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南黄海冷涡沉积和通道沉积的发现 被引量:61
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作者 申顺喜 陈丽蓉 +1 位作者 高良 李安春 《海洋与湖沼》 CAS CSCD 北大核心 1993年第6期563-570,共8页
为解决南黄海及东海北部的沉积环境和物质来源问题,1992年5月对黄海和济州岛西南的泥质沉积进行了多方面调查和研究,发现济州岛西南、南黄海中部和北黄海西部泥质沉积区,分别与那里的冷涡活动区相对应。因此,这些泥质沉积应属于“冷涡... 为解决南黄海及东海北部的沉积环境和物质来源问题,1992年5月对黄海和济州岛西南的泥质沉积进行了多方面调查和研究,发现济州岛西南、南黄海中部和北黄海西部泥质沉积区,分别与那里的冷涡活动区相对应。因此,这些泥质沉积应属于“冷涡沉积”;而在冷涡之间又出现连接它们的“通道”,形成了具有特殊结构的“通道沉积”,它分布于黄海暖流之下,呈南北向延伸。表明冷涡沉积和通道沉积是受控于冷涡、黄海暖流及其相关的环流体系。 展开更多
关键词 冷涡沉积 通道沉积 黄海暖流 沉积
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南黄海辐射沙洲西太阳沙海域钻孔沉积环境分析 被引量:10
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作者 殷勇 邹欣庆 +2 位作者 朱大奎 黄家祥 陈平平 《第四纪研究》 CAS CSCD 北大核心 2007年第5期724-734,共11页
南黄海辐射沙洲枢纽区的西太阳沙海域钻孔岩芯很好地揭示了研究区全新世中晚期潮成沙脊沉积序列和晚更新世末期滨岸潮滩沉积序列。潮成沙脊在垂向上由两个基本的沉积相构成:出现在-5m水深以上的沙脊-浅潮下相以发育小型沙波交错层理、... 南黄海辐射沙洲枢纽区的西太阳沙海域钻孔岩芯很好地揭示了研究区全新世中晚期潮成沙脊沉积序列和晚更新世末期滨岸潮滩沉积序列。潮成沙脊在垂向上由两个基本的沉积相构成:出现在-5m水深以上的沙脊-浅潮下相以发育小型沙波交错层理、水平层理、块状层理和缺乏生物扰动为特点;发育在水深-5m以下的沙脊-深潮下相以出现脉状层理、波状层理和沙波交错层理组合为特点,具有丰富的生物扰动,并保存有风暴沉积。14C测年数据表明潮成沙脊是中全新世以后形成的,在辐射沙脊群形成之前,研究区经历了晚更新世的滨岸潮滩环境以及早全新世的海侵环境。烂沙洋靠西太阳沙一侧潮流通道目前已切入晚更新世滨岸潮滩相地层,潮道底部约8m厚的淤积层夹有强烈变形的滑塌堆积,可能与台风、风暴潮引起的骤然淤积有关,目前已被1992-2003年的海图资料证实。 展开更多
关键词 沉积 沙脊-潮流通道沉积体系 滨岸潮滩沉积体系 沙脊-浅潮下相 沙脊-深潮下相
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Characteristics of modern sedimentation in Qingdao bays
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作者 陈正新 Paul Huang +3 位作者 黄海燕 董贺平 李少泉 李春 《Chinese Journal of Oceanology and Limnology》 SCIE CAS CSCD 2009年第3期683-696,共14页
With available survey data and 237surface sediment samples,the modern sedimentation in Qingdao bays is studied.The research result shows that the east area is shallower(16.4 m) than that in the west(45.8 m).The geogra... With available survey data and 237surface sediment samples,the modern sedimentation in Qingdao bays is studied.The research result shows that the east area is shallower(16.4 m) than that in the west(45.8 m).The geography was formed by a symmetric wave in a sequence of bank-offshore depression-platform-tidal channel-platform-offshore depression-foreshore from south to north.Flood sedimentary systems were formed from inlet of the Jiaozhou Bay in the west to the barrier bar in the east.Lateral sedimentation includes mainly tidal current ridges in two tidal channels.Gravel sandy sediments formed by wave lie in midland of from seashore to wave base.Dynamic functions are mainly tide and wave.Tidal current moves sediment in vertical and horizontal directions,sorting sediments and providing materials for coastwise beaches.The sources of sediment are mainly from eroded headland rocks.In general,grain sizes in this area from the inlet of the Jiaozhou Bay in the west(120°17') to the barrier bar outside in the east(120°35') are coarse-fine-coarse,forming gravel-gravelly sand(G-S),sand(S),gravel clay silt(G-YT),clay silt(YT),gravelly silty sand(G-TS),silty sand(TS),gravelly sandy silt(G-ST),and sandy silt(ST) in turn. 展开更多
关键词 Qingdao bays surface sediments tidal current ridges sedimentary dynamics
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辽河西部凹陷大洼地区沙三段陡坡带近岸水下扇识别与刻画
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作者 叶青 《东北石油大学学报》 CAS 北大核心 2022年第3期13-24,I0001,I0002,共14页
辽河西部凹陷陡坡带近岸水下扇扇体分布及其沉积相特征认识程度低。为了精细识别与刻画大洼地区沙河街组三段(沙三段)近岸水下扇,根据沉积物供给通道与地震属性研究,分析陡坡带近岸水下扇的沉积特征。结果表明:陡坡带具有构造变换控砂... 辽河西部凹陷陡坡带近岸水下扇扇体分布及其沉积相特征认识程度低。为了精细识别与刻画大洼地区沙河街组三段(沙三段)近岸水下扇,根据沉积物供给通道与地震属性研究,分析陡坡带近岸水下扇的沉积特征。结果表明:陡坡带具有构造变换控砂的特征,边界断层具有转换带特征,转换带地势平坦提供沉积物供给通道,物源沿通道入湖形成近岸水下扇沉积;陡坡带地震相特征指示近岸水下扇沉积,沿物源方向地震反射表现为斜交前积反射,垂直物源方向地震反射表现为杂乱丘型反射。陡坡带近岸水下扇具有区别于围岩的高波阻抗和强振幅属性特征,在低勘探程度区刻画两套扇体。该结果为研究陡坡带近岸水下扇油气勘探提供依据。 展开更多
关键词 陡坡带 近岸水下扇 扇体识别 沉积物供给通道 地震相分析 波阻抗反演 振幅属性 沙三段 大洼地区 辽河西部凹陷
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Preparation of diamond/Cu microchannel heat sink by chemical vapor deposition 被引量:2
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作者 刘学璋 罗浩 +1 位作者 苏栩 余志明 《Journal of Central South University》 SCIE EI CAS CSCD 2015年第3期835-841,共7页
A Ti interlayer with thickness about 300 nm was sputtered on Cu microchannels, followed by an ultrasonic seeding with nanodiamond powders. Adherent diamond film with crystalline grains close to thermal equilibrium sha... A Ti interlayer with thickness about 300 nm was sputtered on Cu microchannels, followed by an ultrasonic seeding with nanodiamond powders. Adherent diamond film with crystalline grains close to thermal equilibrium shape was tightly deposited by hot-filament chemical vapor deposition(HF-CVD). The nucleation and growth of diamond were investigated with micro-Raman spectroscope and field emission scanning electron microscope(FE-SEM) with energy dispersive X-ray detector(EDX). Results show that the nucleation density is found to be up to 1010 cm-2. The enhancement of the nucleation kinetics can be attributed to the nanometer rough Ti interlayer surface. An improved absorption of nanodiamond particles is found, which act as starting points for the diamond nucleation during HF-CVD process. Furthermore, finite element simulation was conducted to understand the thermal management properties of prepared diamond/Cu microchannel heat sink. 展开更多
关键词 chemical vapor deposition microchannel nanoseeding Ti interlayer Cu substrate
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Particle inertia effect on sediment dispersion in turbulent open-channel flows 被引量:5
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作者 ZHANG Lei ZHONG DeYu WU BaoSheng 《Science China(Technological Sciences)》 SCIE EI CAS 2014年第10期1977-1987,共11页
Particle inertia effect plays a significant role in sediment dispersion which has not been fully elucidated.In this paper,the profound effect of particle inertia on the sediment dispersion was analyzed.The theoretical... Particle inertia effect plays a significant role in sediment dispersion which has not been fully elucidated.In this paper,the profound effect of particle inertia on the sediment dispersion was analyzed.The theoretical expression for the drift velocity based on the two-phase mixture theory in turbulent open channels is firstly introduced.The influence of particle inertia on sediment dispersion was investigated through three different aspects including vertical dispersion,motion,and flux properties based on the drift velocity.Results show that the dispersion of suspended sediment in turbulent open-channel flows is affected by three major processes including turbulence of water sediment mixtures,particle random motion,and collisions among particles,of which the contributions of particle turbulence and collisions to the sediment dispersion are remarkable for particles of high inertia.With respect to the vertical mean velocity and sediment flux,it shows that the predictive results agree well with the measurements when the term of particle inertia is considered.As a result,particle inertia considerably affects the behavior of suspended sediment.In particular,the influence of inertia must be accounted for in circumstances of flows laden with high-inertia particles. 展开更多
关键词 INERTIA EFFECT suspended sediment DISPERSION
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