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31.
本文介绍了数字化射线照相技术对轻物质进行判断的方法。经实践证明,该方法是合理和有效的,可大大增强对轻物质的识别能力,是一种非常可行的识别技术。 相似文献
32.
33.
平原河网区域来水组成原理 总被引:1,自引:0,他引:1
对于一般树状分布河网,上一级河道总是汇入至下一级河道,位于河道下游断面的流量总是由其上游汇集而至。但对于平原河网地区,特别是人工控制建筑物众多,又受潮汐影响的地区(如太湖流域),河网错综复杂,水流方向不定,要跟踪某个断面的水流去向,或某个河段的水体、断面流量是从哪里汇集而来的,非常困难。但这样的问题在生产实践中往往对其很感兴趣。例如从常熟枢纽引长江水流进入望虞河后,流向何处?河网各断面流量中或各河段水体中常熟枢纽引江水量占多少比重?对这些问题的研究可以估计常熟枢纽引江的效果和影响范围。因此,平原河网区域来水组成方法在生产实践中具有重要意义。重点介绍了平原河网区域来水组成原理及其在太湖流域的应用。 相似文献
34.
目的:针对射线透射图像中轻物质的自动识别存在的难点问题进行研究。方法:提出了基于轮廓特征和灰度特征的识别算法,结果:详细地阐述了利用识别算法进行识别的过程;结论:给出了识别算法的实验结果。 相似文献
35.
为了给双星计划中性原子(ENA)探测仪的研制提供可靠 的理论依据,并为未来中性原子探测数据的分析及研究做好准备,针对双星轨道初步模拟计 算了双星ENA探测仪对磁暴时中性原子的观测特性. 建立了磁暴主相期间环电流离子分布的 一 个近似理论模式,并模拟计算了极轨卫星在极区上空、赤道面以及其他位置上对不同强度磁 暴主相期间环电流区ENA空间角分布及能谱的观测结果. 研究表明,存在环电流区方向和南 北极区环电流粒子沉降带两个中性原子强度极大区域;磁暴越强烈,注入区高度越低,环电 流区观测到的ENA通量越高;处于有利位置的ENA探测器可分辨注入区内边界或注入前沿;EN A探测器能够分辨环电流带离子分布的不均匀性;由于离子交换截面的差异,H,O,He 3种E NA的能谱分布不同;在10~80keV能谱范围内通量较强,易于观测;环电流区H,O两种ENA 通 量较强,有利于观测;而环电流区He ENA通量很弱,不易于观测. 模拟计算研究表明,双星 极轨卫星能够对环电流区ENA进行有效探测;低纬轨道上的ENA探测器也能够对环电流区ENA 进行一些观测;ENA探测器的研制应重视低、中能量范围ENA的探测. 相似文献
36.
D. S. Cohan G. A. Sturrock A. P. Biazar P. J. Fraser 《Journal of Atmospheric Chemistry》2003,44(2):131-150
Atmospheric mixing ratios of methyl iodide (CH3I) and other methyl halides have been measured at Cape Grim, Tasmania (41°S, 145°E), since early 1998 as part of the Advanced Global Atmospheric Gases Experiment (AGAGE). This paper analyses about 1700 ambient air CH3I measurements from the 14-month period (March 1998–April 1999). Mixing ratios peaked during the summer, despite faster photolytic loss, suggesting local oceanic emissions were about 2.2–3.6 times stronger in summer than in winter. Back trajectories show that CH3I levels are strongly dependent on air mass origin, with highest mixing ratios in air from the Tasman Sea/Bass Strait region and lowest levels in air originating from the Southern Ocean at higher latitudes. CH3I mixing ratios were not well correlated with other methyl halides in unpolluted marine air. The large variations with season and air mass origin suggest that high frequency, continuous data from key locations will make a significant contribution to the understanding of sources and sinks of this important short-lived atmospheric species. 相似文献
37.
Two semi-asymmetric flow patterns of typhoons are chosen to qualitatively determine the effect of exchange of horizontal momentum between inflow and outflow layers and the environment on the motion of typhoons. The results show that only the asymmetric flow component (residual after azimuthal mean flow has been removed) could cause a net momentum input into or output from a typhoon and therefore contribute to the changes in speed and direction of the typhoon movement. A typhoon with major inflow and/or outflow channels on its right (left) side would tend to accelerate and turn left (decelerate and turn right); On the other hand, a typhoon with major inflow and/or outflow channels in the rear (front) semicircle would tend to accelerate and turn right (decelerate and turn left). 相似文献
38.
We measured the partial pressure of oxygen (PO2) in the interstitial gas surrounding the sand-swimming Namib moleEremitalpa granti namibensis. At a sand temperature of 26 °C, which produced a nearly maximal rate of oxygen consumption, thePO2near the noses of the animals averaged only 0·9 kPa (6·7 Torr) below the level in the free atmosphere. High oxygen availability was a result of the notably low metabolic rate in the 20 g mammals and the dry, porous and metabolically inactive nature of dune sand. A mathematical model indicated that normal mammals weighing 200 g or more could comfortably exist completely encased in dune sand. We concluded that the moles' small size and low metabolic rate are not adaptations to hypoxia or hypercapnia underground but are probably related to low food availability and the energetic cost of foraging in their desert environment. 相似文献
39.
本文以等物质的量的反应规则建立了岩盐、芒硝中各种化合物的质量分数的计算公式。这些公式既符合法定计量单位的要求,又方便计算。 相似文献
40.
Oxygen Isotope Exchange Kinetics Between Coexisting Minerals and Water in the Aral Granite Pluton of the Altay Mountains, Northern Xinjiang 总被引:2,自引:0,他引:2
Liu Wei Research Center of Mineral Resources Exploration Chinese Academy of Sciences Chinese Academy of Sciences BeijingHe Baichu Changsha Institute of Geotectonics Chinese Academy of Sciences Changsh Hunanand Chen ZhenshengYichang Institute of Geology Mineral Resources Chinese Academy of GeologicalSciences Yichang Hubei 《《地质学报》英文版》1996,70(4)
Coexisting quartz, feldspar and biotite vary widely in their δ18O values and display a remarkable 18O/16O disequilibrium relation; especially, a quartz-feldspar reversal (△ 18OQUartz_feldspar< 0) exsists in the Aral granite pluton of the Altay Mountains, northern Xinjiang. The 18O / 16O exchange reaction definitely occurred between granite and water. Initial δ18O values of the granite and exotic fluid are evaluated by the mass balance consideration. The conventional method of discrimination between various magma derivations simply with δ18O values of either whole rock or separate minerals is misleading and unreliable. Experiments carried out by the authors show that the 18O / 16O exchange reaction is not accompanied by what geologists describe as petrological and mineralogical alteration effect. This decoupling relation implies that exchange reaction occurs at a relatively high temperature during subsolidus-postmagmatic cooling of magmas. The exchange mechanism is mainly diffusion-controlled. It is 相似文献