Curvelet感兴趣区域相关图的纹理图像检索

提出了一种基于感兴趣区域纹理图像的检索方法.对纹理图像进行Curvelet多尺度分解,根据各层子带的能量分布提取感兴趣区域,并量化感兴趣区域Curvelet系数,计算颜色自相关图而构造图像的特征向量.在Brodatz纹理库中的实验结果表明,与原有基于Curvelet的纹理图像检索方法相比,所提出的方法对纹理图像检索的效果更佳.     

Magnetic characteristics and its environmental implications of core YSJD-86GC sediments from the southern South China Sea

Sediments of core YSJD-86GC （referred to as 86GC） collected from the southern South China Sea were selected for environmental magnetic studies. Combined with the published chronological framework, sediment magnetic properties were revealed for the study area since the MIS3 stage. The rock magnetic results indicate that low-coercivity magnetite is the main magnetic mineral within the sediments. Also, a certain amounts of hematite are present. The King plot and Day plot, which reflect the magnetic particle size, show that fine-grained pseudo-sin- gle-domain phase magnetic particles dominate the magnetic minerals in the sediments. Comparison of magnetic parameters and geochemical indicators show that magnetic properties of core 86GC sediments reflect a terrigenous input. Simultaneously, magnetic characteristics of the stud- ied sediment are influenced by the quantity of terrigenous sediment input, oxidation-reduction conditions of the provenance area, and the transportation environment and distance. Sea level fluctuation caused by global climate change was the main factor for variation in concentration of magnetic minerals and magnetic particle size of thestudied core sediments. Thus, variation of sediment magnetic properties in the study area can be used as an indirect indicator of sea level fluctuation.     

Formation of highly crystalline maghemite nanoparticles from ferrihydrite in the liquid phase

Fe5O7（OH）·4H2O ferrihydrite is a low-crystal- linity antiferromagnetic material, γ-Fe2O3 （maghemite） magnetic nanoparticles were prepared from a ferrihydrite precursor, by chemically induced transformation in FeCl2/ NaOH solution. The magnetization, morphology, crystal structure and chemical composition of the products were determined by vibrating sample magnetometry, transmission electron microscopy, X-ray diffraction （XRD）, energy-dispersive X-ray spectroscopy and X-ray photoelectron spectroscopy （XPS）. Ferrihydrite underwent aggregation growth and transformed into α-FeO（OH） （goethite） particles, which subsequently transformed into γ-Fe2O3 nanoparticles, that became coated with NaCI. The γ-Fe2O3 particles had a flake-like morphology, when prepared from 0.01 mol/L FeCl2 and a FeCl2：NaOH molar ratio of 0.4. The γ-Fe2O3 particles were more spherical, when prepared from a FeCl2：NaOH molar ratio of 0.6. The Fe content of the flake-like particles was lower than that of the spherical particles. Their magnetizations were similar, and the coercivity of the flake-like particles was larger. The differences in morphology and magnetization were attributed to the surface effect, and the difference in coercivity to the shape effect.     

Observation of directional change of core field inside flux ropes within one reconnection diffusion region in the Earth’s magnetotail

Two consecutive magnetic flux ropes, separated by less than 30 s （△t 〈 30 s）, are observed within one magnetic reconnection diffusion region without strong guide field in the Earth＇s magnetotail by Cluster multispacecraft. The flux ropes are characterized by bipolar signatures of the south-north magnetic field component Bz accompanied with strong core magnetic field By, intense current J and density depletions inside of them. In spite of the small but non-trivial global scale negative guide field （-By）, there exists a directional change of the core fields of two flux ropes, i.e., -By for the first one, and ＋By for the second one. The directions of the core fields are the same as the ambient cross-tail magnetic field component （By） just outside of flux ropes. Therefore, we suggest that the core field of flux ropes is formed by compression of the local preexisting By and that the directional change of core field is due to the change of local preexisting By. Such a change in ambient By might be caused by some microscale physics.     

浅论电力工程对环境的影响及保护措施

从火力发电、水力发电、核发电、风力发电几方面,分析了电力工程对环境的影响,探讨了减轻影响的措施。     

一种带中间换热器的双热源高温热泵系统

为了提高工业高温热泵系统的热力性能,实现对工业低温余热的高效综合回收,提出了一种带中间换热器的双热源高温热泵系统。第一级热泵以CO2为工质、以空气为热源,在超临界状态下将冷水加热到中间温度。第二级热泵以R152a(二氟乙烷)作为工质,从工业余热源吸收热量,将用水加热到所需的高温,并且在中间换热器中将CO2加热到过热状态。对该双热源热泵系统进行热力学分析,发现给定R152a在中间换热器温降的情况下,CO2存在最大的过热度,使得整个系统达到最佳运行工况。以回收50℃废水余热为例与单热源热泵进行比较,平均供水量是后者的两倍多,单位质量热水的耗功量减少43.2%,性能系数和火用效率分别平均提高41.9%和23.96%。     

微孔玻璃的制备及其吸附分离N_2/CO_2研究

吸附法脱除二氧化碳的关键在于开发高效的吸附剂.采用溶胶-凝胶法制备微孔玻璃,首先通过控制pH值、乙醇用量、温度等参数来得到适宜的干凝胶,干凝胶在高温下熔融形成玻璃体后,依次进行分相和酸浸析处理后得到微孔玻璃.结果表明:在pH值1~2、凝胶温度50℃、熔融温度1 175℃条件下,可以得到孔径集中在0.7~2.0 nm的微孔玻璃;随着盐酸浓度的升高,微孔玻璃的平均孔径逐渐增大,而孔体积和比表面积则逐渐减小;微孔玻璃对N2/CO2具有较高的吸附选择性,分离因子可达8.4以上.     

SASI高光谱数据在油气勘探中的应用

以最新获取的准噶尔盆地吉木萨尔地区高光谱SASI数据为例,首先对该数据进行坏波段去除,大气校正以及波谱重建等预处理;然后对重建数据进行降维降噪,提纯和N维可视化,并且基于光谱特征吸收峰的光谱识别准则,提取出与贮藏油气有关的方解石和伊利石的光谱信息,最后运用混合调制匹配滤波技术对异常区填图.结合已有地质资料分析和野外验证,所提取出的蚀变信息与油气区地质情况基本吻合,准噶尔盆地为高光谱遥感技术勘探油气提供一定的地质依据.     

Microstructure and oxidation resistance of SiC–MoSi2 multi-phase coating for SiC coated C/C composites

In order to improve the anti-oxidation of C/C composites, a SiC–MoSi2multi-phase coating for SiC coated carbon/carbon composites(C/C)was prepared by low pressure chemical vapor deposition(LPCVD) using methyltrichlorosilane(MTS) as precursor, combined with slurry painting from MoSi2 powder. The phase composition and morphology were analyzed by scanning electron microscope(SEM) and X-ray diffraction(XRD) methods, and the deposition mechanism was discussed. The isothermal oxidation and thermal shock resistance were investigated in a furnace containing air environment at 1500 1C. The results show that the as-prepared SiC–MoSi2coating consists of MoSi2 particles as a dispersing phase and CVD–SiC as a continuous phase. The weight loss of the coated samples is 1.51% after oxidation at 1500 1C for 90 h, and 4.79% after 30 thermal cycles between 1500 1C and room temperature. The penetrable cracks and cavities in the coating served as the diffusion channel of oxygen, resulted in the oxidation of C/C composites, and led to the weight loss in oxidation.     

Effects of baria on propane oxidation activity of Pd/Al2O3 catalyst: Pd–BaO interactio n and reaction routes

The BaO-modified Pd/Al2O3exhibits much better catalytic activity than Pd/Al2O3for C3H8 oxidation both before and after the hydrothermal aging treatment. Further studies ascribe its good activity to the influence of BaO species on the physicochemical characteristics of the catalyst and the reaction routes. Firstly, the BaO species inhibits the phase transformation of alumina, resulting in higher surface area of the catalysts and hereby a better dispersion of Pd. Secondly, the basic nature and electron-withdrawing effect of barium oxide maintain palladium at high oxidation state, which leads to a higher PdO content on surface of the BaO-modified catalyst. Finally, the formation/decomposition of carbonate/bicarbonate species can be promoted by the addition of BaO, which provide extra reaction routes and are important for the deep oxidation of C3H8.