吕宋海峡M2内潮生成与传播数值模拟研究     

李欢  陈学恩  宋丹 《中国海洋大学学报(自然科学版)》2011,41(1)

本文在z坐标海洋数值模式HAMSOM中引入了内潮黏性项(Interhal-tide viscosity term),将之运用到吕宋海峡M2内潮的生成与传播过程的数值模拟研究.研究结果表明:(1)在250 m以浅,吕宋海峡产生的M2内潮振幅于温跃层处最大,岛坡附近的内潮明显强于别处,且最大振幅可达到40 m左右;(2)M2内潮的生成源主要集中在伊特巴亚岛西北、巴丹岛西南以及巴布延群岛西北的岛坡;(3)海峡产生的M2内潮向东西2个方向传播.巴丹岛以西的西向能量在吕宋海沟斜向下传播,在到达恒春海脊附近发生反射返回海面,到达海面后再次反射回海底,在此过程中,有高模态的内潮被激发,不同模态间有相消干涉的现象产生.西传的内潮能量分为2支进入南海,产生于巴布延群岛西北的能量分支直接向西南折转进入南海海盆,而产生于伊特巴亚岛和巴丹岛岛坡附近的主要能量则以束状向南海陆架传播,在到达118°E后部分能量折向西南的海盆,其余的能量则沿西北方向传入中国近岸,陆架陆坡地形起着重要的耗散作用.伊特巴亚岛西北有最大的能量产生,向东北传入太平洋.在122°E以东,能量主要以束状向东南传入太平洋.  相似文献   

内蒙古乌拉特后旗潮海地区元素地球化学分布特征及金成矿远景预测     

程新彬 《地质与勘探》2015,51(4):713-721

内蒙古乌拉特后旗潮海地区具有较好的成矿前景,在潮海地区通过开展区域1∶5万地球化学测量及重点工作区1∶1万地球化学测量与成矿元素的空间分布特征研究,认为该区寻找Au及多金属矿的潜力较大。通过元素异常特征及传统地质大比例尺填图的综合方法,发现该区Au矿化可能与二长花岗岩区内部的石英脉及寒武系变质岩系密切相关,区内深大断裂亦为其控矿因素。依据元素区域地球化学异常特征,并结合区域大比例尺地质测量、地球物理特征划分出了乌兰敖包和萨音呼都格两个Au成矿远景区。  相似文献   

半水磷石膏的矿物学特征     

杨林  曹建新  刘亚明 《岩石矿物学杂志》2015,34(6):827-834

讨论了半水磷石膏的化学组成、矿物组成、热性能、微观形貌以及胶凝性能。结果表明:半水磷石膏中主要化学组成为CaO和SO3,其总量达到70%,含有少量的结晶水和P2O5;半水磷石膏中含有放射性元素,但未超过GB/T6566-2010《建筑材料放射性核素限量》的限值;半水磷石膏矿物组成主要是α型的烧石膏相,但其放热峰面积小,主要以不同取向的硫酸钙晶体的聚晶形式存在,胶凝性能差,烘干强度仅为0.38 MPa。半水磷石膏与二水石膏制备的α型半水石膏在微观形貌上存在较大差异,将其直接应用于建筑材料还有待于进一步研究。  相似文献   

半数字化地形测图实习方案的探讨     

余代俊  郑平元  杨容浩  黄强 《测绘科学》2015,(8)

针对传统地形测图方法效率低下的问题,该文提出半数字化地形测图的实习教改方案。选择在模拟地形测图与数字地形测图之间折中,即采用数字化测绘仪器,但仍采用模拟测图的数据采集方案。观测数据不记录在仪器存储卡中,而是记录在观测手簿。为提高绘图时展点速度,提出改传统极坐标展点为直角坐标展点,并研制了一套直角展点尺和展点新方法。新展点尺根据坐标50m的余数快速展点,并在展点尺的右上角留有1/4圆弧,可提高展点精度。试验结果显示,直角坐标展点比传统极坐标展点在精度和速度上均有优势。  相似文献   

GPS-RTK无验潮测深精度影响因素分析   总被引：1，自引：0，他引：1  

刘文勇  郑晖 《测绘科学》2015,(11):7-12

针对目前GPS-RTK联合单波束无验潮测深虽然从理论上消除了潮位模型误差的影响,但未顾及测量船受风浪、海流、潮汐等作用引起的姿态影响、GPS与测深仪信号不同步的影响、测深仪信号延迟和水中声速变化的影响等问题,为了提高海洋测深成果的精度,文章在分析这些影响因素产生机理的基础上,结合当前常用的外业作业设备,仿真模拟了各种测深作业状况,并分别定量计算了各种状况下上述因素引起的定位和测深误差,然后依据分析计算结果,给出了相应的解决办法,可为测深外业作业人员区分误差量级,进而优化作业方案提供参考。  相似文献   

地下水中12种半挥发性有机物的测定     

范艳春  李诚  仝永霞  任云芳 《华北国土资源》2015,(3):69-70,79

利用正己烷液-液萃取提取地下水中的12种半挥发性有机物,提取液经旋转蒸发浓缩、氮吹浓缩,采用气相色谱（ECD检测器）测定11种有机氯组分;乙腈换相后,采用高效液相色谱法（荧光和二极管阵列检测器串联）测定苯并（a）芘。优化了上机条件以及样品前处理等条件,建立了分析方法。在较佳的实验条件下,方法检出限为0.68ng/L~1.60ng/L;方法精密度为3.01%~7.53%;样品加标回收率为80.1%~103%。  相似文献   

黄海在有无潮作用下对“布拉万”不同响应的数值模拟研究   总被引：2，自引：0，他引：2  

孟庆军  李培良 《海洋与湖沼》2015,46(6):1241-1254

黄海是典型的强潮驱动的陆架浅海。为了研究黄海对台风的响应特点,本文利用区域海洋模式(Regional Ocean Modeling Systems,ROMS)分别模拟了在有潮和无潮作用下黄海对台风"布拉万"的响应过程。结果表明,不管潮存在与否,"布拉万"经过黄海后都引起了海表面降温和流速的近惯性振荡响应,这种响应主要分布于黄海中部较深区域,带通滤波提取的近惯性流速具有垂向第一模态特征。同时,研究发现强背景潮流能显著地影响黄海对"布拉万"的响应过程。主要结论如下:一方面,由于潮的存在,近岸垂向混合均匀的较暖水体与远岸较冷水体之间会形成潮混合温度锋面,"布拉万"过后,暖水发生了明显的离岸扩张,尽管路径右侧的混合层降温更显著,但是左侧即黄海西岸的暖水扩张更明显;另一方面,潮的存在减弱了布拉万产生的近惯性振荡响应,半日潮流在黄海仍然占据主导地位。在混合层中潮流的作用减弱了"布拉万"产生的近惯性能量,但也使其更易穿过跃层传入黄海内部。  相似文献   

应用实时定量PCR技术检测秦皇岛近岸海域褐潮原因种——抑食金球藻(Aureococcus anophagefferens)     

GUO Hao  LIU Yongjian  ZHANG Qi  YUAN Xiutang  ZHANG Weiwei  ZHANG Zhifeng 《海洋学报(英文版)》2015,34(2):132-136

Aureococcus anophagefferens, a small pelagophyte algae, has caused brown tide blooms in coastal waters of Qinhuangdao in recent years, presenting significant negative impacts on the shellfish mariculture industry. Under standard light microscopy, it is visually indistinguishable from other small algae in field samples due to its extremely small size. In this study, quantitative polymerase chain reaction(q PCR) based on 18 S r DNA sequences was developed and used to detect and enumerate A. anophagefferens. A linear regression(R2 = 0.91) was generated based on cycle thresholds value(Ct) versus known concentrations of A. anophagefferens. Twenty-two field samples collected in coastal waters of Qinhuangdao were subjected to DNA extraction and then analyzed using q PCR. Results showed that A. anophagefferens had a wide distribution in coastal waters along Qinhuangdao. Elevated A. anophagefferens abundance, category 3 brown tide blooms(200 000 cells/m L) occurred at Dongshan Beach and Tiger-stone Beach in August in 2013. In shellfish mariculture areas along coastal waters of Qinhuangdao, 4 stations had category 3 blooms, and 6 stations had category 2 blooms(35 000–200 000 cells/m L) in August and all stations had category 1 blooms(0 to ≤35 000 cells/m L) in October. Quantitative PCR allows for detection of A. anophagefferens cells at low levels in filed samples, which is essential to effective management and prediction of brown tide blooms.  相似文献   

2008年中国沿岸冬季寒潮激发陆架波的小波分析   总被引：1，自引：0，他引：1  

李君益  郑全安  胡建宇  范振华  朱佳  陈涛  朱本璐  徐莹 《海洋学报(英文版)》2015,34(11):22-31

This study applies the wavelet analysis to the tidal gauge records, alongshore winds, atmospheric temperature and pressure along the China coast in winter 2008. The analysis results show three events of sea level oscillations(SLOs) on the shelf induced by winter storms. The first event occurred from January 9 to 21. The SLO periods were double-peaked at 1.6–5.3 and 7.0–16.0 d with the power densities of 0.04–0.05 and 0.10–0.15 m2·d, respectively.The second event occurred from February 5 to 18. The SLO period was single-peaked at 2.3–3.5 d with power density of 0.03–0.04 m2·d. The third event occurred from February 20 to March 8. The SLO periods were doublepeaked at 1.5–4.3 and 6.1–8.2 d with the power densities of 0.08–0.11 and 0.02–0.08 m2·d, respectively. The SLOs propagated along the coast from Zhejiang in north to Guangdong in south. The phase speeds ranged about 9–29m/s from Kanmen to Pingtan, 5–11 m/s from Xiamen to Huizhou and 11–22 m/s from Huizhou to Shuidong. The dispersion relation of the SLOs shows their nature of coastal-trapped wave.  相似文献   

吕宋海峡M₂内潮的三维数值模拟     

李秉天  曹安州  吕咸青 《海洋学报(英文版)》2015,34(11):55-62

A three-dimensional isopycnic-coordinate internal tidal model is employed to investigate the generation,propagation, vertical structure and energy conversion of M2 internal tides in the Luzon Strait(LS) with mooring observations. Simulated results, especially the tidal current amplitudes, agree well with observations,demonstrating the reasonability and accuracy of the model. Results indicate that M2 internal tides mainly propagate into three directions horizontally, i.e., eastward towards the western Pacific Ocean, westward towards the Dongsha Island and southwestward towards the South China Sea Basin. In the horizontal direction, tidal current amplitudes decrease as distance increases away from the LS; in the vertical direction, they show an obvious decreasing tendency with depth. Between the double ridges of the LS, a clockwise gyre of M2 baroclinic energy flux appears, which is caused by reflections of M2 internal tides at supercritical topographies, and resonance of M2 internal tides happens along 19.5° and 21.5°N due to the heights and separation distance of the double ridges. The total energy conversion in the LS is about 14.20 GW.  相似文献