基于子波分析的悬浮物散射信号特征提取实验研究     

张锁平 《海洋技术学报》2002,21(2):60-63

概述了应用子波分析对悬浮物测量中的声散射信号进行特征提取的方法 ,并对声散射信号识别的研究进行了探讨。对实测数据的实验取得了较好的结果  相似文献   

The Formation and Circulation of the Intermediate Water in the Japan Sea   总被引：1，自引：0，他引：1  

Jong-Hwan Yoon  Hideyuki Kawamura 《Journal of Oceanography》2002,58(1):197-211

In order to clarify the formation and circulation of the Japan/East Sea Intermediate Water (JESIW) and the Upper portion of the Japan Sea Proper Water (UJSPW), numerical experiments have been carried out using a 3-D ocean circulation model. The UJSPW is formed in the region southeast off Vladivostok between 41°N and 42°N west of 136°E. Taking the coastal orography near Vladivostok into account, the formation of the UJSPW results from the deep water convection in winter which is generated by the orchestration of fresh water supplied from the Amur River and saline water from the Tsushima Warm Current under very cold conditions. The UJSPW formed is advected by the current at depth near the bottom of the convection and penetrates into the layer below the JESIW. The origin of the JESIW is the low salinity coastal water along the Russian coast originated by the fresh water from the Amur River. The coastal low salinity water is advected by the current system in the northwestern Japan Sea and penetrates into the subsurface below the Tsushima Warm Current region forming a subsurface salinity minimum layer. This revised version was published online in August 2006 with corrections to the Cover Date.  相似文献   

崂山花岗岩地区含锶、偏硅酸矿泉水的形成机理   总被引：1，自引：0，他引：1  

赵广涛  曹钦臣  孙悦鹏 《中国海洋大学学报(自然科学版)》1996,(2)

报道了崂山花岗岩地区矿泉水的特征。指出其矿泉类型为含锶、偏硅酸型，并讨论了其形成机理。  相似文献   

基于特征提取的目标变化检测方法研究     

朱朝杰  董广军  王仁礼 《海洋测绘》2007,27(2):50-52

针对不同时相遥感影像中特定目标的变化,研究了基于特征提取的目标变化检测方法。该方法首先根据目标的几何特征进行检测与提取,然后对提取出的两目标影像进行比较,得到特定目标的变化。实验结果表明该方法对特定目标的变化检测有较好的效果。  相似文献   

东海温度锋的分布特征及其季节变异   总被引：8，自引：4，他引：8  

汤毓祥 《海洋与湖沼》1996,27(4):436-444

根据１９３４－１９８８年东海水文观测资料，重点分析东海温度锋的分布特征及其季节变异，并结合近期中日黑潮合作调查研究成果，初步探讨温度锋季节变异和水团演变的关系，所得主要结论是：（１）东海不仅常年存在浙闽沿岸锋，东海北部陆架锋和黑潮锋，而且、春、夏两季，在东海南部还出现一条东海中部出架锋。（２）江海温度锋季节变化的特点是：冬季，锋的宽度和强度皆是表层最强，夏季，表层温度锋仅出现在浙江近岸小范围海域。  相似文献   

Three-dimensional inversion of marine magnetic anomalies: Implications for crustal accretion along the Mid-Atlantic Ridge (28°–31°30′ N)     

J. E. Pariso  C. Rommevaux  J. -C. Sempere 《Marine Geophysical Researches》1996,18(1):85-101

We present magnetic field data collected over the Mid-Atlantic Ridge in the vicinity of the Atlantis Fracture Zone and extending out to 10 Ma-old lithosphere. We calculated a magnetization distribution which accounts for the observed magnetic field by performing a three-dimensional inversion in the presence of bathymetry. Our results show the well-developed pattern of magnetic reversals over our study area. We observe a sharp decay in magnetization from the axis out to older lithosphere and we attribute this decay to progressive low temperature oxidation of basalt. In crust which is 10 Ma, we observe an abrupt increase in magnetic field intensity which could be due to an increase in the intensity of magnetization or thickness of the magnetic source layer. We demonstrate that because the reversal epoch was of unusually long duration, a two-layer model comprised of a shallow extrusive layer and a deeper intrusive layer with sloping polarity boundaries can account for the increase in the amplitude of anomaly 5. South of the Atlantis Fracture Zone, high magnetization is correlated with bathymethic troughts at segment end points and lower magnetization is associated with bathymetric highs at segment midpoints. This pattern can be explained by a relative thinning of the magnetic source layer toward the midpoint of the segment. Thickening of the source layer at segment endpoints due to alteration of lower oceanic crust could also cause this pattern. Because we do not observe this pattern north of the fracture zone, we suggest it is a result of the nature of crustal formation process where mantle upwelling is focused. South of the fracture zone, reversals along discontinuity traces only continue to crust 2 Ma old. In crust >2 Ma, we observe bands of high, positive magnetization along discontinuity traces. We suggest that within the discontinuity traces, a high, induced component of magnetization is produced by serpentinized lower crust/upper mantle and this masks the contribution of basalts to the magnetic anomaly signal.  相似文献   

南沙群岛南永2井沉积层"红色事件"和"黑色事件"的成因探讨     

姚衍桃  詹文欢 《热带海洋学报》2006,25(6):39-46

南沙群岛南永2井的红色沉积层和黑色沉积层标志着两次异常事件,简称为“红色事件”和“黑色事件”。这两个特殊沉积层的主要特征是磁化率为正值、锰铝(黑色沉积)和铁铝(红色沉积)含量高。关于它们的成因主要有两种观点:一种是火山喷发或地震活动,另一种是气候突变。将红色沉积层和黑色沉积层与南海其它珊瑚礁钻井资料、南海及其周缘火山活动和深海沉积中的微玻陨石进行详细对比,并综合分析几种成因的可能性大小。“红色事件”和“黑色事件”在南海其它珊瑚礁钻井中的反映不明显或无反映,表明两事件的影响范围很有限。尽管南海周缘的一些火山活动期次、全球气候变化的一些代用指标和深海沉积中的微玻陨石层在时间上与“红”、“黑”两事件有较好的对比,成岩作用也能使某些沉积层位形成铁富集或锰富集,但综合考虑各个因素可以排除周缘火山喷发、气候突变、撞击事件及成岩作用等4种成因。火山或地震活动引起的铁或锰热泉上涌可以对“红”、“黑”两事件作出较好的解释,是可能性较大的成因。  相似文献   

辽东湾葵花岛构造区浅层气分布特征、成因探讨及工程影响     

闫章存  刘燕平  曲伟  亓发庆 《海岸工程》2007,26(3):1-10

揭示了葵花岛构造区浅层气规模小、埋藏浅、分布散、压力低、储层松散等分布特点,根据沉积环境和地质特征,推测浅层气为生物甲烷气,但并不完全排除是热生甲烷次生气藏的可能性,探讨了浅层气潜在的工程危害并提出相应防治措施,为今后海洋工程建设提供科学依据。  相似文献   

Hydrographic features of the plume front in the Hangzhou Bay     

Wang Kangshan  Su Jilan 《海洋学报(英文版)》1993,12(1):17-28

  相似文献   

秦皇岛昌黎黄金海岸的沙丘沉积和发育机理   总被引：7，自引：0，他引：7  

曾照爽  庄振业  祁兴芬  刘志杰 《海洋地质前沿》2003,19(7):23-27

昌黎黄金海岸长40km，分布1～1．5km宽的风成沙丘。主沙丘链高30～40m，顺岸线分布，与其斜交数列新月形横向沙丘链。沙丘以中细砂组成，分选极好，层理构造十分丰富。距今3～4ka以前，沙坝形成时就开始形成沙丘；1915年滦河新三角洲发育以来增加了风沙的输沙量，增高沙丘和扩宽了沙丘带。  相似文献