一种基于RTAI实时操作系统的相关跟踪处理机

引入倾斜校正自适应光学技术到月球激光测距中,详细介绍了倾斜校正自适应光学的相关跟踪原理,给出了一种基于实时操作系统RTAI的相关跟踪波前处理机的设计结果.该波前处理机采用绝对差分算法,使用通用CPU,基于Linux硬实时扩展系统BTAI实现对波前的实时处理.实验结果证明,它的相关跟踪处理帧频为1 KHz,并且具有集成度...     

An Emulation Research on the Radio Occultation Exploration of Martian Ionosphere

The technical system of the Sino-Russian joint satellite-to-satellite Mars ionosphere occultation is analyzed and introduced. The analogue computation of the observed values of the radio waves of the ionosphere occultation event is carried out by adopting the three-dimensional ray tracking method and the electron density profile inversion is conducted by means of the simulated occultation observational data, with the result showing that the emulation algorithm is reliable. By taking advantage of the emulation method the case computation and analysis of the inversion errors caused by the observational error of the occultation radio wave phase and the satellite orbital error are respectively carried out, and it is obtained from the result that the effect of the phase measuring error of the 5% circle on the result of the daytime ionosphere occultation exploration may be neglected, while the absolute error of the night electron density measurement is less than 4 × 108 m^?3, and the main effect of the satellite orbital error on the occultation leads to the lifting or falling of the ionospheric height. The result shows that the technical system of the Sino-Russian joint Mars ionosphere occultation exploration is advanced. It can be expected that the high accuracy electron density profile is obtained and the technical system can be applied to the exploration of the lunar ionospheric environment.     

中国硼矿主要矿集区及其资源潜力探讨

在分析中国硼矿床成因类型的基础上,将中国硼矿床划分沉积变质、现代盐湖沉积、矽卡岩和地下卤水4个矿床类型8个矿床式,最为重要的矿床类型为沉积变质型硼矿和现代盐湖型沉积硼矿床。在硼矿成矿区带划分方案的基础上,综合成矿规律、地质构造背景等因素划分出辽-吉沉积变质型、川-鄂地下卤水型、湘-桂矽卡岩型、西藏现代盐湖型和青海柴达木现代盐湖型5个硼矿矿集区。其中辽-吉老矿区深部和外围、川鄂区的地下卤水及盐湖硼矿的综合利用等方向尚有较大潜力。     

鄂西磷矿矿集区地质及其资源远景分析

鄂西磷矿的分布与产状受神农架背斜和黄陵背斜控制,为荆襄式晚震旦世沉积型磷块岩矿床。受浅海台地台坪亚相,磷块岩、泥(页)岩、白云岩含磷建造和水下隆起古构造等控制。晚震旦世陡山沱期磷矿评价标志为:上震旦统陡山沱阶;浅海台地台坪亚相;磷块岩、泥(页)岩、白云岩含磷建造;成矿地段陡山沱阶厚度一般小于200m,最佳150～50m;水下隆起带;磷块岩矿床一般分布在冰碛砾岩为0m的区域;含磷建造等深线一般小于1000m。评价结果表明,荆襄、宜昌、新华、神农架和保康磷矿区的深部及外围具有较好的资源远景,资源潜力大。     

中国温泉之乡巢湖市的地热资源及其开发利用

巢湖市内汤池、半汤、香泉、昭关等四大温泉,水温42—63℃,日出水量达1万m~3,储量丰富,水质优良。近年来,不断提升巢湖市温泉资源的开发利用和保护水平,温泉度假旅游已成为巢湖旅游业的拳头产品。2009年12月,经国土资源部和中国矿业联合会专家评审,巢湖市被命名为中国温泉之乡。     

A new Voronoi diagram-based approach for matching multi-scale road networks

Journal of Geographical Systems - Object matching is a key technology for map conflation, data updating, and data quality assessment. This article proposed a new Voronoi diagram-based approach for...     

中国国家地质公园空间分布及其演化研究

2001年4月至2013年12月,国土资源部正式批准授牌了七批共240处国家地质公园。随着国家地质公园数量的增长,其在空间上呈现出一定的分布结构和演化规律。通过GIS空间分析发现:中国国家地质公园在空间上呈现显著凝聚分布;空间分布不均,具有空间集群分布的特征;分布的高密度地区为1个带状区域和4个块状区域。通过对不同阶段国家地质公园空间分布的分析,发现中国国家地质公园分布重心向北迁移、与区域中心城市的关系日趋紧密。地质构造条件、地质公园的旅游化以及拟建地政府部门认知水平是影响国家地质公园空间分布演化的重要因素。     

Sea surface temperature and salinity reconstruction based on stable isotopes and Mg/Ca of planktonic foraminifera in the western Pacific Warm Pool during the last 155 ka

Changes in sea surface temperature(SST), seawater oxygen isotope(δ 18 O sw), and local salinity proxy(δ 18 O sw-ss) in the past 155 ka were studied using a sediment core(MD06-3052) from the northern edge of the western Pacifi c Warm Pool(WPWP), within the fl ow path of the bifurcation of the North Equatorial Current. Our records reveal a lead-lag relationship between paired Mg/Ca-SST and δ 18 O during Termination II and the last interglacial period. Similarity in SST between our site and the Antarctic temperature proxy and in CO 2 profi le showed a close connection between the WPWP and the Antarctic. Values of δ 18 O sw exhibited very similar variations to those of mean ocean δ 18 O sw, owing to the past sea-level changes on glacial-interglacial timescale. Calculated values of δ 18 O sw-ss refl ect a more saline condition during high local summer insolation(SI) periods. Such correspondence between δ 18 O sw-ss and local SI in the WPWP may refl ect complex interaction between ENSO and monsoon, which was stimulated by changes in solar irradiance and their infl uence on the local hydrologic cycle. This then caused a striking reorganization of atmospheric circulation over the WPWP.     

青海互助一次局地强降水天气多普勒雷达回波分析

利用西宁CINRAD/CD多普勒天气雷达资料及自动站观测数据等从影响降水的主要因子方面探讨了2011年7月2日晚青海互助县一次局地强降水的成因,结果表明:多单体强回波带的活动是造成互助短时强降水的主要原因;速度图上强的辐合和逆风区是预报强降水的关键因子;垂直风廓线图上强烈的垂直风切变是不稳定能量积聚的表现,与强降水联系紧密;垂直累计液态含水量(VIL)和回波顶高也能为强降水预报提供有效信息。     

四川盆地东部垫江盐盆早三叠世嘉陵江组四段杂卤石成因及对成钾的指示

四川盆地三叠纪是主要的成钾期,目前发现的主要含钾矿物为杂卤石,有关早三叠世嘉陵江组四段石盐岩中杂卤石成因一直存在争议.采用薄片鉴定、扫描电镜、稀土元素和锶同位素等手段,分析了四川盆地东部垫江盐盆长寿地区嘉陵江组四段石盐岩中杂卤石矿物形态特征,初步探讨了该杂卤石成因及对寻找海相钾盐的指示意义.扫描电镜下与石盐岩共生的杂卤...