Radio Observation of the 11-Month Fermi-AGN at Urumqi Observatory

We carry out flux observation at 5 GHz for 124 sources from the ‘clean’ sample of Fermi catalog 1LAC (The First LAT AGN Catalog) with Urumqi 25 m telescope. We find that it is obvious that there is a correlation between the γ-ray and the radio flux density for blazars. For the subclasses, the correlation for FSRQs is strong, but the correlation for BL Lacs is weak.     

Variability of GPS Radio Sources at 5 GHz

We carry out flux monitoring on a sample of 169 Gigahertz Peaked Spectrum (GPS) radio sources at 5 GHz and find that about one-third of them show considerable Inter-Month Variability (IMV), and these IMV phenomena are likely to be caused by interstellar scintillation (ISS). Furthermore, we find that those showing IMV tend to be point-like or core-jet structures at VLBI scale.     

用MapReduce框架构建虚拟天文台数据节点

MapReduce是一种大规模分布式并行处理框架,最初被用于互联网服务中的海量数据处理,并逐渐扩展到各个行业领域。目前,虚拟天文台面临着越来越多的地面及空间望远镜观测到的海量天文数据。为了提高中国虚拟天文台数据节点处理海量天文数据的能力,首次提出基于MapReduce框架构建中国虚拟天文台数据节点的方法,并以批量星表交叉认证为例描述了具体实现过程,性能评估结果证明基于MapReduce框架构建虚拟天文台数据节点,可以在性能、扩展性与成本等多方面获得收益。     

GIS-based method of delimitating trade area for retail chains

Delimitating trade area with accuracy is a major concern for retail and service companies who want to adapt their marketing strategy to be competitive in today's highly competitive chain industry. A collection of methods have been proposed to delimitating trade area, but either some are too simple or the necessary data are not available. In this article, a geographic information system-based method for precisely delimitating trade area is proposed. It is based on the fact that the social and economic activities are actualized along the street networks. The trade area can be delineated in terms of time distance with high precision taking the practical traffic situations into account. In addition, centered on this method of delimitating trade area, a wide array of functions can be extended to support both operational day-to-day and long-term strategic decision making for retailers.     

非开挖施工地下管线的改进措施

非开挖施工地下管线有很多工艺方法,这些工艺中存在某些需要改进的地方。并且在适当条件下可以采用新的方法代替现有的方法。第一是非开挖施工“超重地下管道”时,拉管工序中的局部连接新方法的设想。第二是在特殊情况下施工地下电力管线时PE管管节连接方式的选择。第三是在合适的地层中采用“拔管法”更换废旧地下管线的施工工艺。     

1980西安坐标系与2000坐标系坐标成果转换方法及精度分析

利用不同的解算软件,采用三维七参坐标转换模型和二维四参坐标转换模型,把1980西安坐标系成果转换成2000坐标系成果,利用大量检核点进行坐标转换成果精度检查,并对检查点点位精度做了详细的统计、分析;不仅阐述坐标转换方法和要求,而且得出在2种坐标转换模型应用的条件与要求。     

Post-earthquake changes and prediction of debris flow scales in Subao River Valley,Beichuan County,Sichuan Province,China

Subao River lies along the Beichuan–Yingxiu fault in Beichuan County, which has been heavily impacted by the Wenchuan earthquake on 12 May 2008 and has become sources of many geo-hazards. On 24 September 2008, a rainstorm triggered a large debris flow in the catchment, causing several deaths and significant damages. A case study on changes of the debris flow was conducted in the river. The peak discharges were calculated in the Guanmenzi, Huangnidi, and Daanshan gullies. Results indicated that the peak discharges corresponded to various return periods in different gullies: 200 years in Daanshan, 100 years in Huangnidi, and 50 years in Guanmenzi. However, the triggering precipitation in these three gullies was only of a 20-year return period. The debris flows had undergone significant changes. Analysis indicated that the changes should be ascribed to the flow characteristics, initiation conditions, and the channel blockage impacted by the rapid accumulation of loose material. Channel blockage was the principal factor increasing the scale of the debris flow. The values on the blocking coefficient were presented based on density, height, and other characteristics of dams. Finally, all of the peak debris flow discharges of the Subao River Valley for a 20-year return period were calculated using the recommended blocking coefficient values.     

石炭纪-早二叠世滇黔桂盆地北缘深水区的地层序列及沉积演化

通过分析石炭纪-早二叠世滇黔桂盆地北缘深水区的地层序列和沉积特征,探讨沉积演化过程及其控制因素。研究区深水地层序列包括下述的9个岩石地层单元:鹿寨组(C₁lz)、巴平组(C₁bp)、下如牙组(C₁xr)、上如牙组(C₁sr)、王佑组(C₁w)、睦化组(C₁m)、打屋坝组(C₁dw)、南丹组(C₁-P₁nd)和船埠头组(C₁c),并且可以识别出4种主要的深水沉积相:台间盆地相、斜坡相、深水陆棚相和台前斜坡相,以砂岩、碳质页岩、硅质泥岩、硅质岩、钙屑碎屑岩、泥晶灰岩和白云质灰岩为主要特征,与桂西南深水盆地的差别显著。依据地层序列和沉积组合的时空分布特征,可以将石炭纪-早二叠世滇黔桂盆地北缘深水区的沉积演化划分为3个阶段: 1)裂谷作用强烈期(早石炭亚纪汤耙沟期早期); 2)裂谷作用减弱期(早石炭亚纪汤耙沟期中期-德坞期); 3)裂谷作用稳定期(晚石炭亚纪-早二叠世)。     

The occurrence and distribution of phenylphenanthrenes,phenylanthracenes and binaphthyls in Palaeozoic to Cenozoic shales from China

The distributions of phenylphenanthrenes, phenylanthracenes and binaphthyls in sediment extracts have been investigated in a set of lacustrine shales from the Eocene Shahejie Formation (well SG 1) in the western Depression of Liaohe Basin, East China. All isomers of these phenyl substituted polycyclic aromatic hydrocarbons (PAHs) have been identified in the m/z 254 mass chromatograms by comparison of the mass spectra and standard retention indices with those published elsewhere. The 2,2′-binaphtyl/1,2′-binaphthyl ratio values show a linear increase with increasing maturity, and have a good correlation with T_max (°C). Therefore, they can be used as an effective maturity indictor for source rocks in this study. In the main phase of the oil generation window, the 3-phenylphenanthrene and 2-phenylphenanthrene prevail over other isomers, and some thermodynamically unstable isomers including all phenylanthracenes, 4-phenylphenanthrene and 1,1′-binaphthyl are present at very low concentrations or below the detection limit in the m/z 254 mass chromatograms. The absolute concentrations of individual phenylphenanthrene and binaphthyl isomers were obtained by comparison of the peak areas with that of internal standard phenanthrene-d10. All isomers are present at low concentrations at low maturity stages and then show an abrupt increase at a depth of ≈3100 m, corresponding to the onset of the intensive C₁₅₊ hydrocarbon generation. The Phenylphenanthrene Ratio (2- + 3-PhP)/[(2- + 3-PhP) + (4- + 1- + 9-PhP)] shows a reverse change with increasing maturity at the low maturity stage. It displays a drastic increase at a depth of ≈3100 m and then remains at a nearly constant value. This study can expand the understanding of the formation and distribution of phenyl substituted PAHs in sedimentary organic matter deposited in various environments.