三角洲平原高弯曲分流河道内部结构单元三维建模   总被引：1，自引：0，他引：1  

尹艳树  张昌民  尹太举  俞宸 《地质论评》2013,59(3):544-550

以大庆萨尔图油田北三区西部西块SⅡ12小层典型三角洲平原高弯曲分流河道为例,进行了三角洲平原高弯曲分流河道内部结构单元建模。首先根据高弯曲分流河道沉积层次性,以及河流弯曲机理,解剖了分流河道内部结构,识别出点坝以及侧积层单元,提取了侧积层形态参数和统计参数。其次采用椭球形方程建立了侧积层平面数学函数表达式,采用直线方程描述侧积层剖面形态,从而建立侧积层空间三维几何形态。最后,分两步建立了高弯度分流河道内部结构单元三维地质模型。首先采用序贯指示建模建立分流河道微相模型;随后根据侧积层数学模型描述侧积层空间分布。并在分流河道微相内部将侧积层模型嵌入,形成精细的高弯曲分流河道内部结构模型。以此思路为指导建立了SⅡ12小层结构模型,以此结构模型为基础的储层参数模型很好地再现了点坝内部侧积层对流体渗流的遮挡,为油藏数值模拟和剩余油挖潜奠定了基础。  相似文献   

Modeling residual circulation and stratification in Oujiang River estuary     

林伟波  王义刚  阮晓红  徐群 《中国海洋工程》2012,26(2):351-362

A 3D,time-dependent,baroclinic,hydrodynamic and salinity model was implemented and applied to the Oujiang River estuarine system in the East China Sea.The model was driven by the forcing of tidal elevations along the open boundaries and freshwater inflows from the Oujiang River.The bottom friction coefficient and vertical eddy viscosity were adjusted to complete model calibration and verification in simulations.It is demonstrated that the model is capable of reproducing observed temporal variability in the water surface elevation and longitudinal velocity,presenting skill coefficient higher than 0.82.This model was then used to investigate the influence of freshwater discharge on residual current and salinity intrusion under different freshwater inflow conditions in the Oujiang River estuary.The model results reveal that the river channel presents a two-layer structure with flood currents near the bottom and ebb currents at the top layer in the region of seawater influenced on north shore under high river flow condition.The river discharge is a major factor affecting the salinity stratification in the estuarine system.The water exchange is mainly driven by the tidal forcing at the estuary mouth,except under high river flow conditions when the freshwater extends its influence from the river’s head to its mouth.  相似文献   

Glauconitic coating on a gastropod,Fusitriton laudanum,from the Chatham rise,New Zealand (note)     

G. P. Glasby 《新西兰海洋与淡水研究杂志》2013,47(3):383-386

Superficial coatings of glauconite grains have been observed on the gastropod mollusc, Fusitriton laudanum, from the Reserve Bank, Chatham Rise. The glauconite predates the shell on which it accretes and is incorporated on to the shell surface by agglutination of sand‐size material by mucus secreted by epizoic anemones.  相似文献   

太平洋不同海水层结条件下的内波波致声场起伏研究     

李佳讯  张韧  金宝刚  陈奕德 《海洋学报》2013,35(3):78-86

基于Argo资料对太平洋海域海水层结进行分类区划,利用内波动力学方法对内波致声起伏进行数值求解,对不同层结状况下的内波致声起伏进行模拟试验。结果表明:垂直方向海水层结的不均匀和跃层的存在,使海洋内波斜压模态受到了歪曲变形。层结峰的个数和深度与声速起伏存在很好的对应关系。有内波的声传播特征总体上与没有内波时的相似。不同层结情况下,声场对内波扰动的响应不一致。  相似文献   

The diel verticalmigration of sound scatterers observed by an acoustic Doppler current profiler in the Luzon Strait from July 2009 to April 2011     

YANG Chenghao  LIAO Guanghong  YUAN Yaochu  CHEN Hong  ZHU Xiaohua 《海洋学报(英文版)》2013,32(11):1-9

Acoustic Doppler current profiler （ADCP） receives echoes from sound scatterers, then their speed is calcu- lated by the Doppler effect. In the open ocean, most of these backscatterers are from the plankton. The sound scatterers descend down to depth at around dawn, their mean speed is 2.9 cm/s, then they ascend up to the surface layer at around dusk with a mean speed of 2.1 cm/s, in the Luzon Strait. The descending speed is faster, which suggests that this zooplankton population may accelerate its downward migration under the action of the gravity. The vertical distribution of a mean volume backscattering strength （MVB- S） in the nighttime has two peaks, which locate near the upper and lower boundary layers of halocline, respectively. However, the backscatterers only aggregate near the surface layer in the daytime. The diel ver- tical migration （DVM） of sound scatterers has several characteristic patterns, it is stronger in summer, but weaker in winter, and the maximum peak occurs in September. The DVM occurrence is synchronous with the seawater temperature increasing at around dawn and dusk, it may affect the ocean mixing and water stratification,  相似文献   

湿层结参数非常数时雨团模型中的位势不稳定   总被引：1，自引：0，他引：1  

于杰  张铭 《气象科学》2012,32(5):550-558

建立了圆柱坐标下湿层结参数在垂直方向不为常数时的非轴对称雨团数学模型,着重讨论了其中的位势不稳定问题。抽象出了暴雨发生前期、盛期和发生后的三种典型湿层结参数的垂直分布。得到了此时位势不稳定的判据,分别给出了不稳定扰动增长率与稳定扰动振荡圆频率的上、下界。并在该参数取分2段常数的情况下,进行了解析求解。得到以下结论:该模型雨团在水平方向可有螺旋结构,这与用雷达资料得到的实际情况一致。在暴雨发生前期,有位势不稳定发生;且螺旋臂条数越多,雨团半径越小,不稳定增长率的上界越大。在暴雨盛期,整层为弱位势稳定层结,无位势不稳定发生;扰动螺旋臂条数越少,半径越大,其振荡圆频率下界越大。在暴雨结束后,整层为强位势稳定层结,也无位势不稳定发生;扰动螺旋臂条数越多,半径越小,其振荡圆频率的上界越大。在该参数取为2段常数情况下,且下层与上层其分别为负、正值时,有位势不稳定发生,且雨团的螺旋臂越多、半径越小及不稳定层次越厚,其增长率越大。该不稳定雨团的垂直结构在下层大体为半个正弦波,波长随不稳定层次的增厚而增大;在上层则为指数分布,且随高度增加迅速趋于0。  相似文献   

闽北一次初春强降水的成因分析     

何小宁  吴幸毓 《气象研究与应用》2012,33(3):21-24,37,114

利用常规观测资料、NCEP 1°×1°再分析资料、新一代天气雷达资料,对2012年3月6日-7日福建省北部地区暴雨成因进行诊断分析。结果表明:此次降水过程在高空西风槽南下带来的冷空气与西南暖湿气流交汇的背景下产生,暴雨区位于低空西南急流北侧、低层切变南侧、地面冷锋附近;强降水落区位于层结不稳定的湿区中,低层辐合、高层辐散有利于对流发展;干冷空气的侵入时高层高值位涡库向北向下伸展,促使中低层气旋涡度发展,从而导致强降水的发生;雷达回波分析表明,低层暖平流、高层冷平流、区域上空辐合形势都有利于对流性降水的产生。  相似文献   

Temperature Inversion in the Bay of Bengal Prior to Summer Monsoon Onsets in 2010 and 2011          下载免费PDF全文

LI Jian  YANG Lei  SHU Ye-Qiang  WANG Dong-Xiao 《大气和海洋科学快报》2012,5(4):290-294

Freshwater input such as runoff and rainfall can enhance stratification in the Bay of Bengal(BOB) through the formation of a "barrier layer",which can lead to the formation of a temperature inversion.The authors focused on the temperature inversion in spring,especially before the onset of the summer monsoon,because previous research has mainly focused on the temperature inversion in winter.Using the hydrographic data from two cruises performed during 24-30 April 2010 and 1-4 May 2011,the authors found that inversions appeared at two out of nine Conductivity-Temperature-Depth Recorder(CTD) stations across the 10°N section and at seven out of 13 CTD stations across the 6°N section in the BOB.In 2010,the inversions(at stations N02 and N05) occurred at depths of approximately 50-60 meters,and their formation was caused by the advection of cold water over warm water.In 2010,the N02 inversion was mainly influenced by the warm saline water from the east sinking below the cold freshwater from the west,while the N05 inversion was affected by the warm saline water from its west sinking below the cold freshwater from its east.In 2011,the inversions appeared at depths of 20-40 meters(at stations S01,S02,S07,S08,and S09) and near 50 m(S12 and S13).The inversions in 2011 were mainly caused by the net heat loss of the ocean along the 6°N section.  相似文献   

天津市秋季典型环境污染过程个例分析   总被引：2，自引：0，他引：2  

张晓云  郭虎  易笑园  张广泉  汪靖 《辽宁气象》2012,(4):33-37

选择天津市秋季典型PM10污染过程2010年10月3—12日环境空气质量监测资料和常规气象资料、探空资料及NCEP资料,研究大气环境天气背景场、大气层结稳定度的特征及其对污染过程的影响。结果表明：高低空环流背景场与污染过程密切相关。在污染上升阶段,层结稳定度迅速增加,500 hPa高空处于槽前,地面在华北地形槽中,高低空风速辐合;在污染峰值阶段,层结稳定,逆温层加强,环流场稳定少变,地面风力微弱;在污染下降阶段,层结稳定程度骤降,地面冷锋和高空槽过境,降水出现,高低空偏北风增大。同时,PM10污染过程与多项层结稳定度参数显著相关,与对流凝结高度单相关系数为0.84,因此,高低空环流背景场的配置和层结稳定度变化是PM10污染出现的主要原因。  相似文献   

城市地下空间开发分层体系的研究     

辛韫潇  李晓昭  戴佳铃  王睿 《地学前缘》2019,26(3):104-112

为统一城市地下空间在规划开发过程中的分层标准,文中统计了国内外主要城市的地下分层情况和相关规范要求,并分别就自然因素和社会因素对城市地下分层的影响进行分析。其中自然影响因素主要有地形地貌和工程地质分布,该因素决定了地下空间开发的难度和成本;社会影响因素主要有城市规模、区位条件和地方政策法规,城市人口规模和经济水平决定了地下空间的需求量。结果表明,区域的开发需求量和开发难度决定了城市地下空间的开发规模,进而影响到地下空间的分层。多数城市常以15 m、30 m为界将地下空间划分为浅层、次浅层、深层;浅层地下空间受地形地貌影响较大,宜分区域进行分层,陡坡处宜沿着与地面垂直方向进行分层。在此基础上建立了一套地下分层评价指标体系,对后续的城市地下空间规划工作具有指导和借鉴意义。  相似文献