长江河口涨、落潮槽内的沙波地貌和输移特征   总被引：3，自引：0，他引：3       下载免费PDF全文

王永红  沈焕庭  李九发  茅志昌 《海洋与湖沼》2011,42(2):330-336

涨、落潮槽是河口区的重要地貌单元,槽内由于不同的优势流作用而表现出不同的泥沙运移特征。沙波是底沙输移的表现,因此研究槽内的沙波特征对于涨、落潮槽的水动力和沉积地貌研究有重要的意义。本文依据现场声纳观测、测深仪测深、表层取样和现场水动力观测等方法获得河槽床面沙波和水动力资料,对沙波的几何形态、波高和全潮周期的迁移距离进行...  相似文献   

声学法深海热液速度场测量重建算法研究   总被引：1，自引：1，他引：0       下载免费PDF全文

白燕  毛洁  樊炜  潘华辰  刘云峰 《海洋科学》2011,35(3):42-49

介绍了利用声学法测量深海热液速度场的基本原理.利用往返飞渡时间差与流场速度的关系,应用反问题求解技术重建测量区域的速度场.应用最小二乘法对两种典型的热液口速度场模型进行了仿真重建,分析了换能器数量、实验测量误差以及换能器的布放对重建结果的影响,并对重建结果进行了流量分析.仿真重建的绝对误差、相对误差以及流量分析结果表明...  相似文献   

复杂岛屿海域的台风浪局地特征模拟与分析——以舟山海域为例   总被引：1，自引：0，他引：1  

毛科峰  陈希  萧中乐  王骥鹏  梁毅 《海洋学研究》2011,29(4):8-15

为了研究舟山海域复杂地形条件下的台风浪特征,在高分辨数值模拟中采用了利用海图资料处理复杂岛屿地形分布的方法,利用WAVEWATCHⅢ和SWAN模式相嵌套模拟了影响该海域的西北行路径的典型台风浪过程.分析表明,舟山海域的东南部、东北部、西北部、内部海域受台风的影响各不相同,台风浪特征分布与海域的岛屿分布、水深分布等因素密...  相似文献   

单点高频地波雷达资料估算潮能耗散的方法   总被引：1，自引：0，他引：1  

毛华斌  陈举  邱春华  练树民 《热带海洋学报》2011,(6)

使用嵊泗站所布设的地波雷达观测获取的径向流数据,以及嵊泗、芦潮港、岱山3个潮汐观测站水位资料,采用两点近似投影方法反演流场全矢量流速,并用T-Tide程序计算调和常数,分别计算O1、K1、M2、S2各分潮流速场及迟角场,并计算各点上的潮能通量及潮能耗散,得到嵊泗岛以西杭州湾口区域潮能耗散同地形存在良好对应关系,充分证明了采用地波雷达观测数据进行潮能耗散计算这一方法的可行性,供相关工作者作进一步研究和讨论.  相似文献   

丛粒藻形态多样性与遗传多样性研究   总被引：1，自引：0，他引：1  

王朋云  茅云翔  孔凡娜  马梅  马飞 《中国海洋大学学报(自然科学版)》2011,41(5):63-70

观察了采集自不同地点的3株丛粒藻(Botryococcus braunii)(AGB-Bb01、AGB-Bb02和AGB-Bb03)的显微结构和亚显微结构,以18S rDNA和ITS区序列为目标位点比较分析了16株丛粒藻藻株的遗传距离和序列相似性,重建了系统发生树。结果表明:丛粒藻不同地理株在细胞大小、聚落大小和聚落细胞数目方面存在较明显的差异,亚显微结构显示不同藻株的杯状鞘厚度及细胞包埋程度也存在差异;不同地理株间具有较高的遗传多样性,系统发生树显示所有藻株可分成2个簇群和4个亚群,存在一定程度的地理隔离。研究证明了18S rDNA和ITS区序列是进行丛粒藻基因分型和遗传多样性研究的良好位点。本研究为系统了解丛粒藻的遗传多样性和开展优良藻株选育工作奠定了基础。  相似文献   

日本枪乌贼的营养成分分析   总被引：2，自引：0，他引：2  

刘玉锋  毛阳  王远红  吕志华 《中国海洋大学学报(自然科学版)》2011,(Z1):341-343

本文采用国家标准营养分析方法及仪器分析方法测定了日本枪乌贼的营养成分。结果表明,日本枪乌贼中粗蛋白含量9.29%,粗脂肪含量1.43%,水分含量85.82%,灰分含量1.79%;18种氨基酸占总干重的55.09%,8种必需氨基酸占氨基酸总量的44.46%,必需氨基酸与非必需氨基酸比值0.80;多不饱和脂肪酸二十二碳六烯酸DHA、二十碳五烯酸EPA、二十碳四烯酸ARA及十八碳二烯酸LA之和占总脂肪酸含量的24.94%;富含无机元素镁,磷,钙,锌。日本枪乌贼蛋白质含量较高,必需氨基酸含量较丰富,粗脂肪含量较低,是营养价值较高的一种海产品。  相似文献   

Ore-forming Fluid Characteristics of the Saishitang Cu-polymetallic Deposit in Qinghai Province, China     

LAI Jianqing  JU Peijiao  MAO Yin  AN Jianghu  WANG Xiongjun 《《地质学报》英文版》2015,89(2):485-504

Saishitang Cu-polymetallic deposit is located in the southeast section of Late Paleozoic arcfold in the southeastern margin of Qaidam platform. Accoring to the geological process of the deposit,four mineralization episodes were identified: melt/fluid coexisting period(O),skarn period(A),first sulfide period(B) and second sulfide period(C),and 10 stages were finally subdivided. Three types of inclusions were classified in seven stages,namely crystal bearing inclusions(type I),aqueous inclusions(type II) and pure liquid inclusions(type III). Type I and II inclusions were observed in stage O1,having homogenization temperature from 252 to 431°C,and salinities ranging from 24.3% to 48.0%. Type I inclusion was present in stage A1,having homogenization temperature from 506 to 548°C,and salinities ranging from 39.4% to 44.6%. In stage B1,type II and III inclusions were observed,with homogenization temperature concentrating between 300–400°C,and salinities from 0.4% to 4.3%. Type II inclusions were present in stage B2,with homogenization temperature varying from 403 to 550°C. In stage C1,type I and II inclusion commonly coexisted,and constituted a boiling inclusion group,having homogenization temperatures at 187–463°C,and salinities in a range of 29.4%–46.8% and 2.2%–11.0%. Type II and III inclusions were developed in stage C2,having homogenization temperature at 124–350°C,and salinities ranging between 1.6% and 15.4%. In stage C3,type II and III inclusions were presented,with a homogenization temperature range of 164–360°C,and salinities varying from 4.0% to 11.0%. The results of micro-thermal analysis show that fluids are characterized by high temperature and high salinity in stage O1 and A1,and experienced slight decrease in temperature and dramatic decrease in salinity in stage B1 and B2. In stage C1,the salinity of fluid increased greatly and a further decrease of temperature and salinity occurred in stage C2 and C3. Fluids boiled in stage C1. With calculated pressure of 22 MPa from the trapping temperature of 284–289°C,a mineralization depth of 2.2 km was inferred. Results of Laser Raman Spectroscopy show high density of H2 O,CH4 and CO2 were found as gas composition. H-O isotope study indicates the oreforming fluids were the mixture of magmatic water and meteoric water. Physicochemical parameters of fluids show oxygen and sulfur fugacity experienced a decrease,and redox state is weakly reducing. Along with fluid evolution,oxidation has increased slightly. Comprehensive analysis shows that melt exsolution occurred during the formation of quartz diorite and that metal elements existed and migrated in the form of chlorine complex. Immiscible fluid separation and boiling widely occurred after addition of new fluids,bringing about dissociation of chlorine-complex,resulting in a great deal of copper precipitation. In conclusion,Saishitang deposit,controlled by regional tectonics,is formed by metasomatism between highly fractionated mineralization rock body and wall rock,and belongs to banded skarn Cu-polymetallic deposit.  相似文献   

The Oil-Bearing Pore Size Distribution of Lacustrine Shale from E2S42 Sub-Member in Damintun Sag, Liaohe Depression, Bohai Bay Basin, China     

CHEN Guohui  LU Shuangfang  LI Jinbu  WANG Weiming  TIAN Shansi  SHAN Junfeng  HU Yingjie  MAO Jinli  HAN Xia 《《地质学报》英文版》2015,89(Z1):8-10

<正>1 Introduction There is a set of organic rich shale at E22S4sub-member in damnintun sag.The organic material is typically type I.In recent years,breakthrough was obtained in shale oil exploration.The wettability of organic and inorganic pore is different.As a result,the mobility of oil in organic and inorganic pore is different.So it’s necessary to distinguish  相似文献   

北京山区泥石流自动监测预警系统的建立与应用     

王海芝  冒建  任凯珍 《城市地质》2015,(Z1):150-155

自动监测预警系统,是目前山区突发地质灾害预警预报有效的预警模式。本系统是在详细调查的基础上,以调查数据为底层分析数据库,以.net为语言运行环境,经所建立的预警模型分析计算后,产生预警预报产品,进行预警发布。  相似文献   

嗜酸微生物与生物冶金技术     

周洪波  毛峰  王玉光 《矿物岩石地球化学通报》2015,(2):269-276

生物圈中广泛分布着自然酸性环境和人造酸性环境,为嗜酸微生物(最适生长p H3)提供了生存场所。嗜酸微生物在铁和硫等重要元素的地球化学循环等方面起着重要作用,可应用于冶金领域,具有流程短、成本低、环境友好等优势,目前已经成功地应用于铜、金、铀等金属的提取,成为世界矿物加工的前沿技术。该技术在国外已经实现工业化生产,中国也在逐步推广应用,但仍然存在浸出率和浸出效率低等问题。本文主要介绍嗜酸微生物和生物冶金技术的研究进展,为加强基础理论和应用技术研究提供启示。  相似文献