A New Approach for Studying Hubble Diagrams of Quasars   总被引：2，自引：0，他引：2  

Y.P. Qin  G.Z. Xie  J.C. Wang  M.C. He  J.H. Fan 《Astrophysics and Space Science》1997,253(1):19-26

In this paper, a new approach for studying Hubble diagrams of quasars is introduced. The purpose is to reduce the well-known very large scatter in the diagram. We believe that the scatter is mainly caused by the wide spread of luminosity distribution of quasars. Based on a large number of quasars having been discovered, we introduce a new quantity, the collective apparent magnitude of certain amount of quasars in a corresponding redshift interval, and make a plot of the collective apparent magnitude versus redshift with the data published by Hewitt and Burbidge (1993). The quantity is contributed by individual apparent luminosities as well as the luminosity distribution of quasars. Scatter is expected to be largely reduced in the corresponding diagram, and this is indeed true as shown by the figures. By discussing several possible effects and from the figures, we find that the assumption that redshifts of quasars are distance indicators is confirmed, and the standard cosmological model is supported. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

快速数论变换的一种算法     

何永富  陈涛  王柏钧 《成都信息工程学院学报》1993,(3)

本文构造了一种快速数论变换算法,该算法是一种以数论为基础,有效高速的数论变换算法,并且这种算法易于在计算机上实现。  相似文献   

GPS共视法时间比对在陕西天文台的建立     

吴贵臣  和翠英  董绍武 《时间频率学报》1994

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生物生态防治虾病研究     

何筱洁  庞田胜  刘思俭  黄丽萍 《广东海洋大学学报》1990,(1)

本文探索虾病防治新途径,采用低值海藻江蓠和对虾混养的生态学方法,江蓠吸收水中二氧化碳进行光合作用,产生大量氧气;同时吸收有机物的分解物 NH_3—N,加速有机物分解。减少 H_2S 积累;从而消除水中紧迫因子威胁,大大减少池水自污及病害,起到抑菌、抑虫、净化水质作用,提高成活率,试验圹对虾成活率达95.1%,对照圹56.6%。试验结果表明,虾病防治效果显著,经济效益明显。  相似文献   

Contemporary processes of environmental information in the atmosphere-glacier-runoff system in an area of typical monsoon temperate glacier     

He  Yuanqing  Yao  Tandong  Zhang  Xiaojun  Chen  Tuo  Yang  Meixue  Sun  Weizhen  Li  Fengxia 《中国科学:地球科学(英文版)》2001,44(1):275-283

Sampling was carried out at Baishui No. 1, the largest glacier on Mt. Yulong, China, during the summers of 1999 and 2000, to investigate the spatial variations of oxygen isotopes in the atmosphere-glacier-river system. The results confirm that there is an inverse relation between the oxygen isotopic composition of precipitation and air temperature/precipitation amount. This suggests that a strong “precipitation amount effect” exists in this typical monsoon temperate-glacier region. There are marked differences of the δ¹⁸O values of winter-accumulated snow, glacial meltwater, summer precipitation and the glacier-fed river water. Spatial and temporal variations of isotopic composition are controlled by climatic conditions. Isotopic fractionation and differentiation occur during phase changes, snow-to-ice and ice-to-meltwater transformations, and runoff processes. Variations of stable isotopes in glacier runoff can indicate variations of sources of supply, as well as different discharge-related processes. Ionic changes occur as a result of meltwater contact with glacier bed materials.

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Deepwater Ventilation and Stratification in the Neogene South China Sea     

李前裕赵泉鸿  钟广法翦知湣 田军成鑫荣  汪品先陈木宏 《中国地质大学学报(英文版)》2007,18(2):95-108

Combined data of physical property, benthic foraminifera, and stable isotopes from ODP Sites 1148, 1146, and 1143 are used to discuss deep water evolution in the South China Sea (SCS) since the Early Miocene. The results indicate that 3 lithostratigraphic units, respectively corresponding to 21-17 Ma, 15-10 Ma, and 10-5 Ma with positive red parameter (a*) marking the red brown sediment color represent 3 periods of deep water ventilation. The first 2 periods show a closer link to contemporary production of the Antarctic Bottom Water (AABW) and Northern Component Water (NCW), indicating a free connection of deep waters between the SCS and the open ocean before 10 Ma. After 10 Ma, red parameter dropped but stayed higher than the modern value (a*=0), the CaCO3 percentage difference between Site 1148 from a lower deepwater setting and Site 1146 from an upper deepwater setting enlarged significantly, and benthic species which prefer oxygen-rich bottom conditions dramatically decreased. Coupled with a major negative excursion of benthic δ13C at ~10 Ma, these parameters may denote a weakening in the control of the SCS deep water by the open ocean. Probably they mark the birth of a local deep water due to shallow waterways or rise of sill depths during the course of sea basin closing from south to east by the west-moving Philippine Arc after the end of SCS seafloor spreading at 16-15 Ma. However, it took another 5 Ma before the dissolved oxygen approached close to the modern level. Although the oxygen level continued to stabilize, several Pacific Bottom Water (PBW) and Pacific Deep Water (PDW) marker species rapidly increased since ~6 Ma, followed by a dramatic escalation in planktonic fragmentation which indicates high dissolution especially after ~5 Ma. The period of 5-3 Ma saw the strongest stratified deepwater in the then SCS, as indicated by up to 40% CaCO3 difference between Sites 1148 and 1146. Apart from a strengthening PDW as a result of global cooling and ice cap buildup on northern high latitudes, a deepening sea basin due to stronger subduction eastward may also have triggered the influx of more corrosive waters from the deep western Pacific. Since 3 Ma, the evolution of the SCS deep water entered a modern phase, as characterized by relative stable 10% CaCO3 difference between the two sites and increase in infaunal benthic species which prefer a low oxygenated environment. Thesubsequent reduction of PBW and PDW marker species at about 1.2 Ma and 0.9 Ma and another significant negative excursion of benthic δ13C to a Neogene minimum at ~0.9 Ma together convey a clear message that the PBW largely disappeared and the PDW considerably weakened in the Mid-Pleistocene SCS. Therefore, the true modern mode SCS deep water started to form only during the "Mid-Pleistocene climatic transition" probably due to the rise of sill depths under the Bashi Strait.  相似文献   

基于SuperMap IS的WebGIS开发   总被引：1，自引：0，他引：1  

张贺  孙德军  朱虹 《测绘工程》2007,16(3):56-58

WebGIS是将Web技术和GIS技术相结合的新技术,有着广泛的应用。通过WebGIS技术,客户端仅需使用浏览器(不一定包含专门插件)就可以对分布在Web上的GIS数据进行查询、分析等交互操作。探讨了利用Super-Map网络GIS技术,以SuperMap DeskPro作为后台GIS服务平台,通过SuperMap IS实现用户利用浏览器获得一个地理信息系统中的数据和功能的服务,论述开发和建设WebGIS的过程。  相似文献   

Cretaceous–Tertiary geology of the Gangdese Arc in the Linzhou area, southern Tibet     

Shundong He  Paul Kapp  Peter G. DeCelles  George E. Gehrels  Matthew Heizler   《Tectonophysics》2007,433(1-4):15-37

Knowledge of the Cretaceous–Tertiary history of upper crustal shortening and magmatism in Tibet is fundamental to placing constraints on when and how the Tibetan plateau formed. In the Lhasa terrane of southern Tibet, the widely exposed angular unconformity beneath uppermost Cretaceous–lower Tertiary volcanic-bearing strata of the Linzizong Formation provides an excellent geologic and time marker to distinguish between deformation that occurred before vs. during the Indo-Asian collision. In the Linzhou area, located  30 km north of the city of Lhasa, a > 3-km-thick section of the Linzizong Formation lies unconformably on Cretaceous and older rocks that were shortened by both northward- and southward-verging structures during the Late Cretaceous. The Linzizong Formation dips northward in the footwall of a north-dipping thrust system that involves Triassic–Jurassic strata and a granite intrusion in the hanging wall. U–Pb zircon geochronologic studies show that the Linzizong Formation ranges in age from 69 Ma to at least 47 Ma and that the hanging wall granite intrusion crystallized at  52 Ma, coeval with dike emplacement into footwall Cretaceous strata. ⁴⁰Ar/³⁹Ar thermochronologic studies suggest slow cooling of the granite between 49 and 42 Ma, followed by an episode of accelerated cooling to upper crustal levels beginning at  42 Ma. The onset of rapid cooling was coeval with the cessation of voluminous arc magmatism in southern Tibet and is interpreted be a consequence of either (1) Tertiary thrusting in this region or (2) regional rock uplift and erosion following removal of overthickened Gangdese arc lower crust and upper mantle or break-off of the Neo-Tethyan oceanic slab.  相似文献   

武汉市1：1万土地利用数据库建设与应用     

李宗华  黄河  曾忠平  狄秀梅 《国土资源信息化》2007,(1):15-19

1:1万土地利用数据库是土地管理信息化的基础,其最终目的是为国土资源管理以及其它行业服务。本文在土地管理基本理论和武汉市土地利用数据库应用实践的基础上,研究了数据库应用的多种方法,总结了数据库的应用模式以及多种应用成果表达方式。结果表明,土地利用数据库在日常地籍管理、土地资源与资产管理以及经济社会发展等领域有着广泛的应用。  相似文献   

Initial results of centralized autonomous orbit determination of the new-generation BDS satellites with inter-satellite link measurements   总被引：3，自引：0，他引：3  

Chengpan Tang  Xiaogong Hu  Shanshi Zhou  Li Liu  Junyang Pan  Liucheng Chen  Rui Guo  Lingfeng Zhu  Guangming Hu  Xiaojie Li  Feng He  Zhiqiao Chang 《Journal of Geodesy》2018,92(10):1155-1169

Autonomous orbit determination is the ability of navigation satellites to estimate the orbit parameters on-board using inter-satellite link (ISL) measurements. This study mainly focuses on data processing of the ISL measurements as a new measurement type and its application on the centralized autonomous orbit determination of the new-generation Beidou navigation satellite system satellites for the first time. The ISL measurements are dual one-way measurements that follow a time division multiple access (TDMA) structure. The ranging error of the ISL measurements is less than 0.25 ns. This paper proposes a derivation approach to the satellite clock offsets and the geometric distances from TDMA dual one-way measurements without a loss of accuracy. The derived clock offsets are used for time synchronization, and the derived geometry distances are used for autonomous orbit determination. The clock offsets from the ISL measurements are consistent with the L-band two-way satellite, and time–frequency transfer clock measurements and the detrended residuals vary within 0.5 ns. The centralized autonomous orbit determination is conducted in a batch mode on a ground-capable server for the feasibility study. Constant hardware delays are present in the geometric distances and become the largest source of error in the autonomous orbit determination. Therefore, the hardware delays are estimated simultaneously with the satellite orbits. To avoid uncertainties in the constellation orientation, a ground anchor station that “observes” the satellites with on-board ISL payloads is introduced into the orbit determination. The root-mean-square values of orbit determination residuals are within 10.0 cm, and the standard deviation of the estimated ISL hardware delays is within 0.2 ns. The accuracy of the autonomous orbits is evaluated by analysis of overlap comparison and the satellite laser ranging (SLR) residuals and is compared with the accuracy of the L-band orbits. The results indicate that the radial overlap differences between the autonomous orbits are less than 15.0 cm for the inclined geosynchronous orbit (IGSO) satellites and less than 10.0 cm for the MEO satellites. The SLR residuals are approximately 15.0 cm for the IGSO satellites and approximately 10.0 cm for the MEO satellites, representing an improvement over the L-band orbits.  相似文献