荆州电子地图公交查询算法与实现

以荆州市最新的交通地图为基础,编写出荆州市旅游交通电子地图公交查询功能的算法,并利用地理信息系统组件MapObjects 2．3、高级编程语言VB6．0和数据库SQL Server 2000实现了该公交查询功能,这对于发展荆州市旅游经济有着重要的意义。     

一种改进的降落影像序列特征匹配方法

针对传统SIFT匹配方法用于嫦娥三号降落影像匹配效率低的问题,提出了一种改进的降落影像序列特征匹配方法。重构了着陆器垂直降落阶段拍摄过程的几何模型,并得到了不同降落影像中的同名匹配点之间的几何约束关系,然后通过SIFT方法进行影像中极值点的提取和特征描述,最终将几何模型约束用于极值点的匹配点搜索过程中,优化了匹配过程。采用嫦娥三号着陆器真实降落影像进行了试验,结果表明,改进方法能够取得较为稳定的匹配结果,且平均可以减少约为18%的匹配耗时,研究结果对后续深空探测任务的开展具有重要的参考价值。     

Derivation of Cloud-Free-Region Atmospheric Motion Vectors from FY-2E Thermal Infrared Imagery

The operational cloud-motion tracking technique fails to retrieve atmospheric motion vectors(AMVs) in areas lacking cloud; and while water vapor shown in water vapor imagery can be used, the heights assigned to the retrieved AMVs are mostly in the upper troposphere. As the noise-equivalent temperature difference(NEd T) performance of FY-2E split window(10.3–11.5 μm, 11.6–12.8 μm) channels has been improved, the weak signals representing the spatial texture of water vapor and aerosols in cloud-free areas can be strengthened with algorithms based on the difference principle, and applied in calculating AMVs in the lower troposphere. This paper is a preliminary summary for this purpose, in which the principles and algorithm schemes for the temporal difference, split window difference and second-order difference(SD) methods are introduced. Results from simulation and cases experiments are reported in order to verify and evaluate the methods, based on comparison among retrievals and the "truth". The results show that all three algorithms, though not perfect in some cases,generally work well. Moreover, the SD method appears to be the best in suppressing the surface temperature influence and clarifying the spatial texture of water vapor and aerosols. The accuracy with respect to NCEP 800 h Pa reanalysis data was found to be acceptable, as compared with the accuracy of the cloud motion vectors.     

Comparison of SARAL and Jason-1/2 altimetry-derived geoids for geophysical exploration over the Indian offshore

Satellite with ARgos and ALtika (SARAL) altimeter includes the ALTIKA payload, a 35.75 GHz Ka band radar altimeter. High pulse repetition frequency of SARAL (4 KHz) satellite provides better along-track information. Jason-1/2 data have been extensively utilized as a follow-up of TOPEX/Poseidon altimeter data for its accurate measurements of the sea surface heights, particularly for geodetic mission of Jason-1. In this study, we have compared SARAL and Jason-1/2 altimetry-derived classical and residual geoids over the Indian offshore using Rapp’s, EGM96 and EGM08 gravity model coefficients, which are of interest for better understanding of geological and structural evolution/interpretation. SARAL and Jason-1/2 data have also been used over the two prominent geological features over the Indian offshore, namely the Bombay High in the western offshore and the 85°E Ridge in the Bay of Bengal. The SARAL altimetry-derived geoids could delineate these major geological/structural features with distinct residual geoidal lows.     

凡纳滨对虾TOR蛋白下游信号传导因子eIF4E2和eIF4E1A基因克隆与功能分析

为研究mTOR信号通路在凡纳滨对虾(Litopenaeus vannamei)氨基酸代谢中的调控作用,本研究利用RACE技术首次克隆获得了凡纳滨对虾肌肉组织中eif4e2和eif4e1a基因的全长c DNA序列。eif4e2基因c DNA序列全长1 069 bp,开放阅读框699 bp,编码232个氨基酸;eif4e1a基因c DNA序列全长3579bp,开放阅读框627bp,编码208个氨基酸。氨基酸序列比对和进化分析均证实eIF4E2和eIF4E1A为目前已知的eIF4E家族蛋白的同源蛋白。利用实时荧光定量PCR的方法研究了eif4e2和eif4e1a基因在凡纳滨对虾不同组织中的表达差异以及注射雷帕霉素或氨基酸后肌肉中eif4e2和eif4e1a基因表达量的变化情况,探讨了eif4e2和eif4e1a基因在细胞生长中的调控作用。结果表明,凡纳滨对虾eif4e2和eif4e1a基因在眼柄、肝胰脏、肠道、胃、鳃丝和肌肉等组织中均有表达;其中eif4e2基因在肌肉中的表达量显著高于其他组织(P0.05),eif4e1a基因在肠道和肌肉中都有较高表达量,且在肠道中的表达量显著高于其在肌肉中的表达量(P0.05);注射雷帕霉素后2 h内肌肉中eif4e2和eif4e1a基因表达量都出现显著下降(P0.05);肌肉中eif4e1a基因的表达量在单独注射亮氨酸或精氨酸4 h内均未出现变化,但在同时注射亮氨酸和精氨酸后表达量显著增加(P0.05);肌肉中eif4e2基因在注射亮氨酸、精氨酸及亮氨酸加精氨酸后表达量都明显提高(P0.05),且同时注射亮氨酸和精氨酸后,基因表达变量明显比单独注射亮氨酸或精氨酸后变化量大。本研究从动物分子营养学角度出发,克隆了凡纳滨对虾mTOR信号通路中eif4e2和eif4e1a两个基因,并证明其能够通过mTOR信号通路接收不同氨基酸信号来调控细胞生长,对于深入了解对虾的生长和代谢调控机制、饲料配方的优化以及建立合理的养殖管理模式都具有重要的意义。     

Late Cretaceous arc igneous activity: the Eğrikar Monzogranite example

The geochemical and Sr–Nd–Pb isotope properties, as well as the Laser Ablation Inductively Coupled Plasma and Mass Spectrometry (LA-ICP-MS) U–Pb zircon age, of E?rikar Monzogranite in the eastern Pontides, are primarily investigated in this study with the aim of determining its magma source and geodynamic evolution. The U–Pb zircon age obtained from E?rikar Monzogranite is 78 ± 1.5 Ma, thereby re?ecting the age of monzogranite. The I-type E?rikar Monzogranite comprises quartz, plagioclase (An_35–45), orthoclase, muscovite, and biotite. The geochemical analyses of the E?rikar Monzogranite indicate being medium K calc-alkaline, peraluminous, and resembling magmatic arc granite. The E?rikar Monzogranite is enriched in large ion lithophile elements and light rare earth elements relative to high field strength elements. Chondrite-normalized rare earth element patterns have concave upward shapes (La_N/Yb_N 2.47–8.58) with pronounced negative Eu anomalies (Eu_N/Eu* = 0.29–0.65). Initial εNd_(i) values vary between 1.85 and 2.18 and initial ⁸⁷Sr/⁸⁶Sr values between 0.7048 and 0.7067. Fractionation of plagioclase, hornblende, and apatite played an important role in the evolution of E?rikar Monzogranite. The crystallization temperatures of the melts ranged from 770°C to 919°C based on zircon and apatite saturation temperatures. The geochemical and isotopic data suggest being generated by the partial melting of ma?c lower crustal sources.     

四川盆地高石梯—磨溪地区震旦系灯影组储层特征及主控因素

经过数十年的勘探,勘探家们在四川盆地高石梯—磨溪地区获得了万亿方级的探明储量。为研究高石梯—磨溪地区震旦系(≈埃迪卡拉系)灯影组白云岩储层特征及成藏主控因素,开展了岩芯观察、薄片鉴定、阴极发光分析、物性测试、扫描电镜观察、主微量元素和碳氧同位素分析、包裹体均一温度测试、沉积相带划分、宏观构造对成藏控制作用解析等。结果表明:(1)高石梯—磨溪地区灯影组四段发育优质白云岩储层,包括泥晶藻云岩、砂屑白云岩和晶粒白云岩。(2)灯影组四段优质储集层遭受了桐湾Ⅱ幕的大气淡水岩溶作用和埋藏期热液改造作用,溶蚀孔隙广泛发育,平均孔隙度为4.8%,平均渗透率为0.5×10-3μm2,为"低孔—特低渗"型储层。(3)有利相带、白云石化作用控制了优质储层的发育和分布,多分布于裂陷槽边缘的台缘带内,尤其是藻丘滩相白云岩为研究区的主力产气层;埋藏期的热液白云石化作用改善了其储集物性和孔隙结构,主要证据包括:裂缝和溶蚀孔洞中可见各种热液矿物、溶蚀孔洞和裂缝中充填的鞍状白云石具有典型的雾心亮边结构、氧同位素组成"偏负"、流体包裹体均一温度平均值高达175.7℃、高含Mn和阴极发光下发明亮红光等。该研究成果对拓展古老碳酸盐岩油气勘探具有重要理论意义。     

东营凹陷民丰地区沙四段古水体量化恢复及其地质意义

正近年来,随着深层油气勘探的推进,深部地层研究越发受到重视,东营凹陷中深层沙四段是近年来重点勘探层位。基于ICP-AES元素、C-O同位素等分析表明民丰地区沙四段总体处于干湿交替的沉积环境,期间经历了多次的湖侵-湖退-湖侵的演变过程。沙四上沉积期总体处于局限的强还原-还原环境,沙四下总体处于相对开放的强还原、     

Combining MODIS and AMSR‐E observations to improve MCD43A3 short‐time snow‐covered Albedo estimation

Land surface albedo plays an important role in the radiation budget and global climate models. NASA's Moderate Resolution Imaging Spectroradiometer (MODIS) provide 16‐day albedo product with 500‐m resolution every 8 days (MCD43A3). Some in‐situ albedo measurements were used as the true surface albedo values to validate the MCD43A3 product. As the 16‐day MODIS albedo retrievals do not include snow observations when there is ephemeral snow on the ground surface in a 16‐day period, comparisons between MCD43A3 and 16 day averages of field data do not agree well. Another reason is that the MODIS cannot detect the snow when the area is covered by clouds. The Advanced Microwave Scanning Radiometer for EOS (AMSR‐E) data are not affected by weather conditions and are a good supplement for optical remote sensing in cloudy weather. When the surface is covered by ephemeral snow, the AMSR‐E data can be used as the additional information to retrieve the snow albedo. In this study, we developed an improved method by using the MODIS products and the AMSR‐E snow water equivalent (SWE) product to improve the MCD43A3 short‐time snow‐covered albedo estimation. The MODIS daily snow products MOD10A1 and MYD10A1 both provide snow and cloud information from observations. In our study region, we updated the MODIS daily snow product by combining MOD10A1 and MYD10A1. Then, the product was combined with the AMSR‐E SWE product to generate new daily snow‐cover and SWE products at a spatial resolution of 500 m. New SWE datasets were integrated into the Noah Land Surface Model snow model to calculate the albedo above a snow surface, and these values were then utilized to improve the MODIS 16‐day albedo product. After comparison of the results with in‐situ albedo measurements, we found that the new corrected 16‐day albedo can show the albedo changes during the short snowfall season. For example, from January 25 to March 14, 2007 at the BJ site, the albedo retrieved from snow‐free observations does not indicate the albedo changes affected by snow; the improved albedo conforms well to the in‐situ measurements. The correlation coefficient of the original MODIS albedo and the in‐situ albedo is 0.42 during the ephemeral snow season, but the correlation coefficient of the improved MODIS albedo and the in‐situ albedo is 0.64. It is concluded that the new method is capable of capturing the snow information from AMSR‐E SWE to improve the short‐time snow‐covered albedo estimation. Copyright © 2012 John Wiley & Sons, Ltd.     

Travelling wave convection in a rotating layer

Abstract

Small amplitude two-dimensional Boussinesq convection in a plane layer with stress-free boundaries rotating uniformly about the vertical is studied. A horizontally unbounded layer is modelled by periodic boundary conditions. When the centrifugal force is balanced by an appropriate pressure gradient the resulting equations are translation invariant, and overstable convection can take the form of travelling waves. In the Prandtl number regime 0.53 < [sgrave] < 0.68 such solutions are preferred over the more usual standing waves. For [sgrave] < 0.53, travelling waves are stable provided the Taylor number is sufficiently large.