河口区斜压梯度对余水位的累积影响及其机制探讨   总被引：1，自引：1，他引：0  

杨昊  欧素英  姚鹏  郭晓娟  杨清书  蔡华阳 《海洋学报》2019,41(1):21-31

余水位（即潮平均水位）是河口区径潮相互作用的典型结果,研究其形成演变机制对探讨河口区的水资源高效开发利用具有重要科学意义。本文基于不同径潮边界条件下的三维斜压水动力数值模拟及切比雪夫机制分解,初步探讨了概化地形条件下斜压梯度对余水位沿程变化的影响。数值模拟结果表明:河口区余水位的沿程变化明显受径流量、潮波振幅、辐聚地形及斜压梯度等因素的共同影响,斜压梯度对余水位的影响是一种累积效应且影响区域集中在回水区,同时其影响强度具有明显的大小潮变化、洪枯季变化。利用数值模型提供的水位及流速场信息,通过切比雪夫分解非线性摩擦项分离出控制余水位变化的3个主要因素,即径流、潮流和径潮相互作用因子,并与斜压梯度产生的余水位进行对比分析,结果表明:回水区域余水位主要以径潮相互作用因子为主导;斜压梯度对余水位影响主要体现在小潮期间,有可能成为影响余水位变化的主控因子。  相似文献   

Laboratory flume studies on monochromatic wave-fine sandy bed interactions Part 2. Sediment suspensions   总被引：2，自引：0，他引：2  

Shiaw-Yih Tzang  Shan-Hwei Ou  Tai-Wen Hsu 《Coastal Engineering》2009

As reported in preceding paper (Part 1. Soil Fluidization), the observed phenomena of sediment suspensions above a fluidized sandy bed of Sand II (d₅₀ = 0.092 mm) under monochromatic wave actions are quantitatively investigated. The suspended sediment concentration (SSC) at a single point within 5 cm above the bed was synchronously measured with water waves and bed soil's pore pressures with an intrusive optical sediment-concentration probe. The measurements show that SSC initiates several wave cycles after initiation of bed soil's fluidized response and grows to a peak value mainly in the post-fluidization phase. Under similar wave loadings in the same test series, SSC is usually higher over a resonantly fluidized (RF) bed than over a non-resonantly fluidized (NRF) bed. On the contrary, only relatively low SCC can be identified above an unfluidized bed. The analyses illustrate that to certain extent, peak values of SSC are directly proportional to the thickness of fluidized soil layer d_f. Values of d_f usually decrease with repeated fluidized response, longer consolidation periods, and in deeper water depths. Once the fluidized responses initiate, pore pressures are generally much significantly amplified in both shallow fluidized soil layers and near below the fluidized layer, especially during the resonance event. The resulting depth gradients of dynamic pore pressure amplitudes in shallow layers are likely to have caused higher initial rises of SSC in a RF bed than in the subsequent NRF bed. Those in deeper layer should have contributed to sustain the fluidization state for further SSC increments. Immediately after termination of wave loading, re-deposited suspended sediments always result in a typical flat bed form. For a pre-fluidized bed, wave-induced drastic sediment suspensions are still obtainable very near above the bed with even a rather thin fluidized surface soil layer.  相似文献   

pH对4种鲷鱼精子活力的影响     

黄巧珠  区又君  喻达辉  李加儿  江世贵 《广东海洋大学学报》1999,(3)

用不同 ｐＨ 的海水对真鲷（Ｐａｇｒｏｓｏｍ ｕｓ ｍ ａｊｏｒ）、平鲷（Ｒｈａｂｄｏｓａｒｇｕｓ ｓａｒｂａ）、黑鲷（Ｓｐａｒｕｓｍ ａｃｒｏｃｅｐｈａｌｕｓ）和黄鳍鲷（Ｓ．ｌａｔｕｓ）精子进行激活实验。结果表明,四种鲷鱼精子对ｐＨ 的适应范围较广,其最适ｐＨ 值与其生态习性相关。  相似文献   

大范围3DCM场景实时并行绘制的任务划分及策略     

李朝奎  杨偶  吴柏燕  殷智慧  李拥 《地理与地理信息科学》2012,28(6)

针对三维城市模型(3DCM)场景并行绘制的几何图元分布特性,利用动态负载平衡算法实现3DCM场景绘制任务划分和分配.给出了负载平衡性能的一种度量权,提出一种递归划分算法:即把按顺序执行的任务集,根据其子任务间潜在的并行性,划分成若干个可并发执行的任务子集,并把每个子集分配给处理机,使各处理机之间的数据通信量尽可能同步,同时兼顾各处理机之间的负载平衡,从而实现了一种新的负载平衡算法.  相似文献   

Line-by-line radiative transfer model for infrared spectrum of AERI     

Kwang-Mog Lee  Joong-Hyun Park  Myoung-Hwan Ahn  Mi-Lim Ou  Yoonjae Kim 《Asia-Pacific Journal of Atmospheric Sciences》2012,48(2):135-143

Infrared radiance spectra measured in space or on the ground have been used for many applications, such as the retrieval of atmospheric temperature and humidity profiles. The Korean Meteorological Administration (KMA) recently installed an Atmospheric Emitted Radiance Interferometer (AERI) system at the Korea Global Atmosphere Watch Center (36°32??N, 125°19??E) in Anmyondo to measure the downward radiance spectra on the ground. For further utilization of such interferometeric radiance measurements, an accurate line-by-line radiative transfer model is required. This study introduces a line-by-line radiative transfer model developed at Kyungpook National University (KNU_LBL) and presents comparisons of spectra simulated using the KNU_LBL model and measured by the AERI system, that is installed inside a secure container. When compared with the Atmospheric and Environmental Research (AER) radiative transfer codes, the KNU_LBL model provides nearly identical spectra for various model atmospheres. The simulated spectra are also in good agreement with the AERI spectra for clear sky conditions, and a further improvement is made when taking into account of the emissions and absorption by CO₂ and H₂O for the light path inside the container, even though the path is short.  相似文献   

晚三叠世卡尼期黑色页岩事件在龙门山地区的沉积学和古生物学响应   总被引：1，自引：0，他引：1       下载免费PDF全文

时志强  欧莉华  罗凤姿  李云  钱利军 《古地理学报》2009,11(4):375

龙门山前缘地区卡尼阶-诺利阶马鞍塘组中部发育一套薄-中层状黑灰色、灰黑色、黑色（含介壳）钙质泥（页）岩,在该套岩石中瓣鳃类生物多见,原生二价金属硫化物（黄铁矿）发育,水平层理发育,显示着低能环境贫氧条件的典型特征。与马鞍塘组中部黑灰色、灰黑色钙质泥（页）岩相当层位的卡尼期晚期沉积,在松潘-甘孜地区、昌都地区、可可西里地区均可见到,多显示为黑色、灰黑色色调,岩性为泥（页）岩或粉砂质板岩、钙质板岩,反映了一次黑色页岩地质事件在中国西部古特提斯东部地区产生了大范围的影响。全球对比表明,该套深色泥（页）岩在西特提斯、印度喜玛拉雅等地均有分布,覆盖在卡尼期早期碳酸盐沉积之上。据此,作者认为晚三叠世卡尼期特提斯范围的黑色页岩事件,很有可能与卡尼期全球性的碳酸盐生产危机有关,马鞍塘组中部发育的深色泥（页）岩即是此次事件在扬子地台西缘的反映。根据对川西北地区绵竹汉旺、安县雎水、江油马鞍塘等剖面的实际考察与研究,认为代表缺氧事件沉积的马鞍塘组中部黑灰色泥（页）岩之下为卡尼阶灰岩段（即汉旺组中下部灰岩段,主要为鲕粒灰岩、海绵礁灰岩等）,之上为诺利阶灰色粉、细砂岩夹灰岩、泥岩段（相当于石元组）。黑灰色钙质泥（页）岩不仅是该组岩性变化的转折点,亦是古生物、古生态急剧变化的转折点。在马鞍塘组下部广泛可见的六射海绵、海百合、苔藓虫、珊瑚等海相化石在马鞍塘组中上部地层（上卡尼阶至诺利阶底部）中很少看到,仅见丰富的瓣鳃类、菊石、腕足类等有壳类动物化石。
  相似文献   

地球公转自转与地壳动力学     

安欧 《地壳构造与地壳应力文集》2009,(0)

经典力学是有相对性的,但在地球公转自转力学和地壳构造动力学的研究中有一定可用性。地球的公转和自转是地壳构造应力的天体力源,在此力学体系中的岩体力学基本方程还须做重要改进或重建。  相似文献   

邻二氮菲分光光度法测定赤泥和石灰石混匀度   总被引：1，自引：1，他引：0  

李令  朱云勤  张菊  刘凯萍  孟铁宏  江鸥 《岩矿测试》2009,28(4):394-396

用盐酸提取赤泥和石灰石的混合料后,通过邻二氮菲分光光度法测定提取液中铁含量,进而求得混合料中氧化铁的质量分数,以此来衡量混匀度。结果表明,该法与重铬酸钾法比较,精密度和准确度均无显著性差异,测定混匀度的相对误差在±2%,且方法简便、快速、准确、对环境友好,可用于生产实时监控。  相似文献   

广西热带气旋灾害评估系统的开发与应用   总被引：15，自引：13，他引：2  

李艳兰  欧艺  周绍毅  周美丽 《气象研究与应用》2008,29(4):1-3

介绍了广西热带气旋灾害评估系统的总体设计、系统主要内容、功能及应用。对广西热带气旋灾害评估工作,大大提高了数据分析和决策的效率,评估结果比较理想。  相似文献   

台风“莫拉菲”暴雨多普勒雷达回波及风场结构分析   总被引：3，自引：1，他引：2  

欧坚莲  贾显锋 《气象研究与应用》2009,30(4):5-9,I0003

使用常规天气资料、卫星云图和梧州S波段多普勒雷达资料对2009年7月19～20日发生在广西的一次典型台风强降水天气过程进行了分析.结果表明,在副热带高压南侧偏东气流引导下,台风向偏西方向移动直接影响广西,加上西南季风的叠加作用,造成了广西大范围的台风云系降水.从多普勒反射率因子图上,整个降水雨带为明显的旋转西进过程;多普勒径向速度图上,低层辐合高层辐散的配置有利于降水的发生发展,暴雨是长时间维持在其上空的强降雨云带造成的.  相似文献