鸭绿江口主汊道常量元素沉积记录的特征及其意义          下载免费PDF全文

刘月  程岩  李红军  李富祥 《海洋科学》2022,46(3):36-47

本文依据鸭绿江口主汊道采集的K1和K12柱状样,进行了常量元素的富集特征、相关系数、主成分分析及含量与特征参数垂向分布的讨论。研究表明:鸭绿江口属于涨潮三角洲,纳潮海湾泥质堆积区快速沉积的时间始于1960年。主汊道的沉积物具有多源性,K12柱状样受粒度控制显著,陆源碎屑为主;K1柱状样受粒度控制不显著,受海洋作用的影响较大。主汊道的沉积记录以1978年为界,分为上下2个沉积单元。主汊道的沉积物受到河口区水动力的强烈改造,与物源区的沉积物相比已经产生了很多的分异和变化。该研究通过对鸭绿江口主汊道常量元素沉积记录的分析,发现了近百年来该区域地貌演变和发育的规律,有效补充了鸭绿江口新生陆地形成过程的全貌。  相似文献   

充液井孔中的相控线阵声波辐射器在地层中产生的声场   总被引：17，自引：4，他引：13       下载免费PDF全文

车小花  乔文孝 《地球物理学报》2004,47(4):731-736

应用有限元法研究了充液井孔中的相控线阵声波辐射器在井外地层中产生的声场,探讨了增强声源向地层的某一特定方向辐射的声波能量的方法. 采用相控线阵声波辐射器并调节其参数可以控制由充液井孔向地层中辐射的声波能量的方向,使声源向地层中的某个特定方向辐射的纵波能量得到明显提高. 在井间地震勘探和反射声波成像测井等领域中应用相控线阵声波辐射器,将有利于增大探测深度、提高探测分辨率和接收信号的信噪比.  相似文献   

末次冰期贵州七星洞石笋高分辨率气候记录与Heinrich事件   总被引：8，自引：0，他引：8  

张美良  程海  袁道先  林玉石  覃嘉铭  章程 《地球学报》2004,25(3):337-344

通过对贵州都匀七星洞Q4、Q6石笋进行高精度的TIMS-U系测年和氧同位素分析,建立了末次冰期60．5kaB P以来都匀凯酉地区高分辨率的古气候变化时间序列。通过与格陵兰GISP2冰心的δ^18O曲线对比分析,初步揭示并探讨了末次冰期以来反映的短时间尺度气候快速变化的D-O旋回事件1-18和Heinrich事件H1～H5在黔南七星洞中的石笋记录,并对冷事件发生的年代给出了界定。研究表明,黔南60．5kaB P以来石笋记录冷暖事件所反映出的古季风环流变化,明显受北大西洋气候振荡的影响,显示与北极地区存在着古  相似文献   

城市地质调查中第四纪地质钻探精细化编录工作方法——以济南市新旧动能转换先行区城市地质调查为例          下载免费PDF全文

王玮  朱恒华  刘柏含  徐建国  刘治政  徐华  刘中业 《山东国土资源》2021,37(12)

查清第四系结构是覆盖区城市地质调查工作的重要任务,而钻探是获取第一手资料的重要手段,在地质编录时应做到尽可能详尽、准确。城市地质调查工作往往为城市工程建设服务,编录不仅要满足第四纪地质研究的需求,还要满足工程地质方面的要求。本文结合济南市新旧动能转换先行区城市地质调查项目第四系编录经验,对第四系和工程地质岩性描述方法、野外岩心照片拍摄和室内色彩校正处理的方法进行了总结,为城市地质调查中钻孔编录工作提供参考。  相似文献   

中国鲉形目棘鲬属一新纪录种——丝鳍棘鲬     

阎珂鸣  林坤  陈春亮  侯刚  王学锋 《广东海洋大学学报》2021,(1)

【目的】记述中国南海海域棘鲬属的一新纪录种,以厘定中国南海海域棘鲬属的分类。【方法】2019年4月于中国南海北部海域海南岛东南渔场采集棘鲬属样品,采用形态学鉴定方法研究其形态特征,描述其生态习性,编制中国棘鲬属分种检索表。【结果与结论】样品中有6尾为中国新纪录种——丝鳍棘鲬Hoplichthys filamentosus Matsubara&Ochiai,1950。主要特征:体延长,平扁,向后渐狭小,背缘低平,腹缘平直;背鳍VI,14~15;臀鳍17;胸鳍13+ⅲ;腹鳍Ⅰ-5;尾鳍17;侧线骨板27;鳃耙2+11~12;体具几条不明显深色横带;胸鳍具黑色斑点;第1背鳍分布黄色斑点,具黑色小点和黑边;第2背鳍中部分布黄色圆斑,每1鳍条根部具黄色圆斑;腹鳍白色,无斑纹;臀鳍无明显斑纹;尾鳍后缘具黑边,中部较随机分布黄色圆斑,下叶颜色较深。该种雌雄异形:1)雄性下颌骨腹外侧具棘,雌性则隐没皮下;2)雄性第2背鳍鳍条均显著延长呈丝状,雌性则无显著延长。  相似文献   

Isolating mesoscale coupled ocean–atmosphere interactions in the Kuroshio Extension region     

《Dynamics of Atmospheres and Oceans》2013

The Kuroshio Extension region is characterized by energetic oceanic mesoscale and frontal variability that alters the air–sea fluxes that can influence large-scale climate variability in the North Pacific. We investigate this mesoscale air-sea coupling using a regional eddy-resolving coupled ocean–atmosphere (OA) model that downscales the observed large-scale climate variability from 2001 to 2007. The model simulates many aspects of the observed seasonal cycle of OA coupling strength for both momentum and turbulent heat fluxes. We introduce a new modeling approach to study the scale-dependence of two well-known mechanisms for the surface wind response to mesoscale sea surface temperatures (SSTs), namely, the ‘vertical mixing mechanism’ (VMM) and the ‘pressure adjustment mechanism’ (PAM). We compare the fully coupled model to the same model with an online, 2-D spatial smoother applied to remove the mesoscale SST field felt by the atmosphere. Both VMM and PAM are found to be active during the strong wintertime peak seen in the coupling strength in both the model and observations. For VMM, large-scale SST gradients surprisingly generate coupling between downwind SST gradient and wind stress divergence that is often stronger than the coupling on the mesoscale, indicating their joint importance in OA interaction in this region. In contrast, VMM coupling between crosswind SST gradient and wind stress curl occurs only on the mesoscale, and not over large-scale SST gradients, indicating the essential role of the ocean mesocale. For PAM, the model results indicate that coupling between the Laplacian of sea level pressure and surface wind convergence occurs for both mesoscale and large-scale processes, but inclusion of the mesoscale roughly doubles the coupling strength. Coupling between latent heat flux and SST is found to be significant throughout the entire seasonal cycle in both fully coupled mode and large-scale coupled mode, with peak coupling during winter months. The atmospheric response to the oceanic mesoscale SST is also studied by comparing the fully coupled run to an uncoupled atmospheric model forced with smoothed SST prescribed from the coupled run. Precipitation anomalies are found to be forced by surface wind convergence patterns that are driven by mesoscale SST gradients, indicating the importance of the ocean forcing the atmosphere at this scale.  相似文献   

基于RPC模型的线阵卫星影像核线排列及其几何关系重建     

张过  潘红播  江万寿  秦绪文 《国土资源遥感》2010,(4)

针对核线影像无几何模型的问题,提出基于有理多项式系数(Rational Polynomial Coefficient,RPC)模型,利用投影轨迹法制作线阵推扫式卫星核线影像及其几何模型的重建方法。利用SPOT 5 HRG、CBERS 2-03异轨立体像对和SPOT 5 HRSI、RS P5、GeoEyeI、KONOS同轨立体像对重建的核线影像几何模型上下视差的中误差在0.2个像元之内;利用重建几何模型和原始影像几何模型进行前方交会计算所得到的地面点平面中误差在1 m之内,高程中误差在0.3 m之内,验证了本文方法的可靠性。  相似文献   

Tight integration of GPS observations and persistent scatterer InSAR for detecting vertical ground motion in Hong Kong     

Qiang Chen  Guoxiang Liu  Xiaoli Ding  Jyr-Ching Hu  Linguo Yuan  Ping Zhong  M. Omura 《International Journal of Applied Earth Observation and Geoinformation》2010

A method for tightly integrating GPS observations and the persistent scatterer (PS) interferometric synthetic aperture radar (InSAR) is proposed to detect vertical ground motion in Hong Kong, China. The tropospheric zenith wet delays (ZWD) derived from GPS observations at sites in the SAR scenes are used first to model and correct for the tropospheric effects in the interferograms generated from the SAR images. The vertical motion rates (VMR) of the GPS sites determined based on the continuous GPS observations obtained at the sites are then used as constraints in the PS InSAR solutions to further enhance the quality of the solutions. Data from 12 continuous tracking GPS sites in Hong Kong and 8 ENVISAT ASAR images acquired during 2006–2007 are used to demonstrate the application of the proposed method. The results from the example show that the method is capable of detecting accurately the vertical ground motion.  相似文献   

有理函数模型下基础矩阵研究     

叶新魁  ;文贡坚  ;王继阳  ;回丙伟 《测绘信息与工程》2009,34(5):36-38

分析了线阵影像的核线关系,提出了有理函数模型下线阵扫描影像的基础矩阵求解方法,验证了线阵影像中精确共轭核线对是不存在的。  相似文献   

Vertical distribution of primary producers and zooplankton grazers during different phases of the Arctic spring bloom     

Fredrika Norrbin  Hans Chr. Eilertsen  Maria Degerlund 《Deep Sea Research Part II: Topical Studies in Oceanography》2009,56(21-22):1945

During a circumnavigation of the Svalbard archipelago in May 2006, simultaneous marine environmental (meteorology, heat flux, ocean turbulence, irradiance) and biological (phytoplankton and zooplankton biomass/species) data were sampled at selected stations. The zooplankton data were supplemented by high-resolution, high-speed VPR sampling down to 100 m depth at most stations. We were able to sample different phases of the phytoplankton spring bloom in Arctic as well as in Atlantic waters, and the stations represented different situations with respect to irradiance, turbulence and water-column stability. Phytoplankton growth and depth distribution were physically controlled, while zooplankton distributions were affected by biological parameters and turbulence. Development of the zooplankton followed the phytoplankton bloom phase, which was progressing in a direction from west to east in the waters north of Svalbard, and southwards in the Barents Sea. Our results also showed that the zooplankton did not avoid Phaeocystis pouchetii colonies, which have earlier been described as toxic. Despite an early retreat of the ice this year there was no apparent mismatch between the phytoplankton bloom and the dominant mesozooplankton, Calanus spp.  相似文献