江西省山地风场风速订正方法研究          下载免费PDF全文

吴琼  桂保玉  徐卫民 《气象与环境科学》2019,42(1):47-53

利用气象站、探空及NASA再分析资料,对江西省4县山地风场的12座测风塔风速进行订正研究。研究结果表明:测风塔与气象站风速数据相关性较低,相关系数一般远小于0.45;测风塔与探空资料的风速相关系数可达到0.6以上,最高可达到0.8;NASA再分析资料可以作为江西山地风场风速订正参证数据,其与测风塔风速数据相关性较高,相关系数可达到0.54～0.77,大多数测风塔相关系数可达0.7左右。海拔高度小于1000 m的测风塔与NASA 50 m风速的相关系数明显高于其与NASA 850 hPa风速的相关系数,高度为1000—1200 m的测风塔与NASA 50 m风速和与NASA 850 hPa风速的相关系数相差不明显,高度大于1200 m的测风塔与NASA 850 hPa风速的相关系数明显大于其与NASA 50 m风速的相关系数。比值法订正效果略好于线性回归法的,订正后的风功率密度总体偏大。  相似文献   

关于《中国扬子区兰多维列统特列奇阶及其与英国的对比》一书若干问题的商榷     

林宝玉  李明  黄莫  邓丽婷 《地质论评》2021,67(3):67040025-67040025

《中国扬子区兰多维列统特列奇阶及其与英国的对比》一书（陈旭,戎嘉余,1996）有以下结论：①将回星哨组、茅山组、西坑组等的层位归属于特列奇阶上部;②将回星哨组、茅山组及其相当地层与英国特列奇阶对比;③将扬子区特列奇阶的顶界置于回星哨组、茅山组及其相当地层之顶;④将回星哨组、茅山组、西坑组等地层资料编制的古地理图称为特列奇期晚期古地理图;⑤将回星哨组、茅山组、西坑组等地层与上覆中泥盆统—中二叠统之间的不整合面代表的上升运动,称为“特列奇期的扬子上升”。笔者等依据多年对扬子地台志留纪地层剖面的实地考察和近数十年来扬子区坟头组中—上部、茅山组、回星哨组、小溪峪组、西坑组等地层中文洛克世、拉德洛世、普里多利世早期古生物化石的发现,认为：①回星哨组、小溪峪组、茅山组、西坑组等的层位是文洛克统—普里多利统;② 回星哨组、小溪峪组等大致与英国的文洛克统—普里多利统对比;③回星哨组、小溪峪组、茅山组的顶界是文洛克统—普里多利统剥蚀后残留的层位随地而异的顶界;④根据回星哨组、西坑组、茅山组等地层资料编制的古地理图应是文洛克世—普里多利世古地理图;⑤“扬子地台整个上升”（黄汲清,1945）的时代是志留纪末期,没有“特列奇期的扬子上升”。特提出商榷。上述这些地层时代的解决,对扬子区志留系4统层序的建立具有重要意义,而且也为中国扬子区与英国命名剖面志留系的对比以及中国南方早古生代加里东运动最后一幕时代的再次确定提供了地层学和古生物方面的依据。  相似文献   

Enhanced fault detection and exclusion based on Kalman filter with colored measurement noise and application to RTK     

Gao  Yuting  Gao  Yang  Liu  Baoyu  Jiang  Yang 《GPS Solutions》2021,25(3):1-15

GPS Solutions - The tropospheric delay is an important error source in the Global Positioning System (GPS) positioning and navigation applications. Although most of the tropospheric delays can be...  相似文献   

Stratigraphy of the Triassic?Jurassic Boundary Successions of the Southern Margin of the Junggar Basin, Northwestern China   总被引：2，自引：1，他引：1  

SHA Jingeng  Vivi VAJDA  PAN Yanhong  Linda LARSSON  YAO Xiaogang  ZHANG Xiaolin  WANG Yaqiong  CHENG Xiansheng  JIANG Baoyu  DENG Shenghui  CHEN Siwei  PENG Bo 《《地质学报》英文版》2011,85(2):421-436

The Triassic?Jurassic (Tr?J) boundary marks a major extinction event, which (~200 Ma) resulted in global extinctions of fauna and flora both in the marine and terrestrial realms. There prevail great challenges in determining the exact location of the terrestrial Tr?J boundary, because of endemism of taxa and the scarcity of fossils in terrestrial settings leading to difficulties in linking marine and terrestrial sedimentary successions. Investigation based on palynology and bivalves has been carried out over a 1113 m thick section, which is subdivided into 132 beds, along the Haojiagou valley on the southern margin of the Junggar Basin of the northern Xinjiang, northwestern China. The terrestrial Lower Jurassic is conformably resting on the Upper Triassic strata. The Upper Triassic covers the Huangshanjie Formation overlaid by the Haojiagou Formation, while the Lower Jurassic comprises the Badaowan Formation followed by the Sangonghe Formation. Fifty six pollen and spore taxa and one algal taxon were identified from the sediments. Based on the key-species and abundance of spores and pollen, three zones were erected: the Late Triassic (Rhaetian) Aratrisporites?Alisporites Assemblage, the Early Jurassic (Hettangian) Perinopollenites?Pinuspollenites Assemblage, and the Sinemurian Perinopollenites?Cycadopites Assemblage. The Tr?J boundary is placed between bed 44 and 45 coincident with the boundary between the Haojiagou and Badaowan formations. Beds with Ferganoconcha (?), Unio?Ferganoconcha and Waagenoperna?Yananoconcha bivalve assemblages are recognized. The Ferganoconcha (?) bed is limited to the upper Haojiagou Formation, Unio?Ferganoconcha and Waagenoperna?Yananoconcha assemblages are present in the middle and upper members of the Badaowan Formation. The sedimentary succession is interpreted as terrestrial with two mainly lake deposit intervals within Haojiagou and Badaowan formations, yielding fresh water algae and bivalves. However, the presence of brackish water algae Tasmanites and the marine?littoral facies bivalve Waagenoperna from the Badaowan Formation indicate that the Junggar Basin was influenced by sea water caused by transgressions from the northern Tethys, during the Sinemurian.  相似文献   

粤东盆地早侏罗世金鸡组物源分析及其对华南构造背景的约束          下载免费PDF全文

刘念  姜宝玉  周雪瑶  周卫明 《高校地质学报》2018,24(1):65

华南早中生代构造背景一直存在争议。粤东盆地位于华南东南缘,记录了华南早中生代构造背景的地质信息。文章 以粤东盆地早侏罗世金鸡组碎屑沉积岩为研究对象,采用锆石U-Pb定年方法,结合岩相学、地球化学和古水流数据,探讨 盆地物源及构造背景。测年结果显示早侏罗世金鸡组样品存在八个峰值：196 Ma、247 Ma、320 Ma、432 Ma、770 Ma、 1060 Ma、1820 Ma和2430 Ma。物源分析表明粤东盆地金鸡组物源主要来自盆地的东北侧和北侧两个方向。粤东盆地碎屑 锆石与位于盆地东北侧的永安盆地和北侧的东坑盆地的物源特征相似,反映出早侏罗世中国东南部盆地尽管还是以稳定的 克拉通边缘盆地为特征,但古太平洋板块向华南板块更东侧的俯冲已经开始为中国东南缘盆地提供物源。  相似文献   

Identification of two Skeletonema costatum-like diatoms by fluorescence in situ hybridization     

张宝玉  陈国福  王广策  陆斗定 《中国海洋湖沼学报》2010,28(2):310-314

A harmful algae bloom (HAB) is a dense aggregation of algae in a marine or aquatic environment that can result in significant environmental problems. To forecast the occurrence of HAB, development of a rapid and precise detection method is urgently required. In this study, two Skeletonema costatum-like diatoms (SK-1 and SK-2), were identified morphologically under a light microscope, and detected using fluorescent in situ hybridization (FISH). Strain SK-1 was isolated from a frequently HAB affected area of the East China Sea, and strain SK-2 from an aquatic farm in Qingdao, China. Fluorescent DNA probes were designed that were complementary to the ITS sequence (including 5.8S rDNA) of strain SK-1. After hybridization, strong green fluorescence was observed in cells of strain SK-1 under an epifluorescence microscope; however, no such fluorescence was observed with strain SK-2, which indicates that probes hybridized only the DNA of the target strain, SK-1, in species-specific manner, and that the two strains do not belong to a same species. This finding was confirmed by ITS sequence analysis. The FISH technique used in this study was sensitive, simple, and rapid, and is a promising tool for detecting target HAB species in natural environments.  相似文献   

河南省区域经济、金融空间结构变化对比分析     

彭宝玉  张敏  郭扬 《地域研究与开发》2012,31(5)

基于泰尔指数和GIS地图分析技术,对河南区域经济和区域金融空间结构变化做对比分析.结果表明:金融业的空间集聚度远大于一般产业,在强大的金融集聚经济作用下,区域经济发展与区域金融发展会表现出显著差异.2000年以来,河南省辖市市区经济实力相对下降,而金融集聚功能上升;县域经济显著发展,而金融发展普遍滞后,郑州市日益成为全省金融服务业的集聚地.金融空间流动带来现代城市的快速成长、功能彰显和激烈竞争,而此种努力的结果往往会抑制一些区域的金融发展,特别是县域和农村地区,需要统筹区域金融中心和乡村普惠金融建设.  相似文献   

无人飞艇低空航测系统自动建模技术研究     

潘宝玉  刘同文  苏国中  张兰 《测绘通报》2015,(4):75-77,85

探讨了基于无人飞艇载四组合宽角相机低空航测系统的城市三维自动建模技术,实现了一次飞行同时获取城市建筑物4个侧面和顶面的纹理图像,依据组合宽角影像自动提取建筑物高度信息和自动选择最佳纹理图像,基本达到了城市三维建模过程的自动化,大幅度提升了城市三维建模的效率,为智慧城市建设提供了一种全新的技术途径.  相似文献   

煤炭开采对煤层底板变形破坏及渗透性的影响     

孟召平  王保玉  徐良伟  吴志远  白刚  路波涛 《煤田地质与勘探》2012,40(2):39-43

煤层底板变形破坏除受地质因素控制外,还受开采因素影响。通过试验和理论分析,系统研究了煤炭开采对回采工作面底板应力、应变和破坏及渗透性的影响。研究结果表明,不同岩性岩石的渗透性在全应力-应变过程中为应变的函数,在微裂隙闭合和弹性变形阶段,岩石的原生孔隙和裂隙容易被压密,岩石的渗透率随应力的增加由大变小明显,当应力增大至极限强度时岩石试件破坏形成贯穿裂隙,岩石的渗透率迅速增大至最大,不同岩性岩石存在一定差异性;随着回采工作面推进,煤层底板岩层在横向上划分为原岩应力区、超前压力压缩区、采动矿压直接破坏区和底板岩体应力恢复区4个区。煤层底板岩体的渗透性随着煤炭开采底板岩体变形破坏而呈规律性变化。   相似文献   

中国流动人口多阶段流动的空间格局及变动特征——基于初次流动和当前流动的对比     

林洁  柯文前  林李月  朱宇  肖宝玉 《热带地理》2022,42(5):824-833

基于2017年全国流动人口动态监测数据,运用描述统计和社区发现等方法,研究流动人口在初次流动和当前流动的空间格局及其变动特征。结果发现：1）从区域差异看,流动人口初次流动和当前流动的流出地格局保持相对稳定,流入地格局的变化主要体现在：在当前流动阶段,流入中部地区的比例下降而西部地区比例上升;流入特大城市的比例明显下降而I型大城市、中等城市和I型小城市的比例上升;流向直辖市和计划单列市的比例上升而流向副省级和省会城市的比例下降。2）从行政地级市间净迁移格局看,流动人口初次和当前流动的净迁移格局稳定性强,净迁入地区以“块状”分布于东部沿海省份的发达地市和“点状”分布于中西部省会及部分资源型和口岸型地市,净迁出地区连片分布在中西部地区的大多数地市与沿海省份的内陆地市。3）流动人口初次和当前流动以就近迁移与远程迁移交织的流迁模式为主,且由此刻画的行政地级市间迁移网络格局呈现以“胡焕庸线”为界的“东密西疏”现象;但也出现在当前流动阶段迁往京津冀的迁移流规模降低,长三角取代珠三角成为流入地首选区域的特征。4）流动人口生计策略的稳定性与人口迁移流动的空间惯性,是流动人口初次和当前流动空间格局表现出相似性的主要原因,而产业结构转型升级及在不同地市间的梯度转移是促使流动人口在流入地选择上发生变化的重要力量。  相似文献