wind change,whereby the summer monsoon is strengthened and winter monsoon weakened.Future temperature fluxes and their seasonal variations are larger than in the CCSM3 result.Downscaling 100 years’ temperature increments are comparable to the CCSM3,with a minimum in B1 scenario of 1.2-2.0°C and a maximum in A2 scenario of 2.5-4.5°C.More detailed temperature distributions are shown in the downscaling simulation.Larger increments are in the Bohai Sea and middle Yellow Sea,and smaller increments near the southeast coast of China,west coast of Korea,and southern ECS.There is a reduction of advective heat north of Taiwan Island and west of Tsushima in summer,and along the southern part of the Yellow Sea warm current in winter.There is enhancement of advective heat in the northern Yellow Sea in winter,related to the delicate temperature increment distribution.At 50 meter depth,the Yellow Sea cold water mass is destroyed.Our simulations suggest that in the formation season of the cold water mass,regional temperature is higher in the future and the water remains at the bottom until next summer.In summer,the mixed layer is deeper,making it much easier for the strengthened surface heat flux to penetrate to the bottom of this water. 相似文献
76.
77.
总结了目前国内主要的物探找水技术方法,分析了各种方法的优缺点及其适应范围。以云南个旧市的找水成果作为典型案例,重点介绍了EH4电磁成像找水方法的技术特点、在岩溶区找水的可行性分析、数据处理和成果解释过程,最后推断出可能存在地下水的位置,并布设井位用于指导施工。后期追踪调查表明,勘察区已成功打出地下水,证明了使用EH4电磁成像技术在岩溶区找水的可行性。 相似文献
78.
79.
本文利用Geant4模拟了FD3013数字γ辐射仪探测器探测晶体,对137Cs(0.661MeV)的γ射线的探测效率,和TH-PPLCT教学仪防护铅罐对137Cs源的防护效果,并建立了简易人体模型,仿真计算了人体吸收剂量,结果显示防护铅罐屏蔽后的辐射剂量在可接受的水平内。 相似文献
80.