东营港拟建航道沿线滩面沉积物特性及航道可挖性分析

通过对现场底质取样和试挖槽观测,对东营港拟建5～15万t级航道沿线滩面沉积物特性进行了研究,同时结合海域的水动力及泥沙环境分析,对东营港航道可挖性进行了探讨。研究结果表明-18 m等深线(10万t级码头)以内水域滩面泥沙以粉砂和砂质粉砂为主,d50为0.03⁰.04 mm,活动性强,发生骤淤的可能性大,不宜开挖航道;-18 m等深线以外海域滩面以粘土质粉砂为主,d50小于0.02 mm,泥沙活动性较差,开挖航道后出现大风骤淤的可能性较小。     

粉沙质海岸建港的新模式

根据东营港所在海域的自然条件,从泥沙角度探讨了东营港扩建工程中新的建港布置形式,采用陆连岛方案,将拟建港区设置在岸外-8 5m深水区,通过栈桥和实堤与陆相联。     

滨州港外航道大风天泥沙骤淤沿程分布预报

根据波浪预报理论、能量传递理论和能量平衡原理,将风生浪—浪掀沙—潮输沙—航道淤积这一复杂的海洋动力转化过程简化;抓住开敞式航道泥沙骤淤的源头因素,建立航道泥沙骤淤与大风天有效风能的关系,根据实测资料进一步建立骤淤淤强沿程分布计算关系式。滨州港外航道大风天泥沙骤淤沿程分布预报主要采用类比分析方法;依据相邻港口黄骅港的实测资料拟合淤积率相关系数,通过对不同口门位置不同航道等级不同大风重现期等多方案组合的计算分析,为滨州港外航道平面布置方案的比选提供了技术支撑。     

一种高效的简化可辨识矩阵集成算法

基于可辨识矩阵的约简算法,需要生成许多无用的元素,因而算法效率不高.针对这一问题,基于动态思想,设计了一个新的集成算法,新算法在生成可辨识矩阵的过程中不用生成大量的无用元素,减少了存储量和计算量,从而使算法的效率得到提高.最后给出了一个实例说明新算法的高效性.     

北京地铁七号线达官营站洞桩法开挖数值模拟研究

应用FLAC3 D软件,对静力作用下达官营站洞桩法开挖过程进行了数值模拟,研究了洞桩法施工各个阶段的地表沉降、桥基变形、管线变形、车站结构受力等。研究表明：洞桩法施工中,2＃桥基及各个管线的最大沉降量都超过了限值,应在施工过程中加强监测并采取控制措施。中柱作为结构的主要受力构件,承受较大竖向荷载、剪切荷载的双重作用,是结构的最不利位置,因此在施工中应重点监测,及时采取相应的加强措施,确保施工安全。     

潮段平均流速计算方法研究

在海岸、河口、海湾等地区,潮流是最基本海水运动和主要的水动力因素之一,受海底地形、岸线和岛屿的影响,潮流运动基本呈现为往复运动,即涨潮流速和落潮流速方向相反,相差180°左右。描述往复运动潮流动力强弱的重要指标之一是潮段平均流速和潮平均流速。结合实际海区的实测潮过程,文中对潮段平均流速的3种计算方法和对水文全潮的潮平均流速的3种计算方法进行了对比研究。研究结果表明,不同的计算方法其结果存在着误差,建议潮段平均流速采用积分平均方法,潮平均流速计算采用加权平均法。     

锦州港第三港池25万吨级油品码头工程设计方案优化

通过潮流、泥沙数学模型试验,研究了25万吨级码头航道与港池的淤积形态;通过整体及断面物理模型试验,验证了泊稳条件,确定了码头面的合理顶标高,解决了引堤护面块体稳定性的问题,达到了优化的目的。     

基于粗糙集与支持向量机的推土机故障诊断

提出了一种基于粗糙集理论和支持向量机算法的推土机发动机故障诊断方法。首先利用粗糙集理论对故障诊断决策系统进行约简,消除样本噪声和冗余,然后在此基础上设计支持向量机多分类器,进行故障检测分类。这样,可以有效减小SVM训练的数据,加快多分类器的处理速度。实验结果显示它能提高故障诊断的准确性和效率。     

Fluxes of biogenic carbon in the Southern Ocean: roles of large microphagous zooplankton

The Southern Ocean is an extreme environment, where waters are permanently cold, a seasonal ice cover extends over large areas, and the solar energy available for photosynthesis is severely restricted, either by vertical mixing to considerable depths or, especially south of the Antarctic Circle, by prolonged seasonal periods of low or no irradiance. Such conditions would normally lead to low productivity and a water column dominated by recycling processes involving microbial components of pelagic communities but this does not seem to be the case in the Southern Ocean, where there is efficient export to large apex predators and deep waters. This paper investigates the role of large microphagous zooplankton (salps, krill, and some large copepods) in the partitioning of biogenic carbon among the pools of short- and long-lived organic carbon and sequestered biogenic carbon. Large microphagous zooplankton are able to ingest microbial-sized particles and thus repackage small, non-sinking particles into both metazoan biomass and large, rapidly sinking faeces. Given the wide spatio-temporal extent of microbial trophic pathways in the Southern Ocean, large zooplankton that are omnivorous or able to ingest small food particles have a competitive advantage over herbivorous zooplankton. Krill efficiently transfer carbon to a wide array of apex predators and their faecal pellets are exported to depth during occasional brief sedimentation episodes in spring time. Salps may be a significant link towards some fish (directly) and other apex predators (indirectly) and, at some locations (especially in offshore waters) and time, they may account for most of the downward flux of biogenic carbon. Large copepods are a trophic link towards fish and at least one whale species, and their grazing activity generally impedes the export of organic particles to depth. As a result, biogenic carbon is channelled mainly towards apex predators and episodically into the deep ocean. Without these original interactions, Antarctic waters might well be dominated by microbial components and recycling processes instead of active export from the generally small primary producers towards large apex predators.