省级连续运行卫星定位服务系统的运行测试

对福建省连续运行卫星定位服务系统(FJCORS)进行介绍,阐述FJCORS系统测试的内容及其方法,并对系统测试数据处理中遇到的相关问题进行详细分析,获得FJCORS系统测试的结果。     

联合实、复相关函数的干涉SAR图像配准方法

SAR复图像配准是干涉SAR数据处理中的关键步骤之一,配准精度直接影响后续产品的质量。提出一种基于联合实、复相关函数的星载干涉SAR图像配准方法。首先,在分析已有配准测度函数各自特性的基础上,结合国际上干涉SAR数据处理经验,认为在全球干涉测量任务背景下,相关函数是一种稳健、普适性的干涉SAR图像配准测度函数。然后,针对相关函数存在实、复相关计算,分析实、复相关函数各自的特点以及适应情况,提出配准灵敏度准则,从而能够有效地自适应地选取相应的配准相关度量。最后,给出配准算法的详细实现步骤。复杂地区的实测数据处理结果验证了方法的有效性。     

融合SFM先验信息的城市三维线段重建算法

针对城市场景中大量存在的边线结构特征,该文提出了一种融合SFM先验信息的城市三维线段重建算法.该文算法首先在影像金字塔中构建精简的二维线段集;然后将相机位姿及稀疏点等数据作为先验信息,引入极线约束、方向约束和深度约束构建匹配线对;最后根据匹配线对重建出三维线段集.实验结果表明,该文提出的三维线段重建算法,在保持场景完整性的同时,能够有效地减少线段误匹配和重建结果冗余,缩短重建时间,提高三维线段重建结果精度.     

北秦岭宽坪岩群变质沉积岩年代学及地质意义

宽坪岩群位于北秦岭造山带,主要由广东坪岩组斜长角闪岩、四岔口岩组云母石英片岩及谢湾岩组的大理岩组成。通过LA-MC-ICPMS锆石U-Pb测年研究,宽坪岩群谢湾岩组碎屑锆石年龄为400~3502 Ma,其中最年轻一组的²⁰⁶Pb/²³⁸U年龄在380~418 Ma,结合黑云母⁴⁰Ar/³⁹Ar（370.9±2.0）Ma的变质年龄,表明谢湾岩组形成在晚泥盆世。四岔口岩组碎屑锆石年龄介于512~3598 Ma,最年轻的一组锆石²⁰⁶Pb/²³⁸U年龄在512~549 Ma,其黑云母⁴⁰Ar/³⁹Ar变质年龄为（370.4±1.8）Ma,表明该组形成于512 Ma（早寒武世）之后,晚泥盆世之前,主体很可能形成于早古生代。宽坪岩群是由不同时代的地层和岩片构成,应该进一步解体。宽坪岩群物源来自华北陆块、秦岭造山带和扬子陆块。其变形变质时代为晚泥盆世,代表了北秦岭造山带碰撞造山的结束时代。     

红河(元江)流域的典型鱼类游泳能力探究及在过鱼设施流速设计中的应用

为探讨红河（元江）流域的典型洄游鱼类游泳能力,给过鱼设施修建设计和鱼类行为学研究提供基础参数,本研究以该流域的野生暗色唇鲮（Semilabeo obscurus）、华南鲤（Cyprinus carpio rubrofuscus）和红魾（Bagarius rutilus）3种鱼类（体长范围0.05~0.45 m）为研究对象,在野外现场布置游泳能力测试水槽分别测试了感应流速、临界游泳速度和突进游泳速度.研究结果表明：（1）对比绝对游泳能力与体长相关性,3种鱼的相对游泳能力与体长的相关性更高,均呈显著负相关;（2）3种鱼之间的游泳能力存在差异,红魾的感应流速最大,为（0.10±0.01）m/s,华南鲤的临界游泳速度最大,为（0.66±0.01）m/s,华南鲤的突进游泳速度最大,为（1.48±0.18）m/s;（3）拟合趋流率与水流速度的相关曲线,所有测试鱼的趋流率与流速的函数关系为Pre=19.80V-1.13（R²=0.96,P<0.05）,得出95%目标鱼的趋流速度为0.11 m/s;利用生存分析方法,得出95%目标鱼累积疲劳的临界和突进游泳速度分别为0.58、1.01 m/s.（4）当以暗色唇鲮、华南鲤和红魾为主要过鱼对象时,建议过鱼设施的内部流速不应小于0.1 m/s,入口的设计流速范围为0.6~1.0 m/s,休息区域的流速范围为0.1~0.6 m/s,孔口或竖缝等高流速区的设计流速不宜超过0.8 m/s,若过鱼设施孔口边壁或底部加糙,可适当增至0.8~1.0 m/s.本研究中红河（元江）流域鱼类游泳能力等资料为过鱼设施修建及珍稀鱼类保护提供了数据支撑.     

风沙流中风速廓线的数值模拟与实验验证

如何描述风沙流中被风沙运动改变了的风速廓线是风沙相互作用研究中的关键问题之一.该文中将跃移风沙流视为一种颗粒拟流体,将跃移颗粒对气流产生的阻力用颗粒流的阻力系数来表达,建立了描写两场相互作用的数学模型.颗粒流的阻力系数采用了前人在液态流化床研究中得出的阻力系数表达形式,通过引入一个修正系数,使其适用于风沙流(气-固两相流).将风沙边界层划分为跃移颗粒所产生的阻力不可忽略的内边界层和跃移颗粒阻力可以忽略但受内边界层影响的外边界层,分别建立了内边界层和外边界层的风速廓线表达式.应用所建立的数学模型,根据由风洞实验测定的跃移风沙流的浓度分布和速度分布资料,计算了跃移风沙流中的风速廓线,并与风洞实测结果进行了对比.结果表明,计算风速廓线与实测风速廓线吻合得比较好,在半对数图上均为上凸的曲线,有别于无风沙运动时的直线.跃移边界层外风速分布可较好地用对数函数来描述.对风沙流中风速廓线的进一步分析证实了风沙物理学奠基人Bagnold在其早期观测风沙流中的风速廓线时提出的"结点现象"(Bagnold结),该结点的高度随风速的增大而升高,随颗粒粒径的增大而降低.根据数值模拟和模拟实验,可以认为有风沙运动的动床剪切风速是综合反映风场与跃移层以及地表之间相互作用的物理量.     

我国8个水电站15种过鱼对象游泳能力研究

近几年我国水电站过鱼设施设计已将过鱼对象游泳能力作为重要参考.以我国8个水电站主要过鱼对象为研究目标,在野外实验设施条件下测试了15种鱼(四大家鱼组、裂腹鱼组和鳅组)的感应流速和爆发游泳速度.采用多元线性回归法分别分析了各组鱼体长及水温对游泳能力的影响,并构建了优化的游泳能力预测模型.结果表明,四大家鱼组、裂腹鱼组和鳅组的感应流速和爆发游速皆与体长呈负相关,感应流速与水温也皆呈负相关关系.水温升高使四大家鱼组和裂腹鱼组的爆发游速能力增强,而水温对鳅组鱼的爆发游速影响不大,可能与鳅科鱼类特殊的腹部吸附行为有关.利用绘制的鱼感应水流和爆发未疲劳的数量百分比的生存曲线进行上行及下行过鱼设施流速设计.结果表明:当鱼感应水流的数量百分比为90%时,四大家鱼、裂腹鱼和鳅组幼鱼感应流速分别为3.00、1.67和3.22 BL/s,裂腹鱼和鳅组成鱼感应流速分别为1.27和2.09 BL/s;当鱼爆发未疲劳的数量百分比为90%时,四大家鱼、裂腹鱼和鳅组幼鱼爆发游泳速度分别为8.13、9.27和9.61 BL/s,裂腹鱼和鳅组成鱼爆发游泳速度分别为7.64和7.77 BL/s.当以裂腹鱼或鳅成鱼为主要过鱼...     

A New Intergrowth Consisting of FeO and SiO_2 Phases from Lower Mantle

1. IntroductionIn order to confirm the presence or absence of diamonds in the Luobusa ophiolitic chromitite in Tibet, about 1500 kg chromitite sample was collected for separating its associated minerals, in which diamond, moissanite, octahedral pseudomorphic serpentine and chlorite, native silicon, native chromium, some alloys and other minerals were found. A wide variety of minerals, including about 70-80 types of mantle minerals from the Luobusa ophiolite, were identified by energy dispersi…     

Unusual Mantle Mineral Group from Chromitite Orebody Cr-11 in Luobusa Ophiolite of Yarlung-Zangbo Suture Zone, Tibet

A wide variety of unusual mantle has been reported from podiform chromitite orebodies Cr-31 and Cr-74 in the Luobusa (罗布莎) ophiolite, Tibet. A detailed investigation of chromitite ore-body Cr-11, located in the Kangjinla (康金拉) district at the eastern end of the ophiolite, has revealed many of the same minerals, including diamond, moissanite, and some native elements, alloys, oxides, sulphides, silicates, carbonates, and tungstates. This orebody is particularly rich in diamonds, with over 1 000 grains recovered from about 1 100 kg sample of chromitite. More detailed studies and experi-ments are needed to understand the origin and significance of these unusual minerals because they have not been found in situ. It is a great breakthrough in mineralogical research that we have picked up more than 40 kinds of minerals from the Kangjinla chromite deposit in Luobusa. It is notable that a large amount of diamonds were firstly discovered from the Kangjinla chromite deposit as well as many other unusual minerals, such as moissanites, rutiles, native irons, and metal alloys. Especially, that diamond was found again in different chromitites In the same ophiolite belt provided new key evidence for discussing the origin of the diamond and the hosted ehromitite and ophiolite. The mantle mineral group in Tibet has great significance in mineralogy and geodynamics.     

Factors Affecting UV/H2O2 Oxidation of 17α‐Ethynyestradiol in Water

In this study, bench‐scale experiments were conducted to examine the UV/H₂O₂ oxidation of 17α‐ethynyestradiol (EE2) in water in a batch operation mode. The EE2 degradation exhibited pseudo‐first‐order kinetics, and the removal was ascribed to the production of hydroxyl radicals (^?OH) by the UV/H₂O₂ system. Typically, the EE2 oxidation rate increased with increasing UV intensity and H₂O₂ dose, and with deceasing initial EE2 levels and solution pH. At EE2₀ = 650 µg/L, UV intensity = 154 µW/cm², H₂O₂ = 5 mg/L, and neutral pH, the UV/H₂O₂ treatment was able to remove 90% of the EE2 content within 30 min. Four anions commonly present in water were found to inhibit EE2 degradation to varying degrees: > > Cl^? > . Our results demonstrate that the described UV/H₂O₂ process is an effective method to control EE2 pollution in water.