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1.
浅地层剖面测量是海洋工程勘察、灾害地质调查和大陆架海洋地质科学研究的重要手段,资料解译的准确程度将对地质调查和研究成果的可靠性造成直接影响.由于C-Boom型浅地层剖面仪的发射换能器与水听器是分开安置的,当调查区域的水深过浅时,将其近似为自激自收的单道地震系统会导致地层的畸变,水深越浅地层畸变率越大.根据浅地层剖面仪的基本原理,推导出了C-Boom型浅地层剖面仪地层畸变率的计算公式及地层畸变校正公式,为用C-View软件更准确地解译此类浅地层剖面资料提供了参考.  相似文献   

2.
根据能量守恒原理导出计算人工岛自振频率的能量公式,浅海人工岛可按剪切型结构进行动力计算,动水压力和动土压力对结构振型参与系数的影响很小,可以忽略。地震时人工岛内回填土只有一部分有效质量参与地震响应,通过模型试验,高径比小于1/3的人工岛回填土有效质量系数在0.2左右。有效质量系数随土壤粘结力的增大而提高,随高径比的增大而增大。一般圆柱形人工岛结构的振型参与系数可采用1.2。  相似文献   

3.
在考虑冰-水-桥墩流固耦合的基础上,利用有限元分析软件ADINA,研究了不同水深和不同类型地震等条件下,桥墩周围固结海冰的边界范围对桥墩地震反应及动水压力的影响。结果表明:墩身位移和加速度、墩底最大弯矩和剪力随着冰体边界范围的增大而增大,但水深超过桥墩高度的4/5时,冰体边界范围对墩身位移和加速度基本无影响。同时,桥墩侧面动水压力也随着冰体边界范围的增大而增大,且增大程度越来越显著。另外,与冰体边界范围为桥墩横截面尺寸30倍时相比,冰体边界范围为桥墩横截面尺寸40倍时墩底最大弯矩和剪力可增大332.34%和245.20%以上,因此,在进行冰水域桥墩抗震设计时应着重考虑冰体边界范围为桥墩横截面尺寸30倍以上的冰体对结构地震反应的影响。  相似文献   

4.
不规则波Boussinesq型方程的造波,消波和反射   总被引:5,自引:1,他引:4  
对前人提出的造波、消波和反射边方法分析表明,其方法是极浅水波近似,不适用于任意水深的水域,本文就任意水深变化Boussinesq型方程,提出了不规则波新的造波原理、方法和消波边界及部分反射边界波动方程,试验表明,本文提出的造波、消波和反射方程有效而可靠的。  相似文献   

5.
浅地层剖面测量是海洋工程勘察、灾害地质调查和大陆架海洋地质科学研究的重要手段,资料解译的准确程度将对地质调查和研究成果的可靠性造成直接影响。由于发收分置型浅地层剖面仪的激发装置与接收装置是分开的,当调查区域的水深过浅时,将其近似为自激自收的单道地震系统会导致地层的畸变,水深越浅地层畸变率越大。根据浅地层剖面仪的基本原理,推导出了浅部地层厚度畸变校正公式,为用C-View软件更准确地解译此类浅地层剖面资料提供了参考。海底沉积物的声速直接影响浅地层剖面地层厚度解译的准确性,利用卢博等建立的适用于中国东南近海的声速经验公式,在某人工岛构造调查中,根据地质钻孔获取的孔隙度参数计算各沉积层的平均声速,建立相应的声速结构剖面,对地层厚度进行校正,取得较好的效果,用孔隙度预测声速的方法参数容易获取,能够提高浅地层剖面资料的解译精度,使地层的厚度更接近于实际,具有一定的实用意义。  相似文献   

6.
随着卫星遥感技术的不断发展,高分辨率卫星影像逐渐应用到水深遥感反演领域。利用Worldview-2高分辨率卫星数据和电子海图数据,基于双波段比值法,反演获得实验区域20m以浅的水深。实验表明,Worldview-2等高分辨率多光谱卫星数据,具有一定反演浅水水深的能力,但在5m以浅的水域反演误差较大;双波段比值法,这种半经验半理论的模型,在水深遥感反演中具有更好的适用性;对比了一次线性、二次多项式、指数、对数等拟合方法,发现对数拟合的方法获取绝对水深,其精度相对其他方法更高。  相似文献   

7.
湿地系指天然或人工、常久或暂时之沼泽地、湿原、泥炭地或水域地带,带有静止或流动、咸水或淡水、半咸水或咸水水体,以及海洋和低潮时水深不超过6米的浅海水域。湿地的类型有珊瑚礁、滩涂、红树林、湖泊、河流、河口、沼泽、水库、池塘和水稻田等。湿地表面常年或经常覆盖着水  相似文献   

8.
广西钦州湾海域表层沉积物分异特征与规律   总被引:1,自引:0,他引:1  
根据2008年12月广西钦州湾海域表层沉积物粒度分析结果,结合沉积物结构、地形和水动力条件,探讨了沉积物的分布规律及其作用机制。结果表明,钦州湾海域表层沉积物在横向上,自西向东呈现出西部粗、东部细,分选程度西部好于东部的特征;在纵向上,沉积物粒径呈现由内向外粒径从粗到细的特征,大致在5m水深处存在一个明显的界限,该水深以浅区域的砂含量较高,且主要沉积砂等较粗物质;该水深以深区域以粉砂质黏土为主,砂含量较低。Flemming的三角图式表明,钦州湾海域沉积动力相对较弱。在此基础上,根据水动力差异与物源不同,将研究区划分为5m水深以浅的西部区、5m水深以浅的东部区和5m水深以深的区域等3个沉积区。  相似文献   

9.
基于TM影像的胶州湾水深遥感   总被引:3,自引:0,他引:3  
以胶州湾20m以内浅水域为研究区域,并按照0~2m、2—5m、5—10m、10~20m的水深对其进行分区,利用Landsat-5 TM数据进行水深遥感。结果表明:各区分别建立线性回归模型反演水深的精度要高于不分区时建立的模型;无论分区与否,多波段组合模型的反演精度最高,且在既不是太深也不很浅的区域反演效果最好;新建立的多时相单波段模型反演水深的精度在水深较浅的区域精度有较大的提高。  相似文献   

10.
通过开展物理模型试验,进行不规则波作用下不同间距大直径圆筒防波堤的波峰压力分布规律研究,分析了圆筒相对间距、相对水深、波陡等主要影响因素对圆筒波压力的影响规律,并通过波压力试验值与各家理论公式计算值的比较,进行不同间距圆筒波压力的计算方法研究。基于直立墙结构和大尺度孤立墩柱结构波压力公式给出修正系数以及横向衰减函数的拟合公式,用以计算圆筒周身不同位置处的波压力,从而为工程设计和理论研究提供参考。  相似文献   

11.
马吉明  谢省宗等 《海洋工程》2003,21(1):19-23,33
从柱座标系下的势流方程出发,推导了异重流体在谐振情况下的势流方程的解,得到了柱内外与环域中的异重流体压力的理论计算公式。给出了壳体内外表面压力系数的计算式。依据所推公式进行了计算,绘制了曲线图,曲线显示了合理的变化趋势。  相似文献   

12.
Qin  Li-cheng  Ding  Hong-yan  Zhang  Pu-yang  Li  Huai-liang  Yu  Wen-tai 《中国海洋工程》2021,35(6):933-942

In this study, the Jinzhou 9-3 CEPD float-over installation project was investigated. During the undocking condition, the water depth of the motion path of the working barge gradually changed from 10.31 m to 9.41 m. The undocking clearance of the HYSY 228 is smaller than 1 m; therefore, the barge shows highly nonlinear hydrodynamic characteristics, and it is difficult to be accurately simulated by numerical analysis. Thus, it is necessary to obtain the hydrodynamic characteristics and laws of the float-over barge at different water depths by using tank model test, to provide some reference and guidance for float-over operations in shallow water.

  相似文献   

13.
海洋浅层土质剪切波速与深度的关系分析   总被引:1,自引:0,他引:1  
剪切波速是工程场地地震安全性评价最重要的参数之一。应用测试的大量海洋浅层土质的剪切波速数据,利用最小二乘法通过三种模型探讨了不同土质类型的剪切波速与深度的关系,给出了不同土质类型的剪切波速与深度拟合最佳的统计公式。并与《构筑物抗震设计规范》的推荐公式在某一海域工程场地的测试结果进行对比分析,结果表明:本文所建立的统计公式对剪切波速的预测效果明显好于规范所推荐的统计公式。所推荐的海洋不同土质类型的剪切波速与深度间的统计公式,可供无波速测试的海洋工程场地使用。  相似文献   

14.
孤立波是浅海水域中经常出现的一种波动现象,常用来描述海啸和风暴等引起的巨浪以及波长较长的表面波的某些特性。采用"水体瞬间坍塌"的方法产生孤立波,在二维波浪水槽内进行系列实验。实验结果表明,产生的孤立波波高与水深之比可达1.29;箱体宽度及箱内水体高度对波高影响较大;得到孤立波波高计算公式,可较好地反映孤立波波高与箱体宽度、水深和箱内水体高度之间的变化关系,并给出了公式的适用范围。  相似文献   

15.
To deal with the moving boundary hydrodynamic problems of the tidal flats in shallow water flow models,a new wetting and drying (WD) method is proposed.In the new method,a "predicted water depth" is evaluated explicitly based on the simplified shallow water equations and used to determine the status (wet or dry) together with the direction of flow.Compared with previous WD method,besides the water elevation,more factors,such as the flow velocity and the surface shear stress,are taken into account in the new method to determine the moving boundary.In addition,a formula is deduced to determine the threshold,as critical water depth,which needs to be preset before simulations.The new WD method is tested with five cases including three 1D ones and two 2D ones.The results show that the new WD method can simulate the wetting and drying process,in both typical and practical cases,with smooth manner and achieves effective estimation of the retention volume at shallow water body.  相似文献   

16.
《Ocean Engineering》2004,31(3-4):305-341
The paper seeks to examine hydrodynamic coefficients of a rectangular structure in shallow water and to establish analytical formulae for fast computations. A two-dimensional rectangular profile is considered with the under-bottom clearance assumed to be small compared with structure dimensions and the water depth. Following the method of matched asymptotic expansions, the radiation problem is solved under assumptions of the linear wave theory, by matching two ‘outer’ flows with the ‘inner’ flow near the structure edge. Closed asymptotic formulae are obtained for all hydrodynamic coefficients for heave, sway and roll motions. The zero and infinite frequency values of the added mass are examined and formulae are derived intended for quick engineering estimations. Numerical results compare well with those published in literature, and the approach is shown to be consistent with known fundamental relations in the body–wave interaction theory.  相似文献   

17.
The hydrodynamic properties of long rigid floating pontoon interacting with linear oblique waves in water of finite arbitrary depth are examined theoretically. The flow is idealized as linearized, velocity potentials are expressed in the form of eigen-function expansions with unknown coefficients. The fluid domain is split into three regions, region (1) wave-ward of the structure, region (2) in the lee of the structure, and region (3) beneath the structure. The different hydrodynamic quantities of interest such as the exciting forces, added mass and damping coefficients, reflection and transmission coefficients were studied for an applicable range of wave/structure parameters. Assuming rigid body motions, dynamic responses of the moored structure is approximately calculated through three equations of motion. Floating pontoons proved to be a convenient alternative for protection from waves in shallow water. The present method of solution was found to be computationally efficient, and results are comparable to those obtained through other techniques.  相似文献   

18.
Semisubmersible will work well when oil exploitation goes to ultra-deep water because of its variable load capacities, and good motion performance in extreme waves. It is considered to be a main type of platform while the water depth is more than 3000 meters. This paper establishes a multi-objective optimization model of semisubmersible for ultra-deep water, and it is solved by a multi-objective genetic algorithm--NSGA-Ⅱ. The model is applied to a practical design, and Pareto results are obtained. The effectiveness of the method is verified by hydrodynamic analysis.  相似文献   

19.
For many reasons, e.g., port operations, coastal construction planning, undersea structure survival, and underwater transport, man wishes to know the extreme values that are likely to occur in coastal oceanographic variables. This paper presents a hybrid statistics/ computer simulation method that uses archived oceanographic observations to estimate confidence levels on the most extreme values likely to occur over a given period in the future. The difference from previously developed methods is the ability to estimate the most extreme value over a time period for a given probability (as opposed to estimating the probability of exceeding a given value) and the ability to obtain results from empirical data without a great deal of theoretical oceanography. The method is applied to the California coast for a period of 100 years on the following variables: bottom surge particle velocity by water depth, wave height by water depth, wavelength by water depth, wave period, current velocity, regions of high density, regions of low density, and earthquake magnitude. Values are given for the 99- and 99.9-percent probability levels.  相似文献   

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